ML20126G685
| ML20126G685 | |
| Person / Time | |
|---|---|
| Site: | Maine Yankee |
| Issue date: | 10/31/1977 |
| From: | Hamawi J, Laznow J, Littlefield P YANKEE ATOMIC ELECTRIC CO. |
| To: | |
| Shared Package | |
| ML20126G683 | List: |
| References | |
| YAEC-1138, NUDOCS 8103310257 | |
| Download: ML20126G685 (200) | |
Text
{{#Wiki_filter:J b o-E d b W 4 SKIR0!!: A Computer Code for Determining Atacapheric Dispersion Conditions for Design Basis Accident Evaluations By John N. Hamawi and Joseph Larnow October, 1977 l' Prepared By W O t1 /8 - A 9-- 7 7 (Date) [ Prepared By M _4A # M. 2. 9, / 8I 7 7 M . (Date) Approved By ] /d Af dD Approved By .
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~ (Dats)
Yankee Atomic Electric Company Nuclear Services Division l 20 Turnpike ' toad Westborough, !!assachusetts 01581 810 3 310)N . 1
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*s o-DISCLAIMER OF RESPONSIBILITY This document was prepared by Yankee Atomic Electric Company for its own use. It is being made available to others as a public service without monetary or other compensation to Yankee, upon the express understanding that neither Yankee Atomic Electric Company nor any of its of ficers, directors, agents or employees assumes any obligation, responsibility or liability, or makes any warranty or ..
representation, with respect to the contents of this documents or its accuracy or completeness, e J l l I l l i 11 I
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ABSTRACT l l l SKIRON is a computer code developed at Yankee Atomic Electric j Company for implementation'of the recent NRC (Nuclear Regulatory. 1 Commission) position on atmospheric dispersion conditions for design. basis accident evaluations. The new position requires a probabilistic ' assessment of atmospheric dispersion and takes into consideration the varying site boundary distances of a nuclear power station' and the varying wind direction frequencies. Each sector,is evaluated independently and the dilution factors for the critical sector are " selected for the design evaluations. SK1RON also incorporates. the features of Regulatory Guide 1.111 which provides guidance'for estimating atmospheric dispersion of gaseous-effluents in routine releases from light-water-cooled reactors. The code is fairly comprehensive and includes the following basic features: , use of hourly meteorological data; straight-line' airflow model with= - Gaussian diffusion; plune centerline and- sector-average models. for short-term and long-term dispersion,' respectively; distinct vertical and horizonta1' atmospheric stabilities, part-time ground level'and. part-time elevated releases (split-H); terrain features; plume rise; building wake effects; and plume meander. A significant feature is the inclusion of a seabreeze model for coastal sites which consists ' of the identification of seabreeze conditions, determination of the
- thermal internal boundary layer (TIBL), and the treatment of plume trapping and fumigation. Another important feature is the determination of certain " effective gamma. dilution factors" (X/Q's) which permit >
evaluation of external whole body doses from finite clouds of multi-energetic gamma sources. It SKIRON is written in FORTRAN IV for use with CDC machines. consists of a main program with block data and 21 subroutines (approx-imately 2100 cards) and requires 245400 octal 60-bit central memory words for execution. Conversion to IBM can be accomplished with minor modifications. S i iii l
*)
O~ TABLE OF CONTENTS P,, age, ABSTRACT iii LIST OF FIGURES vi
1.0 INTRODUCTION
1 2.0 METEOROLOGICAL PARAMETERS S 2.1 Data Input 5 2.2 Data Reduction 6 2.2.1 Wind Direction 6 2.2.2 Wind Speed- 6 2.2.3 Atmospheric Stability 6 1 2.2.4 Seabreeze 6
. 2.2.5 General 8 3.0 BASIC DISPERSION MODELS 9 3.1 Dispersion Equations 9 3.2 Plume Meander 11 j 3.3 Plume Standard Deviations and Building Wake 13
]
3.4 Entrainment 13 3.5 Vertical Dispersion and Reflection 14 3.6 Effective Release Height 16 3.7 Plume Rise 17 19 ! 3.8 Mixing Depths 3.9 Recirculation Correction 19 4.0 SEABREEZE ANALYSIS 24 4.1 The Nature of Seabreezes 24 4.2 Criteria for TIBL Formation 26 i iv
~ ,
_j e-TABLE OF Conte 1rtS (Continued) . Iage, 27- - 4.3 TIBL Ceometry 28 4.4 - Dispersion Modes and Regimes.
- 31 4.5 Cround-Level Concentrations .
37 5.0 CAMMA DILUTION FACTORS' ., 37 , 5.1 Finite-Cloud f" - x Dose Rate Equation 40 5.2 Application 43 > 6.0 DILUTION FAC7 ORS FOR ACCIDL'IT EVALUATIONS , 44 6.1 Relative Concentration Assess =ent 1 44 6.2 Averaging Procedure and Models i 47 , 6.3 Statistical Distribution ! 50- ' 7.0 CODE PARTICt h*45 ? 50 . 7.1 General Structure I 5: 7.2 Input Information 69 ' 7.3 Sanple Input and Output -i 88 REFERENCES i 1
-[
4 V l 1
'tvg W -
w-- = + c g , w er r + 'v- w- T--7* v' = - - " -
4
's4 LIST OF FICURES Title Page Number Figure 3.3.1 Heander as a Function of Wind Speed and Stability (Based on Preliminary Results 21 of Tracer Studies) (From Ref. _1)
Figure 3.3.2 Horizontal' Standard Deviation of Material in a Flune (Letters Denote Pasquill 22 - Stability Class) (From Ref. 7) Figure 3.3.3 Vertical Standard Deviation of liaterial in a Plume (Letters Denote Pasquill Stability 23 Class) (From Ref. 2) 34 Figure 4.1.1 Typical Fumigating Plume During a Seabreeze Figure 4.4.1 Diagram of Vertical and Horizcntal Plume Geometry Used in Modeling Continucas 35 Fumigation . Figure 4.4.2 Area Under the Gaussian Distribution Curve 36 From -- to p. (p Figure 5.2.1 Linear Energy-Absorption Coefficient (p) f)or and Linear Attenuation Coef ficient Air at 0 C and 760 mn Hg in Units of Inverse , Meters as Functions of Photon Energy in MeV 42 , (From Ref. 17) 63 Figure 7.1.1 General Code Structure (Subroutine Calls) 65 Figure 7.1.2 Simplified Logic Flow Diagram - SKIRON 66 Figure 7.1.3 Simplified Logic Flow Diagram - CHIQS 67 Figure 7.1,4 Simplified Logic Flow Diagram - METDAT 68 Figure 7.1.5 Simplified Logic Flow Diagram - SUMRIES 4 vi
e 1 e -
1.0 INTRODUCTION
SKIRON is a computer code that determines atmospheric dispersion
- conditions for assessing the potential ef fsite radiological consequences which cc.311 result from accidental releases of radioactive materials from commercial nuclear power stations. The code is fairly compre-hensive and has been designed to incorporate both the recent position of the Nuclear Regulatory Commission for design basis accident evaluations (Position KMB ) and the models in Regulatory Guide 1.111( } which provide guidance toward implementation of Appendix 1 to 10 CFR Part 50 and the "as low as reasonably achievable" objectives.
The basis of the new NRC position is recognition that dispersion models should reflect variations that occur as a function of varying site boundary distances and varying wind direction frequencies. The position requires probabilistic assessment of atmospheric dilution in such a , way that probability levels for individuals at different locations around a nuclear power station are sector-dependent. For airborne releases from nuclear power stations, the concentra-tion of radioactive material in the surrounding regions depends on the l l airflow patterns of the site, the topography of the region, and the characteristics of the effluents themselves. Parameters to be included ) in the estimation of transport and dispersion of ef fluents include: e height of the release e size and shape of the release point
. e location of release point in relation to obstructions e buoyancy and vertical velocity of the emitted plume < . l I
i 9 d 3 e ambient windspeed, temperature and atmospheric stability P e airflow patterns, wind variability and recirculation , e geographic features such as hills, valleys and large bodies of water , SKIRON employs the following basic features: use of hourly-meteorological data; straight-line airflow model.with Gaussian diffusion; plume centerline and sector-average models; distinct vertical and horizontal atmospheric stabilities; part-time ground-level and part-time - t elevated releases (split-U); terrain f eatures; plume rise; building c wake effects; and plume mesander. A significant f eature is the inclusion
-of a seabreeze model for co.cta) sites which consists of the identifi-cation of seabreeze ' conditions, determination of the thermal internal boundary layer (TIBL), and the treataerd of plume trapping and fumigation.
Another important f eature is the determination of certain " effective gamma dilution factors" (X/Q's) which permit evalustion of external whole body doses from finite clouds of multi-energetic gamma sources. Definition of these factors was determined by reducing the finite-cloud 0 dose rate equation in Regulatory Guide 1.109 to that for a semi-infinite cloud; their determination is based on the model described in Ref. (5). Ilourly dilution factora are computed for either ground level or elevated releases using both the plume centerline model and the sector i average model. Plume centerline values are for estimating short-term atmospheric dispersion (up to 8 hours) and sector average values are for dispersion during longer periods of time. In the plume centerline model, for ground level releases during neutral and stable _ atmospheric conditions and low wine speeds, atmospheric dispersion is corrected l
.6 J
for either plume meander effects or. for thi additional dispersion of the c.f fluent plume within the wake caused by buildings adjacent to'the , rel2ase point. During all other atmospheric stability and/or wind
. t In speed conditions, credit is taken only for building wake effects.
the nector-average model, dispersion is based on Regulatory Guide 1.111 and meander effects are ignored. Both building wake and plume meander are excluded from the equation for elevated releases. Atmospheric dilution fact ors are computed by the above models for , each sequential hour of measured meteorological data and for receptors The positioned in the 16 cardinal compass directions around the plant. hourly dilution f actors obtained as described and the corresponding direction in which the wind is blowing during each hour are then stored in sector dependent arrays fcr sequential processing. This involves , the averaging of selected hourly dilution values over successive, overlapping time intervals. For each selected interval size, the processing begins with the first hourly dilution value on record and then repeated for the same interval size starting with each subsequent hour of dispersion data. In the averaging process, the only values within a given time interval that are considered in evaluating the mean dilution factor for the interval are those for the specific wind direction i being analyzed. Missing data are handled by imposing the condition that at least half of the entrict within an averaging interval correspond to valid observations. Missing data points are not included in the averaging. The average dilution f actors computed as described are subsequently [ classified, for ea ch 22-1/2 degree sector, into groups, and correspond- P ing cumulative probability distributions are prepared. A normalized 7
e pre,chility percentile point, which defines the percent of time a dilution value is. equalled or' exceeded, is determined for each sector I using- the wind-direction frequencies. The corresponding dilution value for each sector's percentile point is then determined and the l maximum sector value is chosen as the accident dilution factor to be used in the design basis accident evaluation. Dilution factors are determined for each time interval of interest in the DBA evaluation. Most of the basic features of SKIRON were extracted' from AE0LUS( }, a computer code developed at Yankee Atomic for evaluating atmospheric dispersion of routine radioactive effluents from commercial nuclear power stations. Description of these models is repeated in the sections that follow for the sake of completeness. SKIRON is written in FORTRAN IV for use with CDC machines and consists of a main program with block data and 21 subroutines (approx-imately 2100 cards). Conversion to IBM can be accomplished with minor modifications. e
2.0 METEOROLOGICAL PARAMETERS 2.1 Data Input SKIRON accepts either raw meteorological data (on an hourly basis) For the first option, the or data processed in an earlier SKIRON run. following meteorological parameters are input to the code (via Tape 10): o wind direction e direction fluctuation (optional) e wind speed e temperature difference e ambient air temperature (optional) i e sea water surf ace temperature (optional) f o solar radiation (optional) The data must be in monthly records and may be in any order, any units and any format (card-image form). The first data card for each month must identify the number of hourly records in that month (13 format). In its present form, the code can handle up to 12 months of I hourly meteorological data. l (via Tape 5): . The following inf ormation is also required as input ! l e 7-parameter format for reading in the meteorological data (zeros or blanks must be provided for parameters for which data is not availabic) l e sequence number of each meteorological parameter in the input format e maximum value for each parameter acceptable as a valid observation e conversion factors
n-i
.- l l
SK1RON has the capability of replacing non-valid hourly observations l l by data from preceding hours. This option should be used with care since a long list of identical parameters may yield unreliable results. Mon-valid observations are excluded from the analysis. 2.2 Data Reduction 2.2.1 Wind Direction ! The N Wind direction data is reduced to the 16 compass sectors. sector ranges between - 11.25 and 11.25 , and each sector has been assigned an identification number according to the clockwise sequence: 1 for N, 2 for NNE, 3 for NE, etc. Valid data range between 0 and a user-specified maximum (typically 540 ). , 2.2.2 Wind Speed The Valid wind speeds range between two user-specified limits. lower limit should be selected to represent the starting speed of the measuring instrument and the upper limit should be less than the value used to identify missing data. Wind speeds less than the lower limit default to a user-specified value. 2.2.3 Atmospheric Stability Atmospheric stability in the vertical and horizontal planes is determined from: (a) the vertical temperature gradient (AT model), and (b) the standard deviation of the horizontal wind-direction iluctuation (o gmodel). The stability categories for these two models are as follows (Ref. 6):
,' Classification of Atmospheric Stability Pasquill 0 Stability 0 Classification Categories (Degr ess) ( C/100m)
Extremely unstable A 001 22.5 M i -1.9 . Moderatley unstable B 22.5 > os 1 17.5 -1.9 < E 1 -1.7 Slightly unstable C 17.5 > os > 12.5 -1.7 < K 1 -1.5 Neutral D -1.5 < ar 1 -0.5; 12.5 > os 1 7.5 Slightly stable E 7.5 > os 1 3.8 -0.5 < & 1 1.5 Moderately stable F 3.8 > 00 1 * *
#1
- Extremely stable G 2.1 > 0 0 .0 < &
All three dispersion models in SKIRON utilize the dT stabilities to determine effluent dispersion in the vertical plane. Horizontal concentrations are either assumed to be uniform, or.to follow a Gaussian distribution about the plume centerline. In the latter case, horizontal dispersion may be based on either the vertical temperature gradient or the horizontal wind-direction fluctuation. 2.2.4 Seabreeze in evaluating ground-level concentrations from power-plant gaseous ef fluents, consideration should be given to special meteorological and geographical conditions which may exist. A significant feature of SKIRO'1 is the inclusion of a s,eabreeze model( } for coastal sites. Sea and lake breezes, which occur comonly during spring and sumer near large bodies of water, may lead to the phenomena of fumigation and trapping which .could result in greater ground-level concentrations near the release point. I
- j 4 s Typical conditions under which'these phenomena can occur are 1
as follows: i e spring and summer eensons e daytime (e.g. 0800 to 1800 EST)
. e onshore winds with an overwater fetch of 5 miles or so l l
e appropriate wind speed (2 to 10 mph) e adequate solar radiation (approximately 1/3 the peak values during clear summer days) Input to SK1RON for seabreeze identification includes the following: e hourly sequence numbers at start and pnd_of seabreeze season (sequential numbers from first hourly record input) e daytime limits e seabreeze sectors (maximum 12) e tower AT stabilities suitable for seabreeze e minimum and maximum wind speeds e minimum solar radiation 2.2.5 General Both raw and processed meteorological data may be included in the computer output for a number of user selected hourly records. Included in the output are also the following: e numbers of valid observations for each meteorological parameter , e -number of minimum wind speed observations e number of seabreeze occurrences (if any) e number of AT and stability occurrences 0
- e number of wind occurrences in each sector Monthly. records of processed meteorological data are written on tape 11 in binary form. This information may be saved and used in later SKIRON runs in lieu of the raw data.
f 3.0 BASIC DISPERSI,0N N0DELS_ Atmospheric dispersion in SKIRON is based on the straight-line airflow model with Gaussian dif fusion. Three models are included: (1) a plume centerline model with both vertical and horizontal dispersion based on the' vertical temperature gradiant (AT model)- (2) a plume centerline model with vertical dispersion bazed on the vertical temperature gradient, and horizontal dispersion based on the wind-direction fluctuation (split-sigma model) l (3) a vector average model with uniform horizontal concentration, and vertical dispersion dependent on the vertical temperature 1 gradient. Hourly dilution factors are computed using one of the plume center-line models, as selected by the user, and the sector average' model. As described in Section 6, plume centerline values are for estimating short-term atmospheric dispersion (up to 8 hours) and sector average This section values are for dispersion during longer periods of time. deals with the methodology of evaluating hourly dilution factors for computing ground-level concentrations of radioactive materials from both ground-level and elevated releases. 3.1 Dispersion Equations 1 According to the straight-line airflow model with Gaussian dispersion, the equations for the hourly dilution factors are as follows: (a) Plume centerline, split-H, with building wake: E (1-E )
+
(x/Q)pc " su: II yz b 'G # 'E
/z
(b) Plume centerline, split-H, with plume meander: E (1-E ) C3 (2} (X/Q)PcM " I M oz C M+ g E i (c) Sector average, split-H, with building wake: I El ( ' (X/Q)SA " - CG+ E Xu z z In these equations, X is the activity concentration (Ci/m ), Q is the activity release rate from a specific location of a power , plant (C1/sec). C is a recirculation correction factor (see Sec. 3.9), X is the downwind distance from the release point (m), u is the hourly average wind speed (m/sec). E is the entrairunent coefficient (equal to unity for ground-level . g releases and to zero for elevated releases; see Sec. 3.3), M is the meander factor (a function of atmospheric stability and . 1 wind speed; see Sec. 3.2).- e is the vertical plume standard deviation at distance X for the 4T atmospheric stability prevailing during the hour of interest (m), e is the horizontal plume standard deviation based on either the 4T , or asatmospheric stability (m). I, is the vertical plume standard deviation corrected for building wake effects (m), I is the horizontal plume standard deviation corrected for building
. y wake effects (m), i
1 (g is the reflection correction for ground level releases with building wake l E is the reflection correction for ground level releases with plume M meander , and (E is the vertical attenuation and reflection correction for elevated releases. The terms within the brackets represent, respectively, the contribu-tions to the dilution factors from the entrained and non-entrained portions of the release during the hour of interest. The effluent is considered to occur as an elevated release (1-Eg ) x 100 percent of the time (1 hour in this case) and as a ground-level release (E g) x 100 percent of the time. Details on the various parameters are given in the sections that follow. The above equaticns apply during normal atmospheric conditions. Section 3.2 below describes the plume meander model and the conditions under which it applies. The effects of fumigation sad trapping caused by seabreezes and cashore gradient flows are described in Sec. 4. Note that the horizontal plume standard deviation parameter (o ) appearing in the plume centerline equation is based on the atmospheric stability determined from either the vertical temperature gradient (AT) or the standard deviation of the horizontal wind-direction fluctuation ; in the latter case, the model is referred to as " split-sigma". 3.2 Plume licander According to the recent NRC technical position on diffusion conditions for design basis accident evaluations (Position KKB( }),
- . , m credit can now be taken for the benefit of pli.sne meander in reducing of f site radiological consequences from postulated accidental releases.
The basis of this new position is recognition that dispersion models should provide more realistic, yet reasonably conservative assessment of atmospheric dispersion. Results of atmospheric tracer studies evaluated by the Nuclear Regulatory Commission indicate that atmospheric diffusion f rom ground-level sources during light vind and stable condi-tions is substantially improved by plume meander and building vake effects. Figure 3.3.1 shows the new curves reconsended by the Coeusission f or meander credit as a function of vind speed and atmospheric stability for distance up to 800 m. Beyond this dis'.4nce use is made of the adjusted meander factor defined as: (4) M' = (M-1) [r (800)/c } + 1 where c (800) is the lateral standard deviation of the plune at 600 meters. Note that for unstable conditions (stabilities A, B and C) and for vind speeds greater than 6 =ps (independent of stability) the meander factor is equal to unity. In addition, the combined effects Thus, in the of plume meander and building vake are not allowed. plune centerline case, dilution f actors are conputed using both Plume neander is not Eqs. (1) and (2) and the lesser value selected. allowed for elevated releases. L p 4 J
3.3 Plume Standard Deviations and Building Wake Values of a and o, are computed by applying parabolic interpola-tion (on a log-log basis) to tabular data of these parameters versus distance. The data was extracted f rom Pasquill-Gifford curves for atmospheric stabilities A through G shown in Figures 3.3.2 and 3.3.3 reproduced from Refs,(2) and (7), o values are restricted to a maximum of 1000 m. For ground-level releases, consideration is also given to additional dispersion of the effluent plume within the wake caused by buildings adjacent to the release point. In such cases, use is made of the adjusted standard deviations defined as: E = (c y + 0.5A/w) (5) y and I, = (o,2 + 0.5h3 27 ,)1/2 (6) where hg is the height of the building causing the additional dispersion (m), and A is .its anallest vertical cross-sectional area (m ). The maximum values of I andz I are restricted by the conditions: y (7) (I y)nax = 5 o y , and o (8) (I E) max = /3~ 2 Recall that plume meander and building wake have been assumed to be mutually exclusive. 3.4 Entrainment As outlined in Regulatory Guide 1.111, effluents are considered as ground-level releases (E = 1.0), elevated releases (E = 0.0), or mixed
e releases (0.0 < Eg < 1.0) depending on (a) the elevation (h,) of the release point above grade relative to the height (h3 ) cf adjacent solid structures and (b) the ef fluent-exit velocity (W,) relative to the speed of the prevailing wind during the time period of interest. The alterna-tives are as follows: i for h, i h3 E = 1.0 t for h,1 2hB E g = 0.0 for h *h s < 2hB B Eg = 1.0 when W, /U 11 Eg = 2.58 - 1.58 (W ,/U) when 1 1 W,/E 1 1.5' (9a) E = 0.3 - 0.06 (W G) when 1.51 W,/U 15 (9b) t Et = 0.0 when W , 6 1 5 3.5 vertical Dispersion and Reflection Cg and (E in Eqs. (1), (2) and (3) represent the exponential decrease in ground-level concentrations with increasing plume height, and the increase in concentration from multiple eddy reflections from the ground and stable atmospheric layers aloft. Definition of these parameters was based on the plume trapping equation in the US EPA workbook on atmospheric dispersion (Ref. 8): (10) g c 3=[-n ,-(83) (E "j= n
^
and (12)
= e (Sj)
(M j=-n where h (13) a = ~ oz(2 6 =,EL* (14) z and (15) g' . _C L , z / h, is the effective plume height above ground, L is the height of the Parameters reflection layer and 2n is the total number of. reflections. li, and L are discussed further in Sections 3.6, 3.7 and 3.8. l i.e., when uniform Note that in the case of multiple reflections, vertical mixing has taken place, Eq. (11) reduces to: o (16). (E l 2 I as can be seen by writing l g . f"e-(a+Sq)dq (17)
=f E Similarly, for ground-level releases l
E r (18) (c " [i Y q When Eqs. (16) and (18) are substituted into Eq. (3), the latter reduces to. j (x/Q)3,g
= 2.o32c ( )1/2
_ (19) .l 1 XuL j
,2.55C f
XuL 1
]
.~
which is the f amiliar form of the sector-averaged dilution equation with uniform vertical mixing. In SKIRON, n was conservatively set equal to 6; n = 3 or 41a normally sufficient to include the important reflections. 3.6 Effective Release Height Effective release heights, h,, are determined in accordance with Regulatory Guide 1.111 from: h, = h, + h pr ~h -c (20) t where c is the downwash correction for low relative exit velocity (see below), h is the rise of the plume above the release point according to pr Sagendorf (Ref. 9) (see Section 3.7) (m), h, is the physical height of the release point (m), and h is the maximum terrain height (above the release-point grade elevation) between the release point and the receptor (hg 3,0) (ml The downwash correction factor is defined as( ): c = 3(1.5 - W,/5)d when W, /6 < 1.5 (21) and c=0 when W, /5 3,1.5 (22) where d is the inside diameter of the release vent (e.g., stack) (m) ,
'W is the vertical exit velocity of the plume (m/sec), and o
E is che hourly average wind speed tm/sec). I l
~.
t 3.7 Plume Rise Plume rise is computed on an hourly basis using formulas reported by Sagendorf (Ref. 9) and Briggs (Ref.10). SKIRON will calculate Plume rise caused by either momentum g buoyancy depending on the heat emission rate input to the program. Nuclear power stations generally have cold plumes, so the heat emission rate is read in as zero and plume rise is calculated from the momentum equations. For neutral and unstable conditions, the transitional rise is computed by the equations: h pr d (23) ~
= 1.44 (W
, /U)2/3 (X/d)1/3 and (24) h pr "'3( o/ ) d and the lesser value is used.
For stable conditions, the results from Eqs. (23) and (24) are compared with the results from the following two equationr: . h = 4(F /S)I! (25) pr h = 1.5(F /u)I S'I 0 (26) pr a-A the smallest value of h pr is used. In the last two equations, F is the momentum flux parameter and S is a stability parareeter. They are defined as: F = (W d/2)' (27) and S=(g/T)h (28) 1
-1 7 -
en r---
.' I .' i where l g is the acceleration of gravity (m/sec ).
T is the ambient air temperature (hourly data ar user selected def ault value (deg r.)) , and 30 is the vertical potential temperature gradient (deg K/m) dtfined Bz as (Ref. 10): (29)
= + 0.0098 ,
If plume rise is to be calculated for buoyant plumes, the heat emission rate must be input to the code. Plume rise to distances less than some distance X* is given by: (30) h = 1.6F X (u) where 3 s ( } F = 3.7 x 10-5 ( 4, ec ) Oh e For neutral and unstabic and Q h is the heat emission rate (in cal /sec). conditions: < 2/5 h (32) X* = 2.17 F s
~ (hs< 305 m)
(33) X* = 67.3 F (h, > 305 m) where h, is the elevation of the release point above grade (in meters). At distances beyond X*, plume rise under neutral and unstable conditions is calculated by: 2
/33,2/3{ + + ( )] {3 )
1.6F h = 2 Pr
,(1 u + g ,)
At X = SX* the plume in assumed to' reach its maximum height. Under i stable conditions, Eq. (30) holds'to a distance:
~1 (35) i X = 2.4 uS after which the plume rise is given by:
hp ,
- 2.9(F/uS) (36) t where all parameters are as previously defined. -
3.8 Mixing Depth _s, Vertical diffusion'of the plume is inhibited by the existence of a ; stable atmospheric layer (an elevated inversion) alof t. The rate of vertical mixing is reduced in such cases and the stable layer can be considered us an ef f ective lid on vertical transport of pollutants. Although there are many hours in the year characterized by unlimited mixing depths, it was assumed that all hours can be characterized by an average mixing depth for the year. Low mixing depths should be selected for conservatism (typically 600 to 800 m). The effect of plume trapping is included in the C terms of Eqs. (1), (2) and (3), and was , discussed in Section 3.5. 3.9 Recirculation Correction The straight-line dif fusion model does not consider the ef fects of spatial and temporal variations in airflow. Therefore, appropriate corrections may be applied to long-term average concentrations calculated by this model. There are three basic categories of regional airflow characteristics that are related to topography:
(1) inland, in open terrains, including gently rolling hills, with airflow dominated almost entirely by large-scale weather patterds , (2) In pronounced river valleys, with airflow patterns largely dominated by terrain , and (3) Along and near coasts of large bodies of water, with consider-able land-water boundary layer ef fe:ts on airflow patterns., SKIRON was programmed to include the following options regarding recirculation correction factors: e no correction e user-selected f actors f or each distance and sector based on topographic characteristics. 1 I 4 l
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1 1.0 10 100 0.1 PLUME TR AVEL DISTANCE (KILOMETERS) ! Figure 3.3.3 Vertical Standard Deviation of Materialin a Plume (Letters Denote Pasquill Stability Class) (From Ref. 2) O t 4.0 SEABREEZE ANALYSIS In discussing the straight-line dif fusion model, Regulatory Guide 1,111 states that correction f actors should be applied to the concentra-tions calculated to account f or the eff ects of spatial and temporal variations in airflow in the region of the site. The guide states that for coastal sites with significant land-water boundary layer effects on air flow, specific correction f actors should be developed and applied. Some factors to be considered are the characteristics of aea or lake breezes, the variation of the mixing layer height with time and distance from the shore (e.g., fumigation and trapping), and the ef fects of shore-line bluffs or dunes. These f actors should be considered in relatien to the locations of the meteorological towers, plant structures, and release points with respect to the land-water boundary layer. The model employed in SKIRON to address the special f eatures of The following sections coastal sites was extracted from AEOLUS( }. present a discussion on _the nature of seabreezes sod the computational models. 4.1 The Nature of Seabreezes Seabreezes occur commonly during spring and summer along the coastline. Because the land warns more rapidly than the water on a sunny day, the air temperature over the land is of ten higher than the Thus, when the synoptic temperature of the air mass over the water. flow is generally weak, a circulation develops from the water to the land at low levels and f rom the land to the water alof t.
-2 4 -
t
During the morning hours- of a clear spring or summer day with light winds, the seabreeze will begin as a gentle breeze. As the intensity of the solar radiation increases, the breeze becomes stronger and penetrates further inland. The seabreeze may extend inland to distances of fif teen to twenty miles. By midafternoon the seabreeze has developed to the greatest extent and begins to weaken as the sun sinks. Af ter the sun sets and the seabreeze has dissipated, a land breeze frequently forms. The land breeze, which is usually weaker than the daytime seabreeze, is caused by a water temperature which is higher than the temperature over the land. The land breeze reaches its maximum development during the winter. The wind structure during a seabreeze is depicted in Fig. 4.1.1. The cold air over the water surface can be characterized as stable. During an onshore wind, the cool and stable marine air is heated from below by the land surf ace and becomes unstable in the lower levels. The depth of the unstable layer increases with inland distance until i the marine inversion is destroyed. The layer of unstable air beneath the marine inversion is known as the thermal internal boundary layer l (TIBL). The importance of a TIBL in the behavior of ef fluents can best be understood with the aid of Fig. 4.1.1. The ef fluent plume is trans-ported inland at a height h, above the ground surf ace. When the plume begins to intercept the top of the TIBL, the material in the plume is l mixed rapidly downward in the unstable air within the TIBL. This could ) result in higher ground icvel concentrations than would be estimated by ignoring the TIBL cffects. This rapid downward mixing is known as fumigation. As the TIBL continues to grow, more material in entrained
l
. 1 d
( until the plume is entirely within the TIBL. For greater downwind distances, the continued growth of the unstable layer provides a greater mixing volume and the ground level concentration will begin to decrease. 5 For releases which occur at ground level, the material is trapped e within the TIBL. This lid will limit the mixing volume to a greater ertent than the average mixing depth for the area around the site and can result in higher ground level concentrations. Although this discussion has defined the flow trom the water to the innd as a "seabreeze", this phenomenon occurs near all large bodies of water where the daytine temperature dif ferences develop. Also, a TIBL will form not only during the occurrence of a classical seabreeze as described but also during conditions of onshore gradient flow with sufficient solar radiation to cause a land-water temperature- , dif f erence. For purposes of calculating concentrations of pollutants, the two cases are treated identically. 4.2 Criteria f or TIBL Formation The f ollowing criteria have been established: (a) TIBL's can occur only during spring and summer when the land-water temperature difference is suitable. A seabreeze season extending from April through September is typical. (b) TIBL's can occur only during daytime when there is suf ficient solar intensity (typically between 0800 and 1800 hours during the seabreeze season). (c) The wind direction must be onshore with an overwater fetch sufficiently long to stabilize the air mass. A fetch of five to ten miles will result in a marine inversion several hundred ) feet deep (Refs. 11, 12). 1
-2 6-I l
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. i l =
e Too low a (d) The wind speed must be in an appropriate range. wind speed will not support a TIBL. If the wind speed is too high, mechanical turbulence will overcome any thermal effects and a TIBL will not be formed. A range of wind speeds
~
between 2 and 10 meters per second characterices the conditions of interest. (e) Solar radiation must be suf ficiently strong-since it is the heating of the land which causes the development of a TIBL (typically 0.35 Langleys/ minute or mory). This magnitude of solar intensity occurs early and late on bright days and is approximately 1/3 the peak midday values during clear , summer days. 4.3 TIB_L Geometry The best basis for defining the depth of the TIBL as a function of inland distanca is a field measurement program at the site of interest. Visible tracers, turbulence measurements, temperature soundings, and other techniques have been used in some instances to locate the interface between the TIBL and the' stable layer. However, there are many sites for which this type of information is not available. For generalized 11, 13, 14): application, the following relation was selected (Ref s. 1/2 h TIBL(*) " ^I-uho wher e hTIBL(x) is the depth of the boundary layer above the ground surf ace , (met er s), x is the distance f rom the shore along the wind trajectory (m), A is the site-dependent constant (typically equal to 8.8),
u is the hourly average wind speed (m/sec) , and 60 is the potential temperature difference between the top and bottom of the marine , inversion. This relationship was verified at the Pilgrim Station in Plymouth, , Massachusetts, during a series' of smoke release experiments (Ref.15). In SKIRON, the Note that the TIBL is assumed to follow the terrain. maximum depth of the TIBL is limited to the climatological mixing height. 60 is computed using the equation . (39) 60 = T, - Ty + 0.0098 h gny where is the ambient air temperature at the top of the meteorological T, tower,'which is assumed to be approximately equal to the tempera-ture at the top of the inversion layer ( C) , Ty is the temperature at the air-water interface (#C) , and h is the depth of the marine inversion layer (m). inv If hourly water temperature data and/or ambient air temperature data is not available SKIRON defaults to a user-selected 60 value for use in Eq. (38). A def ault value of approximately 4 C is reasonable. 4.4 Dispersion Mode and Regimes ; I There are three cases of interest in the evaluation of ground These are: level concentrations resulting from nuclear reactor ef fluents. (a) Effluents released at or close to ground level, j
. (b) Ef fluents released from an elevated location when the release l I
point is within the TIBL, and
'(c) Effluents released from an elevated location when the release point is above the TIBL.
y In cases (a) and (b),the ef fluent is released underneath the TIBL and is assumed to se trapped. In SKIRON, the plume is not allowed to f punch through the TIBL even though the plume rise equations may. predict , so. The plume follows the TIBL till it attains its maximum predicted height and then levels off. Recall that TIBL's have been assumed to follow the terrain and that plumes reach their maximum elevations above ground at the release point. In case (c), the dispers'ionregime downwind of an elevated source is divided into three zones as shown in Fig. 4.4.1. The first zone is essentially the unriodified elevated plume in a homogeneous stable layer. It extends from the release point to point XB where the turbulence Analytically, just begins to disturb the lower portion of the plume. this was defined to be at the point where the plume centerline is ! is the vertical plume standard devia- , 2.15e meters above the TIBL. e tion for stability F computed at point X7 where the plume centerline intercepts the TIBL. The second zone is the fumigation regine and extends from XB* r the point where the entire plume is underneath the TIBL (point Xg ). The profile of concentrations below the TIBL within this unstable layer is considered to be partially uniform in the vertical though still I Gaussian in the horizontal. Additional horizontal mixing results from i the intense turbulence that it occurring at this time and is given by (Ref. 16): i (40) i oy "" = oFy 4 ../8 f . e
- Departure from complete vertical mixing is represented by the factor
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where I42) P = (hYIBL(*) ~ he }!# . - In Eqs. (40) and (42), h, is the effective plume height at the point of interest in zone 2 defined by Eq. (20) and x is the distance from the shoreline to the receptor. A graphical presentation of Eq. (41) is shown in' Fig. 4.4.2. . Zone 3 extends beyond point XE and is essentially the same as In this zone, plume trapping except that the lid height is variable. the entire plume is within the unstable layer and complete uniform Lateral disper-concentration has been attained in the vertical plane. sion is now entirely dependent on the unstable layer but since the turbulent condition only begina af f ecting the plume between XB "" E' values in this zone. complications arise in the choice of appropriate e y ' I'e use of a o Y for an unstable condition based on the actual distance i j tom the release point would grossly overestiaate the lateral dispers on. More realistic plume widths and concentrations in this zone may be obtained by basing the analysis on a virtual source located at Xy 6). In S I ON, Xy is selected such that the betweenBX and XE(e.
~
V) r the unstable horizontal standard deviation at a distance (X E stability to equal to: (43) , cy(XE V} ~ # y(X7 ) + h,(X7 )/8 ,
~
h,(X7 ) is the ef fective plume height at the point where the plume cente line intercepts the TIBL. To determine X7 , is was necessary to assume terrain slope f rom the release point to the that there is a constant ; receptor. With reference to Fig. 4.4.1 it is clear that: (44)
~ *) ~ (X I/X)h t hTIBL( S + I) = (h, + h pr
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9 6 where X 3 is the downwind distance from the shore to the release point Substituting and the othe'r parameters are as previously defined. Eq.- (38) into (44) and solving for g leads to: (45) X7 = (b ,b2 - 4ac')/2a where (46) a - (ht/X) 2 (47) b = 2(h, + h r
- c)(h /X)+A /Ea0 and 2 2 (48) c' = h - (A X,/ua0).
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X7 = (h, + h pr - c) (ua0/A ) - X3. The downwind distance from the virtual source to a receptor in zone 3
?
is given by: (50) X' = X - X y = (X - X E ) + (X7 -X)y where X is computed from E (51) h y TIBL( S + k} " TIBL( S + X )+2.150 through the use of Eq. (38), and (X E - Xy ) is obtained from Eq. (43) versus by applying parabolic interpolation to the tabular data of a distance. 4.5 Ground-Level Concentrations Ground-level concentrations during conditions of seabreeze and onshore gradient flow are calculated in SKIRON using the straight-line airflow equations described in Sec. 3. Equat'ons (1), (2) and (3), in fact, apply directly with the following modifications and conditions:
)
~
i. (a)- Pasquill stability F prevails above the TIBL for both AT and 1 split-signa models (af fects both dispersion and plume rise for ' releases above the TIBL) . l (b) Only user-selected stabilities (as determined by the tower AT data) are acceptable below the TIBL whenever the TIBL is 1 above the levels of measurements.(e.g., stabilities A through D acceptable with E, F and G defaulting to D); all i stabilities default to a single user-selected stability whenever the TIBL is below the upper-Igvel instruments. (c) Only user-selected stabilities (as determined by the tower wind-fluctuation data) are acceptable below the TIBL for use in the split-signa dispersion model. (d) Effluents released beneath the TIBL are trapped and not , permitted to penetrate the TIBL even if the plume rise equations predict so; mixing height L in Eqs. (l') and (15) is replaced B by the height of the TIBL. (e) Effluents released above the TIBL that become instantly entrained attain uniform vertical mixing at the release point; mixing height L is replaced by the height of the TIBL and zI is set equal to twice this height to ensure the limit in Eq. (18) is attained. (f) Effluents released above the TIBL that are not entrained disperse according to the three modes described in the previous section: e In zone 1, presence of the TIBL has no effect on the dispersion; plume-rise is based on stable conditions and the temperatur e gradient within the marine inversion
~
l e In zone 2, o is replaced by twice the TIBL height and I o is computed by Eq. (40); the second . term in Eqs. (1), (I) and (3) is multiplied by the fa.: tor in Eq. (41) to i correct for the partial vertical mixing I e In zone 3, o is replaced by twice the TIBL. height; o r is based on Ehe virtual source concept and the stability i underneath the' TIBL selected in (b) or (c) above . 9 f i I f O t e t
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J. . b d j l 5.0 GAMMA DILUTIO'1 FACTORS Evaluation of long-term external gamma doses from routine atmos- l pheric releases is normally based on extensive simplifying assumptions that are essential in reducing the complexity of the problem. An evaluation model that is of interest to the nuclear power industry is described by D. H. Slade in " Met.corology and Atomic Energy - 1968" (Ref. 7 Sec. 7-5.2.5). The model, which is characterized by a finite sector-averaged plume with Gaussian activity distribution in the vertical plane, is of interest because it provides a meaps of. establishing effluent. emission limits and making dosage estimates that are more realistic than ' those based on uniform semi-infinite clouds. The model has been included r in Regul6 tory Guide 1.109 (Ref. 4) as guidance toward evaluating compliance with 10 CFR Part 50, Appendix I. This section presents the method by which the finite-cloud dose rate equation in Regulatory Guide 1.109 has been reduced to that for a semi-infinite cloud via the definition of an eff ective gamma dilution factor. 5.1 Finite-C1 cud Gamma Dose Rate Equation According to Regulatory Guide 1.109, gamma air doses from elevated , releases (and ground-level releases as well) may be computed using the ! i equation: A py ,260C 7 i nsI "a k ki (52) finite XA4 n s.k,1 n l 1 where A 18 the Photon yield f or garana-ray photons in energy group k from i
, ki the decay of radionuclide i, in photons / disintegration , '
i l l
~.
C is the recirculation correction factor, is the annual t tal gamma air dose at a distance X in the inite sector at angle 4, in arad/ year, X is the distance from the release point to the receptor, in meters -
"E is the energy of the kth photon energy group, in MeV/ photon, k
f is the fraction of the time that stability class s and wind speed , n occur for sector $ dimensionless, 5 is the result of the numerical integration accounting for the distribution of radioactivity according to meteorological conditions , of wind speed and atmospheric stability, is a function of the photon energy E p and is t i = 57 + Ki 2 (53) as formulated in Slade (Ref, 7) (K is the air buildup f actor) Qj is the release rate of radionuclide i, in C1/yr u is the mean wind speed of wind speed class n, in m/see at is the sector width over which atmospheric conditions are averaged, in radians, and u is the air energy absorption coefficient for the kth photon energy group, in n-1, From Eq. (52) is is possible to define an energy-dependent gam a dilution f actor for use in computing hourly air dose rates as follows: 2C p (iy + KI2) (54) (X/Q)y " E uX of As shown in Ref. (5), the integrals iy and 1 2 I" *hi" '9"*'I " reduce to the following limits when the size of the finite cloud becomes large:
?
T= y exp (-h*/2o2*) (55) Eya-z
+
and (56) 1"1 2 y'k is 'the air total linear. attenuation coef ficient for the kth~ photon energy group. For,this condition, since k k K=(uk - p,)/u, .(57) Eq. (54) reduces to exp (-h,/2a ) -(58) (X/Q) * , Xuo, and is independent of gamma' energy. Eq. (58) is the basic equation for sector-averaged semi-infinite clouds. To reduce Eq. (52) to a forn similar to that for a semi-infinite cloud, it is necessary to define a few more parameters as follows: ' i A A
- k01 ki (59) k E Q,. ;
ii , IE Q' A (60) i g , i ki i ki ! k - 7 q, A L. i ki IEA (X/Q)Y (61) < k k k (y/q)Y , k EE A , k k k and n (62)
~
(X/Q) "hi I ((X/Q)T) 3-33 . . In these equations, Egg is the actual energy of a gamma ray in group k emitted by isotope 1. Equation (62) is the average gamma
dilution factor for a receptor located in a specified sector; m is the number of hourly values computed for the' sector and N is the total nun.ber of values for all sectors during the period ot' interest. Substitution of these equations in Eq. (52), and replacing f ,
. by (1/N) for the hourly factors, results in:
.1 x1 (X/Q) IQg (DF)g (63)
Ofinite " L where 60 C Ag gE (64) (DF){=Ik 2 x 3.17 x 10 is the gama air dose f actor f or radionuclide i as used in Regulatory. Guide 1.109. 3.17 x 100 is the number of PCi per Ci divided by the number of seconds per year. Note that Eq. (63) is similar in form to the dose equation for semi-infinite clouds. 5.2 g lication SKIRON uses Ege. (54), (61) and (62) to comp'ite effective gamma dilution factors for evaluating air gamma doses from finite clouds for both ground-level and elevated releases. Equation (54) is computed on an hourly basis for as many as 16 gamma energy groups covering the range 0.01 to 10 tieV. Data for I k and E. , as defined by Eqs. (59) and (60), is required as input to the code. Energy-averaged factors are then computed by Eq.(61) for both elevated and entrained portions of the plume and are combined to provide
- the overall hourly gamma dilution f actor:
(65) (x/Q)}3- c (E (X/Q)G + ( ~ t)(X/Q)f). t is the Recall that C is the recirculation correction f actor and E t entrainment coefficient.
The integrals I gand I ing Eq. (54) are computed by numerical integration using the model described in.Ref. (5). Data for the linear energy absorption and attenuation coefficients built in SKIRON is shown in Fig. 5.2.1 (from Ref. 17). Camma dilution factors during seabreeze conditions are calculated by ignoring the presence of the TIBL and applying the following modifica-tions to account for the increased concentrations near the ground:- e For ground-level releases (trapping conditions) I is limited 15 the height of to the maximum value of 0.47 N TIBL the TIBL at thereceptorlocatidBL,whereh n. e For trapped elevated releases, the plume effective height and standard deviation are adjusted to ensure that the entire plume is within the TIBL while maintaining the ground-level concentration:
^ y" TIE 1. (66) z z (h,/c g + 2.15) and T
o h +hT=h -* (67) e e e a, e For releases above the TIBL that becone entrained, I is set equal to 0.47 h TIBL e For releases above the TIBL that are not entrained, o is retained for distances less than the plume-TIBL inter $ept and is set equal to 0.47 h for receptors beyond that point; receptors within the fddkgation zone are assumed to be exposed to both an elevated plume and a fully entrained plume, the contribution from each plume being based on Eq. (41). e
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_ - -. -- -. . . . . - - ~. - -. i ,
,o -
-- 6.0 D1LUTION FACMRS FOR: ACCIDENT EVALUATIONS.
Estimates of off-site exposures following accidental releases of radioactivity to the atmosphere are normally-based on' conservative-assumptions that affect both the' amount released and' che manner in which it disperses.- in particular, according to-the most recent ,. promulgated sethods of analysis. calculational techniques .do not explicitly reflect the hour-to-hour variation in wind direction and?
. predicted doses are assumed to apply in any sector.
Radiation exposure from a specific release could be high or low depending on the prevailing atmospheric conditions and the airflow - pattern during the release. For ground-level releases, for instance, high exposure would result if the release takes place during stable atmospheric. conditions with low wind speeds and if the radioactive material is transported toward the receptor over extended periods of time. Relatively lower doses would result if atmospheric dispersion is more pronounced and/or if the receptor is downwind only during part' of the exposure interval. . Obviously there is a range of radiation levels to which a receptor can be exposed. The procedures for determining dilution factors for design basis accident evaluation should reflect variations in atmospheric dispersion that occur as a function of wind direction frequencies and varying site boundary distances. It is recognition of this fact that has led to (1)). a new series of field tests and the new NRC position (Position HKB The position requires probabilistic assessment of atmospheric dilution in such a way that probability levels for individuals at different
. The locations around a nuclear power station are sector-dependent.
following sections describe briefly the models built into SK1RON for computing accident dilution factors in accordance with this new procedure. 43 - r
- - m. __,
I l
\
1
. 6.1 Ralative Concentration Asgesement ;
I The current method of assessing the atmospheric dilution factors l l for design basis accident evaluations is the selection of values which could be exceeded no more than 5 percent of the time. An inherent ] f inadequacy of this model is that the wind,has an equal likelihood of ! l flowing into each of the 16 cardinal direction sectors. As such ! I the model does not provide directionally dependent dilution factors ; for individuals at different locations. According to the new NRC position, each sector is now to be eval-usted independently. Dilution factor values for each sector are to , he determined by normalizing the frequency of occurrence of dif f usion conditions in a given direction sector to 100 percent, and then selecting ; the X/Q value which is equalled or exceeded F ' percent of the time, where F '= (5 x_1 x 100) 1 (68) 16 f
= 31.25/f.
In this equation, f is the frequency (in. percent) of the winds blowing into the sector of interest, and 0.3125 is the probability level (in percent) of experiencing the "5 percentile" dif fusion conditions coincident with a given vind direction. Dilution values are computed for each sector as described and the highest value is selected for use in the accident consequence analysis. 6.2 Averaging Procedure and Models in determining the accident dilution factors, SKIRON uses the l plume centerline and sector average models described in Section 3, and the gamma dilution model described in Section 5. Dilution factors are computed by the above models for each sequential hour of measured l meteorological data and for receptors positioned in the 16 cardinal compass directions around the plant. These hourly factors and the
-4 4 -
i
, - -, ~ _ _ - . - ,
r l
. - corresponding direction in which the wind is blowing during each-hour are then stored in sector dependent arrays for sequential processing.
. Ten models'are presently built into the code for this analysis. They are as follows: ' Time Window Accident (hours) Time Interval jio,. Dispersion Model_
- 1. 0- 1 hour 1 Delta-T, Plume Centerline 1 0- I hour 2 Split-Sigma, Plune Centerline 2 1-' 2 hours-3 Delta-T, Plume Centerline 2 1- 2 hours 4 Split-Sigma, Plume Centerline 8 2- 8 hours 5 Delta-T, Plume Centerline 8 2- 8 hours 6 Split-Sigma, Plume Centerline 8 2- 8 hours 7
Delta-T, Sector' Average 24 8- 24 hours 8 Delta-T, Sector Average' 96 24- 96 hours 9 Delta-T, Sector Average 720 96-760 hours 10 Delta-T,-Sector Average The last column indicates the time interval af ter the postulated The " Time Window" accident during which the X/Q factors are to be used. column gives the number of hourly dilution factors used in computing Note that plume centerline the average value for each time interval. values are for estimating short-term atmospheric dispersion (up to 8 hours) and sector average values are for dispersion during longer periods of time. Average dilution factors are computed for each sector according to the expression \ be (69) (x/Q), = 1_}{_0 3 (x/Q) ,+3 1 n31 4
- 4 5-I l
~. - ' where n is the hourly sequence in the meteorological input stream at which initiation of the radioactive release is assumed to occur (1 1 n 1 N+1-j,),
N is the total number of hourly meteorological records input, j, is the radiation exposure interval (in integral hours), jn is the number of valid observations during the interval (equal to j, if all observations are valid), and 8 is equal to unity if the wind direction during the 3 (n+j-1) th hour is in the sector of interest, and is equal to zero otherwise. For each selected interval size, the processing begins with the first hourly dilution value on record and then repeated for the same interval size starting with each subsequent hour of dispersion data. In the averaging process, the only values within a given time interval that are considered in evaluating the mean dilution factor for the interval are those for the specific wind direction being analyzed. Missing data are handled by imposing the condition: (70) jn > 9 $m where q is a user-selected parameter that determines the If this minimum number of valid observations per averaging interval. condition is not satisfied the average dilution factor calculated by Eq (69) is excluded from the analysis. As an illustrative example, consider a 4-hour interval and the follow- - ing sequence of hourly wind directions: WWWWSMWMMWSSSSS. In this sequence, W is for the west sector, S is for the south sector and Assuming that each hourly dilution factor H represents missing data. 46 -
h
. .is equal to unity, and limiting the total number of valid observations per averaging interval to at least 2, (i.e. , q = 0.5 in Eq. 70), the sequence of' averaged dilution factors for the west sector are as follows: 4/4, 3/4, 2/3, 2/3,'1/2, bladh 2/2, 1/2, 1/3, 1/4, 0, and O.
6.3 statistical Distributions Application of Eq. (69) produces an array of dilution factors for each sector and exposure interval of interest. These factors must now be classified, for each sector, into groups and corresponding frequency histrograms and cumulative distributions prepared. Since atmospheric dilution factors typically range over a number of decades in value, group boundaries in SKIRON are defined on a logarithmic scale as'follows: i-2 (71) Li = (X/Q[in R 132 and 1-1 Li+1= (X/Q) min (72)
.I where R = [ (X/Q) max ) k 2 (73).
(X/Q) min Li is the lower boundary of group i, Lg+1 is the upper boundary of group i (and the lower boundary of group i+1), , (X/Q[in is the non-zero minimum dilution f actor calculated for the sector, (X/Q) is the maximum dilution f actor, and Max
. k is the number of groups in the histogram. ;
Group 1 was reserved for zero dilution factors which result when the receptor is not downwind during the exposure interval. Group indices , are determined from the largest whole number in the expression
-4 7 -
I J
r log, [(X/Q)] - log, [(X/Q)minl (74) i= 42 log, [ R ] where (X/Q) is the non-zero value to be classified , A total of $41 groups are used to enable determination of selected percentile points with f air accuracy. These percentile points, which range between 50 and 100 percent in increments of 5, identify the expected probabilities that dilution f actors for a given receptor will not be exceeded. The histogram is then reduced to 37 groups for output presentation. In addition to the otandard percentile points, SKIRON also determines atmospheric dilution valuesat percentile points computed according to the relative concentration assessment procedure described in Section 6.1. A normalized prob 3bility percentile point, which defines the percent of time a dilution value is not exceeded, is determined for each sector using the equation . (75) F = 100 - F' where F' is given by Eq. (68). The corresponding dilution value for each sector is then determined and the maximum sector value is chosen as the accident dilution f actor to be used in the design basis accident evaluation. SK1RON produces two full pages of output for each receptor point (one in each sector) and exposure interval: one page for the i dilution factors for determining ground level concentrations, and one f page for the gamma X/Q's. The ground level concentrations are for l computing the potential thyroid and wholebody beta doses from occidental l t releases of radioactivity, and the gamma X/Q's are for the - corresponding wholebody gamma exposure according to the sector average l finite' cloud model. J L r 1 J
?
e l
-4 9 -
7.0 ' CODE PARTICUIARS 7.1 General Structure SK1RON is written in FORTRAN IV and consists of a main program with block data and 21 subroutines. Figures 7.1.1 shows the general strucuure of the code in terms of subroutine calls. A number of simplified logic flow diagrams are shown in Figs. 7.1.2 through 7.1.5. i Functions of the various subroutines are as follows: , SKIRON Maine routine BLKDAT Block data routiae CFACTOR Handles overall recirculation correction factors as described in Sec. 3.9. CHIQS Calls on 11 subroutines to compute the hourly dilution f actors , (plume centerline, sector average and gamma) for receptors in each of the 16 cardinal direction sectors. ECHO Produces a card image printoutof the input data. FREQCY Prepares cumulative probability distributionsof the hourly dilution factors and identifies values at a number of percentile points; prins l results.
~
GAMMA A routine called by GMCHIQ for computation of gamma dilution factors using the gamma energy spectrum and Eq. (61) GMCHIQ Computes stability-dependent gamma dilution factors (via subroutine 1 l
-. . . . . . . .-.. . . - . . . . - . . . ~ - , . , - - ,
4
' GAMMA) at each receptor point for a number'of effective plume heights; prins sample results.
HEADING Produces new output page and prints heading, page number, title, date, dispersion model selected. INTEGR Computes integrals I and I in the gamma dilution formula as described in Ref. (5) INTPOL A routine for linear or parabolic interpolation and linear extra-polation using Aitkin's method of divided differences. IZEROT Initializes integer arrays. . METDAT Reads in and processes hourly meteorological data including seabreeze occurrences. PLUMRS l Computes plume rise (on an hourly basis) using Sagendorf's model (Ref. 9) l SEABRZ A routine called by METDAT for determination of seabreeze conditions l SIGMA Uses parabolic interpolation (via INTPOL) on a log-log scale to compute vertical and horizontal plume standard deviations at each receptor point; prints results. SUKRIES Computes dilution factors averaged over selected intervals for s l
.' each receptor point; calls FREQCY for the probability distributions.
VIRTU Computes virtual source location and horizontal standard l deviation for receptors in zone 3 of Fig. 4.4.1 during a seabreeze. 1 WRTCHQ Output routine called by CHIQS; prints selected hourly results for verification. WRTMET Output routine called by METDAT; prints selected hourly raw and processed meteorological data, and frequencies of occurrences. WRTSUM Output routine called by SUMRIES to print summaries of the accident dilution factors.
.XIVAL Computes plume vertical dispersion and reflections according to Sec. 3.5.
ZEROUT An array initialization routine. 7.2 Input Information Input to SKIRON is provided by (a) Tape 5, and (b) Tape 10,11 or
- 12. Tape 5 contains the general information required by the code as described below. Tape 10 was reserved for the raw meteorological data.
This data must be in card-image form as noted in Sec. 2.1, and in monthly records, and the first data card of each month must identify
' the number of hours in that month (I3 format) . During execution SKIRON prepares monthly records of processed meteorological dats and writes them on Tape 11, in binary form. This information may be saved Similarly, it and used in later SKIRON runs in lieu of the raw data.
~
P is possible to save and re-use the hourly dilut ion factors which SKIRON prepares and writes on Tape 12. This information could be useful in evaluating different exposure intervals without having to recompute the dilution factors. Note however that at the end of a run with more than one problem, Tape 12 would contain only the results for the last problem executed. Tape 5 input is as follows:
)
I l l l f i I
. 1
4 4 SKIRON (MOD 1) - INPUT DATA INFORMATION l l l Card 1 l Col. 1-80 TITLE Any alphanumeric'ebsracters for problem identification 1 Card 1 ' Col. 5 10PT Tape input control: I 1 if starting from raw met data (mount tape 10) if starting from processed met.. l 2 data from earlier run (mount 1 tape 11) 3 if starting from X/Q data from l an earlier run (mount tape 12) , Number of monthly meteorological Col. 9-10 NMONTH records input (right justified) col. 13-15 IPRINT Print control parameter (right justified) , O suppress hourly results printout 1 print all hourly results (2 lines per hourly record - watch out for voluminous output) n print only first n hourly records in each month (2in324) m print every s'th hourly record in each month (m>24) Col. 20 IBW Set greater than 0 to include meander analysis in plume centerline model Col. 25 ICF Recirculation correction factor control 0 no correction .. 3 your own correction factors for each distance and sector (see Cards 20 A.-20B) Col. 30 ICEA Seabreeze option 4 i
. . . _ , ._ _ ._, _- .._ . . . . . - . _ . _ ~ . _ _ . - . _ ,
O for inland sites
>0 for coastal sites (includes trapping and funigation)
W.C Number of gamma energy groups for Col. 34-35 gamma 1/Q (nie. O, max. 16) I Card 3 f Col. 1-10 D1AMTR Exhaust stack internal diameter (meters) DLML Average depth of limited mixing Col. 11-20 layer (meters) EXITV Stack ef fluent exit velocity Col. 21-30 (m/sec)- (may be zero) f HELD Height of building adjacent to Col. 31-40 ralease point (meters) (used for the l determination of the entrainment coef ficient l and the building wake ef fects in the vertical plane - see BAREA) HREL Height of release point above ground Col. 41-50 level (meters) EFMX Maximum allowcd plume center-line height Col. 51-60 at release point (m) TAMENT Def ault average ambient temperature Col. 61-70 for plume rise effects (degrees K) (hourly data used if available) Col. 71-80 Qh Stack effluent heat content (cal /sec) (if >0 only bouyant plume rise vill be calculated) Card 4 2 BAREA Building cross-sectional area (z ) Col. 1-10 for calculating the effects of building wake in the lateral direction Distance from release point beyond Col. 11-20 MWDIST which building wake is ignored
- Card SA - Omit this card if NEG = 0 First group gamma energy (MeV) for Col. 1-10 EGAM(1) samma X/Q computation
Col. 11-20 EGAM(2)- Second group energy Col. 71-80 EGAM(8) Eighth group energy Card 5B - Omit this card if NEG <9 Col. 1-10 EGAM(9) Nineth group energy EGAM(NEG) Last group energy Card 6A - Omit this card if NEG = 0 Col. 1-10 ABUND(1) Abundance (or relative intensity) of EGAM(1) Col. 71-80 ABUND(8) Abundance of EGAM(8) Card 6B - Omit this card if NEG <9 Col. 1-10 ABUND(9) Abundance of EGAM(9) Col. ABUND(NEG) Abundance of EGAM(NEG) Card 7 - Omit this card if IOPI >l Col. 1-80 1MT Met. data input format (7 parameters, example - (10X, 7F10. 3)) (Read blank columns for data not available; use only one set of parentheses) Card 8 - Omit this card if 10PT >l Col. 5 ID(1) Sequence number of direction data in IMT (1, 2, 3, 4, 5, 6, or 7; use 0 if data not available) Col. 10 ID(2) Sequence number of wind range data in IMT Col. 15 ID(3) Sequence number of wind speed data
in INT > Col. 20 ID(4) Sequence number of temperature gradient in IMT Col. 25 ID(5) Sequence number of air temp. in IMT . Col. 30 ID(6) Sequence number of water surf ace temp. in INT col. 35 ID(7) Sequence number of solar radiation in INT Col. 40 IREPL Missing data hand 11ag control: O do not replace missing data 1 replace missing hourly data by data from previous hour Card 9 - Omit this card if IOPT >l Col. 1-10 WDMAX Max wind direction acceptable as valid observation Col. 11-20 RMAX Max. wind range Col. 21-30 WSMAX Max wind speed (same units as in hourly data) Col. 31-40 DTMAX Max. temp. difference Col. 41-50 TMPAMX Max. air temperature Col. 51-60 TMPWMX Max. water surface temperature Col. 61-70 SUNMX Max. solar radiation Card 10 - Omit this card if IOPT >l 1 Col. 1-10 RCONV Factor to convert input wind range data to standard deviations (typically 1 or 0.166667) Col. 11-20 WSCONV Factor to convert input wind speed to m/sec Col. 21-30 DTCONV Factor to convert input temperature
' difference to "C l
Col. 31-40 TMPCON Constant coefficient to convert
- temperature to C (along with l DTCONV) l 1
1
.. )
1 "C = ( F + TMPCON)DTCONV Col. 41-50 SUNCON Factortocon3ertsolarradiation to cal / min /cm WSHIN Min. wind speed acceptable as valid Col. 51-60 observation (m/sec) WSD Wind speed default value when wind Col. 61-70 speed is less than WSMIN (m/sec) Temperature sensor separation (meters) Col. 71-80 DH Card 11 - Omit this card if 10PT >l or ISEA $0 ISEAH1 Hourly input sequence number at start Col. 1-5 of seabreeze season ISEAH2 Hourly input sequence number at end Col. 6-10 of sembreeze season ISEATl Geabreeze earliest daytime limit Col. 14-15 (hours) (>1) ISEAT2 Seabreeze latest daytime limit Col. 19-20 (hours) (124) ISEASC(1) First seabreeze sector (1 for N, Col. 24-25 2 for NNE, etc.) ISEASC(2) Second seabreeze sector (may be 0) Col. 29-30 Col. 71-80 ISEASC(12) 12th seabreeze sector Card 12 - Omit this card if 10PT >l or ISEA f,0 IDTSB Highest 6T stability index for seabreeze Col. 5 (e.g. if IDTSB = 3, seabreeze assumed to occur only with stabilities A, B or C) IDDT1 Highest 6T stability allowed below the Col. 10 TIBL (thermal internal boundary layer) when entire met. tower is below the TIBL (stability indexes greater than IDDTl default to IDDTI) IDDT2 Default 6T stability index when TIBL is below Col. 15 the met. tower upper sensors. IDST1 Highest 00 stability allowed below TIBL Col. 20 l
(stability indexes greater than IDST1 default to IDSTI) Card 13 - Omit this card if 10PT >l or ISEA 5.0 e Min. wind speed for seabreeze (m/sec) Col. 1-10 FWSMIN Col. 11-20 WSMAX Max. wind speed for seabreeze Col. 21-30 SUNMIN Min. solar radiation for seabreeze 2 (may be 0.0) (cal / min /cm ) Col. 31-40 SUND Default solar radiation value Card 14 - Omit this card if ISEA 10 Col. 1-10 HINVL Depth of inversion layer during seabreeze (m) Col. 11-20 HTOWER Height of met. tower above base of release point (a) TDILD Default value for TIDL, the potential Col. 21-30 temperature difference between lower and upper boundaries of the inversion layer if data not input or if TIDL less than TDILMN Minimum value acceptable for TIDL Col. 31-40 TDILMN : l Col. 41-50 AA Constant coefficient in the TIBL l equation - TIBL = AA*SQRT (distance / i wind speed /TIDL) Cards 15A-15B - Omit these cards if ISEA 10 Distance from release point to Col. 1-10 DSHRP(1) shoreline (N sector) Col. 11-20 DSHRP(2) Distance. . . (NNE sector) DSHRP(16) Distance. . . (NNW sec cor) l Cards 16A-16B - Omit this card if ISEA 50 Col. 1-10 DSHMT(1) Distance from met. tower to shore-line (N sector) 4 Col. 11-20 DSHMT(2) Distance. . . (NNE sector) 4 i DSMNT(16) ~ Distance...(NNW sector) Card 17 e Col. 1-10 PCT Minimum acceptable number of valid observations per averaging inter val (expressed in percent of total observations per interval; e.g. 50.0) Col. 15 MDL(1) Set greater than zero to include Nbdel 1 , described below Col. 20 MDL(2) ...for model 2 Col. 60 MDL(10) ...for model 10 . Model Dispersion Model Interval Width (hours) 1 Delta T, plume centerline 1
+
2 Split sigma, plume centerline 1 3 Delta T, plume centerline 2 ; 2 : 4 Split sigma, plume centerline Delta T, plume centerline 8 5 8 6 Split sigma, plume centerline Delta T, sector everage 8 7 Delta T, sector average 24 8 Delta T sector average 96 9 Delta T, sector average 720 10 NOTE: In the plume centerline case, user can select either the delta T model or the split sigma model, but not both. Selection of Model 1, 3 33; , 5 automatically excludes Models 2, 4 and 6. Cards 18A-18B r Col. 1-10 DIST(1) Distance (meters) from release point to receptor in N sector
- Col. 11-20 DIST(2) ' Distance to receptor in NNE sector Col. 21-30 DIST(3) Distance to receptor in NE sector I
s
.. j l
t J l DIST(16) Distance to receptor in NNW sector Cards 19A-19B HTERN(1) N sector terrain height (meters) Col. 1-10 at DIST(1) relative to grade elevation . of release point HTERN(2) Terrain height - NNE sector Col. 11-20 HTERN(3) Terrain height - NE sector Col. 21-30 HTERN(16) Terrain height - NNW sector Cards 20A-20B - Include these cards only if ICF = 3 in Card 2 Col. 1-10 CF(1) N sector recirculatian ' correction factor Col. 11-20 CF(2) NNE correction factor CF(16) NNW correction factor Go to Card No. 1 for next problem. I
- d d
,.' 5<
i FORMAT LISTING i i Card Format No. Card Format No. 1 11 2 . 1 2 12 2 2 3 13 3 3 3 14 3 4 3 15 3 5 6 3 16 3 1 17 5 7 4 18 3 8 3 19 3 9 10 3 20 3 Format 1 20A4 . 2 1615 ' 3 BE10.3 4 16(4X,11) 5 F10.2,1015 READ STATEMENTS i Cards Subroutine , 1- 6 MAIN 7-13 METDAT 14-17 MAIN 18-19 CHIQS 20 CFACTR l d 1
ECHO Oh HEADING 0. SKIRON BLKDAT HEADING 0
'M I ERM METDAT
~
SEABR2 llEADING 0 WMT Y~ I O : ZERot1T
~
HEADING O. CFACTR I
~ INTPOL CHIQS t
- HEADING O OL SIGMA O HEADING !
M- IhTPOL l GMCHIQ 1 GA414 INTEGR 2 INTEGR HEADING
- INTPOL GAhNA 0
M- INTEGR Fig. 7.1.1 General Code Structure - Subroutine Calls (Part A) i t l l
.l i
l
#- IZEROT i
SKIRON CHIQS (continued) (continued) M- ' PLUMRS ) A d- INTPOL i JJ VIRTU I EPOL I i 1 e d- INTPOL 2 h= ' IEPOL A- GAMA da INTEGR
~
INTPOL ' M.- XIVAL j I R 10 WRTCHQ " __ HEADING 0_ HEADING I
- SUMRIES -
0 m -- FREQCY 0
- HEADING 0a
- WRTSUM 0 10 STOP d- conditional call 1 Input via Tape 5 n number of calls O Output via Tape 6 I
Fig. 7.1.1 General Code Structure - Subroutine Calls (Part B)
,. - .. . _ . _ . . . - _ . - .._ . . _ . _ . _ . _ _ . _ . . . __ _ . . , _ . . . . _ . . . . _ _ _ _ . . ~ . - . . .- . . . _ . _ . . _ . ..
- SKIRON START d ,
Read input data. Call METDAT to read and process l meteorological data and to print selected raw and processed data and summaries r No . coast al ' site Yes Read in data for seabreeze analysis;4 exposuremodels 1r 1r , Call CHIQS to compute dilution factors for each sector and print selected hourly results and averages , i r. Call SUMRIES to compute dilution factors averaged over selected intervals for each andsector 6 their probabilities corresponding cummulative distributions
<r re N Go to START l Yes cas s [(END f
Fig. 7.1.2 Simplified Logic Flow Diagram - SKIRON 9
+ . .-. . ,,=* i CHIOS h
Read distances and terrain heights for all sectors 9> > Call CFACTR for recirculation correction. + Call SIGMA for plume standard deviations. t .fg N Yes Is data for dilution factors inputy gl 4 No Call GMC111Q. Initialize routines 4
./ N NO loop on IM, No. of months /
4 Read monthly record of processed met. data from Tape 11. E 4, k0 Loop on M. No. of hours ) 4 If hourly met, data is valid:
- compute TICL height at met. tower, releaae point and dose point 3 if of interest
- identify dispersion mode (normal, trapping or fumigation)
- select stabilities for ground-level and elevated portions of plume
- compute plume rise, effective height and mixing factor in fumigation tone, if any
- compute entrainment coeffi cient
- select or compute proper plume standard deviatiens for ground-level and elevated portions and correct for building wake
- compute plume meander factor
- compute terms for gamnedilution factors
- compute vertical attenuation and reflection terms Compute hourly dilution factors (plume contirli..e, sector average, and gamma).
Enter results in arrays for tape storage. ] M 1 l Transfer monthly record of hourly results to Tape 12
' h O !
Call WRTCilQ for printout i, l RETtlRN Fig. 7.1.3. Simplified Logic Flow Diagram . CHIQS
METDAT ,
"" No ;
Dats 7
, , Yes Read input data. Read data for seabreeze if of interest, Initialize arrays.
ir ' JgDO loop on IN, No. of months - a 1P Read monthly data from Tape 10 ir Do loop IH, No. of hours 3 Reduce meteorological data. Call SEABRZ to identify seabreeze if of interest. ir Include results in array for tape storage 4
- IH d
l Transfer monthly record of reduced data to Tape 11 l ' IM g was ,, A
**InpNS*
f Yes Call WRTMET for printout 1r
- 4 v
RETURN Fig. 7.1.4 Simplified Logic Flow Diagram - METDAT
/
SubmIES o Read entire record of dilution factors : r from Tape 12 (all months) , u _ us/ 4> - W Loop on IH, No. of exposure model v 18 No
' 'model of ntere g
Yes
. ,/"
s , - ,sm DO Loop on KS, No. of sectors v Use the sliding-window approach to compute dilution factors averaged over the selected interval. Identify minima 6 maxima (exclude non-valid data in the averaging) w CALL FREQCY o o Call WRTSUM l
)
i tr 1 i REM l I i e Fig. 7.1.5 Simplified Logic Flow Diagram - SUMRIES 7.3 Sample Input and Output Following is a pcrtial computer output for a snaple probles using five months of meteorological data and a ground-leve2 source. Note that . the site boundary distances are arbitrary, and that the critical sectors for the ground-level X/Q and the gamma X/Q are S and E, respectively, as-can be seen from page 87. Also note that the gamma X/Q is approximately 7 times less than that from a semi-infinite cloud with uniform concentration, a point to remember when computing external wholebody doses from gamma radiation. l 4 1 l 1 l l l l
- l infre/71 k=65 1
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= vakkEr ATCPIC ELEttp1C CD 321cCM tat *0SF*EDIC DISUERS10A FCD CWs (WsLUaffC%C) OtLT&=T Stae1LITY *00EL-Ge0UND LFvEL RELFaSF
= 1 *CUa C*1/cs8 t *~- _4 Sa=FLE FeC8LES = 5 =CATHS CF nata =
ppCuantLITY CIStelmuT10kS 00=%=140 SECTCc h Ga**a C*1/0 (SEC/*33 =
= t== pus awEssGes nt*ETEm3) e Teo.n SECTre avENaGE VALUES j
fu"UlaTIVE
= lamer OF FFRCEAT OF PeteutgCv 01SfeleuT10m anAct TcTal CRS. PtttENT 088EhvaYlCh5 2.013 2.nt3 3 a.69m t
FCO* 2.5583E=06 TO LT.CR.EC. 2.nm3aE=06 a 2.6n5 2.883aE=0h TO Lt.C4.EC. 3.2a97E=06 1.3a2 6.cse - PnC* 3.6626E=06 2 6.711 F"C* 3.2m97E=06 TO LT.Co.EG. 671 , 3.6e26E=06 TO LT.C9.EC. 4.1279F=06 1 2.013 8.725 Fa0* a.652aE=c6 3 10 n67 FrC# s.1279E=06 TO LT.CR.EC. 2 1.382 FK0p a.652aE=06 TO LT.CE.FC. 5.2435E*06 2.013 12.cm1 3 5.9097E=06 5.369 17. min FRO
- 5.2a35E=06 TO LT.C#.ES. 6.6*06E=06 8
2a.532 F80* 5.9097E=06 TO LT.Ca.EG. tt 7.383 6.6606E=e6 TO LT.CH.EQ. 7.5n6AF=06
- 6.nso 10.572 i PRO
- 7.5068E=06 TO LT.CE.EG. 9.an06F=0* a 5.369 36.7a2 FRO
- om.193 pn0* 8.4606E=0h 70 t?.08.EG. 9.5355E=nh 19 12.752 FROP 9.5355E=06 TO LT.CR.EC. 1.0 7m7E=o5 A.05a 57.aa?
12 Fn0* 1.07a7E=0S TO LT.C4.EC. t.2tt2E=05 7 a.h96 At.Tss 1.2112E=05 TO LT.C4.EC. 1.345tE=0% 3.356 65.191 FRO * % 8A0* 1.3651E=c5 TO LT.CS.EC. 1 5386E=05 17 ti.a09 7A.Sto , KHGa 1.5366E=05 TO LT.CR.EG. 1.73 ale =05 6 a.027 en.537
- TO LT.CR.EC. 1.95 ace =05 3.3se 83.m91 FAC* 1.7341E=05 5 86.577 F80" 1.95aaE=05 70 LT.C4.EG. 2 2027E=05 a 2.6a5 F#0* 2.202TE=05 TO LT.04.EQ. 2.a526E=os 5 3.356 89.953 2.T9a0F=05 1.3a2 g1.274 F#C* 2.asanE=e5 TO LT.CR.EQ. 3.iggsg=o5 p 93.299 F#0* 2.T9aoE=e5 70 tt.co.En. 1 2.013 3.1535E=C5 TO LT.OR.EG. 3.55stE=05 1.3a2 98.631 FRO
- 2 95.973 FsC" 3.55 ale =c5 TO l.T.CA.EC. a.on57E=05 2 1.3a2 F#C* m.0057E=05 70 LT.08.EQ. a 5ta6E=05 a 2.685 98.65R F40* a.51a6F=05 T0 t. T .C4.EG. 5.08e2E=05 .671 99.329 FRO
- 5.one2E=05 TO LT.Ca.EC. 5.73a7E=n3 1 0 0.n00 99.329 se0* 5.=3a7E=05 TO Lt.LA.EL. 6.a633E=c5 0 0.00n 99.329 70 LT.CR.EG. 7.26a5E=05 9g.129 Fs0* 6.a633E=05 0 0.00n FROM 7.28m5E=05 TC LT.CR.EC. 8.2100F*05 0 0.000 99.529 FRO
- 8.210nE=05 TO LT.Ch.EQ. 9.253tE=05 0 0.000 99.129 F805 9.253tE=05 TO LT.CW.EC. 1.cm29E ca n 0.00n 99.329 FRO
- 1.0a29E=0a TO LT.LR.EC. t.175st=0a 0.000 99.329 0
FRO
- 1.175aE=0s 70 LT tn.EG. 1.32 ATE =ca 0 0.000 99.329 FRO
- 1.32a7E=0a TO LT.CE.EC. 1.a930E*06 e o.nOn 99.429 FRO
- 1.a930E=0a TO LT.ra.Ec. 1,eg27E=na 671 100.cca 1
1.pp15E=pa Fa0" 1.6627E=na TO LT.09.EG. Trial ta9 1
=1% he*PFe uF VALID C8SEwwaTIC*5 pew avEmastAG IwfEuwaL =
hu*BER CF ZEa0 F6TNIFS SteF 1.16aE=p5 55 on PERCENT PC1kT 50.00 # E R C E *'T POIAT t.n9et.ns n5.00 pERCE %t 0G141 1.%t2t=p5 60.90 #ERCEh? print 1.2mgE=05 1.70a>=e5 7".00 #EECENT phia1 1.623E=n5 75.00 #EsCEST PCIAT 95.no ataCEAT PCIAt 2.2%3E=nS 60.no DEECs=T pr5I A T t.phst=c5 3.penE=ns 95.nn rEnCENT p01AT 90.e0 **hCEh? DetNT 2.711E.05 (=RC TEtw%Itat PCS!?!Oh ' = RELafivE Cr=CtateaT105 Pecuasttlfv1 92.62 DEnCEh? pel*T 3.5t?E=ns . _.e_ _ - . _ _ __ - _ _ _ _ - . - _ _ - _ . .,.w,_- . _ . - _ . . - . _ _ _ _ _ . _ _ _ -
(*D0 01 opics/77) - to/gus77 p a r.g go Sat:02 tat *C87*20tC b!SEE stch FC0 nga Fv&Lustichs)-= va%2Et atC*IC ELECTOIC CO , sa*TLE PC09tte = 5 ECATHS OF cata - GC0thD LEVEL EfLEaSE = 1 MOUD CPI /Oss CEtta=t sta8ILITY *t0EL' ,, i.
'~
GaCU4n-LEvft CMI/c (SEtrat) = pernamILITv otstelaufIn*5 t'O=hal%D SEEfre %wt n(=tttwS1 e 709.0 #Lu=E rE*TEELINE vatuss = 1=WChe avresGES soEQUE=CV 018t4190T104 WAAGE turmE# CF PERCFNT OF Ce=ttle t t vt OPSEnvat!O%5 70 Tat ass. . ps h Ct 's t F40" 1.6720t=06 TO Lt.08.EC. I.ena3F=06 3 1.784 1.7ko Fe0" 1.*Pe3t=0e to LT.OR.EC. 2.3551 Face 7 a.167 %.o%2 8E0" 2.3551t-n4 T85 Lt.On.EC. 2.7850F*** 5 2.976 d.*>* pe0m 2.7*5nE=06 TO Lt.0a.EC. 3.3172E=0* 5 2.976 It.*e% Fa0" 3.3t??L-0, 70 LY.CR.EO. 3.4370 tant 2 1.190 13.**% 880# 3.9170E=04 Tit Lt.ca.EQ. a.6725E=06 0 0.000 - F80p e.6725E=96 tr Lt.04.EC. 5.%egar=06 o 0.000
**C* 5.5sset.n6 70 LT.0m.EC. 6 5ataE=os e 0.000 880* e.541eE=06 f t' L T .C # . F.C . 7.mit0Fene n 0.000 FGCp 7.3((pg=ce TO LT.04.EQ. 9.2702E*00 1 860" 4.2702E=ca 7t' Lt.C#.EC. 1.tec2F=ns 2 SEC* 1.1002t=c% 78' Lt.C4.EG. 1.3058E*p5
- sec. 1.305aE=o5 in LT.CR.EQ. 1.5agtr.os FECW {,5eg?[=rs 79 (T.Ca,gg, t.p392{=p5 880* 1.8192E=05 ?" LT.CR.EG. 2.t**~
FNC* 2.182aE=05 TO Lt.CN.EG. 2 8808 2.5006E=0S TO Lt.0#.EO. 880* 3.0786E=05 TO LT.ca.EO. room 3.6a90E.05 F8C" 8.3300E=* . dg raco 5,ggger T Fa0> 6.100* .* a reCw t,s-FR* , e 1
. ~ ,_ _ _ .., _
f.tD o?. en/65/711
- 10/c2/77 Dat;E e2 3ntLGk (at>C37mE> niiWEaSICA FC2 coa t eatt aTICh5) . vaw2EE" atCatt ELECTGIC Ct' etLta.t Sta91 LIT
- prnet u_ e
. 5 *CkTMS CF Data . Geot:kD t s vet. # ELE aSti
. t NCuu CHI /Ces . to.
Baa>LE PkCPLt* ,, iSCU*C.Ltv5L r*T/C f55C/M3) . P40pam1 Lit? 01stulpettrAs no.%.twe $sCTC# *** . Tao,0 pl0*E CE*TEoLImr valess . 1.>00* &&EsacS5 Ot*ETERSt a
'tWCENT OF CO.9LatgvE
*t.*mER CF 8hEQUE*rv DISTRIPut1CA RakGE tefat CNS. Pt dCE'. T OPSEevatIC*S p 3.75e 1.75e poC* 1.e 10 ns, .0 > TO LT.t;e.EQ. 7. pasts.nh 4.%ee 7.637aF.09 7 1.798 DECm 2.2a5ttsob tri LT.06.EC. 9 a.3Mh 7.50%
Shr* 2.e374E.0e TO LT.Cw.EC. 3.ne92F*oe .P77 m.777 840 1.cee2E pn 70 LT.CA.EC. 3.481e5.o6 t n 0.nce ".772 TO LT.LS.Eu. e p?nes.no FeG* 3.ealaE.06 o n.onn p.777 puC* s.27eet.0e in LY.Cu.EG. 5.nP67F*r* o n 000 p.777 rsC* 5.02e7E*06 TO LT.C#.EC. 5.00^tF*n6 O n.000 S.77# Phtm 5.9astE.c6 tit L.T.lW.EC. 6. ele 2F*o* e n.non v.777 SEGa s. ele 2F =ne in Lt.C4.EO. 4.tstut.im 1".52* e.97e25*ne i 1.758 Sata e.1%3nE=0* 10 Lt.Cb.E4 t ,m77 ti ans 8*Le 9.57e2E=ne 10 Lt.Ce.EC. 1.12ssr.ts 3 7.612 12.n3s 1.1255E=n% tt. Lt.La.f o. t.3pp=E.e% tr.03% re0* 1.55375=c5 a n.enn-56C* 1. 322 e E.e TO Lt.th.f4 1.np%F=ns 7 1.7%e 15.7m= sore t.%s375.es TO tT.re.EC. 7 1.75e tv.5en
*EGa 1.8255E.05 to Lt.C8.E9. 2.tesaE.6% 977. in.azt
- t
- sn0* 2.14eeE 05 TO Lt.CE.EC. 2.%70nE.o5 3 2.412 21.053 F80m 2.5200E.05 TO Lt.Co.EC. 2.eenmE=05 0 0.000 21.053 2.9608E*05 TO LT.Ca.EC. 3.a747E.05 FROW t 877 71.eln F#0* 3.e787E.05 TD Lt.08.EC. 4.nP72E=n5 7 6. tan 74 n70 8
an0* e.0872E.05 TO Lt.C8.EC. a.a021E*05 77 23. ens 53,7%e f '#C* e.4021F.e4 to 1.1.co.FC. 5.ne77F n3 12.2ml 6e.035 5.6e22E.05 10 LT.On.EO. 6.42ett.05 to F#0* 4 e.3"* A8.e71 eur* e.620lE-05 ti. Lt.tu.ts. 7.?*R7p n5 85.0Pd to 16.667 FEC* 7,7447E.g5 in (7.0R,[Q. g.g5tifeg% 8.772 93.non 9.1512E.05 TD tt.08.EQ. t.0752E.ca to th0m ,p?? go,737 t.pA33E.ca t FRC* 1.n757t.ca TO (t.Co.EG. 2 1.75m en.ao* 8 5 t.. 1.pm336.ca to ( f .r e t s, t aea st.ms o 0,00n es. set 880* t.analt.Os to t,t.Cs.EG. l.7a3et.ne ,377 07.3Am FAC* 1.Te39F.0a 70 (f.LW.EC. 2.0 emet.no 2.st7eF=pe t 877 en, pee FRO
- 2.capet.ne TO Lt.LN.EQ. o n. con op Pan F80* 2.e073E.08 TP Lt.CE.EC. 2.pF85F.ca ea.76*
3.3232F=ce o n.000 8tum 2.M285E.re TO LT.CW.EG. n n.nne on.2=e
*RC* 3.3232E.ca Ts. LT.em.Ec. 3,90a*E.na ee.tyt 1 .att F80* 3.ece6E.0a TO Lt.Cn.EQ. .e.587eE.co n 0cn- ee.tpt saan a 5ateE.ca in LT.C8.EC. 6.36spF.no 5.3ectE.ca O
.att t o n .n ein FEOS 5.3eetF. 0a in (T.Ca.g o.
t r't al 1te 1 h0*9ER OF FE#0 EhicIts 3e03 eth AUweto UF wallo CMMEosat?C=3 t'te ave m a n!Nt. l'TEuwat a l 55.Pe PEnrFNT PCJkt 5.p0nE=05 50.n0 #EtCE%T *nt*? 5.e63t.n5 e.nans.o5 ._ l 60.nn *Entt%T poikt 6 toeE.c4 as.no PEntt.: rrt.t L 7s.rm pr ett *
- srgst 7.m3tp.ns 70.00 #5stst? pot %1 7.7eet.0% ns.no pf pct s t DCIAT P. shut.n%
me.on steCEkt poi %t 7 ae3r.n% og.co ptactst FCI. T 1. tope.cs 90.00 PtEC7ht *01st e,7 ppt.cg faut TFCua.fCAL PC$lf]Oh . WFlPelvt LONCT%thatjra *grea4}L1Tw) 90.3e DEstE** pntst t.nter ca
+.rasyr -m.,ii,e- -# = y w c- y ar*'w i.'**~Mrp ee 4 _- ._m__ __s __ _ _ _ _ - _ _ . _
_ _ _ _ _ _ _ _ _ _ . - _ _ _ _ . _ _ _ _ _ _ _ _ _ _ - - . _ _ _ _ _-__m___________-m._ _ _ _ _ . - _ _ _ _ _ _ _ _
("On et. oppr5/771 e e/6% p F 7 pact- a3
= vakapt atC*TC FLEttpft CO 3:1003 taltCgspfk!C ntS3EESICA 500 nun EvaluattCts) ttLTa.T stantLITV #00EL . j
= GR0040 LEWEL #fLtASE = 1 NCbR CN!/cs8 gappLE progLEp . 5 FCstk5 CF Data Ga*WA Chiru tstr. pas) . pwCoastLtt, t,;5f t labt !C-S Du=AuthD SECTOW who SEttre avEmaGE valtie s = 1.*t t's awr eact s Ot*EtERS) e 700c4
*EaCEst nF CbMLtstivt SUMPE8 CF PELCt'1 F8EGLEACv 01518tMtJtlCh ma%CE DN5tovattCAS trt at CB5 i 877
.R77 -
2.*5e?t=06 1 1.tsa 7.637 FCOs 2.307ttenb to Lt.C4.FC. 2.P?99t=0e 7 3.5aa F#C* 2.55?PE=ns -10 tf ts.tu. I .At7 a . t a r. PFC* 2.8359E.06 to Lt.Ce.tc. 3. tea 75-06 3 2.632 3.se60E=06 7.632 8.77/ FeC# - 3. lea 7E.no en t.t.Ca.s.0. 3.p6aet=c6 3 8.77# Fnow 3. men 0E*n* TU Lt.C5.fC. e n nne i ff* Lt.Ch.EC. a.pmS1E*e6 p.non m.?rp F8r* 3.66a9E=04 s.7509t=c6 0 M.FF# FEC*- m.Pe53t.no .triLt.Co.Ea, n n.noo seC* a.750*E=re in Lt.t#.EC. 5.7673F=06 7.n37 tt.aoa 5,m3995.c. 3 33.15 FNC* 5.2673E=0h it+ L t .ta .F c. 2 1.7%s to Lt.LE.Ec. 6.s7c7F=06 1.5n9 14.*AT j Fu0* 5.e349F.Ce 7.t7ae**06 a 22.en? Futh 6 a7a7E=nn to L t .ca.t'c. 7' 4. tao 25.s3a FAC* 7.l?R*E=ce TO L1.LE.tc. 7.45895.=ce 3 2.632 i e.mpatrano 7.nta 32.sse FEC* 7.*5**E=ne te it.rs.FC. 9.7m3at.ne m me.737 F6C' B.*PotE=ce TC Lt.CS.EC. 12.7P1 1.nea75=05 la 57.e37 FEC* 9.783at.ee in Lt.ca.EC. 1.7076E=n5 9 7.R9% 9.6m9 62.2At FRC# 1.06a7E=05 TO Lt.ta.Ec. 1.3333F=c5 11 69.29A FEC# 1.2026E=05 TO Lt.Cn.EC. t.a763E=c% P 7.ot* Fa. Set F80* 1.3333E.05 TO Lt.tp.EC.
- 5.763 79.82%
F#0* 1.a783E=n5 to Lt.UU.EC. 1.6390F*c5 A %.7h3 enc = 1.639et.n5 to Lt.C".Ec. 1.917tE=ns 1 2.637 87.m%n 7.pta7F=p% n.ccc m2.e56 dg ser* 1.st?tt=05 tr Lt.C=.EO. 7.7337F=05 0 9e,3%1 1 F#0* 2.0ta7E=05 to Lt.cs.Eg. p q7AEF=c5 0 7. pet 92.987 - wor" 7.23378.n3 tr Lt.C#.Fi. '2.7a57E=c5 3 2.632 9a.737 Fn0* 2.a765E.05 to Lt.C4.EQ. 2 1.75m 3.naa2F=05 1.75m 96.84) rsch 2.7a57E=0570 to( Lt.Ca.ro. f .Ca ,F C. 3.3753E=05 7 on. net FeC" 3.paa7E.cM n n.oca to Lt.Ch.EC. 3.va7ef=n% e.unn 96.aot 8M0* 3.175tF=n% a.tassF=05 o 97.1a m FSCM 3.7a20E=05 TO Lt .00.E O. I 877 a.599aF=c5 98.pa. EsCM a.tae8E=05 TO Lt.Ca.EC. I .R77 5.n99eE=e5 98.7mm Psr* a.599PE*05 TO Lt.CE.FO. 5.aSe7F=05 e n.nne 99.t74 FRO
- 5.p*9mE.n5 fft Lt.Ca.F.Q. t .a77 sa0* 5.*5a2E=05 to Lt.Cn.tc. 6.7A88E=os a n.non 99.173 e.45n3E=ns 99.121 peCp e.268AE=05 TO Lt.Ca.fc. e n.orn 99.1/3 Fa0# 6.9503F.n5 TO Lt.C4.FC. 7.vo5ns=o5 n n.000 PRO
- 7.7058E=05 10 (t.Ca.Ec. m.%e35$=ns t 877 ten.cni 88C* 9.5a35E=05 TO Lt.C#.EG. 9.an?38 ns invat tem t
3a03 "Iw A'*eEh 0F watin Cantavat tres pFN n*Emastac INtravat e hu=REW OF ZE80 EktEfts 5%.00 *ERCEST #Cist 1.715t.45
$n.00 PEBCEkT P01=t 1.17mF=05 1. tate =a%
n%.co OERCset vlf%t eo.cn *Escant e nI *.T 1.3aaf=n; 75.no PFeCest prist 1.*3tt.o% 10.00 #FECENT p o t .i t t.sant.0% pg.cc steCt h? PCtk 7 7.2haE n% RO.00 #FECFat entht 1.?mit.05 95.0c SEkCg%t Pf;t m e d.Re$t=n5 9n 00 #EeCENT Pt* ) = t 7.197(=O%
= NFlaftvt CCACFwtwatics wwr.h ap tL t t.i 90.36 PEhCEAT *til % t 7.343E=ns (=nC Ytrwuttet PCSITIOk s
_ . _ _ _ _ . _ _ _ _ _ . . _ _ _ _ _ m.u - ___ _ _ . _ _ _ _ _ _ _ _ _ _ _ . _ _ _ _ . _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ - _ _ _ _ _ - _. _
-_ w - ..
. 19/00/71 OsGf. ce
(*0e e*. a##15#77)
$21:0* tat *CSPHE0tt 0157E251HN 800 e@a Evatustirss) a vak:Ef stC.!C ELECTS!C Co 9ttia.T statiLI?9 arrEL c 0LND tFvEL CELEa8E . I wcua cul/ocs '
sample peceLEm . 5 PChtw$ te nata .
't .
t.H tm avEvents aCClot At titof f ow p aCTOSS pF u **C TECHNItat restt res Sopwaev . GWCUAU.LFvEL Cw!#o (SEC/*3) ca=.a rufic retts=30sopts nisfaNCS Pr# CENT (3Ettou s v te s e.S porn 7 (plu=E CENTEntIst .cntt) SECTCn ("ETEas) 1.53a7E.0a 3.bl6eF=05 b 700.0 *2.62 1.6103E.no 3.25 int.05 7pa.n 91.an 2.%9731.o% 4*f 47.33 1.2933E.ns
*E 800.0 9.6e528.ne 2.mme0t.0S F45 90n.0 07.36 3.A?tif.n5 J e5.30 2.368eE.08 E 900.0 2.6899F.04 3.2h72t=ut 956.0 95.07 2.7n=3t 05 FSE 95.se 2.37a9E..a 2.32n95 05 SE in50.o 1.76a35.no tino.O 96.57 2.*nolt.ns SSE
*7.e7 2.655aF.os. 2,e1366 0%
5 125n.0 1.9695E.ca SS. 1300.a 9%.97 t.7593t.na 2.5226t.a5 12an.o es.a2 1.59656 0% 5 o.3n=5F.05 a5 tonn.n on.ct 6.A937E.0% t.07216 0%
. 95n.n 7*.11 7.7esne.6% t.92S$t=05
.A* 859.e a%.5a 2.6262t*05 a9.3% 0.en5cE.05
*. Sno.o 1.ot35E.ca 2.39285 0%
h%. 700.0 9a.36 3.p232L.oS 2.655et.on CRITICAL SECTC#
. ....... ,sn ns ownote. .... . . . .
$3 I
s I
, , - - m -w ,we-- -,-+y*-e& ---gw-w9m e--- e, =iwwiswe _ a- y y- iwy-yw
0 sp k REFERENCES
- 1. NRC Draft Branch Technical Position HMB, " Diffusion Conditions for Design Basis Accident Evaluations",1977.
- 2. 4RC Regulatory Guide 1.111. " Methods for Estimating Atmospheric Transport and Dispersion of Gaseous Ef fluents in Routine Releases From Light-Water Cooled Reactors", Revision 1. July 1977.
- 3. J. N. Hamawi, "AEOLUS", Yankee Atomic Electric Company, YAEC-1120, 1977.
- 4. NRC Regulatory Guide 1.109, " Calculation of Annual Doses to Man From Routine Releases of Reactor Effluents for the Purpose of Evaluating Compliance with 10 CFR Part 50, Appendix 1" March,1976.
- 5. J. N. Hamavi, "A Method for Computing the Gamma-Dose Integrals l y and 12 f r the Finite-Cloud Sector-Average Model", Yankee Atomic E1cetric Company, YAEC-1105 (March 1975).
- 6. Regulatory Guide 1.23, "Onsite Meteorological Programs", U.S.
Atomic Energy Commission, February 1972.
- 7. D. H. Slade (Ed.), " Meteorology and Atomic Energy - 1968", USAEC Report - TID-24190, 1968.
- 8. D. Bruce Turner, " Workbook of Atmospheric Dispersion Estimates".
U.S. Environmental Protection Agency, Publication No. AP-26, Revised Edition 1970.
- 9. J. F. Sagendorf, "A Program for Evaluating Atmospheric Dispersion from a Nuclear Power Station", NOAA Technical Memorandum ERL-ARL-42, 1974.
- 10. G. A. Briggs, " Plume Rise", AEC Critical Review Series, TID-25075, j
. 4 1969.
l b
f 0 Y
- 11. Isace Van der Hoven " Atmospheric Transport and Diffusion at Coastal Sites", Nuclear Safety, 8(5):490-499, September, October 1967.
I Gilbert S. Raynor, et. al. ," Studies of Atmospheric Diffusion from 12. a Nearshore Oceanic Site", Journal of Applied 'leteorology,14(9): 4 1080-1094, September, 1975.
- 13. George F. Collins, " Predicting Seabreeze Fumigation from Tall Stacks at Coastal Locations", Nuclear Safety, 12(2):110-114, March - April, 1971. -
- 14. Boris Veisman and M. S. Birt, " Dispersion Governed by the Thermal Internal Boundary layer", Presented at the 68th Annua 1' Meeting of the Air Pollution Control Association, Boston, Massachusetts, June 15 - 20, 1975.
Amendment 1, Appendix 0,
- 15. Pilgrim Station Unit 2 Environmental Report, Site Investigation of the Seabreezes, May 20, 1974.
- 16. Walter A. Lyons, " Turbulent Dif fusion and Pollutant Transport in Shoreline Environments", included in Lectures on Air Pollution and Environmental Impact Analyses sponsored by the American Meteorological l l
Society, September 29 - October 3, 1975, Boston, Massachusetts
- 17. " Radiological Health Handbook", U.S. Department of Health, Education and Welfare, Public Health Service, Rockville, Maryland, p. 135, J
January 1970. . I e
_ _ _ _ _ _ ~ _ . _ . . .- i l
'l Attachment 2: One hour EAB X/O 6t 0.5% exceedance' probability' developed from Maine Yankee site meterological data January - December, 1977 s l
I The input parameters are listed in pages 1, 2 and 3. Pages 4 through 8 give monthly samples of ' the' input meterological data (50. . hour intervals). I i Pages 12 through 16 list the calculated X/Q values (both for.the plume centerline model and for the sector averaging model) for'the monthly-50 hour' I sample points. The plume centerline model is used for 0-8 hour X/Qs. Pages 18 through 51 give the probability distributions for all sixteen sectors. Given at the bottom of each page are the' sector X/Q values at various percentile values and the X/Q value corresponding to the NRC Technical position of using a X/Q value that is exceeded 0.6% of the total time. (Note: At the time this computer run was made, November 24, 1978,- the NRC had recently changed its position regarding the 0.6% total.exceedance probability' , given in draft Regulatory Guide 1.X73. The final version of the draft j Regulatory' Guide 1.XXX called for . 0.54 otal exceedance probability. As'a j result, the worst' case one hour XiR calet .ated by the SKIRON program' (5.133 x i 10-4) was adjusted by linear interpoiscb a between the two adjacent values to the value of 5.36 x 10-4), Pages 18 through 51 list both ground' level X/Q's and effective gamma X/Q's. (The gamma X/Q's are for use in- calculating finite cloud whole body - gamma doses and are not relevent to this analysis.) A summary of sector one hour X/Q's which exceeded 0.6% of the total time is presented on page 52 for the 610 meter Exclusion Area Boundry. The highest of the 16 sector values is compared with the 5% overall site X/Q and the higher value selected for use as the site one hour X/Q. This value 5.36 x , 10-4 sec/m3 (see note above) is an atmospheric dispersion factor which is ) exceeded only 0.5% of the total time (one years worth of hourly data) for each j of the 16 wind sectors and is associated with the SSW sector. The times that this X/Q is exceeded for winds that are blowing only into the-SSW sector, during the course of a year, is only 8.5% of the time. i l
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I .. 821RON (AINbSPMERIC u!5FENSION FGW Db4 EVALUATIONS) - YANMtE ATOmit EltCTNIC Cu (M00 03, u7/24/76) 11/28/78 PAGE t.
)' + . MY 1977 12 m0 NTH 5 - GkUUND-LEvtL NELE*3E = VARIABLES MEPLaCED = EXCLUSION AREA . . . ) TAPE INPUT OPTION (10PT) e 1 NUMBER OF MONTMLY METEUROLOGICAL NECURDS ANALYSED s ~ ~ ~ ~
12 PRINT CONTROL'0PTION e ' 50 - .) MEANDEN ANALYSIS CONTROL UPTION (Ism) a 1
- ~~
CONNECTION FACTON OPTION (ICF) e 0 SEA 8REEZE OPTION (ISEA) e 0 -- U
~
'O.00 '
ENMAU4T STACK INTERNAL DIAMETEN (METERS) e -
- DEPTM OF LIMITED MINING LAYER (METERS) a 900.00 STACM EXIT VELUCITY (M/SEC) = 0.000u
~ ~ ~' M A RIMUM ADJACENT SUILDING HEIGHT (METERS) e 45.00 -- ~ ' - - -
RELEASE HEIGHT A80VE GNOUND (METERS) e 0.00 MAX. EFFECTIVE PLUME NtIGHT ALLuaED (METER 3) a " ' 400.00 '~~~~~ ~ '- AM81ENT' TEMPER ATUNE '(CECREES MELw!N) e 280.00
~
STACK EFFLUENT MEAT CCNTENT (CAL /8EC) = 0
~ ' ~ ' ~
SUILDING CNOSS= SECTIONAL AREA (SW.METENS) a 1830.00 DISTANCE SEYOND NHICH BUILDING MAME IS IGNORED 1000E+01: '
-- - ~ ~
C ANN A R Ay- EhERGIES-(MEV) ~AND RELATIVE ABUNDANCES FOR GAMMA CHI /O
' - ~~ ~ - - ~ ~ ~ ~
NUNHER ENEkGY 48uhDANCE 1 500 1,0000 9
-- -. -- - - _ ~ - . - . . . . . .. ..- .- -
) 6
~T r\'
SXIRON (AIMLSPMERIC u!SPENSION FOR D6 A EVALUSTIOuS) - Ya%#tE ATOh!L ELECTWIC Co impo e3. v7/24/70) 11/24/70 PAGE
- /%
MW 1977 12 auNTHS - GkU9ND-LEvtl HELEa3F = vaHIaklFS NEPLSCED = EXCLUSION AREA TAPF INPUT OPTIUN (In#T) e 1 o NUdHEN nr MONTMLt METEup0LUGICAL hECORDS ANALYSED t 12 PWINI C ON T wot. osailum a 50 "EaNDEW ANALYSIS CuNTROL UPTION t i ts m ) s t 3 ~~ - COHRECTION FACTUN OPTION (ICF) e U
~ ' - - - -
SEARHEEZE OPTION (ISEA) e- o m 4 ExMauST STACK INTEhMAL DIAMETEN ("ETERS) m 0.00 DEPTH OF LIMITED MI*1NG LAVEN (METERS) = 900.00 '5 STACM EMIT VELUCITY (M/SEC) e 0.0000 ' - ~ MARImum ADJACENT su1LDING HEIGHT (METERS) = 45.00 HELEASE HEIGHT aHOWE GNOUNO (METEMS) e 0.00 'N
' ~ -
MAa. EFFECTIVE PLunE HEIGHT ALLU"ED (METERS) a 400.00 -- AMBIENT TEMPERAtuME (CEGHEES MELVIN) a 280.0u STACK EFFLUENT HEAT CONTthi (CAL /SEC) = 0 (3 BUILDING CNOSS= SECTIONAL AREA (SW.METENS) a 1830.00 - - ' - ~ ' ' ~ - ~ ~ ~ ' ' - ~ DISTAhC C BEV0kO~hMICH~tu!LDING'=AKE IS IGh0 reb 1000E+06 ~- O'
-- - ~'GANMA RAY ENE#GIES (MEV) AND RELATIVE ARONDANCES FOR GAkMA CHI /O O'
N U_M B,E R __ ENENGY_ _ , _ ABUNDANCE ,___ , __ _ _ , _ t 500 1,0000 0 O O O O O
. . . . . _ - - . - - - . - - . - .- .- -. - . . . _ - _ - ~ . _. . . . . _ . - _ . - . _
O O-O _O O
^ .
w k____ _ _ __ _ _ _ _ - _ _ _ _ -_ _ _ . _ _' ___. _ - . .--v e + w
~s SMICOM (ATMUSPMERIC DISPENSIUN FUR UbA EV&LUATIONS)
)' YANMEE ATOMIC ELECINIC Cu (muu v3 u7/2e/70)
=
11/24/F6 FabE 3 MY 1977 12. MUNTHS = GhuumD= LEVEL NELEASE = VANIABLES NEPLACED = EXCLUStum AkEA ) NUM8ER OF HOURLY RECORDS INPUT 8760
^~ -
' ~~
TOTAL NUMBER OF'(ALID'08SERVATIONS'IN THE INPUT DATA
~ ~~~ ' ~ ' ~ ~ ' -
3
~~' ' '
WIND DINEC110N na99 DIRECTION RANGE' 5933 ~~~~ - 3 m!ND SPEED 8720 l TEMPERATUNE DIFFERENCE 8751 AIR TEMPENATUNE 8745
~'~ ~ ~~ ~' ~~~
)
~'
MATER SURFACE TEMPENATURE O
- ._ __SUL AR RADIATION 6391 3 TOTAL NUMBER OF LOW WIND SPEED ObSENVATIONS 6 TOTAL NUm8ER OF WANIABLE WINDS REASSIGNED 516 TOTAL Num8ER OF SEABREEZi UCCUNENCES
)
~ ~ ~ ' ~
0 $ SEQUENCE CLASS DELTA T. 088 SIGMA THETA 088 D 2 B 66 666 3 C 187 1889 4 0 3588 2156
- ' ~ ~ ~ ' '
D 5 E 3347 353 F
- 6. _. .
7 _ _ . . 900_ _. 12 .. . . _ . . . _ _ . . . _ . _ . __ _ _ _ _ D _ _ ____ DISTRIsuTION OF WALID n!ND DINECTION 08SERVATIO48 __ D w!ND FROM OCCUMENCES D NNE 501-NE 366 g ,, . . . . _ . _ . . . _ _ - D ' E 192 ESE 187 ' - - ' ' - - - ' - ~ ~ ~ -'~ ~ - - - ~ ~ ~ - - ' ~ SE " 295 ~' ) SSE 652 _ _ _ _ _ _ ~ _ . _ . - _ . _ _ . . _ . _ . - ~ 3 922 SSN 684 ~~ ~ ' ~ ~ ' ~ ^ ~ J SM 418 WSM 4e7
, ..3,$ _
_ _ _ _ _ _ _ _ _ _ . _ _____.__________m _ . _ _ _ D uNN 691 Nw 1092 NNW 801 ~~~~ - D
~ - - -
j s - , 3MINUM (ATMUSPMENIC UIB7ENSION FOR Oba EvALU6110NS) = vahnEE STO4IC ELECINIC Cu (Mou 03e 07/de/7e) 11/24/7e eAut a my 1977 12 MONTHS = GNOUNO-LEWEt. *ELEASE = VAH1 ABLES HEPLALED = EXCLUSION AREA i LIST OF MOUMLY ME1Eue0 LOGICAL DATA 7CCFei1ND-DIREC ^ MIND ~~ TEMP Ala' mATEM SULAN D.IEM SIG.TH WIND SPEED DELTA I AIR T MAT.suNr SULAN *t. SEAbHZ SEC. DIR. RANGE SPEED DIFF TEM 8.YEM RAD CLA50 CLAS8 FRD4 (m/SEC) (M/100M) (C) TEMP (C) (LY/ MIN) IF GT.0 ! MON 7H I 1 _ 314, _ 12,e _ 5.50 ,10 _ 8,0 0.0 0.00 E D Nm 2,46 _ _=.110 =13.33 999.01 0.00 ,0 51 344 5.9 3.30 5.10 19.0 0.0 0.00 G E_ NNa 1.e4 5.599 -7.22 999.01 0.uc 0 101 354, 10.8 4.50 2.40 19.0 0.0 0.00 F D N 2.01 2.635 =7.22 999.01 0.00 0 _ 151 76, 7,4 11.00 =,70 25.0 0.0 0.00 0 E EhE 4,92 =.769 ~3.89 999.01 0,00 0 __ 201 316 . 10.1 4.00 =.10 10.0 0.0 21 E D Na 1.79 =.110 =12.22 999.01 .21 0 251 249 18.1 16.50 =1.00 19.0 0.0 50 0 C m8m 7.38 =1.098 =7.22 999.01 50 0 301 309,__ 18,6_._10,60__=,90 11,0 0,0 ,59 D 8 NW 4,74 =,988 =11,67 999.01 59 0 351 327. 7.1 5.00 . 70 15.o 0.0 3e D E NNW 2.24 =.769 =9.44 999.01 34 , . 0 C01 306 9.8 8.80 =.eu 8.0 0.0 01 E D Ng 3.93 a.439 =13.33 999.01 01 0
- C51 17.9 1.90 3.30 te.o u,o 0,00 F 8 8m 85 3.623 =10.00 999.01 0.00 0 ~ ~ ~ ~
' - ~ 501 ~' 88R. 329.. 8.9 10.70 =.20 23.0 0.0 0.00 E D NNa e.78 =.22u -5.00 999.01 0.00 0 551 3e7 19.9 2.u0 2.eb 20.0 0.0 0.09 F 8 Nha 89 2.035 =6.67 999.01 0.00 0 001 2953 10,7 _ 6,40 _=,40 _ 31,0 9,0 0,00 E D *Nw 2,86 . 439 = 56 999,01 u,00 __ _0 c51 2st. 9.7 8.10 =.30 12.0 0.0 0.00 E D >Sa 3.62 =.329 =11.11 999.01 0.00 0 701 250 14.2 7.50 . 40 2.0 0.0 0.00 E C mSd 3.35 =.439 =16.67 999.01 0.00 0
~ ONTH' M 2~ ~ '-
1 230 7.5 7.50 =.50 12.0 0.0 0.00 D D SN 3.35 a.549 =11.11 999,01 0.00 0 51 2e6, 20,3 3.00 ,60 15.0 0,00 8 NSW 1,34 659 999.01 0 16.0- 0,0 a E. ~=9.44 0,00 I tot 332. 7.4 2.90' 4.40' 040-'9.00 G E NNW ~1.30 e.831' =8.89 999.01 0.00~ ~ 0 < 151 300 9.2 6.20 =.40 12.0 v.0 0.00 E a mNw 2.77 =.e39 =11.11 999.01 0.00 0 201 ~888 17.1 1.90 .3.00 15.0 0.0 .e3 F C N 85 3.294 =9.se 999.01 43 0 ' - ~ ~ 251' 181. '8.1 10.70 =.60 35.0 0.0 24 D D 5 4.78 =.659 1.67 999.01 24 0 301 108 9.5 12.00 =.50 38.0 U0 03 D D ESE 5.36 =.549 3.33 999.01 .u3 0 351 343 8,9 5.80 = 60 33.0 0.0 03 ~DD' D 2.59 =.659 56 03 0 801 319 9.8 ~11.30 7 ,0022.0
. U.0 -~ .11 D' NNW
~ Nw ~5.05 =.e59 999.01
=5.56~ 999.01 - - ' .11' o est 271 5.0 3.20 0.00 31.0 0.0 0.00 E E a 1.43 0.000 =.56 999.01 0.00 0 I 501 295 5.0 14.00 =.30 24.0 0.0 0.00 E E NNW 6.26 =.110 =4.44 999.01 0.00 0 ' -~
' ~ 551 61. 12.1 ~ 7.70 . 80 26.0 0.0 0.00 D D ENE 3,44 ..e78 =3.33 999.01 c.00 0" C01 236. 3.5 a.30 60 35.0 0.0 0.00 E F Sw 1.92 .e59 1,67 999.01 0.00 0 051 341, 7,8 5.00 2,40 38,0 0,0 _0,00 F D NNw 2.24 2.635 3.33 999,01 0.00 0 MONTH 3
' ~ 1 262. 8.8 3.10 70 29.0 0.0 0.00 E D W 1.39 769 =1.e7 999.01 0.30 O ~ 51 225. 12.2 4.70 . 20 31.0 u0 0.00 E D Sa 2.10 =.220 =.56 999.01 0.00. O 4 101 50 11.4 9.00 =.40 36.0 0.0 0.00 E D NE 4.02 a.439 2.22 999.01 0.00 0 151 111.1 1.50 1.60 32.0 0.0 01 F Na 67 1.970 0.00 999.01 01 0 ~ 201-~ 19 488 2.~ ~ 12. u '~ 5.9 0 =.40 37.0 0.o 54 E D S$a 2.64 =.439 2.78 999.01 59 0 251 48 17.0 a.eu =.50 56.0 0.0 90 D C NE 1.97 = 549 13.33 999.01 90 0 301 90 12.5 m.co ..lu - =e.o v.o .le E C E 1.97 =.!!0 6.67 999.01 .te o 351 2 12.4 8.70 .70 40.0 o.o 14 D D = 3.89 =.769 4.e4 999.05 .te 0 act 300 12.9 2a.60 .co 3e.n 0.0 27 o C aka 11.00 =.e78 1.11 999.01 27 0 c51 317 11.5 18.60 =.20 34.0 0.0 0.00 E D Nw 6.62 =.220 1.11 999.01 0.00 0 ~ 501 209 53.9 2.90 3.20 3n.e u.o u.oo F A 53* 1.30 3.513 3.33 999.ut 0.00 o 551 320 B.2 10.50 ..co St.o u.0 u.uu E D Na e.e9 ..d39 .50 999.01 0.00 0 3 601 333. 10.6 13.10 =.co 31. ee 0.0 U.e E D uNa 5.66 =.e39 =.56 999.u1 0.00 .o 4 651 29 69*.1 0.20 4.90 31.0 u.o u.ou G N*E 98 9.772 =.56 999.01 0.00 0 701 14 20.= 2.90 3u 36.u 0 . t. o.ou E B NE 1.30 . 329 3.33 9u4,01 0.00 0
. _ _ _ _ _ _ _ _ _ . _ _ _ _ _ -1 - _ _ _ _ _ _ - - _ . _ _ - . _ v r-- r , n g .- e +w=-. .4_.... ,m _ y
4) 8%IWON (ATMUSPMERIC UISPERSION FOR D84 evaluations) - YANmEE 410MIC ELECINIC 00 (MOD 03, U7/24/76) !!/de/Te Pabt 5 (D .
, MY 1977 12 MONTMs = 6RouhD= LEVEL NElttSt = var 1 ABLES MEPLaCED - ERCLUSION a>Ea GD ' LIST OF MOURLY METEUNOLOGICAL DATA
-- HOURLY-^ KIND D!aEC -~ m!ND-- TEMP ~ 'Atk waTEN SOLAR D. TEM SIG.TH MIND SPEED DELTA T AIR T hat. SURF SOLAN R. SEA 8RZ-~~
dp SEG. DIR. HANGE SPEED DIFF TEM 5. TEM WAD CLA8S CLASS Fh0M (M/SEC) (n/100M) (C) TEMP (C) (LY/ MIN) IF GT,0 () MONTH e 1 310 11.0 . 20 39.0 0.0 99.90 E D Nw 5.81 =.220 3.89 999.01 999.01 0 51-- 137. 11.e--13.00 15.40- e.50 40.0 0.0 99.90 0 -D~ SE 6.88 . 589 a e4 999.01 999.01 ' ~ 'o C) 101 til. 11.4 12.50 =.60 37.0 0.0 99.90 0 0 ESE 5.59 . 659 2.78 999.01 999.01 0
~~
151 250 16.3 11.10 . 80 33.0 0.0 28 D C nsa e.96 a.878 56 999.01 28 0 201' 307 12.4 17.00 =1.20 21.0 0.0 87 D D Nn 7.60 =1.318 -6.11 999.01 87 0~~~-~~~ () 251 179 12.8 8.40 =1.30 36.0 0.0 1.1) D C S 3.75 =1.427 2.22 999.01 1.17 0 301 169 5.5 17.60 =.40 51.0 0.0 1.06 E -E S 7.87 ..e39 10.56 999.01 1.06 0 35 f-- 32 3 11.5-~ 2 2. 5 0 ~ = 1. 2 0 -- 4 8. o - 0.0 65 0 D wn ~10.06 =1.318 8.89 999.01 65 ~o CD 401 167 7.1 11.60 =.e0 49.0 0.0 27 E E SSE 5.19 . 439 9.44 999.01 .27 0
~'
451 131. 7.e 5.10 . 70 es.o 0.0 01 D E SE 2.28 . 769 6.67 999.01 01 0
~~-
501 13.3 9.Su 70 59.0 v.00 4.25 769 201.~ 0.0 E C SSw 15.00 999.01 0.00 0' () 551 59 12.2 e.eo .60 e4.0 0.0 0.00 0 D ENE 1.97 =.659 6.67 999.01 0.00 0 601 335 8.3 3.10 40.0 0.0 0.00 E D NNw 1.39 . 220 e.44 999.01 0.00 0 651-- 167 5. 7 -- 6. 6 0 '-".=.20 3 0 ---44.0' O.0 0.00 E -'E" SSE 2.95 329 6.67 999.01 0.00 0 CD 701 270 27.6 2.30 3.30 35.0 0.0 01 F A w 1.03 3.623 1.67 999.01 01 0
~ MONTH 5
() 1 888 14.5 1.40 9.00 38.0 0.0 0.00 G C NNE 63 9.881 3.33 999.01 0.00 0 51 355, 6.8 a.50 20 48.0 0.0 0.00 E E N 2.01 220 8.89 999.01 0.00 0 101 20 12.7-- 3.00 5.50-- 3 6 . 0 ~ 0.0 02 G~ ~~~ C' NNE 1.34 ~6.039 2.22 999.01 02 ~0~ D 151 291. 18.3 a.7u . 60 49.0 0.0 26 D 8 *Na 2.10 =.659 9.44 999.01 26 0 201 15 12.1 11.20 -1,20 43.0 0.0 45 0 D NE 5.01 =1.318 6.11 999.01 45 0 '-- 251 347 ~11.0 17.70 =t.20 51.0 0.0 75 D D NNn 7.91 =1.318 10.56 999.01 75 0
- 2) 301 326 11.5 20.30 =1.30 56.0 0.0 85 D D NW 9.07 -1.427 13.33 999.01 85 0 351 170 8.7 14.80 . 50 56.0 0.0 1.02 D D 3 6.62 . 549 13.33 999.01 1.02 0 z83.-~999.0 '.27 -- ~ nNw ~-
~~
401 15.00 =;60 87.0~~ o.0 D -- 6.7i~ .659 30.56 99 9. 01 ' - ~ ~ ~ ' . 2 7 ~ ~ 0 'C) C51 182 8.9 6.80 =.80 48.0 0.0 06 0 D 3 3.04 . 878 8.89 999.01 06 0 501 168 15.3 3.90 =.30 51.0 0.0 0.00 E C SSE 1.7e =.329 10.56 999.01 0.00 0
^
202 7.10 64.0
^
-~~ 551 ~12.5 20 0.0 0.U0 E C 53= 3.17 220 17.78 999.01 0.00 0
() C01 337 10.8 16.60 =.50 62.0 0.0 0.00 0 D hNn 7.42 =.549 16.67 999.01 0.00 0 C51 10 13.0 2.20 8.70 42.0 0.0 0.00 G C N 98 9.552 5.56 999t *; 0.00 0 1 7 01-~~~~4 8 8 19.3 1.70--~5.20~-~44.c - 0.0 05' G ^'~B ~ ~~~~ ~ S e ~ ~ ;76 ~5.709' ~ 6.67 '999.0t 05 ~~'O~- O I CONTH 6 1 - 171.' " t e '. 2 - 's .9 0 ~ ~. 4 0 ~ ~ 55.0 0.0 0.00 E 8 8 ~2.19 439 12.78 999.01 0.00 0-------- l2) 11 347 11.4 2.10 50 55.0 0.0 0.00 E D hNe 94 549 12.78 999.01 0,00 0 l 101 888 31.0 1.90 5.20 5s.O 0.0 01 G A E8E 85 5.709- - 12.22 999.01 01 0 l 131 37 19.1-- 5.10 - . 8 0 -- 4 9. 0 -~~ u . 0 '.05- D ~B N E ~~- 2. 2 8 ~ ~ ~ = . 8 7 8 ' 9.44 999.01"--- 05' ~ ~~ 0 C) 201 177 14.0 5.70 =1.00 58.0 0.0 9e D C 3 2.55 =1.098 14.44 999.01 94 0 251 7 12.3 12.90 . 60 55.0 0.0 13 O D N 5.77 =.659 12.78 999.01 13 0 ~ - - ~ ~ - -
^301 1F3 16.0 5.60 =.10 69.0 0.0 71 E C 3 2.50 . 110 20,56 999.01 71 0'
(> 351 322 13.4 14.10 -1.40 78.0 0.0 1 ve C C NM 6.30 =1.537 25.56 999.u1 1.08 o Got 160 999.0 9.00 30 58.9 0.0 02 E SSE 4.02 329 14.44 999.91 02 o c51
~~
153.~ 999.0 ~e.50- . 90 56.0 0.0 15 0 SSE 2.01 . 988 13.33- 999.01 15 -~0 () 501 159 999.0 2.00 . 70 56.0 0.0 0.00 0 SSE 89 =.769 13.33 999.01 U.00 0 551 206 999.0 5.00 . 50 60.0 0.0 0.00 n SSa 2.24 . 5e9 15.56 999.01 0.00 0
~-~ Col 162 999.0 11.00 80 60.0 0.0 0.00 t SSE e 92 875 15.56 999.01 0.00 0 -
() C51 888 39.9 1.80 3.50 5E.0 0.0 0.u0 F A NNn 80 3.843 14.44 999.01 0.00 0
. ~ __.
) +.
SMICOM (ATMOSPNEh!C UtbPEN$tum Fua use EVALUATIONS)
- YANMEE atum1C LLECTRIC Cu ImuD u3e 97/24#76) 11/de/re pa4E 6
)'
. MY 1977 12 MONTH 3 = GROUND = LEVEL HELt abF = var 1aHLES HEPL ACED = EECluh10N ahEa 7 -- - - .
[) LIST OF NOURLY METEORDLUEICAL DATA HOUILY =IND-~DIREC'^ntND~~ TEMPAIN" =aTEN 'autaR D. TEM SIG.TH nihD SPEED DELTA T AIR T mat.SudF SOLAR R. ~ SEA 8RZ [) SEG. DIN. RANGE SPEED DIFF TEM S. TEM WAD CLASS class FNOM (M/8EC) In/tuum) (C) TEMP IC) (LY/ MIN) IF GT.0
~ ~ ~ ' ~ 7 01 226 12.7 7.80 . 20 63.9 0.0 05 E C Sw 3.e9 =.22u 17.22 999.01 05 0'-~~~,
MONTH 7 1 191. 18.1 3.80 1.90 64.0 0.0 0.00 F B 3 1.70 2.086 17.78 999.01 0.00 0 [) 51 327 e.1 3.9u 3.10 56.0 0.0 01 F E NNu 1.74 3.404 13.33 999.01 01 0
~~~~ tot 256 10.e 3.40 1.90 m2.0 0,0 04 F D >Su 1.52 2.086 16.67 999.01 04 0 151' 358, 29.1 3.90 =.80 59.0 0.0 77 D A N 1.74 =.878 15.00 999.01 77 0
[) 201 248 32.0 3.20 =2.30 61.0 0.0 42 A a man 1.43 =2.525 16.11 999.01 42 0 251 181,~~ 17,8~~-6,90 =1,20 72,0 0,0 _1,26 0 8 5 3,08 =1.318 22.22 999.01 1.26 0 301 162 999.0 5.30'=l.20 '71.0' ~ 0.0 52 0 SSE 2.37 =t.118 21.67 999.01 52 0 E) 351 196 14.9 8.90 =1.00 79.0 0.0 1.03 D C SSa 3.98 =1.096 26.11 999.01 1.03 u 801 192 15.2 7.30 =.20 78.0 0.0 34 E C SSw 3.26 . 220 25.56 999.01 34 o
~ ~ ' 451 211. 15.0' e.80 2.00 84.0 0.0 .u? F C SSm 2.15 2.196 28.89 999.01 07 0 ~~~~~~~-
E) 501 227 11.6 2.80 0.00 71.0 0.0 9$490 E D am 1.25 0.000 21.67 999.91 999.04 0 551 232,~ 9,0 2,80 ,80 0,0 99190 E, D Su 1,25 878 ~ 17.22 999.01 999,01 0 60l'"~285 14.8-~~4.00 1.40~~43,0~~~0.0 62.0 99/30 F C mNW 2.68 ^^ 1.537 16.67 999.ut' 999.01' 0 E) 651 888 31.0 1.50 3.50 52.0 0.0 99.40 F A NNa 67 3.843 11.11 999.01 999.01 0 ____701 143. 24.5 2.70 70 60.0 u.0 99.80 E a et 1.21 769 15.56 999.01 999.01 0 _ _ _ , E) M0aTH 8 1 139 14.5 2.10 1.30 0,0 ^0.01 E C SE 94 1.427 16.11 999.01 0.00 0 51~~ 888 16.7~- 1.70- 5.20~~~61.0 60.c ~' O.0 0 G C NE
".76 - ~'5.709'~~15.56 999.01 01 ~~~0 o 101 888 18.9 1.50 2.00 64.0 0.0 .ut F B S 67 2.196 17.78 999.01 .cl 0 151 20 9.1 4.00 10 68.0 0.0 21 E D hNE 1.79 110 20.00 999.01 21 0 L ~--201 298 '10.4 12.00 -1.10 73.0 0.0 9 D D >Nm 5.36 =1.208 22.78 999.01 90 0
- " ~ ~ ~ ~ ~
g 251 22 999.0 3.50 =1.50 67.0 0.0 45 C hwE 1.56 =1.647 19.44 999.01 .e5 0 301 173 999,0 7.10 . 90 72.0 1.18 0 8 3.17 =.988 1.18 0 351 266 21.8-- 10.50~=1.Io 73.0~~0.0 0.0 ~ ~.92 ~ D ~ ~8~'~w 22.22 . 999.01 999.01 -~ ~~~. 92
' ~ 4. 6 9 - - =1.2c8'.22.78~~ ~0 j) 801 205. 18.8 6.e0 . 20 72.0 0.0 15 E 8 esw 2.86 . 22u 22.22 999.01 15 0 451 204 22.5 3.50 60 62.0 0.0 02 E A $3m 1,56 659 16.67 999.01 02 0 501 145.' '17.4 ~2.50 1.40' 57.0 U.o u.00 F C SE 1.12 1.537 13.89 999.01 0.00 0' ~ ~ ~ "
h) 551 160 27.6 2.29 1.00 62.0 0.0 01 E A SSE 98 1.098 16.67 999.01 01 0 401 888 39.4 1.40 1 52.0 0,0 0.00 E A NW 72 1,427 11,11 999.01 0,00 0 651-~~217 16.2~~~~4~30 0,30 00 65.0 u0 -~ 0. 0 0 ~ " E ~~ C - ~~ S w ~ l . 1.9 2 ~ ~ 0. 0 0 0 18. 3 3 ~~~ 9 9 9. 01 ~ 0. 0 0 0 D 701 347 10.7 2.10 2.00 68.0 0.0 0.u0 F 0 NNw 94 2.196 20.00 999.01 0.00 0 D 1 146 25.7 2.60 .to 59.0 0.0 0.00 E 4 SE 1.16 110 15.00 999.01 0.00 0 51 22, 11.4 2.50 =.20 67.0 0.0 8,00 D NNE t.12 =.220 19.se 999.01 0.09 0 101 888 30.5 1.90 3.30 54.0 0. 0 ~ 0. 0 0 ~~~~ F ~ A ^ - ~~ n'~ 85 3.623 ~~12.22 ~ 999.01 - -~ 0.00 O 151 342 9.7 5.3u 2.00 Se.0 0.0 25 F 0 NNw 2.37 2.196 12.22 999.01 25 0 2u1 131 15.7 a.uu . 20 56.0 v.u 46 E C SE 1.79 . 220 13.33 999.01 .e6 o
~~- ^ 2 51 315 11.7 '17.80 =1.10 62.0 0.0 97 0 D Nm 7.96 =1.208 16.67 999.01 97 0
~ ~ ~ ^ ~ ~ ~ ~
U 301 152, 13.6 3.70 =.90 59.0 0.0 27 D C SSE 1.65 =.988 15.00 999.01 27 0 351 295 18.7 8.10 =.90 62.0 0.0 ~~ 44 D 8 mNw 3.62 =.988 16.67 999.01 64 0 401 9 8.'~~~ 18. 7 -~~ 3. 0 0 ' ' . 3 0~'57.0 0.0 04 E 'M E 1.34 =.329 13.89- 999.01 .oe~ ~~~0 451 888 26.8 1.9u 1.70 31.0 0.o 01 F a SSw 85 1.866 16.11 999.01 01 0 501 356 10.0 8.70 =.2u e6.0 0.u .ut E D N 3.69 . 22u 7.78 999.01 01 0
~~~" 551 ' 888 53.2 1.40 1.20 50.0 v.o 0.90 E A SSE 63 1.318 10.00 999.01 0.00 0~~~~~~~
481 38 15.2 3.30 30 47.o 0.0 01 E C NE 1.48 329 8.33 999.01 01 0
. _ _ _ _ _ _ _ _ _ _ . _ _ _ _ _ _ . _ _ _ _ _ _ _ .. __ _ _ _ _ . . , ,_._____1__ _ , ., - , . . , . ,, .w., - , _ . _ . m. . . , . . . ~ . .. .
q k~ 3EIRUN (ATMU5PMERIL UI5 PENSION FON Det EVALuATIuNS)
- YANMEE ATOMIC ELECidIC CO (MOD u3, o7 2e/76) 11/2e/78 PAbE '7 D
- "- MY 1977 12 MONTM8 = GNuuhD= LEVEL MELEA3t = VARIABLES MEPLACED = ERCLUSION AREA __. ..
[)' LIST OF MOURLY METEOROLOGICAL DATA M00ACY- w!ND-DIREC~w!No TEMP AIR " HATER" SOLAR D. TEM SIG.TH -w!ND SPEED ~ DELTA T AIN T MAT. SURF SULAN R .'" SEneRz
.[) SES. DIR. RANGE SPEED DIFF TEM S. TEM HAD CLAS5 CLASS FNOM (M/SEC) (K/100M) (C) TEMP (C) (LY/ MIN) IF GT.0 ;
----~ 451 221 95.0 2.40 2.40 54.0 0.0 01 F Sa 1.07 2.635 12.22 999.01 01 0
' ^ - - ~ ~ - ~ '
- 5) 701 320, 75.7 2.00 2.20 e4.0 0.0 01 F A Nw 89 2.415 6.67 999.01 01 0 MDMTH 10 D 1 135 999.0 ,e.20 =.10 54.0 0.0 0.00 E SE 1.88 =.110 12.22 999.01 0.00 0 51 999.0 7.70 . 50 50.0 0.0 0.00 D N 3.44 . 5e9 10.00 999.u! 0.00 0 ~~~ " ~~~
101 ~ 356, 295. 999.0 e.10 2.40 F 1.83 2.635 44.0 0.0 0.00 *Na 6.e7 999.01' O.00 0 3 151 336, 999.0 e.90 1.70 40.0 0.0 13 F kNm 2.19 1.866 4.e4 999.01 13 0 201___127t __999,0__13.20_ f,50___53,0,___0,0 ,0 e _ D SE 5.90 =.5e9 11.67 999.01 04 0 2$1 999 999.4 4.00 .t.10 53.0 0.0 .99.90 D 1,79 =1.208 11.67 999.01 999.01 0 E) 301 999 999.0 8.00 a. Po 54.0 0.0 99.90 0 3.58 .878 12.22 999.01 999.01 0 351 999 999.0 9.00 =.50 ~~45.0 0.0 99.90 D e.02 . 549 7.22 999.01 999.01 0
~~- 401 "60.' 999.0~ 3.00 =.30 48.0 0.0 99.90 E ENE 1.34 . 329 8.89 999.01 999.01 o'
~ ~ ~
[) 451 89 999.0 6.00 10 50.0 0.0 99.90 E NE 2.68 110 10.00 999.01 999.01 0 501 233 999.0 2.00 6.40
~
48.0 99.90 -- G Sa 89 7.027 8.89 999.01 -0 3.00-~2.20- 37.0 -~~o0 0.0
~~
551 3e5.-- 999.0 99.90 F NN= ~ 1.38 ~~~ 2,415 ~2.78 - 999.01 999.01 999.01 0 [) 401 89 999.0 2.00 3.50 49.0 0.0 99.90 F E 89 3.e#3 9.se 999.01 999.01 0 051 347 999.0 3.00 0.00 51.0 0.0 99.90 E NNm 1.34 v.000 10.56 999.01 999.01 0
---- 7 61 ~ ~ ' 3 5 s . 999.0 5.00 3.30 36.0 0.0 99.90 F N 2.2e 3.623 2.22 999.01 999.01 0
~
MONTM 11 .
. 1 88I.- 999.0 1.00 5!90~~ 34.0 0.0 - 99.90 'G ~ NNd 45 6.478 ~1.11 999.01 '999.01 ~~0
[) 51 223 999.0 4.60 =.60 49.0 0.0 99.90 D Sw 2.06 . 659 9.e4 999.01 999.01 0 101 16, 999.0 11.e0 . 70 54.0 0.0 99.90 D NNE 5.10 =.769 12.22 999.01 999.01 0 151 ~91 '999.0 ~~9.30 . 30 41.0 0.0 99.90 E
~
NNE 4.16 . 329 5.00 999.01 999.01 'O
' ' ~ ~ ' - -
D 201 39 999.0 6.60 =.30 54.0 0.0 99.90 E NE 2.95 =.329 12.22 999.01 999.01 0 251 204 999.0 16.00 =1.00 59.0 0.0 99.9u ~ D 85m 7.15 =1.098 15.00 999.01 999.01 -00 301 318? 999.~ 0^8.8 0 .G 90-~~ 35. 0 0.0 99.90 D
- ~~
Na ~ ~ 3.9 3 - - . 988 ~ 1.67 999.01- ~999.01 9 351 224 999.0 4.00 =.80 38.0 0.0 99.90 0 Sn 1,79 =.878 3.33 999.01 999.01 0
#01 163 999.0 14.10 =.20 .53.0 0.0 99.90 E SSE 6.30 . 220 11.67 999.01 999.01 0 451 '289 999.0 ~10.10 . 40 36.0 0.0 99.90 E hNw 4.51 =.439 2.22 999.01 999.01 0'
-~~
. 501 189 999.0 13.50 =.60 49.0 0.0 99.90 D 3 6.03 . 659 9.e4 999.01 999.01 0 551 105, 999.0 4.60 =.40 39.0 0.0 .99.90 D E8E 3.84 =.878 3.89 999.u1 999.01 0 601 ~9 5.--~ 9 9 9. 0-' 10. 3 0- 6 7 0 -~~~4 4. 0 0. 0 99.90 0~~
E 4.60~ =.769 6.67 '999.01'~ 999.01 ~ ~~ 0 ' h) 651 311. 999.0 3.40 =.60 22.2 0.0 99.90 D Na 1.52 . 659 =5.56 999.01 999.F1 0 701 347 19.8 2.90 5.30 24.0 0.0 99.90 G 8 NNw 1.30 5.619 -e.4e 999.01 999.01 0 KONTH 12 1 42 999.0 4.80 =.60 33.0 0.0 99.90 0 NE- 2.15 =.659 56 999.01 999.01 0 51' 232. ~999.0 ~9.00 =.20' 38.0 0.0 99.90 E S* 4.02 =.22o 3.33 999.01 999.01 0 ~~~---"-- p 101 319 999.0 6.30 20 26.0 v.o 99.90 E Na 2,82 220 =3.33 999.01 999.u1 0 l 151 325 999.o te.uo .70 27 o 0.0 99.9u D Nn 6.26 a.769 =2.78 999.01 999.ut 0 201 161 999.0 13.7u =.60 35.0 0.0 99.90 0 bSE 6.12 . 878 1,67 999.u1 999.01 0 251 297 999.0 14.90 =1.10 e.0 0.0 99.90 o mNa 6.66 =1.20e =15.56 999.01 999.01 0 301 22 999.0 7.20 =1.00 12.o 0.0 99.90 0 NNE 3.22 =1.096 =11.11 999.01 999.01 0
--~ ' 3 51 340 999.0 9.40 =.80 35.0 0.u 99.90 D NNa 4.20 . 876 1.67 999.01 999.01 0~-
~ ~ ~ ~ ~
y Oct 313. 999.0 7.eu .30 33.u u,0 99.90 E Nw 3.31 =.329 .56 999.91 999.01 0 651 23 999.0 12.6u =.70 32.0 u.o 99.99 0 NNE 5.63 =.769 0.00 999.01 vv9.ut u 501 130 999.0 23.80 =.20 46.o 0.0 99.90 E SE 80.6e . 22u 7.7e 999.01 999.01 0 g 551 217 999.0 10.60 =.50 41.0 0.0 99.9u o Sn e.74 .Sov 5.00 995.u! 999.01 0
L SMICOM (AT>OSPMENIC Ot3 PENSION FON 094 EVALUATIONS) - vt.hnEE ATOMIC ELECTRIC Cu tmuu u3. 07/2s/70) 11/2e/73 vaut e my 1977 12 *0NTHe = GNUUND* LEVEL "EL Ea3E - w triable 5 MEPLACEO - EXCLUSION AREA
)' LIST OF MouRLY METEUNOLOGICat oafa
~
HOUffY WIND ~D1 HEC ' HIND ~ TEMP ~~~ AIM MATER 80LaN D. TEM 81G.TH m1ND SPEED DELTA T alN T wai.8UNF SOLAR 4 StaBRZ D SEG. DIR. NaNGE SPEED DIFF TEM 8. TEM Na0 CLASS Cla58 FNOM (M/5EC) (m/100M) (C) TEMP (C) (LT/Mih) IF GT.0
~~ ~ C01 333. 999.0 6.50 =.50 35.0 0.0 99.90 D NNm 2.91 a.S49 1.67 999.01 999.01 0
~
). C51 350 999.0 5.40 1.ko 12.0 0.0 99.90 E N 2.41 1.318 -11.11 999.01 999.01 0 701 See. 999.0 1,70 3.10 14.0 9.0 99.90 F _ n8m 76 3.404 *10.00 999.w1 999.01 0 D
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SnIRON (ATMOS?MERIC UISTENSIUN FOR Osa EVALUATIONS) - vaNMtE A10 MIL ELECTRIC Cu (mou o3. 07/2=/183 11/24/70 PAGE 10
)
_ , MY 1977 Id MO'sTMS = GWOUND=LEVLL MELLASE - VARIABLES HEPLACED = EXCLUSION ANEA ._.
)~ HORIZONTAL PLUME STANUAkD DEVIATIONS SIGMA (Y) = (METERS)
~
0.SECTUN STABILITY-A ~STABILITT H STABILITY C STAu!LITY D STA81LITT E STA61LITY F 3TABILITY G
~
)
~
N 1.339E+02 9.625E+01 7.363E+01 e.716E+01 3.398E+01 2.355L+01 1.7u1L+ot NNE 1. 3 3 R
- 02 9.625E+01 7.363E+01 4.716Et01 3.398E+01 2.355E+01 ~ 1.701E+01
~
) NE 1.339E+02 9.625E+ut 7.363E+01 4.716E+ot 3.198E+01 2.355E+ot 1.701E+01 SAE _1.339E+02___ 9,625E*01_ 7,363E+ut _4,716E+01 3.398E+01 2,355E+01 1.701E+01 E 1.339E*02 9.625E+ut 7.363t+01 4.716E+01 3.396E+01 2.355E+01 1_. 7 u l t + 01
) ESE 1.339E+02 9.625E+ul 7.363E+01 4.716t*01 3.398E+ut 2.355E+01 1.T01E+01 SE 1,339E+02 9,e25F+01 7.363E+01 4.716E+01 3.396E+01 2.355E+01 1.701E+01 SSE 1.339E+02 9.625E+ut 7.363t+01 4.716E+01 3.398E+ot 2.355E+01 1.701E+01
~~~ ~
) 3 1.339E+02 9.625E+01 7.363E+01 4.716E+01 3.398E+ot 2.355E+01 1.701E+0!
884_ 1,339E+02_ _ __9.625E+ut 7.363E+01 4,716E+01 1.398E+01 2.355E+01 1.701E+01 Sw 1.339E+02 9.625E*01 7.363E+01 9.716E*01 J.390E+01 2.355E+01 1.701E+01
) wSa 1.330E+02 9.625E+01 7.363E+01 4.716E+01 3.398t+01 2.355E+01 1.701t+01 ~
w 1.339t+02 9.625E+01 7,363E+01 4.716E+01 3.398E+01 2.355E*01 1.701E+01 WNw 1.339E+02 9.625E+01 7.36 3t
- 01 e.716E+01 3.398t+01 2.355E+01 1.701t+01
~
Nm 1.339E+02 9.625E+01 7.363t+01 4.716E+01 3.398E*ut 2.255E+ot 1.701t+01 NNw 1,3 3_9 E + 0 2 9,625Et01 7,363E+01 _ 4,716E+01 __ 3,398E+01__ 2.355C+01 1,701E+01 __ h _ _ , _ _ VENTICAL PLUME STANDARD DEVIATIONS SIGMA (Z) = (mETLRS) i D.8ECTUR STABILITY A STABILI1Y s STABILITY C STABILITY D STABILITY E STABILITY F STABILITY s
~
N 1.674E+02 6.566E+01-~
'~
~~e.161E+01~ '2.192E+01 ~ ~1.573E+01- '9.535E+00
~
5.899t+00 ~
) NNE 1.67eE+02 6.566E*01 4.161E+01 2.192E+01 1.573E+01 9.535E+00 5.899t+00 - ~ ~ ~
NE 1.67eE+02 6.566E+01 4.161E+01 2.192E+01 1.573t+01 9.535E+00 5.899E+00
~ ENE ' 1.67eE+02 6.566E+01 4.161t+01 2.192E+01 1.573E+ot 9.535E+00 5.899t+00
-~ ~ ~ ~ ~
) E 1.67eE+02 6.566E+01 e.161E*01 2.192E+01 1.573E+01 9.535E+00 5.899E+00 . j- E8E 1.674E+02 6,56*E+01 - ~~-4.1411+01 2.192E+01 1.573E+01 5.899E+00 SE 1.674E+U2 6.566E+01 4.161E+01- ~2.192E+01 9.535E+00 ~ ~ ~ ~ '5.899E+00 -
~1.573E+01~ ~ ' 9.535E+00 8SE 1.674E+02 6.566E+01 4.161E+01 2.192E+01 1.573E+01 8
9.535E+00 5.899E+00
- - ~ ~ ' '
1.674E+02 6.566Ft01 4.161E+ut 2.192E+01 1.573E+01 9.535E+00 5.899E+00
~SSW ^ ~ 1.674E+02 6.566t+01 4.161t*01 2.192E+01 1.573E*01 9.535E+00 5.899E+00
~~
Sn 1.674E+02 6.566E+ul 4.161E+01 2.192E+01 1.573E+01 9.535E+00 5.899t+00 wSW 1,474E+02 6.566E*01 4.161E+01 2.192E+01 1.573E+01 9.535E+00 5.899t+00 h 1.674E+02 6.566E+01 4.161E+01 wNw 2.19 2 E + 01--~~~ 1. 5 7 3 E + 01" '9.535E+00 - 5.899t+C0 1.674E+02 6.56*E+01 4.161E+01 2.192E*01 1.573E+01 9.535E+00 5.899E+00 Nw 1.67eE+02 6.966E+01 e.161E+01 2.192E+01 1.573E+01 9.535E+00 5.899E+00
~~N W 1;674E+02 ~ ~~6.566Ee01 4.161E*01 2.192E+01 1.573E+01 9.535E+00 5.899E+00
, m me, a om.a e-m m
--- - = - , - a v
- a ,
ween,. m- -m m mam -'-m-o -mmm- ,e m
-_ --_----i-,,__------_-_--_-_---___------_---
O SK! CON (ATMO3PMENIC DISPENSION FOR DBA EVcLUATIONS) - YANMEE ATOMIC ELEC1 HIC CU (MOD 03, 07/24/Foi 11/24/78 PAGE 11 C)- Mt 1977 12 MONTH 8 - GHOUND=LEVtl MELE A3E = VANJABLES MEPLACEO = LXCLUSION AREA
.~~ . ._
[] SECTOH= AVERAGE FINITt CLOUD INTEGRALS It AND 12 FOR GAMMA CHI /W COMPUTATION = 3 AMPLE NESULTS
~ ~ ~
DISTANCE FHDM WELEASL POINT (METEMS) a 610.00
~ ~ ~ ~
[] GAMMA ENENGY( MEv) a 50
" GAMMA LINEAR ATTENUAT!uN COEFFICItNT FUR AIR (t/M) a .U1120 GAMMA LINEAN ENEHGY A850HPitON CUEFFICIENT FOR AIR (1/M) a 00382 '~~
() BUILDUP FACTUN e 1.929 HEIGHT (M)~~~87ASILITY~A ~ ~ ~81A81LITY 8 GTA81LITY C STABIL11Y 0 STABILITY E~ STABILITY F STABILITY G ~~~ O
=ITH 80!LDING hAME
[) 11 0.00 3.497E=01 7.294E=Ut 9.629E=01 1.273E+00 1.395E*00 1.67tE+00 2.050E+00 12 3,ll,2E 2 01_ 5,283E=01 6.167E=01 6.999E=01 7.248E=0! 7.692E=01 8.107E=01
) w!THOUT BUILDING HAKE
'~~ 11 0.00 3.515t=01 7.486F=01 1.016E*00 1.457E*00 1.708E+00 2.107E+00 2.5u5E+00
~ ~ ~ ~
) 12 3.125 tact 5.360F=01 6.334E=0! 7.362E=01 7.742E=01 8.155E=01 8.413E=01 It 3,41 3.5tcE=01 7.477t=01 1.014E+00~ 1.446E+00 1.686E*00 2.34tt+00 12 3.124E=01 ~2.U43E+00
~5.363E=01 6.326E=01 7.342E=01 7.713E=01 8.103E=01 8.327E=01
[] Il 11.G3 3.508E=01 7.e05E=01 9.927E=01 1.362E*00 1.522E+00 1.643E+00 12 3.120E=01 1.582E+00
~~ 5.332r=ut 6.2a2E=01 7.19tE=01 7.490E=01 7.735E=0 7.803t=ut 11 22.86 3.486E=01 7.169E=01 9.260E=01 1.126E*00 1.126E+00 1.016E+00 9.418E=01
~ ~ ~ ~ ~ ~
[) 12 3.104E=01 5.230E=01 6.055E=01 6.733E=01 6.866E=01 6.895E=01 6.874E=01 Il 38t: 0 3.435E=01 6,642E=01 7.889E=01 7.673E=01 6.859E=01 6.139E=01 5.947E=01 Id 3.067E=01 4.998E=01'
~
5.607E=01 5.888E=01 ~5.867E=01 5.815E=01~ '~ 5.794E=01
~ ' ~ ~
SD 11 57.14 3.338E=ol 5.735E=ut 5.882E=ut 4.'3 3 0 E = 01 4.065t=01 3.83ut=01 3.759E=01 12 2.995E=Ut 4.5b4E=Ut 4.810E=01 4.877t=01 4.746E=01 4.69ME=01 4.681E=01
~ ~ ~ !! 80.00 '3.176E=dt 4.483E=01 3.760E=01 2.634E=01 2.465E=01 2.37tE=01 2.340E=01
' ~ ~ ^
() 12 2.876E=01 3.97tE*ut 3.944E=01 3.728E=01 3.672E=0t 3.637E=01 3.624E=01 Il 106,67 2,936E=ot 3.093F=V1 2.127E=01 1.553E*01 1.482E=01 1.439E=01 1.424E=01 Id 2.698E=01~ 3.210e=01 ~~ ~2.977E=01' " 2.764E=01 2.724E=01~' ^2.698E=01 2.688E=01' C) 11 137.14 2.6ttE=01 1.865E=Ut 1.150E=01 9.062E=02 8.729E=02 8.518E=02 8.444E=02
~ ~ ~ 12 2.452E=01 2.400E=01 2.12SE=01 1.965E=01 1.936E=01 1.918E=01 1.911E=01 In 171.43 ~ 2.211E=01 1.002E=01 6.235E=02 5.168E=02 5.005E=02 4.901E=u2 4.864E=02 O 12 2.144E=01 1.683E=01 1.448E=Ut 1.338E=01 1.319E=01 1.306E=01 11 209.52 1.3u2E=01 1.762E=01 5.034t=02 3.363E=02 2.867E=02 2,786E=02 2.734E=02 2.716E=02 32 1;786E=01 1.109E=01 9.448E=02 ~~~8.736E=02 "
' 8. 6 0 9 E = 0 2 -^"" 8. 5 2 5 E = 0 2 ~-~ ~ ^ ' 8. 4 9 5 E = 0 2 Ep Il 251.43 1.306E=01 2.4e8E=u2 1.779E=02 1.542E=02 1.505t=02 1.477E=02 1.468E=v2 12 1.405E=01 6.949E=u2 5.999E=02 5.463E=02 5.384t=02 5.331E=02 5.313E=02
~It 297.14 8,885E=02 1.226E=02 9.158E=03 8.032E=03 7.842E=03 7.717E=03 7.673E=03
' '~ ~~~
q) 12 1.036E=01 4.164E=02 3.54tE=92 3. 2 74 E =02 3.227E=02 3.195E=02 3.184E=02 11 346.67 5.485E=02 5.958E=c3 ~ 4.57tE=03 4.044E=03 3.953E=03 3.894E=03 3.873E=03 12 7.105E=02 2.39tE=02 2. 0 34E =0 2 ' ~~ ~ ~ 1. 8 8 0 E=0 2 ~~~~1.853E=02' ~"~~1.835E=02 ~~'t.828E=02 CD 11 400.00 3.042E=02 2.82TE=U3 2.200E=03 1.966E=03 1.924t=U3 1.897E=03 1.887E=ut 12 4.510E=02 1.316E=02 1.119E=02 1.035E=02 1.020E=02 1.010E=02 1.006E=u2 _ _ _ _ _ NOTE = GAMMA CHI /O ALMAYS BA8ED ON SECTON AVENAGE MODEL , U
~~~
O
O . SK1kUN (ATM03PHEkiC ut3PtN3 ION FUW Den Ev&LUATIUNS) = Y&NMEE aiUMIC ELECTHIC CU (MOu v3. u?/24/78) 11/24/76 PAGE 12 $. My 1977 12 MONiHs = GkuuhD-LEVtt MELEASF
= v&W146Lt3 NEPLACEO = LXCLUSION ANEA DELTA =T STAuILITY MODEL _
[] ~ DISPERSION MOURLY PLUME EF.ME1GHT ENTkAIN. VENTICAL MLANDER PLUME C.L. SEC10R AVEN. GAMMA DOWNh!ND TYPE 8gQ,___ N13(_(M), __ (METtRS) COEF. .BLD,MAKE FAClOR CHI /W. (3/M3) CMI/G (S/M3) CHI /G (3/M3) SECTOR D MO%7M i
) NORM GRND 1 0.00 0.00 1.000 1.518 2.441 9.9291E=05 5.6772E=05 2.0465E=US SE CORM _GRND 51 _ 0,00 _ 0.00 1.000 1,732 6,U00 3.5841t=04 2.2101E=04 4.4134E=05 NORM GHND 101 _ SSE 0.00 0.00 1.000 1.732 3.971 1.7749E=04 1.0027E=04 2.6245t=05 5 ) NORM GRND 151 0.00 0.00 1.000 1.293 1.134 4.5556E=u5 2.39tuE=u5 9.6052E=06 MSN NORM GRND 201 0.00 0.00 1,0Pu 1,518 3.000 1.1106E=ue 7.8062E=05 2.8140E=05 SE
__ _ t0RM GRND 251 0.00 0.00 1.000 1.293 1.000 3.037tE=05 1.5940E=05 6.4055E=06 ENE [) (URM GRND 301 0.00 0.00 1.000 1.293 1.161 4.7275E=05 2.4812E=05 9.9708E=06 SE NORM _GRND 351_ _0.00_ 0.00 1.000 1.293 _ 1.865 7.3884E=05 ,5,2602E=05 2,113eE=05 SSE NORM GRND 401 0.00 0.00 1.000 1.51e 1.525 8.9177E=U5 3.5483E=05 NORM GRND 451 1.279tt=05 SE CD 0.00 0.00 1.000 1.732 4.000 4.1733E=ce 2.3749E=04 6.6896E=05 NE NORM GNND 0.00 0.00 1.000 1.518 1.254 7.3342E=05 2.9182E=05 1.0520E=05 SSE " - - -
-~~ ~ ' N O R M GRND 551 ~ 501 0.00 0.00 1.000 1.732 4.000 3.9647E=os 2.256tE=04 6.3551E=05 SSE
() RORM GRND 601 0.00 0.00 1.000 1.51s 2.097 9.9291E=05 4.8789E=05 1.7587E=05 ESE NORM GRND 651 0.00 3.00 1,000 1.5te 1.657~ 9.6883E=05 3.8549E=05 1.3696E=05 ENE NORMGRND 701 0.00 0.00 1.000 1.516 1.790 9.929tE=05 ~~ 4.1633E=05 1.5008f=05 ENE O MONTM 2
-~^ NORM QRND' 1 0.00 0.00 1.000 1.293 1.444 6.3615E=05 3.5068E=05 1.4092E=05 N E - ~~ - ~ ~ ~ -
C) NORM GRND 51 0.00 0.00 1.000 1.518 3.000 1.4808t=ue 1.0408E=04 3.7520E=05 ENE LORM GRND 101 0.00 0.00 1.000 6.000 4,0784E=04 2.5149E=04 5.0222E=05 3SE
- ~'~ NORM GRND 151 0.00-- '0.00~~ ~1.000 ~~ 1.7321.518 -' 2.165 ~ 9.929tE=u5 - 5.0363E=05 1. 8155E = o S "- - ~ E S E
() NORM GRNO 201 0.00 0.00 1.000 1.732 4.000 4.1733E=oe 2.3749E=04 6.6896E=05 3 NORM GRND 251 0.00 0.00 1.000 1.293 1.154 4.6833E=05 2.458uE=05 9.8776E=06 N NORM QRND' ~ 301 0.00 0E00 1.000 1.293 1.073 4.1760E=05 2.19 tee =05 8.8075t=06 MNn
- - " ~
C) NORM GRND 351 0.00 0.00 1.000 1.293 1.698 6.9946E=u5 4.5347E=05 1.8222E=05 SSE NORM GRND 401 0.00 0.00 1.000 1.115 2.3275E=05 9.3531E=06 SE NORd GRND 451' O .~0 0 0.'00 1.000 ~~- 1.516 1.293 ~ "-- 3.000 ~~'1.3883E=04 ~4.4347E=05 9.7576E=05
-- --- 3.5175E =05 ~~~~ E
() NORM GRND 501 0.00 0 00 1.000 1.518 1 000 5.6054E=05 2.2303E=05 8.0399E=06 E3E NORM GRRD 551 0.00 0.00 1.000 1.293 1.420 6.3000E=05 3.4157E=05 1.3726E=05 MSM
- ~~ NORM GRND 601 ~ ' O.00 0.00 1.000 1.518 3.000 1.0331E=04 7.2616E=05 2.6176E=u5 NE - - - ~ ~ ~ ~
() LORN GRND 451 0.00 0.00 1,000 1.732 3.477 1.8245E=os 9.0245E=05 2.5421E=05 SSE () NORM GRND 1 0.00 0.00 1.000 1.518 3.000 1.4331E=04 1.0073E=04 3.6309E=05 E NORM GRND 51 0.00 0.00 1.000 1.518 6.6436E=05 101--- ~ 2.856 9.9291E=05 - 2.3949E=05 NE NORM GRND' 0. 0 0- ~ ~ 0.00 1.000 1.518 1.491 8.7195E=05 '3.4694E=05 1.2507E=05 SM Cp NORM GRND 151 0.00 0.00 1.000 1.732 4.000 5.2862E=04 3.0082E=04 NORM GRND 8.4735E=05 8E 201 0.00 0.00 1.000 1,518 2.215 9.9291E=05 5.2923E=05 1.9078E=05 NNE ADRK GRND 251 "0.00 0 ;0 0 ---~~ 1. 0 0 0 1. 2 9 3 --~ ~-~ 2. 0 0 0 7.8276E=05 - 5s9775E=05--- ~ 2.4021E=uS ~ SM () NORM GRNO 301 0.00 0.00 1.000 1.518 3.000 1.0097E=04 7.0966E=05 2.5582E=05 M NORM GHND 351 u.00 0.00 1.000 1.293 1.315 5.760ut=05 3.0231E=05 1.2148E=05 5 EORM GRND ~ 401 0.00 0.00 1.000 1.293 1.000 2.0371E=05 1.0691E=05 4.2964E=06 ESE~~~~ C) NORM GRND 451 0.00 0.00 1.000 1.518 1.000 5.3024E-05 2.109eE=05 7.6053E=u6 SE NORM GRND 501 0.00 0.00 1.000 1.732 4.000 1.5560E=04 4.3829E=US NORM GRND 551 0.00-~~ -~~ 0.00 - 2.7343E=04 NNE 1.000 1.518 ~1.278 7.4739E=05' 2.9736E=05 1.0720E=05 ~ -~~~'s! NORM GHND 601 0.00 0.00 1.000 1.518 1.025 5.9905E=05 2.3636E=05 NORM GNND 651 8.5923E=06 SSE 0.00 0.00 1.000 1.732 6.000 5.376tE=04 3.315tE=04 6.6201E=u5 SSM
-~~" NIR M GRND 701 0.00 0.00 1.000 1.518 3.000 1.5319E=04
~~ ---
1.0767E=04 3.8813t=05 SSM M
~
321 HUN LATMDSPMERIC 015PEH81uN Fu3 D:A EVALUATIONS) - YAN3EE ATOMIC LLEC1 HIC Cu (MOD v3. 07/2e/78) 11/24/78 PAGE 13 0 - MY 1977 12 PO2TN3 = GHOuhD-LEvtl kELEast = vaMlagtE3 NEPLACED = EXCLUS10N area otLia=T braBILITY MODEL OISPERSION NuuRLY PLUME EF.NEIGHI EN7NAIN. VERTICAL NEaNDER PLUME C.L. SECTUR AVEM. GanNa DuaNNIND l4D ' 8EG, RISE (M) tmE7tRS) TYPE COEF. BLDea4KE FACTOR CNI/W (8/M3) CNI/O (3/M3) CNI/u (5/M3) SECTOR I O
~~ MONTH 4 ~ ' - - - - -
'() RORM GRND 1 0.00 0.00 1.000 1.518 1.033 6.0366E=05 2.4019E=05 5.65 bee =96 SE CORM GRND 51 0.00 0.00 1.000 1.293 3.2540E=u5 1.7079E=05
-~~ 1.000 - ~6.8630E*c6 NW
'0.00 NORd CRND 101' O.00 1.000 1.293 1.0a6' 4.0089E=05 '2.1041E=05 8.4552E=06 ~~wNw
() t0RN GRND 151 0.00 0.00 1.000 1.293 1.127 a.5146t=05 2.3695E=05 9.5216t=06 ENE RORM GRND 201 0.00 0.00 1.000 1.293 1.000 2.9478E=05 1.5471E=05 6.2171E=06 SE ' - ~ ~ ~ - NORM GRND 251 0.00 0.00 1.000 1.293 1.348 5.9657E=05 3.131tE=05 1.2562E=05 N f() NORM GRND 301 0.00 0.00 1.000 1.518 1.000 4.4588t=05 1.7741E=05 6.3954E=U6 N 00RM GRND 151 0.00 0.00 1.000 1.293 1.000 2.2272E=05 1.1689E=05 NORM CRND Got 4.6973t=06 SE 0.00 0.00 1.000 1.518 1.157 6.7651E=05- 2.6918E=o5 9.7033E=06 NNm-~ () NORM GRND 451 0.00 0.00 1.000 1.293 1.841 7.3346E=05 5.1571E=05 2.0724t=05 Nn NOEM GRND 501 0.00 0.00 1.000 1.51e 1.413 8.2606E=o5 3.286eE=05 1.18eBE=05 NNE
-~ NORM GRND ~ ~ 551 0.00 0.00 1.000 1.293 2.000 7.8276E=05 5.9775E=05 2.4021L 05 m3a
() 20RM GRND 601 0.00 0.00 1.000 1.518 3.000 1.e331E=04 1.0073E=04 3.6309E=05 SSE t0RM GRND 451 0,00 0.00 1.000~ - - - 1,518 2.03e e.7310E=05 1,7054E*n9 hORMGRND 701
~9.9291E=05 NNW 0 . 0 0- ~ ~~~ ~ 0 .~ 0 0 ' 1.000 1.732 ~~~0.00u 3.4475E=un'~~ 1.9619E=04 5.5262E=05 'E CONTH 5 ~'
RORM GRND 1' O.00 0.00 1.000 1.732 8.4481E=ca 5.2094E=04
~~
6.000 1.0403E=04 SSW toRM GRND 51 0.00 0.00 1.000 1.51e 2.983 9.9291E=05 6.9388E=05 2.5013E=05 S NORM GRND 101 0.00 0.00 1.000 1.732 6.000 3.9825L=04 2.a311E=04 e.oS48E=05 85= NORM GRND 151 0.~ 0 0 0.00~" 1.000 ~ 1,293 't.939 ~7.5591E=05 ~5.5960E=05 2.2487E=05 ESE
- 3) NORM GRND 201 0.00 0.00 1.000 1.293 1.121 4.4743E=05 2.3483E=05 9.e366E=06 SN NORM GRND 0.00 0.00 1.000 1.293 1.000 2.8312t=05 1.4659E=o5 5.9712L=06 SSE
'- NORM GRND '- 251 301 0.00 0.00 1.000 1.293 1.000 2.4686E=05 1.2956E=05 5.2004E=06 SE ~ ~ ~ ~ - ' -
j) NORM GRND 351 0.00 0.00 1.000 1.293 1.000 3.3859t=05 1.7771E=05 7.1412t=06 N NORM GRND 401 0.00 0.00 1.000 1.000 3.3408E=05 1.7534E=05
- 1.293 7.ueo0E=06 E8E NORM ~ERND 451 0.00 0 . 0 0 ~- ' t.000 - 1.293 - 1.536 ~ ~ 6.5958E=05 '-- 3.8678E=05 - ' t .5543E=05 " N
- 3) NORM GRND 501 0.00 0.00 1.000 1.515 3.000 1.if91E=04 8.0064E=05 2.do61E=05 NNw
~
NORM GWND 551 0.00 0.00 1.000 1.51e 1.691 9.9291E=05 4.3979E=05 1.5853E=05 NNE NORM GRND 601' O.00 0.00 1.000 1.293 1.000 3.0188E=05 1.5844E=05 6.3669E=06 3SE '- 39 NORM GRND 651 0.00 0.00 1.000 1.732 6.000 5.376tE=04 3.3151E=04 6.62u1E=05 S NORM GRND 701 0.00 0.00 1.000 1.732 6.000 6.9573E=0e 4.2901E=os 6.5672E=05 NE 1p EONTH 6 NORM GWND 1 0.00 0.00 1.000 1.518 2.739 9.9291E=05 6.3724E=05 2.2971E=05 N NORN GRND 51 0.00 0.00 1.000 1.518 3.000 2.tl55E=ce 1.4869E=04 5.3599E=05 S3E 89 NONM GRND 101 0.00 0.00 1.000 1.732 '6.2249E=o4 3.8385E=04 NORM GNND 6.u00 7.6654E*05 wN= 151 0.00 0.00 1.000 1.293 1.841 7.33e6E=05 5.1571E=05 2.u724E=u5 Sa NORM GRND~ ~201 0.00 0.00 1.000 1.293 1.717 7.0396E=05 4.6142E=05 1.d542E=05 N
~'~~~~
b9 NORM GRNO 251 0.00 0 00 1.c00 1.293 1.025 3.6846E=o5 2.03eeE=os 6.193uE=06 8 NOWm GRND 3u1 0.00 0.00 1.000 1.516 2.397 9.Y291t=05 5.5759E=05 2.ulu0E=05 N NORM GRND 351 0.0u 0.00 1.uou 1.089 1.000 1.4Fe5E=o$ 1.1663E=u5 6.1513t=0N SE bg NORM GRND 401 0.00 0.00 1.000 9.515 e.7195E=05 3.4694E=u5 NOMM GWNU 1.491 1.2507E=o5 NNh 451 0.00 U.00 1.000 1.293 1.993 7.68tetav5 5.eee7E=05 2.3467E=05 NNw
- - - - NORM GRND 501 0.00 0.00 1.000 1.293 2.000 1.7221E=ue 1.3151E=04 5.2845E=05 NNn
'~ ~ ~ ~
9 NONM GNND 551 0.00 0.00 1.000 1.293 1.865 7.366eE=o5 5.2602E=05 2.1138t=u5 NNE NOWm GNND 6ut u.uv o.00 1.000 1.51e 1.220 7.13ett=u5 2.83B6E=u5 1.0233E=05 NNm NURM GRND 651 0.00 0 00 1.000 1.732 4.sv52E=ue 2.506eE=0e 4.000 7.u613E=v5 SSE v W L - - - -_- - v . . , _ - - - - - - - _ - , . _ _ _ - - _ _ _ _ - - - - - _ . _ _ _ _ _ _ _ _ - _ _ _ _ _ - - - - _ _ . - _ . - - - - - _ _
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3 . SMICUN (ATMUSPMERIC u! SPEN 310N F03 084 EVALUATION 3) = YamnEE ATOMIC ELECTWIC CO tmou u3 v7/24/76)
) '
wY 1977 12 =0NTMs - GRuuND=LEWEL NELEASE = VARIA6LES NEPLaCED = EXCLUSION AhEA 11/ds/70 PAGE DELIA-T STABILITY MODEL 15 [) ' DISPERSION MOUNLY SEG, PLUME RISE (M) EF.NEIGMT EMTNaIN. VENTICAL MEANDER PLUME C.L. SECTOR AVEN. GAMMA 00mhmIND TYPE (METERS) CotF. SLD. MARE FAC10R CHI /W (3/M3) CHI /G (5/M3) CMI/O (5/M3) SECTOR D tuRM GRND 651 0.00 0.00 1.000 1.732 4.000 3.3039E=04 1.8801E=os 5.2959E=05 NE
--- h0RM GNhD 701 0.00 0.00 1.000 1.732 4.000 3.9647E=04 2.2561E=04 6.3551E=05 SE'~~~
3 MONTM to NORMCRND 1 0.00 0.00 1.000 1.518 3.000" l'.0577E=04' 7.4345E=05- 2.6800E=05 Nu
@) NORM GRhD 51 0.00 0.00 1.000 1.293 1.420 6.3000E=05 3.4157E=05 1.3726E=05 8 NORM GRND ~ 101 0.00
~
0.00 1.000 1.732 4.000 1.9340E=ce 1.1006E=04 3.10u1E=05 ESE ~~~~~~-~ NORM CRND 151 0.00 0.00 1.000 1.732 3.567 1.8149E=04 9.2087E=05 2.5939E=05 83E
'}) h0RM GRND 201 0.00 0.00 1.000 1.293 1.011 3.7964E=05 1.9925E=05 8.0068E=v6 Nn DIS._ DATA 251 _ _ _ _ _ _ ._ ______ _ _ _ _ _ _ ._ .. __ _ _ _. . _._
'[) c18. DATA 351 EORM GRND 401 0.00 0.00 1.000 1.518 3.000 1.4808E=04 1.0008E=04 3.7520E=05 m8M
---' EO R M G R N D "- 451 ~ 0.00 '0400 1.000 1.518 2.237 9.9291E=05 5.2001E=05 1.8760E=05 SW ~~ ~ ~ - - -
]) NORM GRND 501 0.00 0.00 1.000 1.732 6.000 5.9137E=04 3.e466E=04 7.2821E=05 NE CORM GRND 551 0.00 0.00 1.000 ~~ '-~~1.732 4.000 1.5041E=04 4.23e8E=05 NORM GRhD 601 0.00 0;00--~~ 1.000 1. 7 3 2 - -- ~4. u 0 0 ~ 2,6431E=ue - 2.2561E=04 ~
3.9647E=04 6.3551E=05
- ~~88E W
[) CORM GRND 651 0.00 0.00 1.000 1.51e 3.000 1.4808E=04 1.0e08E=04 3.7520E=05 SSE NORM _GRND 701 0.00 0.00 1.000 1.732 3.477 1.8245E=04 9.0245E=05 2.5421E=05 5 Z) MOhTM 11 NORM GRND - 1 0.00 0.00 1.000 1.732 6.000 1.1827E=03 7.2932E=04 1.4564E=04 SSE NORM GRMD 51 0;00 0;00 1.000 1. 29 3 ~ ~--~ 1.965 ~ 7.6193E=05 --~ ~5;7176E=05 ~~ 2. 2 976E= 05 ht E) NORM GNNO 101 0.00 0.00 1.000 1.293 1.109 4.3958E=05 2.3071E=05 9.2711E=06 SSw NORM GRND 151 0.00 0.00 1.000 1.518 1.443 8.4382 Eses 3.3575E=05 1.2103E=05 33W NORM GRND ---~201 0.00 0.00 1.000 1.518 2.034 9.9291E=05 4.7310E=05 1.7054E=u5 - SM - - - - - - - - 9 NORM GRND 251 0.00 0.00 1.000 1.293 1.000 3.1320E=05 1.6438E=05 6.6056E=06 hNE h0RM GRND 301 0.00 0.00 1.000 1.293 1.305 5.6945E=05 2.9888E=05 1.2010E=05 SE 40RM URh'D 151 D .~0 0 0 6 0 0 -~~ ~ 1. 0 0 0 ---~ 1. 2 9 3 -~~ - 2. 0 0 0 - ~ ~~ 8. 610 3 E= 0 5 6.5753E=05 2.6423E=05 Nt E) NORM GRND 401 0.00 0.00 1.000 1.518 1.000 5.5656E=o5 2.2145E=05 7.9829E=ce NNp NORM GRND 451 0.00 0.00 1.000 1.516 1.329 7.7699E=05 3.0916E=05 1.11eet=05 ESE
~~~ NORM GRND O.00~~
501 ~~' O.00 1.000 1.293 1.000 3.7120E=05 1.9482E=05 7.8289E=06 N'- 9 h0RM GRND 551 0.00 0.00 1.000 1.293 1.324 5.8270E=05 3.0583E=o5 1.2290E=05 WNW MORM GRND 401 0.00 ' O.00 1.000 1.293 1.182 4.8652E=05 2.5535E=05 1.0261E=05 N NORK GRND 651 0;00 0. 0 0 - ~ 1. 0 0 r.
~
1.293~ -- 2.000 ~ ~ 1. 013 0E=0 4 - ~~ 7 4 7356E=05--~ 3.10 85E=05 3E b) NORM GRND 701 0.00 0.00 1.00u 1.732 6.000 4.0784E=ce 2.5149E=04 5.0222E=05 SSE
' EONTH 12 ~~
g NORM GWND 1 0.00 0.00 1.uou 1.293 1.913 7.500eE=95 5.4794E=05 2.2019E=05 Sw NORM GRND 51 0.00 0.00 1.000 1.515 1.491 8.7195t=05 '3.4694E=05 1.2507E=05 NE NORM GRND - ~~ 101' O.00 0.00 1.000 1.51e 2.131 9.9291E=05 4.9563E=05 1.7866E=05 SE g NORM GRND 151 0.00 0.0u 1.000 1.293 1.000 3.579at=o5 1.878et=U5 7.5493E=Un SE NORM GNMu 2u1 o.uo u.uo 1.000 1.293 1.000 3.e578E=o5 1.919BE=05 7.7146E=06 NNN NORM GRNO 251 0.00 0.00 1.00u 1.293 1.ono 3.3632E=05 1.7652E=05 7.u933E=06
~
ESE g NORM GHND 301 0.u0 0.00 1.000 1.293 1.eM1 6.4581E=05 3.6579E=05 1.4e79E=ub S3m NURM GRND 351 0.00 0.0u 1.0cv 1.293 1.252 5.3310E=u5 2.7980E=u5 1.124cE=u5 3SE-
~~ -- N O R M GRND 401 0.00 0.00 1.000 1.518 1.814 9.9291E=05 4.2196E=05 1.5211E=05- SE
' - ~ ~ ~ -
ep NORM GRNO e51 0.00 0.uu 1.000 1.293 1.vut 3.9771E=u5 2.0674E=05 B.3861E=06 SSa NURM GhND Sol o.00 0.00 ,1.600 1.515 1.000 3.2973E=v5 1.3120E=US 4.729eE=0e Nw NONM GRND $51 0.00 0.00 1.000 1.293 1.161 4.7275E=05 2.4812E=uS 9.9708t=U6 NE
.mmem. --
N4
. SMIKun (ATMOSPME21C DIhTEH510M FUp coa tvatuaTIO'48) = vahMEE AIUMIC ELECTRIC CO (e00 v3, 07/de/7n) tt/2e/76 PaGt 16 9:
MY 1977 12 MuMTH3 GRuuN0=LE%tt HELEa5E = vaw1 At9LES MEPL ACED = EXClustom aNEn DELTA =I STad!LITY MUDEL ._ . D18PEM810N MuuMLY PLUME EF.NEAGH1 ENTHAIN. VERTICAL MEAhDEM PLUML C.L. 3ECluW avEW, samMa punhminD si TYPE SE 0 e NISE_(M) (aETERU) COEF. BLD.nAKE FACTON CMI/G (3/m3) CMI/G (3/M3) CHI /W (3/M3) SECTOR (: ~ ~ ~ ' NO3M GMND 601 0.00 0.00 1.000 1.293 1.580- 6.7065E=05 a.0463E=05 1.62o0E=05 SSE ^-' ~ ~~ h0RM GnND 651 0.00 0.00 1.000 1.516 2.486 9.9291t=us 5.762eE-05 2.06*eE=05 8 NOMM G4hD 701 0.00 0.00 1.000 1.732 e 000 e.6643E=04 2.6543E.0a 7 e766t=05 EME (i 4. ti h t. l 4'
- . . . ~ . _ -- . .-- -
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, ., . , - , , -t,c-.- _.4 -, = .w - y ______,__m _ _ _ _ _ _ _ _ . m_____.__._-___. _ _ _ _ _ _ . _ _ _ _ _ _ _ _ _
O .
, setICON (ATMDSPnERIC U13 PEW 31tik FUM DM6 E w ALUA T a ura s) - YANAEE ATOMIL ELECTRIC CO (Huo u3, J7/de/i6) 11/2e/ib PAliE 17 O--
my 1977 12 MONTMS = GROUND =LEWE5 NELEa5E = VaWIAbLE5 NEPLACED = EzCLUSION aHEa DELTA =1 STABILITY MODEL O ATMosPMERIC DILUTION FACTUNS AVERAGED DvER EN11RE INTENVAL MANGE Q DuaN>IND DISTANCE V Ah.1 D GROUND = LEVEL CHI /G (SEC/M3) EkUUND= LEVEL CHIW/G (SEC/M3) GAMMA CHI /O (SEC/N3) SEC104 thETEWS) UMBERV. (PLUME CENIENLINE MODEL) (SECTud AVERAGE MODEL) (SECTON AVERAGE NUDEL) [) N 610.0 918 1.a276E=05 8.56 ale =u6 2.7287E=06 NNE 610.0 68e 1.0488E=05 6.1271E=06 1.95 78t =06 NE 610.0 418 ~ ~ ' ~ ~ 7.1251E=06
'~
~ ~ 4.3729E=o6 1.e031E=06~~
C) ENE 610.0 ea7 6.1213E=u6 3.6497E=v6 1.2215E=06
- - - ~ ~
E 610.0 395 7.7722E=06 4.6912E=06 1.4181E=06 ESE 610.0 691 1.0722E=u5 6.2282E=06 1.8741E=06
- ~ ~ ~ ' ~ ~
C) sE 610.0 1091 1.5068E=05 8.7386E=u6 2.5568E=06 88E 610.0 801 1.5586E=05 9.19e3E=ut
~ 79- 2.5717E=06 5 610.0
~~ ~
6 1.2948E=05 7.5961E=06 2.15 0 5E=%- ' C3 854 61o.0 501 1.0746E=05 6.5028E=u6 1.7732E=06
^
Sm 610.0 366 7.14=1E=06 4.aoe6E=06 1.2561E=06
~m8m 610.0 176 2.7758E=06 1.6856E=o6 5.2786E=07
- -~~
Q n 410.0 192 2.579eE=06 1.6156E=06 5.6258E=07 WNW 410.0 187 2.6a70E=06 1.7125E=06 Nw 610.0 '29e e.9357E=06 3.1787E=06
'~ 6.1431E=07 ~
() 1.0970E=06 NNw 610.0 650 9.6290E=06 5.9203E=06 2.0142E=06
~~~
mEIGHTED AVERAGE esto 1.0763E=05 6.3965E=o6 1.9399E=06 3
-e --N A > .h
~-'
, SX1kUN (ATMOSPMERIC OISPEGSIUM FOR Den EvcLUAT10NS) - VAN EE ATOMIC LLECTRIC Cu taou 93. u?/23/78) 11/ce/7M PAGE le P
MY 1977 12 MONTMS = GROUND = LEVEL NELEASE = VARIABLES NEPLACED = EXCLUSION AREA OELTA=T STABIL1TT M OD E t, DunNm!ND SECTOM N GNUUND= LEVEL CHI /u (SEC/M3) = PROBABILITY DISTNIBUTION3 C 0 @ETER8) e PLuMtL CENTERLINE VALUE5
-~ ~-
610.0 = 13MOUN AVERAGES r ~ ~ - -
~ ~ - ~
' FREQUENCY DISTRIBUTION RANGE NUMBER OF PERCENT OF COMULATIvt OBSERVATIONS TOTAL 085 PERCENT C
~ '~ ~
To LT.04.EQ. 1~ ~ ~ ~ ' - '~~
~ ~ '
F20M 1.0942E=05 1.2465E=05 109 109 F%0M FEOM 1.2465E=05 1.4201E=05 TO LT.UR.EW. TO LT.ON.EO. 1.42U1F=05 1.6177E=05 1 1 109 109 218 327 ( FIOM'- 1.6177E=05 'TO LT.OR.EQ. 1.8429E=05
~ - ~~
0 0.000 327 F r.0M 1,8429E=05 To LT.OR.EO. 2.0994E=05 2,0994E=05 70 LT.OR.EQ. 2.3917E=05 2 218 327 545 ( 3 871 FROM-2.3917E=05' 70'LT.0H.EG. FROM 2.7246E=05 6' 654 1.52*i FROM 2.7246E=05 TO LT.OR.EQ. 3.103BE=05 12 1.307 2.832 C - - ~ - FEDM 3.1038E=05 TO LT.UN.Ew. 3.5359E=05 22 2.397 5.229 FROM'~ 3.5359E=05 To LT.0R.EQ. 4.0280E=05
~~'~ ~
35 3.813 9.041 FLOM 4.0280E=05 TO LT.OR.EQ. 4.So67E=05 26 2.832 11.874 C FLOM 4,5887E=05-Tu LT,UR.EQ, 5.2275E=05 - ~ ~~ - 42 ~ 4.575 ~ 16.449 FROM 5.2275E=05 Tu'LT.04.EQ. 5.9551E=05 '41 4.466' 20.915 FROM 5.9551E=05 TO LT.OR.EQ. 6.7841E=05 112 12.200 33.115 C FROM 6.7841E=05 TU LT.OR.Eu. 7.7204E=o5 125 13.617 46.732 8.8041E=05 FRON ~ 7.7284E=05 TO LT.04.EQ. 33 3.595 50.327 FEDM 8.8041E=05 To LT.04.EQ. 1.0030E=04 193 21.024 71.351 C FCOM 1,0030E=04 To LT.OR.EQ. 1.1426E=04 ~ 37 4.031 75.381 1.1426E=04- 70 LT.0R.Eu. 1.3016E=ue
- ~ ' -
FROM ^~ ~~ 26 ~-- 2.832 ~- -- ~ ' - ~~ 78.214 ~~ ~~ FEUM 1.3016E=04 TO LT.04.EQ. 1.4828E=04 25 2.723 80.937 C FROM - 1.4828E=04 fu LT.0W.Eu. 1.6892E=04 9 980 81.917 FIOM 1.9243E=04 1.6892E=04 TO LT.OR.EC. 22 2.397 84.314 FROM 1.9243E=04 Tu LT.UN.EQ. 2.1922E=04 27 2.941 87.255 C FROM 2,1922E=04
~ '
TO LT.OR.EQ u .4973E=04 2 22 - ~ ' ' - - --2.397 89.651 FROM 2 4973E=04 TD ET.OR.EO. 2. 8 45 0 E = 0 4- -~'8 871 - - 9 0 . 5 2 3 ------~~~ - FKOM 2.8450E=04 TU LT.04.Eu. 3.2410E=04 11 1.198 91.721 ( FNOM 3.2410E=04 TO LT.OR.EW. 3.6421E=04 9 980 92.702 - -~ FROM 3.6921E=04 ~TO LT.OR.EQ. 4.2060E=04 13 1.416 94.118
~~ ~
FIOM 4.2060E=04 TO LT.OR.EG. 4.7915E=0a 10 1.089 95.207 ( FIOM 4.7915E=04. To LT.OR.EO. 5.4585E=04 11 1.198 96.405 FROM 5.4585E=04 TU LT.OR.EQ. G2182E=04 11 1.198' 97.603~- FCOM 6.2182E=04 TO LT.OR.EQ. 7.0836E=04 9 980 98.584 ( FROM 7.0838E=04 To LT.OR.Eu. 8.0699E=04 4 436 ~ 99.020 ~ - ' ~ ~ " - - - FROM 4.0699E=04 T0 LT.0R.EQ F 9.1931E=04 3 327 99.346 FCOM 9.1931E=04 TU LT.OR.EQ. 1.0473E=03 2 218 99.564 ( FROM 1.0473E=03 TO LT.OR.EG. 1.1827E=03 4 436 100.000 TOTAL 918 L
~ ' ' ~ ~
~ ' - ~ huMBER OF ZERO ENTRIES 7572 MIN NUMBER OF VALID OBSERVATIONS PER AVERAGING INTERVAL e 1 C
50.00 PERCENT PUINT
~
8.603E=05 ~ ~ - -~ 5S 00 PERCENT POINT 9.864E*05 - ~ 6 0. 0 0~ ~PE RCENT ~ POINT-~ 9. 8 8 8E=05 - - ~ 65.00 PERCENT POINT 9.912E=05 70.00 PERCENT POINT 9.936E=u5 75.00 PENCENT POINT 1.137E=04 -- ~ 80.00 PERCENT POInf 1.471E=04 85.00 PEkCENT POINT 1.936E=04 96.00 PERCENT POINT 2.729E=ce 95.00 PENCENT POINT 4.650E=04 94.45 PERCENT Pu!NT 4.413E=04 (NRC TECHNICAL PU3ITION = RELATIVE CONCENTRATION PRU8 ABILITY)
5% ICON (ATMUSPMEWIC DISPERSION FOR D3A EveLuA110NS) = YAhKEE ATOMIC ELECTRIC CD (MOD v3, 07/24/78) 11/24/78 Fakt 19
)
MT 1977 12 MONTM8 = GROUND = LEVEL NELEASE = WARIAHLES MEFL&CED = EXCLUSION AktA DELTA =T STasILITY MODEL -WSa M
)
- DOWNw!ND SECTOR N GAMMA CHI /O (SEC/M3) = PNU84BILITY D18TR1euTIOm3 DlMETERe fs 61'070 '8ECTUR' AVERAGE VALUES ~E ~1=MUUN AVERAGE 8
' ~' ~~~ ~ ~ ~ ~ ~ '
i:
~~~ ~ ~~
FREGUENCY DISTRItuTION RANGE NuM8ER OF PERCENT OF CUMULATIVE
- ~ ~
, 088ERVATIONS 10TAL 088 PENCENT I PROM a.5649EJ06~~~TO i T.ON.Eo, s '.~0 26 7 E = 0 6 3 327- " "
~327 -
' ~ ~ ~
FROM 5.0267E=06 TO LT.OR.EQ. 5.5352E=06 3 327 654 FROM Tu LT.ON.EG. 6.0951E=ue 4 436 1.089 }.~~ ~FROM ~ 5.5352E=06 6.0951E=06 To LT.04.EQ. 6.7117E=06 16 1.743 2.832
~~ '~ ~
FRON 6.7117E=06 TO LT.OR.EU. 7.3907E=06 16 1.743 4.575 I PROM 7.3907E=06 TU LT.OM.EO. 8.13saE=06
~
31 -3.377 7.952 i ^ FROM 4.138aE=06-~~'10 LT.04.EO.~ 8.9617E=06 ~ ^ 2 3 ' ^ ^'~ ~ 2.505 10.458
~
FROM 8.9617E=06 TO LT.UN.EU. 9.8683E=06 29 3.159 13.617~ I FMUM 9.8683E=06 TO LT.ON.EU. 1.ost7E=n5 38 a.139 17.756 I FROM 1.0867E=05' 70 LT.OR.EO. 1.1966r-u5 36 3.922 21.678
' '~
FROM 1.1966E=05 TU LT.OR.EU. 1.3176E=05 45 4.902 26.580 FROM 3176E=05 70 LT 1.a599E=05 66 7.190 33.769 FROM 1,4504E=05 TO LT,0R.E9 04.EO.~ 1.5977E=05~~~ 51~
^~
1 5.556~ ~ 39.325 FROM 1.5977E=05 YU LT.OR.Eu. 1.7593E=05 67 7.298 46.623 FROM 1.7593E=05 TO LT.ON.EQ. 1.9373E=05 65 7.081- 53.704' i - PROM ~1.9373E=05 To LT.UR.EQ. 2.1333E=05 69 7.516 61.220
' ~ ~~
PROM 2.1333E=05 TU LT.OR.EU. 2.3491E=05 55 5.991 67.211 , FROM 2.3491E=05 70 LT.Ok 2.5868E=05 41 4.466 - 71.678 FROM 2.5864E=05 7 0'LT.OR,EU. ~
. E O .~~ 2 ; 8 4 8 4 E = 0 5 ~' ~ ~ ~ ~ ~ 2 7 ~^ - ^ ~ ~ ~ 2. 9 41 '
~ ~ ' "
74.619 ~
~
PROM 2.Ga84E=05 TO LT.OR.EO. 3.1366E*05 31 3.377 77.996 FRum 3.1366E=05 TU LT.OR.EO. 3.4539E=05 28 3.050 81.ve6
'FROM 3.4539E=05 TO LT.OR.E9 3.8033E=05 28 3.050 84.096
^
~ ~ ~
FROM 3.8033E=05 TU LT.0W.EU. 4 1880E=05 9 980 85.076 , FROM 4,1880E=05' 10 LT,04.EQ. a.6117E=05 14 1.525 86.601 FROM s.6117E=05 TO'ET;0R.EQ.~~~ 5;078 3E=05~ - ~ 19 ' '2.070' ~ ~ ~~48.671 ~
' ~ ' - ~
PROM 5.0iS3E=05 TO LT.OR.EG. 5.5920E=05 13 1.e16 90.067 PROM 5.5920E=05 TO LT.ON.EG. 6.1577E=05 26 2.832 92.919
" - ~ PROM 6.1577E=05~ TO LT.04.EG. 6.7506E=05 16 '1.7e3 9a.662
~ ~ ~ ~ ~
FROM 6.7506E=05- 70 LT.OR.EO. 7.4666E=05 to 1.089 95.752-PROM 7.4666E=05 10 LT.OR.EG. 4.2219E=05 to 1.525 97.277 FROM 8;2219E=05 ~TO~ET.0R.E0; 9.0536E=05" " 6"- ' .654 - ---~~ ~ 9 7 . 9 3 0 ~ ~^ ^~~ ~ ~ FRom g.0536E=05 70 LT.OR.EG. 9.9695E=05 1.089 FROM to 99.020 9.9695E=05 70 LT.ON.EQ. 1.0918E=04 1 109 99.129 FROM~~"1;0978E=04 ~TO LTiOp.E0;' 1,2089E=0a~ 1 109 99.237'
" "~~~~ -
i FRON 1.2089E=04 70 LT.OR.EO. 1.3312E=04 3 327 99.564 FROM 1,3312E=84 TO LT,0N,EO. 1.4564E=04 4 436 . . 100.000 TOTAL 918 -
- ~~ NUMBER OF ZERG ENTRIE8 7572 MIN NUMBER OF VALID 088ERVATIONS PER AVERAGING INTENVAL a 1
~ ~ ~
50.00 PERCENT PUINT 1.850E=05 55.00 PENCENT POINT 1.959E=05-60.00' PERCENT POINT ~2.112E=05 65.00 PERCENT POINT 2.293E=05 ~ 4 70.00 PENCENT POINT 2.470E=05 75.00 PENCENT POINT 2.890E=05
"~
80.00 PENCENT PUINT 3.391E=U5 85.00 PENCENT POINT e.182E=05 90.00 PEaCENT POINT 5.542E=05 95.00 PENCENT POINT 7.018E=05 ~~~ _94.45 PENCENT POINT 4.664k=US (NHC TECHNICAL PUSITION = RELATIVE CONCENTRATION PRudA81LITV) . . ,
. _ . ..2]
, 4%ICUN (4TKUSPHEaIC uts7EC310N PON Det EvALUATIONSI = YANALE ATOMIC ELEC1NIC CU (m00 93, 07/2e/Fel 11/2e//6 Past 20 P'
MY 1977 12 MONfMS = GRUUNu=Ltvtt NtLtabt = WANIAWLES NLPLACED = tsCLU310N aNtA uttTA=f SIAstLitv MuutL-00aNm!ND SECTUN NNE GROUND = LEVEL CHI /O (SEC/Mll = PROUh81LITY 018TN!8UI!UNS fI s' ~~610.0 O(w(TENel PLUNt CENTERLINE v4 LUES = t-HOUN AVENAGES
~^
~
FREuufNCY DISTRIsufluN NANGt NUMBER OP FL4 CENT OF CUMULATIVt
~
~
, OestNVATIONS TOTAL OS$. PENCENT
~
FROM 3.t336E=06 tu LT.UN.E0 -3.6778E=o6 1 1e6 .Ie6 FMUM 3.677eE=06 10 LT.UM.tG. 4.316tE=06 0 0.000 146 C FROM. ,e.3 tete =06 TU LT,04.Eu, 5.0052E=06 0 0.000 1e6 l
, FROM 5.0652E=06 TO LT.ON.to. 5.9eset=06 0 0.000 .tet FROM 5.9eseE=06 TU LT.UR.EO. 6.9 Fete =06 0 0.000 .146 C , PROM _ 6,976tE=06_.TU LT,0R,Eu, e. tee 9E=06 0 0.000 146_-
5 FNUM S.1849E=06 10 LT.ON.EO. 9.6079E=06 0 0.000 146 FRom '9.6079E=0e TO LT.UN.to. 1.1275F=05 0 0.00u .teo C
~~ '
FROM 1,1275E=05 -TU LT.ON.te. 1.3d33E=05 *
.146 292 FROM 1.3233E=05 TU LT.ON.tu. 1.5529E=05 0 0.000 292 FRUM 1.5529E=05 70 LT.UN.EO. 1.8225E=05 5 731 't.u23 C PROM _ t,8225E=05 _TO,LT.ON,EG,_ 2.1388t=05 3 _.
439 1.462 FAUM 2.1300E=05 TO LT.ON.EU. 2.5100E=05 0 0.000 1.462 FROM 2.5100E=05 TU LT.ON.EG. 2.9456F=05 0 0.000 1.462 C FROM 2.9456E=u5 TU LT.Uw Eu. 3.e569E=o5 3 439 1.901 ' ' ~ " ~ ' FROM 3.e569E=05 TU LT.ON.EO. e.0569E=05 11 1.6v8 3.509
"~~~
FROM e.0569E=05 TO LY.ON.EU. e.76 tut =05 36 5.263 8.772 C FROM e 7610E=05 TO LT.ON.EO. 55 S.0e1 16.813 i FRO F 5.,547eE=05 ~TO LT.ON.EW.~5.5674E=05 6.5572E=05~ ~ ~~ ~ ~ 92 ' ~ 13.450 ~ - "~ ~ 3u.263
~ ~ ~ ~
FMUM 6.5572E=05 TO LT.ON.EO. 7.6953E=05 71 10.380 so.6el C FROM 7.6953E=05 TU LT.ON.Eu. 9.0109E=05 36 5.263 45.906
, ~ ~ ~'FROM ~~ 9.0309E=05 TU LT.OR.to. 1.0598E=0e tot 27.193 73.099
~ ~ ~
FRUN 1.0594E=0e TO LT.OR.EO. 1.243eE=0e 23 3.363 76.e62 C FROM 1,4434E=04 TU LT ' " ~ ~ ~ " ~ ~ ~25 3.655 80.117 TOT T,0N,EG,~1.4597t=0e FROM i.4597E=ce .04.EQ. 1.7130E=0e" 18 ~~ ~~~ 2.632 ~~' ~ ~~ 8 2. 7 49 ~ ~
~ " ~ ' "
FROM 1.7130E=0e TU LT.ON.Eu. 2.0103E=04 in 2.632 85.360 C l PROM 2.0103E=0s TO LT.ON.EG. 2.3593F=0e 19 2.776 88.158 ! ~~ ~'~FROM '2.3593E=04" to LT.OR.te.~ 2.7687E=os 13 1.901 90.058
~ ~~
FRUM 2.7687E=04 70 LT.0R.EO. 3.2493E=04 to 1.462 91.520 't FROM 3 TO LT.0w Eu, 3.e133E=0e 12 1.754 93.275 P R O N'~~8133E=04~ 3.,2 4 9 3 E = 0e TO~LT.OR.Eu.-"4.e75tE=04 " ~~
^ ' ' ~ ~ ~
17 2.485 ~~ ~ 95.76u FRUM e.475tE=04 TO LT.ON.EU. 5 25 tee =ce 11 1.608 97.368 s Fdum 5.2518E=ce TU LT.Uw.EQ. 6.163eE=Us 4 .555 97.953 FMUM 6.1634E=ce .TU LT.ON.tu. 7.233tE=0e 6 .877 98.830 FRUM 7.233tE=0e TU LT.UN.tk. 8.4686E=04 7 1.023 99.854' s PROM 8,4486E=0e_,TU LT.UN.EO., 9.856tE=0e t 146 100.000 ,
. TUTAL toe b NUMSEN OF ZENu LNTHIES T896 M1N NUMufR OF waLID 065tRVATIONS PEN AVEhAG1hG lhlEHvaL a 1 ~ ~ ~ ^
50.00 PENLENT PUINI 9.773t=d5 55.00 PtNCkNI PU1NT 9 d56E=US
^ *'so.eu PENCENT PUINT 9,863t=05- 65.00 PENCth? Putmf 9.90bt=05
~
70.00 PENCEmi PUINT 9.931t=05 75.00 PEwCEN! PutNT 1.13FE=Us Po.gu PENCENT PUINT 3.ee2E=ce 85.00 Ptwtt NI PutNT 1.vust=on 90.00 PENCENT PUINT 2.73et.de 95.00 PENCtNT POINT 4.3 bit =ve - 92.55 PLNCLNf PutNI 3.59TL 04 (hWC IECHNICAL PubIlluN = NtLAl[vt-LUNCthlNAt{bN Phu$ag)Ljlt) . _ _ _ _ _ _ _ _ _ _ _ - . , _ - _ -. r .. T , ,
- v , * - . , , . + - .,, ,
i
. Sn1kON (6fMOIPMERIC U13PENSlum FOR dea EVALGATIONS) = YANREE ATOMIC ELECTWIC CU. tauD 03. 97/24/78) '11//6/76 PAGE 21 My _1977 12 MONTHS = GRuuh0=t.EvtL NEtt48E = VANIABLES MEPLACED = EXCLUSION AktA c
DELIA=T STAo1LITV NUDEL _ _ _ DOMMMIND SECTOR NME GAMMA CH1/Q (SEC/M3) = PNUSA81L18Y DISINI6UTIONS C 6'10.6 set:UR' AVERAGE VALUES - OTRE TERS Fs
-1= HOUR AVERAGES FREQUENCY DISTRIBUTION RANGE NUMBER OF PERCENT OF CUMULATIVE 068ERVAT10N8 TOTAL 088 PENCENT E 428tE=06 TO-L~T;DR . EG I 4.'2146E=06~
~
FROM ' '~ ~~~' t 146 ~^ '- ~ ~~~ .t et "
~ ~ ~ ~
FROM 4.2146E=06 TU LT.OR.EQ. 4.6401E=06 0 0.000 .146 C ~ FROM 4.640tE=06 Tu LT.UR.EO. 5.tv86t=u6 0 0.000 146
~FROM ~~5.1086E=06' TO LT.OR.EG. 5.6244E=06 1 146 292
~~
PROM 5.4244E=06 TO LT.OR.EG. 6.1923E=06 0 0.000 292 C FROM 4.1923E=06 TO LT.ON.EQ. 6.8176E*06 ~ ~ 4 ~ ~ ~ ~ ~ 585 877 FR OM 6. 417 6 t = 0670 ' L T . ON . E G .~7. 5060 E = 06 ~~~4 5s5
~~~~1.462
" ~ - ~ ~
PROM 7.5060E=06 70 LT.ON.EQ. 8.2638E=0) 7 1.023 2.485 C
~
FNOM 8.2635E=06 TO LT.UR.EG. 9.0982F=06 22 3.216 5.702 FROM ~ 9.0982E=06 TO LT;04.EG. 1.0017E=05 29 4.240 9.942
~~
FROM 1.0017E=05 TO LT.OR.EG. 1.1028E=05 37 5.4c9 15.351 C PROM 1 1028E=05 TO LT.0R.EO. 1.2142E=05 50 7.310 22.661 i FROR 1,.21~42E=05 T0"LT 0M.EG.~ 1?3368E=oS - ~ ~ ~53 ~ ~
- 7. 7 4 9 '~ ~ ~~-~ 3 0. 4 0 9
~ ~~
FROM 1.3368E=05 TO LT.ON.EG. 1.4717E=05 59 8.626 39.035 C' FNUM 1.4717E=US TO LT.ON.EQ. 1.6204E=05 48 7.018 46.053 P~ FROM '~1~6204E=05 . TO LT.OR.EG. 1.7840E=05 42 6.140 52.193
~ ~ ~ ' ~ '
PROM 1.7840E=05 TO LT.OR.EO. 1.9641E=05 48 7.018 59.211 C FROM- 1.9641E=05 TO LT.OR.EG. 2.1624E=05 26 3.801 63.012 FROM 61624E=05 7 0 LT.OR.EU.~ 2;3807E=05 3 5 -~~ ~ 5.117'"
~ ~
68.129'
~ " ~ ~ ~ ~
FROM 2.3807E=05 TO LT.ON.EU. 2.621tE=05 29 4.240 72.368 C FROM 2.6211E=05 TO LT.OR.EU. 2.8858E=05 16 2.339 74.708 FROM~'2.8858E=05~'TO LT.OR.EG.' 3.1771E=05 21 3.07o 77.778
~ ---
PROM 3.1771E=05 Tu LT.OR.EG. 3.4979E=05 23 3.363 81.140 ( FROM 3.4979E=05 70 LT.OR.EO.*3.8511E=o5 19 2.778 83.918. y . PROM 3.8511E=0570TT.OR;EG. 4;2400E405 ~ 18~ 2.632 86.550 -'-~' - v FROM 4.2400E=05 TO LT.OR.EG. 4.6681E=05. 12 1.754 28.304 L FROM 4.668tE=05 10 LT.OR.EG. 5.1394E=05 17 2.485 90.789
- "~ FRod ~ 5.1394E=05 -~TO LT.OR.EU. 5.6584E=05 to' 1.462 92.251
~~
i FROM 5.6584E=05 TO LT.OR.EG. 6.2297E=05 4 585 92.836 t FROM 6.2297E=05 TO LT.ON.EG. 6.8587E=05 '~ 13 1.901 94.737 FROM 638587E=05 7U LT.OR.EGI7;5512E=05 ~ ~ ~ ~ ~ 16~~- ~ ~
~~
2.339~~~ ~ ~ 97.076 - ~ ~ ' ~ ~ FNUa 7.5512E=05 70 LT.ON.EG. 8.3136E'05 8 1.170 98.246 FROM 8.3136E=05 1u LT.ON.tu. 9.153tE=05 5 731 98.977 FROM 9.1531E=05 TO LT.OR.EU. 1.0077E=04 5 731 99.708
~ ~
FROM 1.0077E=04' TO LT.ON.EG. 1.tuv5E=04 1 146 99.654 s FROM 1,1095E=04 TO LT.uM.EQ. 1,2137E=04 ~ 1 146 100.000 TOTAL 684 L !' NUMBER OF ZERG ENTRIES 7806 MIN NUMBER OF VALID OUSLRVATIONS PEM AVtRAGING IN TE NV AL a 1
~
s
-~'
50.00 PENCENT Pu1NT 't.735t=05 55.00 PENCENI POINI 1.85ut=05 1.998t=05
~
~60.00 PERCENT POINT 65.00 PENCENT POINT 2.215E=05 70.00 PtWCENT POINT 2.456t=oS 75.00 PFWCtNi POINT 2.69tE=05 w 80.00 PEkCFNT Pu1NT 3.413t=u5 e5.00 PERCtN1 POINT 4.007E=05 90.00 PENCENT POINT 5.103t=05 95.00 PENCLNI POINT 7.010E=05 s
92.55 PENCENT POINT 6.034t=05 (NkC TECHNILAL PubilluN = kELAllWL CONCENIRAT1064 PWuhABILITV) . _ . _ _ _ _ - - _ - - _ _ _ _ _ _ _ _m. _ _ . __ W m. _ _ __2 - - - - _ _ m _ m. __i_ -_ er - e _a
i 821Ru4 (AfmotPHERIC UIs7ERSlub fun 08A EvaluaT10m33 = YANKEE ATOMIC ELECTRIC CD (MOD c3. 07/24/78) 11/24/78 PAGE 22 mf 3977_12 RUNTMs = GwouNu= LEVEL NELEA3E = WARIAELES NEPLACEu = ERClubluN AhEn DELTA =T STA8ILITV MUDEL ___
)- 00nNw!ND SECTON NE GN00ND= LEVEL CNI/W (SEC/M33 = PROBASILITY u!5THIBUTIuh3 0 DfmETERS) a 610.0 -" plume CENTERLINE VALUES = t=HuuR AVERAGES
~
) .6
~ - ~ ~
FREeutNCf DISTRIBUTION RANGE NuMSEN OF PERCENT OF CUMULATIVE
~ ' '
) OSSENVATIONS TOTAL 063 PENCENT Q
~
FROM 2.3100E=05 70 LT.uR.EG. 2.5706E=05
~
.239
' ~ ~ ~
1 239
)' FROM 2.570eE=05 70 LT.OR.E9 2.8606E=05 0 0.000 239 Q PROM 2.860sE=05 70 LT.ON.E9 3.1832E=05 0 0.000 239
' F ROM '- 3.1832E=05 TO LT.UR.EO. 3.5e23E=05 6 1.435 1.675
~~
) Prom 3.5423E=US TU LT.OR.EO. 3.9418E=05 8 1.914 3.589 i F#0m___3,9418E=05__Tu LT,uR.EU.__4.3865E=05 __
5 _ 1.196 4.785 PRum 4.3865E=05 Tu LT.ON.EG. 4.8812E=05 20 4.785 9.569 ) FRum s.8812E=05 Tu LT.ON.EW. 5.e31eE=05 11 2.632 12.201 i FRum 6.0485E=05 11 2.632 18.833
~-'~~~~ FROM-~ 5.e318E.05TufuLT.uR.EO.
6.0se5E=05' LT.uM.E4 6.7263E=05 32 7.656 22.ees
- - ' - ~ ~ ) FRom .6.7263E=05 70 LT.ON.EG. 7.4850E=05 11.eu5 FROM e6 33.493. t 7,485cE=05 10 LT,0N.EU. 8.3293E=05 ^ ' ' ~ ' - ~ ~ to- ~ ~ 2.392 .
35.885 FROM 8.3293Ea05 TO LT4uR.EQ.~~ 9;2688E=05 8
~
't.914 ~ ~ ~ ' - 37.799
) FROM 9,2688E=05 TU LT.ON.EW. 1.0318E=04 88 21.053 58.852 4 FROM 1.031eE=ce 70 LT.uk.EG. 1.187eE=08 28 6.699 65.550
~FROM ~ 1.1478E=04 fu LT.9R.EO. 1.2772E=04 3.349 ~~-~^
14 68.900 ) FRum 1.2772E=0e TO LT.OR.EU. 1.4213E=0e 14 3.349 PROM 72.2e9 i 13 4213E=0s TO LT.OR.Ee t 1.5816E=04~ 12 2.871 75.120 FROM 1.5816E60s-~TO LT;0R.EQ._~1.7600E=04 13 ~ ~ ~ - ~ ~ 3.110 ~~ ~'-78.230'
~ ~ - " ~ ~
) FRum 1,7600E=04 70 LT.09.EO. 1.9586E=04 10 2.392 80.622 i FROM 1 70 LT.ON.EG. 2.1795E=04 7 1.675 82.297 FRom- 2,9586E=0e 1795E=04' TO LT.ON.EW. 2;4253E=04 1.110
~ ' "-~
13 85.407
) FROM ~2.e253E=0e Tu LT.UR.EW. 2.6989E=ce 7 1.675 87.081 4 FROM 2,6989E=0e TO LT 04.EW 3.0033E=ce '--11 2.632 89.713 rpOM 3,0033E404- TO CT.,04.E0[-~3;342tE=04 # - . 957
~
90.670
-~
FRum 3.3421E=ce TU LT.ON.EO. -3.7190E=ce 8 1.914 92.584 t FNum 3.7190E=ce TO LT.ON.EW. 4.1385E=0e 6 1.435 94.019 FROM - ~ 4.1385E=04 ' ~ TO LT.OR.E0; ~ 4.605eE=ce 8 1.914 95.933-
'~ ~~
FRum s.605eE=0e TO LT.ON.Ee. 5.1288E=0a 4 957 96.890 C FROM 5.12a8E=04 Tu LT.0#3E9 5.7029E=04 -1 239 97.129 t 5.7029U04-~TO-ET;0R.EG 6;3462E=04 FROM 7 ~~-~F;675 98;804
-~~-
) FROM 6.3462E=04 fu LT.04.EW. 7.0620E=04 FRom 3 '.718 99.522 t 7 0620E=0e TU LT 04.Es. 7.e586E=04 0 0.000 .99.522 FRON T.,8586E=04 ~TO LT.OR;EQ;^ 8;7450E=0e 8 0.000
" ~'
99.522
) FROM 8.7450E=Se TO LT.OR.EO. 9.7314E=04 1 t.239 99.761 .t-PROM 9.7314E 84- TO LT.04.EG. 1.8752E 83 _
1 239 108.808
)
TOTAL ett i
~~ NUN 8ER OF~ZERG ENTRIES 8072 MIN NUMBER-OF VALIO 088ERVATION8 PER AVERA8thG INTERVAL e 1
- ~ ~ " - -
58.80 PERCENT PUINT 9.923E=05 t 55.00 PENCENT Pu1NT 9.982E=05 66;00'PENCENT~Pu!NT-- 1;0s t E=04 65.00 PERCENT POINT"-- 1.136E=0e'~ ^~~~
~ ~ ~ ~ ~ ~
70.00 PERCENT Pu!NT 1.344E=04 75.90 PENCENT POINT ~ 1.53eE=04 0
~
80.00 PENCENT Pu!NT 1.933E=De ~ 85.UU PENCENT POINT 2.338E=ce I
~~'.
90.00 PERCENT Pu1NT 3.16tE=04 95.00 PERCEN) PulNi 4.188E=04- l 87.81 PERCENT Pu!NT 2.733E=ce (NHC_TECNNICAL PuSITIuh =- NELATIVE COMCENTRifION PRU8A81LITV) I
.g
[ -
-- a~ - - - - - - , - + ---- i - -
- 87. ICON (ATKUS7HERIC D187Ed810N FOR 034 EvaLUATIow3) - YANMEE AT0nIC ELECTRIC CD (MOD v3. =7p24/78) 11/28/78 PAGE 23 MY,1977 12 MONTHS = G20UND= LEVEL NEtta5E = wARIACLES HEFLACED = ERCLUSION AREA Optie=T 51661LITY CJOEL _
DDwwwIND SECTON NE GAMMA CMI/W (SEC/m3) = PNubah1LITY DISTRIBUTIONS 6(METEN8)'s '610.0 SECTUR AVENAGE VALUES = 't-HUUN AVERAGES
~-
FREQUENCY DISTRIBUTION NANGE NUM8ER OF PENCENT UF ~CUMULATIM 08SERVATIONS TOTAL 083 PENCENT
-- ~
6' ' ' ~~~
~~
F R O'N 6.9533E=06 TO 1T 04.EW. 7.5475E=06 ~1.435 1.435 FNOM 7.5875E=06 TO LT.UR.EG. 8.1925F=06 9 2.153 3.d99 8.1925E=06 70 LT.UM.EQ. 8.8926E=06 7 1.675 5.263
'~ - - FROM FROM ~ '8.8926E=06 TU LT.OR.EG. 9.6526E=06 12 2.871 8.13e
~ ~ -
FROM 9.6526E=06 TU LT.0H.EQ. 1.0877E=05 16 3.828 11.962 FROM 1,0a77E=05 TU LT.0M.E9 1.1373E=05 11 2.632 la.593 FROM 1.1373E=05- TO 'LT.0W.Eu, 1,2345E=05 8 't.914
~
16.507
' ~
FROM 1.2345E=05 TU LT.04.EO. 1.3400E=05 15 3.589 20.096
~ ~ ~ FROM. 1.3400E=05 TU LT.OR.EU. 1.e545E=05 15 3.569 23.684 FROM 1.4545E=05 TU LT.OR.EG. 1.5788E=05 25 5.981 29.665
~ ~
FROM 1.5788E*05 TO LT.0R.EO. 1.7137E=05 in 4.306 33.971 FROM 7137E=05 1.8602E=05 30 7.177 #1.148 FROM 1,4602E=05 7 0 LT,0H.EQ.TO LT,0R.EO,~2.0191E=05 1
~ ~'
to ~ 6.306 e5.e55 FROM 2.0191E=05 TO LT.0R.EO. 2.1917E=05 20 e.785 50.239
" ' ~~
FROM 2.1917E=05 70 LT.UN.EQ. 2.3790E=05 15 3.589 53.828
' FROM ~ 2.3790E=05 TO LT.OR.EO. 2.5823E=05 17 4.067 57.895
- ~~
FROM 2.5823E=05 TO LT.0#.EO. 2.8030E=05 13 3.110 61.005 FROM 2.8030E=05 70 LT 0R.EG. 3.0825E=05 22 5.263 66.268 FROM 3.0425E=05 70'LT.,OR.EQ. 3.3025E=05 '~-~~~3^- 1 ~ ' ~~~ ~ 3.110 - 69.378
~ ~ ~ -
FROM 3.3025E=05 to LT.0M.EG. 3 5887E=05 20 a.785 74.163 PROM 3.5847E=05 70 LT.OR.EU. 3.8911E=05 15 3.589 77.751
' ' FR04 3.891tE=05 TO LT;0R.EG. 4.2236E=05 12 2.871 80.622
' ' - - ~ ~
FRUM 4.2236E=05 10 LT.OR.EW. 4.5846E=05 13 3.1*0 83.732 FROM a.5846E=05 TU LT.ON.EU. a.9?bsE=05 10 2,392
-~ ~1.914 - -- ~~ 86.12e
~
FROM a;9764E=0570 LT;0R.EG. 53016E=05 - ~ ~~~ ~8 ~~ -
- 88. 038 ^
"' ~ ~
FNOM 5.4016E=05 TU LT UN.F., 5.F632E=05 9 2.153 90,191
~
FNOM 5.8632E=05 TO LT.OR.(U. 6.3643E=05 13 3.110 93.301
'FROM~ 6.3643E=05 TO LT.OR.E). 6.9082E=05 7 1.675 9a.976
- ~ ~~~
FROM 6.9082E=05 To LT.0R.EO. .7.a986E=05 11 2.632 97.608 FROM 7.4986E=05 70 LT.OR.EW, 8.1394E=05 a 957 98.565 PROM 8.1394E=05"~TU~L% DR.'EC 7 8.8350E=05 ~~ ~~ ~~'3 718 9 9. 2 8 2 - ~ ~ ~ ~ ~ - -~ FROM 8.8350E=05 TU LT.OR.EW. 9.5900E=05 0 0.000 99.282 FROM 9.5900E=05 TO LT.ON.EU. 1.0410E=04 1 239 99.522 FROM 1;0s10E=04 TO LT;0R.E0- ~1.1299E=0a 1 239
~ ^ - ~ ^ '
99.761
'~' ' ~ ~ ~ ' ~ -
FROM 1.1294t=0s Tu LT.ON.EO. 1.2265E=04 0 0.000 99.761 FROM 1.2265t=04 To LT.OR.EW. 1.3260E=0e t 239 100.000 TOTAL 418
~ ~ NUMBER OF ZERO ENTRIES 8072 MIN NUMBER OF VALIU DNSERVATIONS PEN AVERAGING INTERVAL e 1 50.00 PERCENT POINT 2.166E=05 55.00 PERCENT POINT 2.45tE=05 60.00 PERCENT POINT 2.682E=05 65.00 PERCENT POINT 2.975E=OS 70.00 PERCENT PUINT 3.309E=05 75.00 PERCENT POINT 3.636E=05 80.00 PENCENT PUINT e.166E=05 85.00 PENCENT PulNT 4.e46E=05 90.00 PERCENT POINT 5.793E=05 95.00 PENCENT POINT 7.024E=05
~ ~
87.81 PERCENT PUINT 5.37eE=05 (NRC TCCHNICAL PUSIT!UN = RELATIVE CONCENTRATION WROWABILITY) t % . m .. _ _ , _ _ . - _
. m em y -m._ , . ~ ,w, , . ~ -
83IKOM (ATMOSPMERIC UISPEN510N FOR DBA EVALUATIONS) = YAN%EE ATOMIL ELECIMIC Cu (MOD 03, v7/24/78) 11/24/78 PibE 24 p
. MT 1977 12 MONTM5 = GMOUND= LEVEL M LEASE = VANIAdLES MEPLACED = EXCLUSION ARLA DELTA =T SIAd!LITY MODEL 00=Nw1ND SECTOR ENE GRouaD LEVEL CHI /W (UEC/M3) = PRuBA8ILITY DISTNIBUTION5 s MME TER 8 Fe ' ~~61 o.0~ PLUME CENTERL1hE VALUES = 1=HUUN AVERAGE 5
(
~
~ ' ' ~ -
l~~ FREQUENCY DISTRIBUTION RANGE NUMBEM OF PERCENT OF CUMULATIVE UBSERVATIONS TOTAL 0B8 PENCENT
~'~
FROM 9.7932E=06 TU LT.UR.EW.- 1.1027E=05 1 224 224 FROM t.102FE=05 10 LT.UN.EQ. 1.2416E=05 0 0.000 224 (
~~~
FNOM 1.2416E=05 TU LT.UW.EG. 1.3980E=05 0 0.000 224 FROM~ 1.3980E=05 Tu LT.OR.EQ. 1;5741E=05 0 0.000 224 FRCM 1.5741E=05 Tu LT.OR.Eu. 1.7724E=05 - t 224 447 ( FROM 1 ,7724E=05 Tu LT.UR.EU. 1.9956E=05 1 224 671 ~ FROM 1.9956E=05 "Tu LT.0M.EQ. 2.2470E=ob 6 1.342 2.013 FROM 2.2470E=05 TO LT.ON.EQ. 2.5301E=05 1 224 2.237 ~~- FMUM 2.5301E=05 TU LT.UR.EQ. 2.8488E=05 4 595 3.132 2.8488E=05 TO LT.UR.EG. 3;2077E=05
~ - - ~ ~
FROM 7 1.566 4.698 FROM 3.2077E=05 TU LT.OR.EG. 3.6117E=05 7 1.566 6.264 ( FROM 4.0667E=05 14 3.132 "- ~ 9.396 FROM 3,6117E=05-TU 4.0667E=05 Tu'LT.OR.EW. LT,0R.EW.-4.5790E=u5' ~ 20
- ~
- 4. 4 7 t- 13.e70
~~
FROM 4.5790E=05 TO LT.UR.EQ. 5.1558E=05 18 4.027 17.897 6 ' FROM TO LT.UN.EO. 5.eU53E=05 15 3.356 21.253
- ' FROM ~ -5.8053E=05 -5.1558E=05
~~~ -~
TU LT.OR.EQ. 6.5365E=05 35 7.830 29.003 FROM 6.5365E=05 TO LT.UR.EW. 7.3599E=o5 22 4.922 34.004 i FNOM 7.3599E=05 To LT.ON.EG. 8.287tE=05 ~ 21 4.696 ~~ 38.702 "~ FROM 8.287 t E=05 TO LT.0R.EQ;-~9;3310E=05 - --'~ ' 25 ~5.593 44.295' FROM 9.3310E=05 70 LT.ON.EU. 1.0506E=04 114 25.503 69.799 ( 1.1830E=0a FROM 1.0506E=04 10 LT.ON.EG. 15 3.356 73.154 ~ ~
~~FROM 1.1830E=04 TO LT.OR.EQ. 1;3320E=04 19 4.251 77.405 PROM 1.3320E=04 10 LT.ON.EU. 1.4998E=04 18 4.027 31.432 (
FROM 1.4998E=04 1.6887E=04-TU LT.UN.E9 TOTT;0R.EQ.- 1.6887E.04~ 1;9014E=04 9
~ - ~ ~
2.013 ~~- ~~83.445 ~" -~ FROM ~ ~ ~ -17 '3.803 87.248 FNOM 1.9014E=04 70 LT.ON.EG. 2.1410E=04 16 3.579 90.828 s , ~ --~~ FROM 2.1410E=04 TO LT.OR.EW. 2.4107E=04 6 1.342 92.170 FROM' 2.4107E=04 'TO LT.OR.EQ.' 2;7143E=04 6 1.342 93.512 FROM 2.7143E=04 TO LT.OR.EG. 3.0563E=04 9 2.013 95.526 s FROM 3.0563E=04 TO LT gDR 3 4413E=04 2 447 95.973 FROM 3.4413E=04- TOT,T.04,EG .EG. 3;8747E=04 4 '.895 - '-~~96.8e8
- - ~ ~ ~~
FROM 3.8747E=04 TO LT.ON.EW. 4.3628E=04 2 447 97.315 t FROM TU LT.UR.EW. 4.9124E=04 1 224 97.539
'FROM-4.3628E=04 4.9124E=04 70 LT.OR.EQT 5.5312E=04 5 1.119 98.658 ~ ^
~
FROM 5.5312E=04 TU LT.OR.E9 6.2240E=04 5 1.119 99.776 t FROM 6.2280E=04 TO LT,0m.EO. 6.9573E=04 1 224 100.000 TO T 447 t
' ' - ' ~ ~
NUMBER OF ZERG ENTRIE8 8043 MIN NUMBER OF VALID UU8ERVATION8 PER AVERAGING INTERVAL s 1 t 50.00 PERCENT POINT 9.874E=US '55.00 PENCENT POINT 9.892E=05 ~ ~ ~ 60.00 PERCENT POINT ~ 9.910E=05 65.00 PERCENT POINT 9.928E=05 70.00 PERCENT POINT 1.078t=U4 75.00 PERCENT POINT 1.269E=04
~~~~
P0.0c PENCENT PUINI 1.440t=04 85.00 PERCtN1 PUINT 1.779E=04 ~ 90.00 PERCENT POINT 2.030E=04 95.00 PERCENT POINT 2.842E=04 88.60 PERCENT Po!NT 1.940h=04 (NRC TECHNICAL Pub 1 TION = RELATIVE CONCtNTRATION PROBABILITY)'
I .- Sn!COM (aTMUSPMEWIC OISPERSION FOR D04 EVALUATIONS) = VAhmEE ATOMIC ELECTHIC Cu 1900 03, 07/24/78) 11/28/78 PaGE 25
). Mf 1977 12 MONTM8 = GwouhD= LEVEL MELEa5E = VARIABLES MEPLACLU = EXCLUSION aWEA DELia=1 STAe;LITY MODEL
)' 00=mwIND SECTOR ENE GAMMA CMI/W (SEC/M3) = PNUSABILITV. DISTRIBUTIONS O(METER 8Fe 410;0 - SECTOR AVERAGE VALUE8 = 1=Muum^4WERAGE8
- ~~ '~ ~
)
~~ ~
~~~
FNEGUENC% DISTR!suTION R4NGE NUMBER OF PERCENT OF CUMULATIVE
) 08SENVATIONS TOTAL U88 PERCENT
~ - ~
~ ~ ~ ~ ~ 671~
~3^
- ~~
FROM e.4975E=06 TO LT.OR.EO.-e.8819E=06 671
) FROM 4.8819E=06 TU LT.OR.E9 5.2991E=06 1 224 895 .;
5.7520E=06 FNOM 5.2995E=06 70 LT.OW.EO. e 845 1.790 . FROM ~ 5.7520E=06 TO LT.0#.EG. 6.2437E=06 0 0.000 1.790
) FROM 6.2837E=06 TU LT.04.EO. 6.7773E=06 5 1.119 2.908 ;
FRDM 6.7773E=06 70 LT.UR.E9 7.3566E=06 6 -~ ~ ~ 1.342 a.251 ;
~ 2.237 ' "
FROM 7.3566E=06 Tu LT.uR.EO. 7.9853E=06-10 6.e88
) FNOM 7.9853E=06 TO LT.0M.E9 8.6678E=06 to 2.237 8.725' -
'~ FNOM 8.6678E=06 Tu LT.OR.E9 9.euB7E=n6 18 4.027 12.752 ~ * ~ ~ - '
FRom '9.4087E=06 70 LT.ON.EO. 1.0213E=05 21 4.698 17.450
) FROM 1.0213E=05 to LT.uM.E9 1.1086E=05 11 2.461 19.911 FROM 1 1086E=05 To LT.OR.EG 1.2033E=05 28 4.47s 24.385 -
PR0d 1,2033E=05
. TD LTiOR.EG,. 1.3062E=o5'
~ ~
31 ~~ ~~ 6.9 3 5
- ~~
31.320
) FROM 1.3062E=05 to LT.ud.E9 1.4178E=05 28 4.264 37.584
. FROM 1.4178E=05 TO LT.OR.EW. 1.5390E=05 17 3.803 41.387
~ ~ FROM '1.5390E=05 TO LT.OR.EO. 1.6705E=05 17 3.803 45.190
~ ~ ~
h PROM 1.6705E=05 70 LT.0M.E9 1.s133E=05 18 4.027 49.217 ; FROM 1.8133E=05 TU LT.OR.EG. 1 9683E=05 ~" to 3.579 52.796 - FRD F 1.9683E=05- TO LT.ON.EG. 2.13651 05 ~--~20~" ~ 4. 4 7 4 " - ~ ~ ~ ~~57.271-
~-
-) FROM 2.1365E=05 Tu LT.OR.E9 2.3191E=05 24 5.369 62.640 FROM 2.3191E=05 Tu LT.OR.EG. 2.517eE=05 2e' 5.369 68.009 " " - - ' - '
- " FROM ~ 2.5174E=05 To LT.OR.EG. 2.7325E=05 11 2.461 70.470
) FROM FROM 2.7325E=05 Tu LT.ON.EO. 2.9661E=05 10 LT.OR.EO. 2.9661E=o5 3.2196E=05 17 14 3.803 3.132 74.273 77.405
~FR0m7.2196E=0570~LT.0R.EG.-' 3.49e 8E =05 ' - ~ ~ ~ " ~ 15 ' ~~~ ~ ~ 80.761 ~ ~~
~ ^ ' ' ' ~ ~
~
~ 3.356 FROM 3.4948E=05 70 LT.Ok.EG. 3.7935E=05 17 3.803 84.564 FROM 3.7935E=05 10 LT.OR.to. 4 1177E=u' to 2.237- 84.401 ~ - ~ ~ ' -
r FROM' ~4.1177E=05 70 LT.OR.EO. 4.4696E=05 17 3.803 90.604 FROM e.4696E=05 TO LT.UR.EO. 4.8516E=05 8 1.790 92.394 FROM 4.8516E=05 fu LT.OR.EO. 5.2663E=05 7 1.566 93.960 ! 5.2663E=05 TO ~LT.04.EG.-' 5.7164E=05 895
- -- ~ ~ " - " -
[ FROM e 94.855 ~ ' p FROM 5.716eE=05 10 LT UW.E9 6.2050E=05 7 1.566 96.e21 FROM 6.2050t=05 Tu LT.uM.tv.. 6.7354E=05 5 1.119 97.539 . FROM 6.735eE=05 10 LT.UR.EO. 7.311oE=u5 7 1.566 99.105 PROM 7.3110E=05 TU LT.UR.EG. 7.93596-05 2 .e47 99.553 FNum 7.9359E=05 Tu LT.04.EO. 8 5672E=05 2 447 100.000 h 10TAL 4e7 6043 NUM6EW OF ZERu ENTRIES MIN NUMdEN OF WAL10 uuStRWATIONS PER AVERAGING INTENVAL a 1 h 50.00 PEWCENT POINT .1.822t=05 55.00 PENCthT P01NT 2,055t=o5 60.00 PERCENT POINT 2.2e7E=05 65.00 PERCENT POINT 2.seuE=05
' - - ~ ~ ~ ~
b 70.00 PtWCENT PUINT 2.629t=05 75.00 PkMCEN1 PUINT .3.117E=05 t 80.ou PtNCFNT Pu1NT 3.en3t=ub 55.00 PEwCtNT Pu!NT 3.e55t =05 - i 90.00 PENCENT PUINT 4.375E=u5 95.00 PENCt41 POINT. 5.755t=05 y. 88.60 PENCENT Pu1NT 4.232t=05 (NWC TECHe*1 Cat PusIT10N: - MtLA11VL CuMCEhikaTION PROBABILITY) _
. _ . - . _ . _ _ _ _ . . - . . _-- - - - - - . . - - - . - ~ ~ ~ _ - . ~ - ~ ~ -
I .
. SMICON (ATEOSPHERIC UISFERSION Fu2 D3A EVALUATIONS) = vaNAEE AIU"IL ELECTNIC Cu (PUU 03, 07/24/78) 11/24/78 PAGE 23
)* e My 1977 12 PONTns = GNOUNu= LEVEL MELLa3E = var 1asLE3 NLPtaCED - EaCLUSION aNta ULLla=T STAu!LITT muutt
?
) 00aNm2ND SECTUN E GROUND =LtvEL CHI /W (SEC/M3) = PRU8a81LITY DISTNIMUT!uN3 (
0(METER 83's~610.0~ ~~PLU"E CENTENLINE vaLUE8 = t=MUUR AVERAGES
) /
- ~ ~ ~
FNEGUENCY DISTRIBUTION RANGE NUM8ER OF PENCENT OF CUMULATIVE $ 085tRVATIONs total 083 PENCtNT ,
- ' - ~
FROM 671855E=06 70 LT.ON.EG. ~7.1592E=06 1 253 253
) FROM 7.1592E=o6 70 LT.04.EO. 8.2e63E=06 0 0.000 253 C FMUM 8.2863E=06 70 LT.ON.tu. 9.5908E=ut 0 0.000 253
- ~~ FROM ~ 9.5908E=06 Tu LT.Uw.EO. 1.110tE=05 0 0.0u0 .253
) FROM 1.1101E=05 10 LT.UM.EG. 1.2848E=05 0 0.000 253 f FR04 _ 1.2888E=05 TU L1,UR.EG. _1.487it=05 0 0.000 253 FROM 1.4871E=05 fu LT.ON.EW. 1.7232E=05 1 253 506
) FROM 1.7212E=05 TU L?.ON.EG. l.9921E=05 2 506 1.013 FRum 1.492SE=05 TO LI.ON.EO. 2.3057E=05 3 759 1.772 - ~ ' ~ ~
'FRom 2.3057E=05 fu LT.OR.EW. 2.6687E=v5 7 1.772 3.See
) FROM 2.6487E=05 TU LT.OR.EG. 3.0888E=05 3 759 e.3cm . 3,0888E=05 TO LT.0M.EG. 3.5751E=u5 6 '1.519 5.823 FROM-3.575tE=05TO LT.OR.EQ. 4.1379E=05 -
' ~ ~ ~ ' ~~'
FRom 8 2.025 7,848 ) FRom e.1379E=05 70 LT.OR.EG. e.7893E=05 10 2.532 10.3e0 'O FROM -4.7893E=05 Tu LT.ON.LU. 5.5433E=05 23 5.823 16.203 ~
~' FROM 5.9433E=05 TO LT.OR.EO. 6.4160E=05 2e 4.076 22.278
) FROM 6.4160E=05 TO LT.ON.EW. 7.4260E=05 26 6.582 28.861 G FROM 7 4260E=05 70 LT,0N.EG 15 3.797 32.655 FRom 8,.5950E=05' TO'LT.ON.EQ,~ 8.5950E=05 . 9.948tF=05' ~~ 69 ~17.408
^~
$0.127'
~
) FRUM 9.9#8tE*05 TU LT.OR.EU. 1.15 tee =ce 32 8.101 58.228 s
~
FROM 1.15 tee =ce Tu LT.UN.EQ. 1.3327E=ce 12 3.038 61.266 ^-~
~ FROM 1.3327E=ce TU LT.ON.E9 1.5425E=0e le 3.5ee 6e.810
) FROM 1.5e25E=ce 10 LT.UR.EO. 1.7853E=ce 11 2.785 67.595 s FROM 1.7853E=04 fu LT.OR.EG. 2.066eE=0e~ 26 ^~ ~ 6.582 74.177 FROM 2.0664E=04 TO'LT.OR.tv. 2.3917E=04 ~~ ' ~ '13 3.291~~ ~~ ~- -- 7 7. e68 ' ~ - - ' - -- ) FRom. 2.3917E=ce Tu LT.ON.EW. 2.7682E=ce 18 a.557 82.025 .
~ ~ ~ ~
FNOM . 2.7682E=0e 10 LT.UR.EG. 3.2039E=ce 21 5.316 87.3#2 - ~ ~ ~ FROM' 3.2039E=0e 10 LT.ON.EO. 3.7083E=0* 1e 3.544 90.886 .) FRUE 3.7043E=0s Tu LT.UR.EU. e.29dtE=0s 10 2.532 93.418 t FROM FN0m-e.2921E=0e TU LT.OR.EG. e.9678Ee6470~LT.ON.EQ;-~5.7e98E=ce
- e.9678E=04 ~' ~ ~~ ~to '
2.532 -~ 95.949 ~ ~ ~ ~ ~ 3' ' ~ '.759'~'~ 96.709 s FROM 5.7a98E=0e Tu LT.UN.EO. 6 6550E*0a 7 t.772 98.481 FROM 6.6550E=0e TO L1.0M.EG. 7.7027E=0m 2 .50s 98.987 ' ~" FROM- 7.7027E=ce Tu LT.ON.tu. 8.9153E=0e 2 506 99.494 , Fdum 8.9153E=04 Tu LT.ON.EU. 1.0319E=03 1 .253 99.7e7 ( PROM 1.0319E=03 fu LT.OR.EG. l.te27E=u3 1 253 100.000-TUTal 395
- humeEW UF ZtNO ENIN!E3 6095 m1N NUMBER OF vaLIO UuSLRwalIONS PEN AVtRaG!NG INTENWaL e 1
~'
50.00 PtkCENT Pu1NT 9.9 eft =ub 55.99 PENCthT POINT 1.085E=ce ' - ~ ~ ' 60.00 PENCENT POINT 1.239E=0* 65.UU PENCENT Pu!NT 1.57*E=um 70.00 PEhttMT PUINT 1.865t=0a 75.00 PEMCthi Pu1NT 2 It7t=ce 80.00 PthCFNT Pu1NT 2.636t=ue 65.00 PLNCthi POINT 3.035t=0e 90.00 PENCENT Pu!NT 3.bueL=de 95.UU PENCENI P014T 4.66eE=0e 57.10 PENCENT Pu!NT 3.175t=0# thkC TELHNICal Pus!T!UN = htLaTIvt LONCLNINATION 9NuoneILITT) , _
() h-SEIKUN (ATM037MERIC UISPENSIuN FU2 D5A EVALUATIONS) = YaMXEE A10MIC LLECTRIC Cu (MOD C3. 07/2s/18) 11/2s/78 PAGE 27
. C5
( _ MT 1977 12 m0 NTH 8 = GRuum0=Lt%EL NELEASE = var 145LES NEPLACEO - ErCLUSION ANEA OtLTa=1 STABILITY MODEL () 00nNmIND SECTON E gamma CMI/O (SEC/M3) = PRU8 ABILITY DISTdIbuTIONS
] D(MtTER8)'s ---- 610. 0~ - ~~ SECTUR AVEWAGE VALUCS = != HOUR AVERAGES
' ^ - - -
i ()
~~
FREQUENCY DISTRIBUTION RANGt NUNHER OF PERCENT OF CUMULATIVE
, () 088ERv&110NS TuTAL 088 PERCENT I -
e.0727E=06 70 LT.OR.E97-~e.e99 0E=06'-~~'
~~
FROM 2 ~ 506 -" 506 () FROM e.4990E=06 fu LT.OW.Eu. 4.9099E=o6 0 0.000 506
-----'-~ FROM e.9699E=0e fu L1.0R.EO. 5.e9u1E=0e 0 0.ovo 506 FROM' 5.e901E=06 To LT.04.EG. 6.0647E=06 2 5ut 1.013 3 () FROM 6.0647E=06 To LT.ON.EG. 6.699eE=06 3 759 1.772 8
FROM 6,699eE=06 TO LT,0R,Eu, 7.4006E=0e
~
~ ~ ~ ~ ~
7 ~ 1.772 3.544 l FROM-- 7.4006E=06- TO L T.uw.EQ.' ~ 8.1752E =06
' ~ ' - " ~ ~ ~ ~ ~ ~ " '
6 1.519 5.063 FROM 8.1752E=06 70 LT.04.EQ. 9.0 3u nt =0 6 12 3.038 8.101 j
! () FROM TO LT.04.EG. 9.9760F=ce 7 1.772 9.873
'FROM ~~ 9.0308E=06 9.9760E=06 TO LT.OR.EU. 1.1020E=05 20 5.063 te.937
~
() FROM 1.1920E=05 TO LT.ON.EW. 1.217eE=05 22 5.570 20.506 FROM 1.217eE=05 TO LT.UN.EG. 1.3488E=US
~
~~
16 a.051 2s.557 FROM 1.3=e8E=05~ 10 LT.04.EO. ~ 1.4855E=05 ~ ~ ~ 11 2.785'~~~ 27.342
'~ '
, () FROM 1.4855E=05 TU LY.ON.Eu. 1.641oE=05 to 4.557 31.899
- FMom 1.6810E=05 70 LT.ON.Eu. 1.8128E=05 11 2.785 34.68e
! - FROM 1.8128E=05 TO LT.04.EG. 2.0025E=05 19 4.810 39.494
)* () FROM 2.0025E=05 fu LT.ON.EQ. 2.2121E=05 23 5.823 e5.316
- FROM 2.2121F=05 TO LT.04.EQ. 2.e#3eE=05 20 5.063 --~ 50.380 f
d C) FR0d FROM 2;es36E=05- TO'LT.OR.EG.~~2.'699eE=05 -~~ 2.699eE=05 TO LT.OR.EW. 2.9819E=05 20
~
5.063
~~
55.es3~
~- ~ ' ~ ~
21 5.316 60.759 M FROM 2.9819E=05 70 LT.ON.EG. 3.2940E=05 le 3.544 es.304 4 --~~ ~ ~ F R OM 3.2980E=05 TO LT.OR.EG. 3.63e?E=05 15 3.797 68.101
% C) FROM 3.6387E=05 To LT.04.EG. 4.0196E=05 17 8.308 72.eu5 P FROM 4.0196E=05 TO LT.04.EG. e.e#U3E=05 19 ~~~~~a.810 77.215 M FRom a;88 0 3E=05 -~TO LT.04.EQ.~~ e.9050E=05 ~ ~~ -~ 19" s.810
~ ~ '~
8 2. 0 2 5 ~~ -~ ~ ~ ~ - C) FROM e.9050E=05 TO LT.ON.EG. 5.e18eE=05 22 5.570 87.595 FNOM 5.s184E=05 10 LT.ON.EQ. 5.9855E=05 13 3.291 90.880
~~---~~ F R OM - 5. 9 8 5 5 E = 0 5 TO LT.OR.EG. 6.6120E=05 6 1.519 92.405 FROM 6.6120E=05 Tu LT.OR.EG. 7.30eeE=05 12 3.038 95.es3 l C3 FROM 7.3040E=05 70 LT.OR.EG. 8.0665E=05 7 1.772 97.215 F R OM--~8 ; 0 6 8 5 E = 0 5~ TU~L T. O R . E Q .--' 8. 912 9 E = 0 5 '3~ 759 97.975-
'~ ~ --~~ -~~
t3 FROM 8.9129E=05 TO LT.OR.EU. 9.8e58E=05 5 1.266 99.281 l FRom 9.8458E=05 TO Lt.0M.Eu. 1.0876E=0e t .253 99.e94 l l FROM ~-~ 1.0876E=0s ~TO LT.OR.EG. 1.2015E=0e 0 0.000 99.49e
' " ~
l { tp FROM 1.2015E=0e TU LT.ON.Eu. 1.3272E=ce 1 253 99.7s7 s PROM 1.3272E=0e TO LT.0R.EG. 1.e56eE=0e 1 253 100.000 I g)
- i TOTAL 395 I - ~ ' ' NUM8ER OF ZERO ENTR128 8095 MIN NUMBER OF VALID 087;HVATIONS PER AVERAGING INTERVAL e 1 t2 50.00 PERCENT Pu!NT 2.405E=05 55.00 PidCENT POINT 2.676E=05 60.00 .eERCENT PUINT 2.943E=05 fggdka PENCENT POINT 3.31eE=05 ----~--
(s 70.00 PEWCENT Pu1NT 3.758E=05 73.00 PENCENT POINT e.218E=05
" ' - ~
80.00 PENCENT Pu1NT 4.8ecE=US 65.00 PENCENT POINT 5.29CE=05
! 90.00 PERCENT Pu!NT 5.785E=05 95.00 PENCENT POINT 7.283E=05 ? (s 87.10 PERCENT Pu!NT 5.38eE=u5 (NRC TECHNICAL Pus! TION =
RELATIvt CONCENTRATION PROBAWILITY) _ _ . V
8:! NUN (ATMOS ~/MERIC DISPERSIUN FOR 034 EVALUATIONS) = YANmEE AIOMIC ELEC1NIC CU (MOD v3, 07/24/7m) Ll#2c/78 Past 28 b MY 1977 12 MONfM5 = GR00ND= LEVEL hELEASE = vaNIablE3 HEPLACEO = EXCLUSIUN ANEA uhLla=I $fA6[LITY MuoEL __
)' DOWNu!ND 8ECTOR E8E GNouMD= LEVEL CHI /W (SEC/M3) = PR08481LITY DISTNIBUTION8 0(METERS)~s~ ~ ~610.0' ' PLUME CENTERLINE VALUES = !=MOUW AVERAGES
)
~~
"-~
FREQUENCY o!87RIOUTION RANbE NuMREW UF PERCENT OF CUMULaflvt
) 085tRVATIONS TOTAL 055 PENCENT FROM 3.2988E=06 TO LT.OR.EQ. 3.8493E=06 1 .145 .145 ) FROM 3.8493E=06 TO LT.OH.EG. 4.4916E=o6 0 0.000 .le5 ~ ~ ~ - ~ ~ PROM 4.4916E=06 Tu LT.UM.EU. 5.2e11F=06 0 0.000 .145 ~ ~ ~ ~ ~
PROM 5.2411E=06 TU LT.0M.EQ. 6 1158E=ce 3 434 579
) FROM 6.1158E=06 fu LT.OR.EQ. 7.1363E=06 0 0.000 579 FROM 7,1363E=06- TU LT,UR.Eu, '8.3272E=06 '
0 0.000 579 ~~ FROM'- 8.3272E=06 TO LT.0W.EG. 9.7166E=U6 0 0.000 579
) FROM 9.716eE=06 TU LT.UR.EG. 1.1338E=05 5 72e 1.302 ~ ~~~~ FROM 1.1338E=05 TU LT.UR.EW. 1.3230E=05 3 434 1.737 ~~
FROM ~~ 1.3230E=05 TG LT.ON.EG. 1.5438E=05 2 289 2.026
) FROM 1.5438E=05 TU LT.ON.EU. 1.8014E=05 4 579 2.6u5 1,801eE=05 TO LT,0N,EG. 11 1.592 4,197 FROM~~~2.1021E=05 To LT.OR.EQ.~~2.1021E=05
~~ ~~ ~ - ~ ~
't.737 ~~
~
~ ~ "
FROM 2.e528E=05' 12 5.933
) FROM 2.4528E=05 TU LT.ON.EU. 2.8622E=05 28 e.052 9.986 ~ ~ ~ ' ' ~ FROM 2.8622E=05 70 L1.UN.EG. 3.3398E=05 36 5.21u 15.195 '- ^~'~~-
FROM 3.3398E=05 TO LT.OR.EQ. 3.8971E=05 42 6.078 21.274
) FROM 3.8971E=05 TO LT.UR.EG. 4 547eE=05 47 6.802 28.075 PROM e.5sfeE=05 Tu LT.OR.EO. 5.3063E=05 ^ ~ ~ ~
50 7.236 35.311
~ ~ 39.074
- ~
FROM 5~
. 3063E=05- TO LT.UR.EQ.~ 6.1918E=05 ~ 26 3.763 ) FROM 6.1918E=05 TU LT.ON.EU. 7.225DE=05 40 5.789 es.863 FNOM 7.2250E=05 TO LT.04.EQ. 8.43U7E=o5 29 4.197 49.059 ~ ~ ~ ~ - ~
FROM ~~ 8.4 3 0 7 E =05 ' 70 LT.OR.EQ. 9.8376E=05 32 4.631 53.690
) FNOM 9.8376E=05 Tu LT.ON.EW. 1.1479E=0e 109 15.77e 69.465 FNOM 1.le79E=04 Tu LT.UR.EU. 1.3395E=ce ~~ 15 ' ' ' ' ~ ' ~ ~ 2.171 71.635 " ~~~
FROM 1.3395E=04~- TO CT.0R.EQ. 1;5630E=04 19 2.750~ ~ "-~ ~ 74.385 Q PROM 1.5e30E=0s 10 LT.OR.EW. 1.8238E=ce 23 3.329 77.713 FROM 1.8238E=04 TU LT.uM.EU. 2.1262E=0* 28 e.052 81.766 - - ' ' ~
~ ~ FROM ~ 2.1282E=0e ~ 70 LT.OR.EQ. 2.4833E=0e 21 3.039 84.805 Q FROM 2.4833E=0e TU LT.ON.EU. ,2.8977E=04 16 2.315 87.120 FROM 2.8977E=0e 70 LT.OR.EO. 3.3813E=0e le 2.026 89.1e6 - ~~ ~ ~ ~ ~
FROM~~~3.3813E=04-~TO LT.OR.EQi- 3.9e55E=0e 25 3.618~ ~ ~~~' 92.764 p FNUM 3.9455E=0e TO LY.UN.EO. e.60e0E=0e 16 2.315 95.0e0 l PROM s.6040E Oe Tu LT.Op.te. 5.3722E=0e 15 2.171 97.250 FROM 5.3722E=0e TO LT.02.EU. 6.2ne7E=os 15 2.171 99.421 h FROM 6.2687E=0e TO LT.OR.EQ. 7.3148E=04 2 259 99.711 FROM 7.314RE=ce TU LT.0M.EG. 8.4451E=0e 2 .289 100.000 , TuisL 691 . NUNNEN OF ZERO ENTRIES 7799 MIN NUMBEM OF %AllD 065tRwaTIONS PEN avERaulus INTERv1L = 1
~
50.00 PENCENT Pu!NI 6.737E=ub 55.00 PENCEN] POINI 9.6s7E=05
~~ '00.00 PERCENT Pu1NT 9.8s6t=05 e5.00 PENCENT POINT 9.921E =US 70.00 PENCENT Pul4T 1.171E=ue 75.99 PENCEN1 PolnT 1.630E=us 80.00 PEkCEnf pu!NT 1.939t=9e e5.00 PENCEM) POINT 2.553E=ne 90.u0 PEWCENT PUINI 3.ee2t=U4 95,00 PENCEnl PUINT e.531E=04 92.o3 PEWCENT PUIMI 3.936t=ve (Nkt TECMNICAL PustTION = RELATIVE CONCENTNa110m PHOBAstLIlf) ,
b __._ _ ___ . . ~ . - ~ _ _ _ _ _ _ _ _ _ _ _
8EICON (ATr.US?NESIC OI5?EW31GN F03 DN EviLUATIONS) = YANREE AIUMIC ELECTNIC CO lt0D 03. u7/24/78) 11/2VFD Pabt 29 My 1977 12 00NTM5 = GRuuND=LEvtl NELEASE = vt.21tBLES MEPLACED = EXCLUSION ANEa O
' DONNw!ND SECTOR E5E DELTA =T STAeILITY "UDLL QAMMA CMI/O 18EC/M3) = __
PkUSABIL!iY DISTRIBUTIONS 0(N(TER8)'~s O i 610!O ~~~ SECTOR AVENAGE WALUES = t=HUUN AVERAGES 1 _ ,i FREQUENCY DISTRIBUTION RANGE O NUMBER OF PERCENT OF Os3ERVATIONS CUMULATIVE - --- TOTAL 063 FERCENT FR04 3
~
FC07 ~ '.409eE=06~~ 70 LT.ON.EQ.~ 3.749 6E=06 - 3.7496E=o6 2 269 FIO4 70 LY.OR.EQ. 4.1238E=06 9 289 4.123BE=06 TO LT.uW.Eu. 4.5353E=06 1.3u2 1.592 701 4.5353E=06 TO LT.OR.EU. 8 1.15e ' FCUA 4.9879E=06 12 2.750 e.9879E=06 TU LT.09.EQ. 5.4857E=06 1.737 4.486 - ~ FCOM 5.e857E=06 9 10 LT.04.EQ. 6.0332E=06 1.302 5.789 26 3.763 7 F ROJ~~6. 0332E = 06 ^ 70'LT.ON.EO.~ 6.'6353E=06 Fron 24
~' - ~
9.551 6.6353E=06 70 LT.ON.EW. 7.2975E=06 3.473 13.025 -
~ - ~
FROM 7.2975E=06 70 LT.OR.EQ. 8.0257E=06 33 e.776 FCO3 8.0257t=06 70 LT.ON.EQ. 8.8266E=06 28 17.600 ' a.052 21.552 FCra 8.8266E=06 70 LT.04.Eu. 9.7075E=06 38 5.J99 FROM 9,7975E=06 TO LT.UN,EQ, 37 27.352 ~
~ ~ ~ ~ - -
1.0676E=05 24 5.355 32.706 FRoa 1.0676E=05 - To LT.OR.EQ. 1.1742E=05 FCOM 1.1782E=05 70 LT.Od.EW. 1.291eE=05 35
~
3.873 ~ 36.179 5.065 ~ 41.245 ~~ FNOM 1.2914E=05 Tu LT.ON.EU. 1.4202E=05 30 4.382 FRDa 25 45.586 FR03 1.4202E=05 TO LT.OR.EG. 1.5620E=05 to 3.618 49.20e () 1.5620E=05 TO LT.OR.EW. 1.7178E=o5 2.894 52.096 FC07 1.7178E=05 TO LT.09.EG. 1.8893E=05 19 2.750 31 54.848 O FC04'- 1.8893E=05 4.4e6 FEO 2.0778E=05 7 TU 0~LT.0R.EQ.^ 2.'0778E=05 23 59.334
~
FEUM LT.Ud.Eu. 2.2852E=05 29 3.329 62.663 2.2852E=05 TO LT.OR.EQ. 2.5132E=05 4.197 66.860 13 1.881 C)
- FZM-FCOM 2.5132E=05 TO LT.OR.EG. 2.7640E=05 2.7640E=05 Tu LT.ON.EU. 3.0399E=U5 16 68.7e1 FROM 15 2.315 71.056 ~
3.0399E=05 TO LT.ON.EQ. 3 3432E=05 2.171 73.227 F10M7;3432E=05-~TO LT.OR.EQ.~ 3.6769E=05 ~ FIOM 12 19 ~~ - 3.737 74.964 () 3.6769E=05 TU LT.ON.EQ. 4.0438E=05 2.750 ~77.713 FCOM a.0438E=05 TU LT.0W.Eu. a.ae7eE=05 20 2.894
~~~ FCOM 19 60.608 a.4474E=05 To LT.OR.EW. 4.8912E=05 2.75u e3.357 (;
FEOM 4.8912E=05 TU LT.OR.EQ. 5.3793E=05 to 2.605 FCOa 18 65.962 -
~~ ~ F204 5.3793E=05 70 LT.OR.EQ. 5.9162E=05 25 2.605 88.567 Ft03 5.9162E=05 TO LT.OR.EQ.'~6 5066E=05 18 -
3.618 92.165 s) 6.5066E=05 Tu LT.OR.Ew. 7.1559E=05 2.605 - 94.790' 20
-~
FCOM 7.1559E=05 Tu LY.OR.EQ. 7.87u1E=05 2.894 FCOM 7.8701E=05 TO LT.OR.EQ. 8.6555E=05 to 97.685 FruM 1.e47 99.132 _ 8.6555E=05 TO LT.0W.Eu. 9.5193E=o5 2 .289 2 289 99.421 FLOM_ _9.5193E=05 TO LT.OR.EQ. 1.0403E=04 99.711 2 289 ss tou. coo TOTAL 691 . _ _ _ _ NUMBEW OF ZERO ENTRIES 7799 v M1h NuM8EH OF WALIO Oe3ENVATIONS PEN AvENAGING INTEHvat 1 s
--- 50.00 PERCENT PulNT 1.47et=05 60.00 PERCENT POINT 1.940t=o5 55.u0 PENCE NT POINT 1.733E=us a i
70.00 PENCENT Pu1NT 2.695t=u5 65.00 PERCENT POINT 2.166E=us -~ ) 80.00 PENCENT POINT 3.990t=05 75.00 PENCENT PuINT 3.3e5E=05
- 90.00 PENCENT PUINT 5.5elt=ob e5.00 PENCLN1 POINT 4.106E=u5 _
l 95.00 PENCENT Pu1NT 6.597E=05 , 92.63 PERCE N T POIN T 5.939t=05 (mWC IECHNICAL Pus! TION = l RtLaiIVE CuNCENiRATION Fwuts ab1L I T T J 3 s
SILICON (ATMOSPHERIC DISPEN810N FON D3A EwALUATION5) = vaNALE ATOMIC ELEC TRIC Cu (M00 03, 07/2e/78) 11/24/70 PAGE 30 '] DtLTA=T STadILITY MODEL 3 ; NY 1977 12 MONTHS = GROUND =LEVt(MELEa5E = var 149LES NEPLaCEu = EacLU310N ANEA __
-t DUw4mIMO SECTOR Sk GROUND
- LEVEL CHI /O (SEC/M3) - PRU6481LITY DISTRIsuTIUN5 ()
~~
OfMETERS) a 410.8 PLUML CENTERLIhE VALUES = 1=MUUR' AVERAGES i O'
^
CUMULATIVE
~ ~'
FREGUENCY DISTRIBUTION' RANGE NUMBER OF PERCENT OF 06SLNVATIONS TOTAL 088 .PENCENT' O ,
~275
^
FC04 1.7507E=06 TU LT.UR.EG. 2.0882E=06'~ 3 275 i PMUM 2.0882E=06 TO LT.ON.EO. 2.4906E=o6 0 0.000 275 C) 1. PROM 2.97u7E=06 0 0.000 275 ~-
-l ~~ FRO 3~2.9707E=06 2.4906E=06~ TO LT.OR.EG. TO LT.OR.EW. 3.5432E=06 1 092 367 1 FK01 3.5432E=06 ~70 LT.ON.EO. 4.2261E=06 0 0.000 3e7 O~I FKO4 e,2261E=06_TO LT,0R,E9u 5 t eeU72 06 2 _,183 ,550 ., _ l F00M 5.0407E=04 TO LT.OR.EO. 6.0122E=0* 6 550 _.1.100 642 1.7e2 ~ C) . !,
FKUM ' 6.0122E=06 TO LT.OR.EG. 7.1709E=06 7 FROM 7.1709E=06 70 LT.OR.EG. 8.5530E=ce 2 183 1.925 ' ~ - - t
~ FK04 ~'~8.5530E=06 TO LT.ON.EO. 1.0202E=05 12 1.100 3.025 !
FROM 1.0202E=v5 TO LT.OR.EU. 1.2168E=05 18 1.450- 4:*75 *
. C) t PROM 13 2168E=05 _T0_LT.0R,EGu t.e513E=05 .
8 733 5.408 ? 1.7310E=c5 '23 2.108 7.51e FE04 FKon 1.4513E=05 Tu L).OR.Eo, 1.7310E=05 TO LT.OR.EO.- 2.06eeE=05 le 1.283 8.799 () -[- FKOM 2.06e6E=05 TU LT.ON.EU. 2.e625E=05 38 3.463 '12.282 'I
~ FROM ~2.4625E=05 '70 LT.OR.EG.
2.9372E=05 65 5.958 18.240 ~ ~ ~~- 7 .i-FK04 2.9372E=05 Tu LT.OR.EG. 3.5033E=05 81 7.424 25.665 C) PEON 3.5033E=05 TO LT.04.EW. e.1785E=05 120 10.999 36.66e ~~ ~ -
-- FR0n 47. 735Ea05~ TOTT.0R.EO. e.9836E=oS~ ~ - ~ 79 ~ '-' -'7.241~ ~ ~ ~ ~~~ ~ e 3.9 05 FROM e.9838E=05 TO LT.OR.LO. 5.9444E=05 67 6.let 50.046 - C) '
FROJ4 5.9es4E=05 To a.T.UR.EO. 7.0900E=05 70 6.416 56.462 i 4
-- FROM-~7.0900E=05' TO LT.OR.Eo, 844565E=05 50 e.583 61.045 .:
FE02 8.45611=05 70 LT.0R.EW. 1.0086E=ce 151 13.881 74.885 E) 1-FROM l t00864=ce TO LT.OR.EU. 1.2030E=0e 26- 2.383 - 77.269 ' FROM 1.4030tac e TOTT.04.EQ. 1;4349Ea04 ~ ~ ~ ~ 18 - ~1.650 78.918' FROM 1.eleW=0e TO L1,0R.E9 1.7115E=0e le 1.650 80.568 Q' FRO?I 1.7115t=0e Tu LT.ON.EW. 2.0e13E=ce 30 2.750 83.318 2.475 85.793 FOOT '2.0413E=i ~ TO LT.UR.EQ.~~24 ele 8E=0e i 27 FROM 2.e348E=wn 70 t.T.ON.EG. 2.9040E=0e 23 2.108 87.901 Q F704 2.9040E=04 TU LT.04.EG. 31 2.841 90.742 ~ ~ ~ FROM 3;8637E=0e70~CT.OR.EQ; 3.4637E=0e 4.1313E=04 ~ - - ~ ^ -- ~ ~ 3 5 ~ ~ -~ ~ ~"3.208J~ 93.951 FNOM e.1313E=0e TU LT.ON.EG. e.9276E=0e 26 2.383 96.334 ss l FROM e.927eE=ue TO LT.ON.EU. 5.8773t-ce 17 1.556 97.892 FRom 5.8773E=ce TU LT.ON.EO. 7.0101E=0e 11 1.006 98.900 FROM 7.0101E=ce 70 LT.0M.E9 8.3612E=0e 6 . 550 99.450 sj i FROM 8.3612E=0e TU LT.ON.EG. 9.8561E=0e 6 550 '100.000 _ 70fAL 1991 se huMbER OF ZERU LNIRIE8 1399 MIN Num8EN OF VALID ueSLRv&TIONS PER AVERAGING 1hiENVAL m. 1 v v ! 50.00 PERCENT PUINT 5.933t=05 55.90 PEHCENT POINT 6.77M-05 ~
~ ~~60.09 PERCF4T POINT 8.02et=05 65.00 PENCtN1 POINT 9.655E=05 j 70.00 PERCENT Pu!NT 9.933t=ub 75.00 PENCtNT PUINT 1.016E=ve i 80.00 PtWCENT Pu!N1 1.e3et=ue 95.de Pt>Cthi POINT 2.33eE=De 90.00 PERCENT POINT 3.285L-de 95.00 PENCENT'Pulhi 4.395E=0e 95.33 PERCENT POINT 4,653L=Ue (reW C TECMNILAL POSITIUN = NELATIVE CONCEhTNATIUN PHusas1LITV). _
J
.- r 8.n1 CON (Afr08PMENIC DISPENSION FOR D3A EvcLUaTIONS) = YANREE A10MIC ELECTRIC CU (Mou 93 u7/24/78) Intd4/78 PAGE 31
~
__ , NY 1977 12 auhTN8 = GROUND = LEVEL NELEASE = VARIABLES MEPLaCED = EECLU310N AREA
-Q l .
DELia-T Stas 1LITY.MUDEL ,__ t 3 DumNw!ND SLCTOR SE GAMMA CHI /O taEC/m3) = PMU8ASIL!iY DIB1418UTIONS
~ ~
O ! 6(METERS)~e 610.'O ~5ECTum AVERAGE VALUES = - 1=HUuR AVERAGES
~ ~~ '~ ~ ~
' ' ~ ~
0l FREQUENCY DISTRIBUTION RANGE NUMBER OF PERCENT OF CUMULATIVE
' ~ - ~ ~
08SERVATIONS TOTAL 088 PENCENT
~
~ ~~
~ '~
FCOM 23386E=06 TU LT.UN.EG. 2.3930E=06 ~ ~ 3- ~ ~ ' ~ ^ ~'.275-~~ 275 FCOM 2.3930E=06 70 L1.OR.EO. 2.677eE=06 0 0.000 275 ' FCOM ~ 2.677eE=06 TO LT.UR.E9 2.996tE=06 0 0.000 275 e FROM 2.9961E=06 TO LT UR.EO. 3.3525E=06 2 183 458 l' FCOM FCO:1 3.3525E=06 10 LT.OR.EW. 3.7513E=06 3,7513E=06 70 LT.OR.EG. 4.197eE=06 - 17 6 550 1.558 1.006 2.566
) ,
F Koi--~4.19 7 6 E = 0 6 Tu LT.0H.EO. 4 .6969E=06 26 ' -' 2. 3 8 3 " ~ ~ ~ ~~ 4.950
- ~ ~ ~ ~
FE03 4.6969E=06 TU LT.OR.Eu. 5.255eE=06 38 3.483 FROM 5.2556E=06 TO LT.OM.EG. 5.8808E=0e 53 8.433 ? 4.858 13.291 l
'FROM 5.8408E=06 .TO LT.ON.EG. 6.5803E=06 63 5.775
~
19.965 FC04 6.5803E=06 TO LT.OR,EG. 7.3631E=0e 78 7.149 26.214 C? FCOM 7,363tE=06 TU LT.ON.Eu, 4.2389E=on 93 8.524 34.739 l FROM-~-4.2389E=06~TD TT.04.EQ.9;2190E=06 ~ ~ ~ ^ 91 ~- 8.341 ~~ 43.080
~ ~ ~ ~
FNOM 9.2190E=06 TU LT.ON.EO. 1.031ef=05 58 5.316 48.396 C) FCua 1.0316E=05 TU LT.OR.EW. 1.1543E=05 56 5.133
~ ~ FNON' 1.1543E=05 fu LT.OR.Eu. 1.2916E=05 53.529 40 3.666 57.195-
~ ~ ~
FROM 1.2916E=05 To LT.OR.EW. 1.4452E=05 45 4.125 61.320 FCOM 1.4452E=05 TU LT.04.EG. 1.617tE=05 38 O l 3.483 -~ ~ 64.803 ' . FRO F 13171E=05 7 0'LT.OR.EQ;~~1;8095E=05~ ~ 34 3.116' e7.919 ' FEUM 1.8095E=05 TO Lt.ON.EO. 2.024FE=05 30 2.750 70.ne9 C) FRUM 2.0247E=05 TO LT.OR.EO. 2.2e56E=05 29 2.658 73.327 t ~~ ~ FCOM 2.2656E=05 70 LT.ON.EG. 2.535tE=05 16 1.467 .74.79t
~~
FZO3 2.535tE=05 TO LT.ON.EO. 2.836eE=05 18 1.650 (y 76.4sn t FCOM 2.8366E=05 10 LT.OR.EG. 3.174tE=05 23 2.108 78.552 FC0a 3.174tE=05 TOTT.0R;EO. 3;551eE=05 ~ '3.208 ~ ~ ~' I 35 ~~~81.760 ~' FCOM 3.5516E=05 70 LT.ON.EG. 3.974tE=05 27 2.475 84.235 C)
~FMUN 3.9741E=05 TU LT.0R.EG. 4.4469F=05 31 2.841 l~
~~FCOM 87.076 ,
4.4469E=05 10 LT.OR.EQ. 4.9758E=05 29 2.658 89.734 FC04 4.9758E=05 70 LT.OM.EG. 5.5677E=05 22 2.016 91.751 V FCOM 5.567FE=05 TU LT.OR.EU. 6.2300E=05 25 2.291 94.042 i PC0 F 6.2300E=05 ^TO LT.OR.EW E L 971tE=05 18 1.650' 95.692 ~ ~
' ~
l FCU" 6.97ttE=05 TO Lt.ON.Eu. 7.8003E=05 21 1.925 97.617 l FRUM 7.8003E 95 TO LT.UR.EO. 8.7282E=05 13 1.192 98.808 FRUM 8.7282E=05 70 LT.UN.EQ. 9.7665E=05 5 458 99.267 l FROM 9.7465E=05 TO LT.OR.EU. 1.0928E=04 3 275 99.542 ~ l FC03 1.0928E=04 TO L1.UR.EG. 1.213fE=ce 5 458 100.000 l l T01st 1991 se NU9eER OF ZERU ENTRIES 7399 MIN NUM8Eh UF WALIO 08SERVATIONS ped avEhaGING INTEHvaL a 1 a
~~'
50.00 PERCENT POINT 1.064E=05 55.00 PEMCENT PUINT 1.d14E=05 60.00 PERCENT POINT 1.406E=o5 65.00 PEMCE'vT POINT 1.631E=05
~~
70.00 PthCtNT pulNT 1.966t=d5 75.00 PENCENT PUINT 2.57CE=US %> 8u.v0 PERCtml PUINT 3.319t=o5 -85.00 PEMCENT PulNT 4.06uE=05 90.00 PERCENT POINT 5.05uE=05 95.00 PENCENT POINT 6.361E=05
~
v 95.33 PENCENT PUINT 6.641t=US (NRC 1ECHNICaL PU31 TION = NELATIVE CUNCLNTNaTION PNU8asIL11T) _. l
,)
_ _ _ _ _ _ _ _ _ _ _ __ _ _ _ _ _ _ _ _ _ _ _ . _ . _ . ___ _ _. .~ . . ._. ., . . _ . . .,, _ . .~ , _ _ _ _ _ ,
a9 8K,10uN (cTMUS?MEd1C 015PECSION PU3 D;A EW4LuaTION5) = YANAEE ATOMIC ELtCTNIC CO (MOD 03, 07/24/78) 11/2C/70 PAGE 32
~
,mv 1977 12 wuNTM5 = GNouND=LEVtt NELEASE = vaNIa6LES MEPLaCEO = EXCLU5 ION area otLTa-T 5TaBILITY MOOLL '
00mNnIND SECTOR stE GRouhD= LEVEL CMI/W (SEC/M3) = PRUBASILITY DISTRIduTIUNS c) i
~
0(METEN8) e~ ~ 610.0 " PLUME CENTERLINE VALUES =
!= HOUR AVERabES i
n, FREGUENCY DISTRIBUTION RANGt NUMBER OF PENCENT OF CUMULATIVL
~
Od8ENVAT10N8 TOTAL 083 PENCEN1 7 F;0M ' 1.8115E=06 TO'LT.OR.EQ.--2.1695E=06 3 375 375 FROM 2.1695E=06 TO LT.OR.EU. 2.5904E=06 0 0.000 375 C) FZOM 2,598eE=06 TU LT.ON,Eu, 3.1120t=06 0 0.000 .375 F201 3.1120E=06 To LT.ON.Eu. 3. 7 a? 71 E =0 6 0 0.000 375 FCOM 3.7271E=06 TO LT.ON.EG. e.e638E=06 0 0.000 375 'O FC01 _ e,4630E=06_. TU LT,0R.Eu.__5.3462E=06 2 250 624 FROM 5.3462E=06 70 LT.0W.EO. 6.4029E=06 2 250 .b74 FIOA 6.4u29E=06 TO LT.ON.EW. 7.6686E=06 4 499 PEUM 1.373 ~) 7.6686E=06 TU LT.DN.EW. 9.1deeE=06 2 .250 1.623 FZOM 9.leseE=06 Tu LT.UN.EQ. 1.1000E=05 1 .125 1.748 FZUM 1.1000E=OS To LT.02.EQ. 1.3174E=05 125 FCOM ~~ 1,3174E=05 70 LT,0N.EG, ~1.5778F=05 1 1.873 ^ 8 999 2.871 FCOM 1.5778E=05 Tu LT.OR.EU. 1;e897E=05'- e .e99 3.371 F 01 1.8897E=05 TU LT.UR.EG. 2.2632E=o5 R 999 4.37u 7 FPUM 2.2632E=05 Tu LT.ON.EW. 2.71utE=05 8 999 F;03 5.368 2.7106E=05 TU LT.OR.EU. 3.2464E=05 23 2.871 8.240
-~~
FCOM 3.2464E=05 10 LT.ON.EQ. 3.BeetE=05 !$ 6.866 15.106 ' FIO1 3 TO LT 04 EQ. 4.6566E=05 ~ *= 5.993 UO r e,8881E=05 6566E=os TO LT.ON.EG. 5;5771E=05
~ 21.099 58 7.241 28.340 FIOm 5.5771E=05 TO LT.uM.EG. 6.6795E=05 83 FNOM 10.362 38.702 C; 6.6795E=05 TU LT.OR.Eu, 7.9998E=US 57 7.116 45.818
'FCOM 7.9998E=05 TO LT.OR.EQ. 9.5610E=05 35 F201 a.370 50.187
~ -~
9.5810E=05 TU LT.OR.EO. 1.1475E=04 108 13.483 63.670 F;UM 1.1475E=0e TU LT.OR.EW. 1.3743E=0e-~ ~~~ 17 2.122 65.793 Ol FR03 ~~ ~ ~~
~~ 19 2.372'
^~~
1.3 7 4 3 E = 0 470~CT. 0 R . E Q .~- 1.~ 6 e 6 0 E = 0 4
~
FZOM 68.165 1.6460E=ce TO LT.ON.EW. 1.9713E=04 40 e.994 73.159 F;01 1.9713E=0e TU LT.ON.EW. 2.3610E=0e 26 s) F001 3.246 76.404 2.3610E=ce 70 LT.OR.EQ. 2.8277E=04 22 2.747 79.151
' ~ - ~ ~
PROM 2.8277E=ce 70 LT.ON.EG. 3.3866E=ou 35 FIUM 4.370 83.521 () 3.3866E=ce 10 LT.ON.EO. 4.0560E=0e ' 37 a.619 88.140 FROM 4. 0560E 0470 LT uN.EQ.
= . e.8577E=04 33 ~~ e,120 - 92.260 FNOM 4.8577E=04 TO LT.ON.EW. 5.8179E=04 FNOM 31 3.870 96,130 w, 5.8179E=ce TO Lt.ON.EG. 6.9679E=0e 27 2.747 96.676 F;0M 6.9679E=04 10 LT.ON.Eu. 8.3453E=04 5 624 99.501
~~
FtuM 8.3453E=0e TU LT.ON.EQ. 9.9946E=04 2 250 99.750 ss _ FCOM_. 9.9948E=04 TO LT.ON.EW. 1.te27t=03 2 250 190.000 ..__. _ _ THTAL But v NUMBER OF ZENU LNTRIES 7669 plN NU" BEN UF WaLID 055tNWAI!UNS PEN aVtRAGING INTENVaL a 1 50.00 PENCENT PUINT 9.53eE=u5 v - - ~ ~ ~ 55.0u PENCtN1 PulNT 9.o66E=us 60.00 PERCENT pu1NT 9.92at=05 65.00 PENCENT POINT 1.247E=04 -- 70.00 PtNCENT Pu1NT 1.e2cE=ou 75.00 PEHttNT PUINT 2.141E=c4 Mo.00 PtpCENT PUINT 2.938t=ue 3.79tE=0e 85.00 PtwCtNT PUInf 90.00 PENCEmi PUIN1 4.20st=O4 95.00 PENCENT PulNT 5.391t=ue 93.64 PENCEN1 PUINT 5.129E=U# (NWC IECHNICal PusIT10N = NLLATIbE CUNCENINATION PNub4ftlLITYJ
I SnITON (ATMOSPMERIL DISPENSION FUM ODA EVALUATIONS) = YAN%EE ATunIC ELECTRIC CO LMOD 03, 07/24/76) 11/24/76 P t4 E 33 O
.MY 1977 12 MONTH 3 = GROUND LEVtL NELEa3E = vaRiaWLES MLPLACtp = EXCLUSION aHEA DLLIA=T SIABILITY MUDEL __
DuhNnIwD SECTLW SSE GAMMA CNI/W (SEC/M3) = PHUBABILITY DISTRIBUTIONS O , D(METDis) e --610.0 SECTOR ~ AVERAGE VALUES = !=HuuR AVERAGES
~ '~
O FREQUENCY DISTRIBUTION RANGE NUMBER OF PtRCENT OF CUMULATIVE 085ENVATIONS TOTAL 083 PEHLENT FROM2,2127E=06 70~LT.0w.EO. 3 ' - -- ~
~
2.4662E=06 375 375 F2On 2.4862E=06 Tu LT.OR.EU. 2.793eE=06 0 0.000 .375 FLO4 2.793sE=o6 TU LT.ON.tu. 3.1366E=u6 0 0.000 .375 FZOM 3.1386E=06 70 LT.OR.EG. 3.5265E=ue 2 250 624
- ~ -
F;03 3.5265E=06 TO LT.OR.EQ. 3 9e23E=06 3 .375 999 T FCOM 3.9623E=06 TU LT.ON.EU. e.e520E=06 2 250 - 1.248 - FCO3 4.4520E=06 TO IT;0R.EQ.- 5;0022E=06' - ~ 6 749 1.998 FC0a 5.0022E=06 TU LT.OR.EO. 5.6203E=06 9 1.124 3.121 7 FCua 5.6203E=06 TO LT.UR.EG. 6.3149t=06 le 1.7e8 4.869 6.3149E=06 70 LT.OR.EO. 7.0953E=06 FR03 21 2.622 7.491 FIOM 7.0953E=06 70 LT.UR.EQ. 7.9721E=06 38 e.744 12.235 ? FROM 7.9721E=06 TO LT.OR.EO. 8.9573E=06 63 - 7.865--~ 20.100 FROM-- 8.9 57 3E= 0 6 10 LT.09.EQ.~ 1;0068E=05
~
4.994 e0 25.094 FN01 1.006eE=05 70 LT.ON.EW. 1.1306E=05 56 6.991 32.085 C FHun 1.1308E=05 To LT.ON.EU. 1,2705E=05 51 6.367 38.452 1.2705E=05 70 LT.0R.E9 1 4275E=05 FROM 36 4.494 42.946 Fi.0M 1.4275E=05 Tu LT.OR.EQ. 1.6040E=05 26 3.2e6 e6.192 C; FC07 1.6040E=05 TO LT.OR.EQ. 1.8022E=05 31 -- 3.870 50.062 ~ s FROM 1.8022E=05 TO LT.OR,EQ. 2;0249E=05~ 36 4.494 54.557 - FLO3 2.0289E=05 70 LT.OR.tu. 2.2751E=05 36 4.494 59.051 C) FION 2,2751E=05 Tu LT.ON.EQ. 2 5563E=05 25 3.121 62.172 - ~ ~ F103 ' 2.5563E=05 TO LT.OR.EQ. 2.8722E=05 3.870 31 66.042 FC04 2.8722E=05 Tu LT.UN.EG. 3.2271E=05 28 3.496 69.538 O' FZOM 3t2271E=05 70 LT.OR.EQ. 3.6259E=05 23 2.671 72.409 '
-~ ~3.620~~ ~~
~ ~ ~ ~ -
FROM 3. 6259 E=0570 EOR.E Q.~- 4. c 74 0 E = 05 ---- ~~29--- ~~ ~~ 76.030 FROJ 4.0740E=05 10 LT.uk.EQ. e.5775E=05 26 3.246 79.276 L) FCOM e.5775E=05 Tu LT.OR.EG. 5.1432E=05 36 4.49e 83.770 ' ' - ~ ~ ~ FLOM 5.1432E=05 TO LT.OR.EQ. 5.7788E=05 24 2.996 86.767 ' FIUM 5.7788E=05 Tu LT.OR.EW. 6.e929E=05 33 4.120 90.886 () FCOM 6.e929E=05 To LT.OR.EQ. 7.2953E=05 35 4.370 95.256 7J0 F 7.2953E=05 TU LT.OR.FQ;~ 8;1968E=05 ~~ 16 -- ~ ~ ~ ~ 1.998
~ 9 7. 2 53 ~~ ~
FIUM 8.1968E=05 TO LT.OR.Eb. 9.2098E=05 to 1.248 98.502 L) F;04 9.2096E=05 Tu LT.0W.EG. 1.03eoE=ce 7 874 99.376 375 FROM 1.0346E=0e 70 LT.OR.EQ. 1.1627E=0e 3 99.750 F h'ua 1.1627E=ce TU LT.ON.EW. 1.3064E=ce 0 0.000 99.750 ss F;0M_ ..._ 1.306eE=ce Tu L.T.0M.EQ. 1.e56eE=0e 2 250 100.uco - TOTAL 501 ss NUMBER OF ZEHu ENTHIES 7689 MIN NUMBER OF VALID OBSLRVATIONS PEN AVERAGING INTtMVAL
- 1
-~ 50.00 PERCLNT PUINT 1.786t=05 55.00 PtHCLNT POINT 2.047E=05 - 60.00 PERCENT Pd1NT 2.387E=05 65.00 PERCtNT POINT 2.798E=US 70.00 PENCtNT PUINT 3.30Pt-95 75.00 PENCENT PUINI 3.957E=05 8u.00 PtkCENT PUINT e.7u7t=o5 85.U0 PtHCtNT POINT 5.418E=95 6.358t=05 90.00 PLNCENT PUINI 95.00 PENCLN1 POINT 7.28eE=u$ 93.60 PtWCEwi PUINT 7. Deut =05 (NHL TtCHN] Cal PO3!! ION = HELATIVt CONCENTRATION PROBaulLITV) _
- sus'
_m___._ __ _ -
8M NUN taTMuSPMEWIC DISPEASION F02 Dea Evaluations) = YANMEE ATOMIC ELECTNIC Cu tMuu U3 07/2e/78) 11/24/78 pal E 33 MY 1977 12 MONTH 5 = GHOUND= LEVEL MELE ASE = W ANI At9LES NEPL ACED = EACLUSION ANEA DELIA-T StaaILITY MODEL G I DOWNm!ND SECTOR 8 GNOUND= LEVEL CHI /O (SEC/M3) i
=
PRu8A81LITY DI57RIBUT1uN5 OfMETERS) a O[ 610.0 PLUME CENTERLINE VALUES = 1 HOUM AVERAGE 8 ~ O FMEQUENCY DISTNIBUTION RANGE quMMER OF PEhLENT OF "- CUMULATIVE I 083ERVATIONS TOTAL 065 PENCENT C) . FCO I 2.1032E=06 TO LT.OR.EG. 2.8903E=06 1 147 .te7 I F;U2 2.4903E=06 TO LT.04.to. 2.9486E=06 FC01 0 0.000 147 O!
-"FROM ~ 2,9e86E=06 Tu LT.ON.EQ. 3.e912E=06 0 0.000 107 3.e*12E=06 TO LT.ON.EU. 4.1336E=06 0 0.000 147 7.
FCOM 4.1336E=06 Tu LT.OR.EU. 4.89e3E=06 0 0.000 147 FC04 _ e,8943E=06 _TO.LT,0N,EQ,__5.79e9E=06 _ 0 0.000 ,te7 () l 1 FNOM 5.7949E=06 TO LT.ON.EU. 6.8613E=06 0 0.000 147 FROM 6.8613E=06 10 LT UN.EQ. 8.1239E=06 FROM 8.123eE=06 fu LT.UN.EU. 9.6189E=06 0 0.000 .te7 Ol 0 0.000 .147 FROM 9.6189E=06 TO LT.ON.EG. 1.1389E=05 i FCOM 1.1389E=05 To LT.0M.EG. 1.3ee5E=05 0 0.000 147
~ ~~
j 0 0.000 107 FrDa 1,3885E=05 TD T,0R.EG O; PRO F t.5966Ee05 1.5966E=05~ TO~(T.0R.EQ,~t.890eE=05 L 0 0,000 147 FCOM
. 1 147 295 1.890eE=05 TO LT.uM.EU. 2.2383E=05 6 88a FROM 2.2383E=05 1.178 O 70 LT.04.dQ. 2.6502E=05 0 0.000 1.17A
~~~FR04 '2.6502E=05 70 LT.ON.EG. 3.1379E=05 7 1.031 2.209 FCOM -3.1379E=05 To LT.OR.EO. 3.7154E=05 37 5.849 i FEON 3,715eE=05 fu LT.ON.EG. 4.3991E=05 7.658 O a2 6.186 PROM 4.399tE=05 Tu LT.ON.EQ. 5.~2u86E=05'
~
-- 29 ~ ~
~ ~-
-13.6es ~ ~ ~
F 04 5.2086E=05 4.271' 18.115
~
Tu LT.ON.EQ. 6 1671E=05 53 7.806 25.920 FCOM 6.1671E=05 70 LT.UR.EU. 7.3020E=05 90 13.255 () i
~ ~PC0a 39.115 '
7.3020E=05 TO LT.OR.EQ. 8.6e57E=05 28 a.124 43.299 FIOM 8.6457E=05 Tu LT.0R.E9 1.0d37E=04 121 FION 1,0237E=04 TO LT 17.620 61.119 C) ! 28 e.124 65.243 FROM 1.2120Ee04 TU CT,UR.EW,~1.2120E=ce .ua.Eu. 1.e351E=ce 23 - ~~ '- --^3.387 ~ ~" ' 66.630 --' ~ ~ ~ - "
~
FROM 1.435tE=ce Tu LT.ON.EG. 1.6992E=ce 15 2.209 FNOM 1.6992E=0e Tu LT.ON.EU. 2.0119E.De 70.839 C) 42 6.166 77.025
' #dO4 ~~2.0119E=0e 70 LT.OR.EQ.' 2.3821E=ce 16 2.356 79.381 - ' - -
FE07 2.3821E=ce fu LT.ON.EQ. 2.82USE=0e FECM 2,8205E=0e TO LT 17 2.50s 81.885 () 3.3395E=0e 2e 3.535 85.e20 FROM 3. 3 39 5 E40 e70 T T.,0N. E G . 3.95e0E=04-- - 04.EQ.~ 18 ~2.651 PCU4 3.95e0E=0e 10 LT.ON.EW. 4 6816E=0e 88.071 26 3.829 91.900 FROM 4.6816(=0e TO LT.ON.EG. 5.5e32E=ce 2e 3.535 () FROM 95.e34 5.5432E=0e~ TO LT.OR.EG.~~6.5632E=0e le 2.062 97.e96 FCOM 6.5632E=04 70 LT.OR.EO. 7.7710E=04 11 1.620 99.116 V _ FROM 7,7710E=08 70 @ R,EG. 9.098cE=ce , s 884 100.000 , I j TUTAL 679 U i NUN 8ER OF ZERO ENTRIES 7811 h!N NUMdER OF VALID ONSERVATIONS PER AVERAGIkG INTERVAL e 1
- ~ ' '
i i 50.00 PENCENT POINT 9.921E=u5 55.00 PENCENT POINT v
- 9.961E=05 ;
6 0i O O'P ER C E NT~Pu!N T--~ 1. 0 0 0 E =0 4 65.00 PERCENT POINT ~ 1.201E=ce
~ ~
l 70.00 PENCENT POINT 1.483E=ce 75.00 PENCENT POINT 1.89aE=ce i 80.00 PENCENT POINT 2.570E=ce 85.00 PENCENT POINT v 3.3 tee =0e
~~~~~ ~ ~ ' 90.0 0 PERCE NT POINT 4.208E=0e 95.00 PENCENT POINT 5.394E=0e 92.50 PERCENT Pu!NT _ 4.712E=ce tukt TECHNICAL PUSITIUN =
RELATIVE CONCENTNATION PROBAMILITT)
~
f
441004 (ATMOSPNENIC DISPERSION FOR D#4 EVALUATIONS) ~ YANREE ATOMIC ELECTRIC Cu (MOD v3. 07/2e/7C) 11/2e/76 Pai.E 35 l O i f3Y 1977 12 MONTH 3
- GNOUND= LEVEL MELEASE = vaNIaBLES HEPLaCEO = EXCLUSION ARtA DELTA =T STABILITY MODEL t 00nNnIND SECTOR 3 GAMMA CHI /u (SEC/M3) = PNUBABILITY DISIRieuTIONS O
- ~~
- -- ~ ~
O(METER 8)'~s 610T0 '8ECTuR AVERAGE VALUES ~. ~ 1=HDUR AVERAGES
~~
- - ~ ~ -
Oi FREQUENCY DISTRIBUTION RANsE NuM8ER OF PERCENT OF CUMULATIVE I OSSERVATIONS TOTAL uus. PERCENT 3 K0J 275692E=06 TO LT.OR.EQ. 2.8538E=06 ~ t ~- ~ .14 7 - -~ ~ ~~~'.147'
~ ~'
i FKUM 2.8538E=06 TO LT.OR.EO. 3.1699E=06 0 0.000 . 147 7 ! F;0M Tu LT.UN.EQ. 3.5211E=06 0 0.000 187 -l
-~FE03 ~~3.1699E=06 3.5211E=06 10 LT.OR.EG. 3 9111E=06 0 0.000 .147
' ~ ~ ~
l FE0a 3.9111E=06 TO LT.ON.EQ. 4.3se4E=06 1 147 295 ) ' FNun 4.3eseE=06 TO LT.OR.EU.
~ e.8257E=06 ^ 2 295 ~ ~ ~ ' - - ' -589 l e.8257E=06 TG LT.0H.EQ. 5.3603E=06
~ ~ ~ --
FROM 0 0.000 589 l Fh0M 5.3603E=06 TO LT.ON.EG. 5.9541E=06 1 .147 736 i ~ FRon TO LT.ON.EU. 6.6136E=06 5 736 1.473 FCD1' PT;0M 5.95etE=06-6.6136E=06 TO LT.OR.EQ. 7.3463E=06 20 2.946 a.418 7.3463E=06 Tu LT.OR.EW, 8.1601E=06 26 3.829 8.247 FCOM 8,1601E=06 TO LT.OR.EG. 33 4.860~-~~ 13.108 FA04 9.0641E=06-- TO LT.ON.EQ. 9.0641E=06~ ~~~~~ ~-~ 27 ~ ~ ~
~ ~
3.976 ~'17.088 l .~ 0 068E=05 FROM 1.0068E=05 Tu LT 3OR.EG. 1.118eE=05 28 4.124 21.208 7 FROM 1.118eE=US TO Lt ON.EQ. 1.2422E=05 e6 6.775 27.982 FROM ~1.2822E=05 To LT.OR.EG. 1.3799E=05 44 6.480 34.e62
~
FIOM 1.3799E=05 TO LT.ON.EQ. 1.5327E=05 51 7.511 41.973 C F;03 5327E=05 Tu LT.OR.EG. 1.7045E=05 35 5.155 1,7025E=05 TO TT.OR.EG. 47.128 rROM l .8911E=05 - ~
~~ ~~ -~
1 ~ - ~ ~ e2 6.186 - 53.314 FNOA 1.89ttE=05 Tu LT.ON.EG. 2.tuuoE=05 17 2.50s 55.817 C' FROM 2.1006E=05 To LT.OR.EQ. 2.3333E=05 29 4.271 e0.088 F;04^'2.3333E=05 TO LT.OR.EQ. 2.5918E=05 28 4.12e 64.212
~ - - -
F;0M 2.5918E=05 TO LT.OR.EQ. 2.8789E=05 26 3.829 68.041 C) ' FC01 2.8789E=05 TO LT.OR.EU. 3.1978E=05 16 2.356 70.398 rXOH7.1978E=0 5-~TOTT.02.EQ. 3.5521E=05' -~~- - - - - - 24- -- - - - 3.535 - ~~~73.932 ~ FR0m 3.5521E=05 To LT.OR.EO. 3.9456E=05 25 3.682 77.614 () FR0m 3.9456E=05 TO LT.Ok.EG. e.3527E=05 17 2.50m 80.1 ?
~ FE02 a.3827E=05 TO LT.OR.EQ. e.8682E=05 20 83.063
~~
FKon e.8682E'05 70 LT.OR.EG. 5.4075E=05 27 2.986 3.976
- 87.040 %)
FED:t 5.4075E=05 70 LT.0H.EQ g .0065E=056 18 2.651 89.691 F;0% 6.0 065E=05- TO LT.0R.EG. 676719 E = 05 '-
~ ~-
2 5 - -- ~~ ~ 3. 6 8 2 '--~~ -- - ~ ~ 9 3 . 3 7 3 - ~~ ~ ~ ~ FROM 6.6719E=05 TO LT.OR.EG. 7.4110E=05 20 2.946 96.318 _ FROM 7.4110E=05 TO LT.OR.EQ. 8.2320E=05 13 1.915 98.233 FE03~- 8.2320E=05 ~TO TT.OR.EG. 9.1439E=05 6 884 ~99.116 F%SG 9.le3*E=05 To LT.ON.EQ. 1.0157E=08 5 736 99.853 s) FROM 1,9157t=0e TO LT,0R,Eu. 1.1203E=04 1
.te? 100.000 TOTAL 679 g,) ~ ~ ~ - NUMBER OF ZERO ENTRIE8 7811 MIN NUMBER OF VALID OBSERVATION 3 PER AVERAEING INTERVAL e 1 U
50.00 PERCENT PUINT 1.815t=05 55.00 PENCENT POINT 2.072E=05 60.00 PERCENT POINT ~ ~2.312E=05 65.00 PERCENT POINT 2.674E=05 70.00 *ENCENT PUINT 3.12eE=us 75.00 PENCEN1 POINT 3.733E=05 s) 80.00 PERCENT POINT 4.328t=05 85.00 PENCENT POINT 5.195E=05 90.00 PERCENT POINT 6.06eEa05
~
95.00 PENCENT POINT 7.257E=05 Q 92.50 PERCENT Pu!NT 6.598e=u5 (NHC TECHNICAL PU5ITIUN = RELATIVE CONCENTHATION PRusa81LITV) _
8dI[GN (ATKUSPMENIC UISPENSIDM FUN ODA EVALUATIONS) = YAmaEE ATO3fC ELEC1NIC Cu (Muo 03 v7/24/78)
~ 11/24/78 PA6E 3a . ~~-g
_ _ _ yn 1977 12 Muh1MS = GNOUNU* LEVEL NELEASE = baHIA8LES HEPLACED = EaCLUSION ANEA t3 + DELTA =T STABIL11Y NuoEL ,_ 4 00eN41NO 8ECTOR 88m GNOUND= LEVEL CH1/u (SEC/M3) = PR08481LITV DISTNIBUTION8 CD 1 O'(METERS) a 610.8 plume CENTERLINE VALUES = t-HOUk AVENAGES l C) ?
' -~
. I i FREQUENCY DISTRieUT!uN MANGE NUNRER OF PERCENT OF CUMULATIVE ! ,
OBSERVATIONS TOTAL ObS. PENCENT () j
~
--~ PA03
~ ' ~ ~ ' -~~
1.1890E=05~~TU LT.OR.EG.~ ~ ~ ~1.338aE=05 1 290 200 'i FA04 1.338eE=05 TO LT.UN.EO. 1.5pieE=05 0 g.000 .200 t _FEU3__ 1,507eE=05 TU LT,0N.EG, 1.6975t=05 200 CD g- . 1 399 F203 1.6973E=05 To LT.OR.EQ. 1.9111E=05 200 599 1 l-FCOM 1.9111E=05 TO LT.ON.EO. 2.1519E=o5 0 0.000 -.599 CD i - LF;0M___2,1519E=05__Tu_ LT,0R,EG, _2.e230E=05 3 599 f1.198 ! F203 ! 2.e230E=05 10 LT.ON.EW. 2.7252E=05 0 0.000 1.198 FKom 2.7282E=05 TU LT.OR.EU. 3.0719E*05 5 998 2.196 ' C) '
- FCOM_ 3,0719E=05 TU LT UN,EQ. 3.e589E=05 13' 2.595 4.100 '
FX04 l 3.4589E=05 TU LT.UN.EO. -3.8946E=05
+ 26 5.190 9.98u FROM 3.89e6E=05 70 LT.ON.EG. 4.3852E=05 22 4.391 'Is.371 C).;: FR03 4,3852E=05__T0_LT,0N,EG,__e.9376E=05__. __ 29 _. ___ _ 5,788 _ _ _ _ _20.160 ! e.9376E=05 5.5596E=05 . PROM TO LT.OR.EG. 31 6.188 26.347 + FROM 15.5596E=05 Tu LT.OR.EW. 6.2600E=05 31 6.18e 32.535 C) l t FRU3 -6.2600E=05 70 LT.UR.EO. 7.oe86E=o5 e6 9.152 e1.717 ~
~- F 0N' '7.0486E=05 TO LT.OR.E9 7.93*5E=05: l 3.593 18 45.309 {
FEON 7.9365E=05 TO LT.ON.EU. 8.9363E=05 15 2.994 48.3u3 C) : F204 -8,9363E=05 TU LT.ON.EG.
~
1.0062E=0e 47 9.381 . 57.685 !
~
t.6062E=04- TO LT.OR.EG.
~ ^~
FROM t.1330E=ce- ~~ ~ ~ - ' 12 ~~ ~ 2.395 60.080' ' -
~'
FION- 1.1330E=04 TO LT.UN.EG. 1.2757E=0e 15 2.994 63.07e - () F204 1.2757E=0e 70 L1.0R.to. 1.436eE=0e 12 2.395 -65.469 ~ ~ ~ ~ ~
~~~ FRON "-'t .4 36eE=c e Tu LT.UN.EG. 166173E=ce 13- 2.595 68.064 FEUA 1.6173E=ce TU LT.ON.te. 1.824tE=0e 12 2.395 70.e59 # C) = g j
[__FION 1,8211E=0e 70 LT 0R.E9- 2.0505E=04 11 -~2.196 72.655 .- FROM 2.0505E=04- Td CT,.OR.EO.- 2.3088E*04 6 1;198 . 73.852"
- ~ ~ - -
1 FE04' 2.3088E=ce TO LT.04.EQ. 2.5996E=0e 5 998 74.850 C) . FKOM 2.5996E=0e TU LT.ON.EW. 2.9271E=ce 7 1.397 76.248 ji )I/ Y'#_ p' }
-~FROM 2.9271E=0a ~ TO LT.OR.EG.~ 3.2959E=0e 11 2.196 78.e43
~ ' ' ~ '
FE03 3.2959E=ce. TO LT.ON.E9 3.7111E=0e 12 2.395 80.838 LJ FOGM F;0a 3,7111E=04 Tu LT.OR.EG. e.1786E=ce a.1786E=0s TO LT.OR.Eu, e.7049E=04 ~
~~2516 ~~
a.990 3.194-85.828 89.022.
~ d- 9 /. 5 f" ~~ "
FROM 4.70e9E=04 TO LT.UR.EQ. 5.2916E=0e to 1.996 91.018 LJ FNUM 5.2976E=os 70 LT.ON.EG. 5.9650E=0e 25 4.990 96.u08
' FIOM ' 5.9650E=04 TU LT.04.EW. 6.716eE=04 to 1.996 98.uut
~ - ~ ~ ~
FIUM 6.716eE=04 TU LT.ON.EG. 7.5025E=0e t .200 98.20e gp FROM _7,5625E=0e- T g ,,(T ,0N . E U. 8 94461E=ce 9 1.796: 100.000-TOTAL 501 (s NUMoER OF ZENG ENTRIES 7989 MIN duMoEN OF WAL10 DOSERVATIONS PEN AVtNAGlhG IN1ENVAL s i v
~~-~~ ~ 50.00 PENCENT PulNT 9.886t=o5 55.00 PENCtNT POINT 9.95eE=U5 60.00 PERCENT PUINT 1.tteE=04 65.00 PENCENT POINT 1.377E=04
~ ~ ~ ' - - -
70.00 PENCENT PUINT 1.774t=04 75.00 PENCENT POINT 2.615E=04 ; 80.00 PENCENT Pu1NT 3.6uut=ue e5.00 PENCENT Pu!NT 3.9846-04 90.00 PENCENT POINT 5.140E=ce 95.00 PENCENT POINT 5.902E=ue
-- 89.83 PENCENI POINT 5.133t=0e (NNC IECHNICAL PUSITION = RELATIVE CONCENTRATION PNUUAWILITV)* _ __
. M w- , - +, - -- - - - - --_ w_-- + - _ - , #- - w --
-,,m- ,vr , , ..r v-,.. v. , ~,. , . - +e, n-
831 CON (ATM03PMENIC OISPERSION FON DM EveLuaTIoms) = YAN EE &IOMIC ELECTHIC Cu (Mou v3, d7/24/70) 11/25/76 PAGt 37 ] e, , MY 1977 12 KONIM5 = bMOUND LEVEL MEtta3E = vaNIA8LES MEPLACEO = EACLUSION ANEA OELTA=T STAeILITY MUDEL ' 00mNalND 8ECTON 85= G4=MA CHI /Q (SEC/41) = PNUdASILITY DISTNIBUT1uss O D(METER 8Fs 610.0 SECTuR AVERAGE VALUES = t=NOUR AVERAGES
~-~
O I FREQUENCY DI8THIeUTION HANGE NUmsER OF PERCENT OF CUMULATIVE
~~ '-
Os3ENVATluNS TUTAL 085 PENCEhl O FR03
- ~
Si8072E=06 T017.0R . E Q .7. 2959 E = 0 e 599 l 3 .599 - F;0M ! 6.2959E=06 TU LT.ON.EQ. 6.8257E=06 7 1.397 1.996 0 i
~
FRON 6.8257E=0e Tu LT.OR.EW. 7.4002E=0e 12 2.395 4.391 F003' 7.4002E=0e TO LY.OR.EQ. 8.0230E=0e 24 4.790 9.182 ~ '- FCoA 8.0230E=06 To LT.UN.EU. 8.6982E=06 18 3.593 12.774 C) L F 0M 8.6982E=06 To LT.ON.Ew. 9.asu2E=06 18 3.593 16.367 ! 9.4302E=0670'LT.OR.EG.
~
2 FRON 1;0224E=05 23 4.591- - 20.958 3 FCOM 1.0224E=05 Tu LT.UN.EQ. 1.tve4E=05 30 5.988 26.946 O FEOM t.1084E=05 TO LT.UN.EU. 1.2017E=05 27 5.359 32.335 FLO7 1.2017E=05 TO LT.OR.EQ. 1.3028E=05 le 2.794 35.130 Floa 1.3028E=05 To LT.ON.EG. 1.et25E=05 18 3.593 38.723 C) l FCOM 1.4125E=05 70 LT.ON.EW. 1.5314E=05 19 3.792 42.515 i FZuW 1.5314E=05 'TO LT.OR.EQ. 1.6602E=05 15 - 2.994 45.509
~
FCO3 1.6602E=05 TO LT.OR.EO. 1.8000E=05 2.994 15 48.503 C) FROM 1.8000E=05 TU LT.ON.tw. 1.9515E=05 8 1.597 50.100
~ FC07 1.951SE=05 TO LT.OR.EQ. 2.I157E=05 10 t.996 52.096 ~ --~~~
FC0a 2.1157t=05 70 LT.08 EQ. 2.2937E=05 9 1.796 53.892 C FLOM 2.2937E=05 TO LY.04.EQ. 2.e868E=05 8 1.597 55.489 : TLDZ 2;a868E=05 ~TO'LT.0R.EQ.-~2;696tE=05 11' -- 2.196
~ ~ - '
57.685
- ~ '~ -
F;01 2.6961E=05 70 LT.ON.EQ. 2.9230E=05 le 2.794 60.479 ()
^
FNUM 2.9230E=05 TO Lt OR.EQ. 3.1690E=05 11 2.196 62.675 ! FROM 3.1690E=05 TO LT.OR.EQ. 3.4357E=05 15 2.994 65.649 ~ ~ ~ - ~ l FZO7 3.4357E=05 10 LT.OR.EQ. 3.7248E=05 6 1.198 66.666 FCO3 3.72e8E=05 70 LT.ON.EU. e.0353E=05 O ' 13 2.595 69.4e1 i F 02--~4;0383E=05- TOTT.OR.EQ.--~4;3781E=05 ~ ~~
~ 13 ' ~ ~ - ~ '2;595- ~
- ' 72.056 ~
- - ~ ~ ~
FC07 a.3781E=05 TO LT.uR.EQ. 4.7466E=05 3.194 75.250 F001 4.7e66E=05 TO LT.ON.EU. 5.146tE=05 le Q 24 e.790 e0.0e0 F203 5.146tE=05 To LT.OR.EU. 5.5792E=05 15 2.994 83.034 FC00 5.5792E=05 70 LY.OR.EO. 6.0407E=05 2.794 FIOM 6.0e87E=05 TO LT.ON.EQ. 6.5578E=05 to e5.828 () 16 3.19e 69.022 F;0r-~6.5578E=05 - 70 TT.0R.EU 7;I 096E=05 '~--- ~ l 7 '~ --~ ~ - ~~~ 3.393 ~ ~ ~ ~ ~ 9 2. 815 FE0a 7.1096E=05 To LT.OR.EQ. 7.7080E=v5 FE03 7.7080E=05 Tu LT.ON.EU. 8.3567E=05 19 3.792 96.208 () 6 1.198 97.405
----- F; 0 M -
8.3567E=05 TO LT.OR.EG. 9.0600E=05 2 399 ~ 97.804 FROM 9.0600E=05 10 LT.UN.EQ. 9.8225E=05 FIDM 9.8225E=05 To LT.ON.EQ. 1.0592E=0a 7 4 1.397 798 99.202 () 100.000 TOTAL 501 U
~ ~ ~ ~
NUM8ER OF ZERO ENTRIES 7989 NIN NUMBER OF VALID OB8ERVATIONS PER AVERAGIhG INTERVAL e t
'~
50.00 PENCENT Pu1NT 0 1.905E=u5 55.00 PENCENT POINT 2.45tE=05 60.00 PENCENT'PUINT 2.858E=05 65.00 PERCENT POINT 3.803E=05 ~~ 70.00 PERCENT PulNT i 4.152t=U5 75.u0 PENCENT POINI e.716E=uS () ; 80.00 PENCENT POINT 5.117E=u5 85.00 PENCtNT POINT 5.78eE=US I 90.00 PERCENT Pu!NT 6.618E=05 95.00 PENCENT POINT 7.298E=05
~~ ~
G _ _ 89.83 PERCENT POINT 6.6 tee =05 (NNE TECHNICAL PU3!TIUN = RELATIVE CONCENTRATION PRueABILITV)
g 3% ICON (ATMUSPMERIL DISPtW310N FON 064 EvaLuaT10NS) - VANnEE AIUMIC ELEC1NIC Cu (NuD u3, o7/24/76) 11/24/78 PAbE 38
. My 1977 12 muMIM5 = GNuuh0=LEVLL NELEASE = VARIAdLES HEPLACEO = EACLUSIUM AREA ottiA=T STAeILI1Y MUDEL-b :
DowNw1ND SECTOR sw GWuumD= LEVEL CHI /O 15EC/m3) = PR08 ABILITY DISTHIBUTIONs 1' O j
~ ~ ~ ~
D(METERS) e ~619.0 --PLUMt CLNTERLINE VALUES = 1=MUuW AVERAGES O {: ,
~~
?;
~ ~ '
FREQUENCY DISTRIBUTION RAmbE NUMRER OF PtRCENT OF CUMULATIVE 083tNVATIONS 10TAL Oss. PENCENT O;
~ ~ - ~
l FCO3 4'.4769EE 06-Tu LT.0R.EQ.-~ '.22e5E=06 5 ~ 2 546 546 1 FROM FROM 5.2285E=06 6.1063E=06 Tu LT.OR.E4 TO LT.OR.EG. 6.1063E=06 7.1315E=06 1 1 273 273 820 1.093 ' ~~ Ol FR03 7.1315E=06 fu LT.OR.EE. 5.3287E=06 1 273 1.366 FROM 8.3287E=06 Tu LT.UR.EG. 9.7270E=06 0 0.000 1.366 () j l FK04 _ 9,7270E=06_ TO LT,UR,E9,_ 1.1360E=U5 . 0 0.000_ _ 1,366 __ 1 FC04 1.1360E=05 TO LT.04.EQ. 1.32e7E=05 1 273 1.639 P:02 1.3267E=05 Tu LT.OR.EO. 1.5495E=05 2 546 2.1e6 O' FROM 1.5495E=05 fu LT.04.EG. 1.809eE=05 0 0.000 2.156 " J ,- ' ~ 'FROM 1.8096E=05 .TO LT.OR.EG. 2.1134E=05 0 0.000 2.186 i FROM 2.1134E=05 fu LT.0;t.EU. 2.a682E=05 1 . 273 2.459 O FC03 _ 2,4682E=05 'Tu LT,OR,EG,_ 2.88d6E=05, _ 3 820 __ _. 3.279_ _ _ _ FK04 2.8826E=05 fu LT.ON.EO. 3.3665E=05 __ 5 _ _ _ _ 1.366 4.645 FROM 3.3665E=05 To LT.ON.EG. 3.9317E=05 8 2.186 6.831 C)
~ ~~ FROM 3.9317E=05 10 Lt.OR.EU. 4.591eE=05 15 a.u98 10.929 ~
FCOM '4.5918E=05 Tu LT.ON.EU. 5.36d7E=05 27 7.377 18.306 , FE04 5.3627E=05 70 LT.OR.EG. 6.263UE=05 30 8.197 26.503 C) FROM 6,2630E=05 fu LT,04,EQ u .31#4E=05 7 69 18.852 45.355 i FROM 7.3144E=05 TO LT.OR.EG. 8.5424E=05 24 6.557. 51.913 FCOM 8.5424E=05 Tu LT.Ud.EG. 9.9765E=05 47 12.842 64.754 C) i FROM 9.9765E=05 TO LT.0M.E9 1.1651E=04 15 4.098 68.852 "'~~
}
FROM ~ 1.1651E=04 ~ TO LT 0W.EQ.~ 1.3608E=04 9 2.459 71.311 t-FROM 1.3608E=84 TU LT.ON.EU. 1.58V2E=04 to 2.732 . 74.044 C) ! FCOM 1.5892t=04 10 LT.OR.EG. 1.8560E=04 . 6 . 75.683 ; PROM 1.8560E=04- TO U~0R EO.-~ 2;1676E=04 8 ~~~ ~ ~ 1.639~~ 2.186 ---~ ~~7 7. 8 69 ~ , FROM 2.1676E=04 70 LT.OR.EG. 2.5315E=04 7 1.913 79.781 () FKun 2.5315E=04 70 LT.OR.EU. 2.9565E=04 6 1.639 81.421 ' ~ -
~ ~FRua 2.9565E=04 To LT.OR.EG. 3.4529E=04 9 2.459 83.e80 ,
FCO3 3.4529E=04 Tu LT.OR.EG. 4 03d6E=04 12 3.279 87.158 tj FEUM 4.0326E=04 Tu LT.OR.EG. 4,7096E=04^- 9 2.459 89.617-
~'~ -'~~ ~~ ' 1 3 .- - ~ ~ -~ ^3.552 ~
~ ~ -
710M 4.7096E=04' TO CT.OR.EQ. 5;5002E=04 93.169' - -
- FNUM 5.5002E=04 TO LT.OR.EO. 6.423eE=64 16 4.372 97.541 V FNum 6.4236E=04 TU Lt.uw.EW. 7.5ud1E=04 5 1.366 95.907 ~~
FRom 7.5021E=04 10 LT.ON.EO. 8.7616E=04 1 273 99.150 FROM 8.7616E=04 Tu LT.OR.E9 1.0233E=03 1 273 99.4Te () FEUM 1.0233E=03 Tu LT.OR.EO. - 1.1827E=03 2 546 luo.uo. 101AL- Joe a. NUMBER OF Ztdu LNTRits b12e MIN NUMBEN uk VALID UbStRVAT10NS PER AvtRaetNC INTruvaL = 1
~
50,00 PEWCENT Pu!NT 7.623t=ub 55.UU PENCLNT PulNT 9.875f=US 60.00 PERCENT P01NT 9.927E=o5 e5.00 PENCENT POINT 1.u11E=04 70.00 PENCENT Pu1NT 1,274t=0e 75.00 PENCtNT Pu1N) 1,613E*P4 80.00 PthCt N T Pu!NT 2.oaat-ce 65.00 PEwCENI Pu1NI 3.772E=be 90.00 PEHCENT Pu1NT 4.919t=ue 95.00 PENCENT POINT 5.932F=de 8 86.08 PEWCENT Pu1Ni 3.940t=0e (NRC 1ECNAlcal PuSIIION *' NELA11vE L0NCthlwai!ON PHUBA51LITT) _
- i
_ _ =___-____.._._c. - - _ _ _ _ _ _ _ _ . - . . . _ _ . _ _ _ - - _ _ - . _ _ _ - _ . - - _ - -_ - - - - - , , a - r n -
4 8alkUN (ATCOSPMEk1C U16PtNb104 P03 DbA EvaLUAT10NS) = YtNMEE ATOMIC ELECINIC CO (aO0 u3, 07/2e/70) 11/2s/18 PAGE 35 '
.ny 19f? 12 MUNfM8 = GROUND =LEttL hELEASE = VARIABLES NLPLACED = EXCLUS104 AhEA O DELTA =T STAu1LITY MODLL +
00nNMIND SECTOR SM GAMMA CM1/e (8EC/=3) = PNueABILITY DISTRIBUTIUN3 () 4 6(METEN8) e 610.0 8ECTOR AVERAGE VALUES ~~ ~ !=MUUN AVENAGE5
~~'
O . ~"- FREQUENCY 0187H18UT10N RANGE NUMBER OF PLRCENT OF CUMULATIVE ! DeSLRVAT10N8 TOTAL De3 PEWCENT 7 3
~
F10M 5 .e686E=06 fu LT.UN.EU. 5.9917E=06 ~1 ~ 273~
~
273
~ ~
FIUM 5.9917E=06 TU LT.UR.EG. 6.56e7E=06 e 1.093 1.360 ' i ~ ~ - FCOM e.5ee7E=06 Tu LT.UN.EQ. 7.1926E=06 4 1.093 2.e59 ! FCO3 7.1926E*06 TO LT.UN.EO. 7.8805E=U6 e 1.093 3.552
-~ ~
FIOM 7.8505E=06 TO LT.up.EW, 8.6342E=0e 9 2.e59 6.u11 FEOM 8.6342E=06 TO LT.OR.EQ. 9.e600E=06 15 a.098 Ffua 4.e600E=06 - 07 ~L T.0d.Eu. 1.0365E=05 '
~ ~ '
13 -~~
~ -- - 10.109 3.552
~ ~~ ~'~
13.601 FEUM 1.0365E=05 To LT.UN.EG. 1.1356E=05 21 5.738 19.399 FNUM 1,1356E=05 70 LT.UR.EQ. 1.2ee2E=05 to a.918 24.317
~'FION 1.2ee2E=05 TO LT.OR.EG. 1.3632E=05 13 3.552 27.869
-~-
F104 1.3632E=05 70 LT.OR.ED. 1.493eE=05 18 4.918 32.767 FIOM 1,4936E=05 70 LT.04.EO. 1.63 bee =05 2e 6.557
~~ 39.344 FROM 1.636eE=0 5- Tu LT.ON.E u. 1.7929E=05 7.377 - ~'46.721 27 FEOM 1.7929E=05 TU LT.UN.EG. 1.96eeE=05 to 3.825 59.546
- F 0M 1.968eE=05 TO LT bH.EO. 2.1523E=05 20 5.464 56.011 FROM 2.1523E=05 TO LT.ON.EG. 2.3581E=05 16 a.372 60.363 FIOD 2.3581E=05 TO LT.OR.EU. 2.5837E=05 1.913 7 62.295 C)
FZON 2.5837E=05 To LT.ON.EG. 2.8308E=05 8 2.186 64.451 FZ084 2.83 08E=05 TO LT.OR.EQ.
" ~
3.1015E=05 ~~~ 1.093-e ~ 65.57e
-~ ~ ~ - '
FNOM 3.1015E=05 TO LT.UN.Eu. 3.3952E=05 10 2.732 68.306 () FROM 3.3982E=05 TU LT.UR.EG. 3.7232E=05 ' 15 e.098 72.40s
FZO4 3.7232E=05 TO LT.OR.EQ. 'e.0792E=05 6 1.639 7e.04e
~ ~ ~ ~ -
FN07 a.0792E=05 TO LT.OR.EQ. e.e694E=05 3.005 FIO1 a.e69eE=05 70 LT.ON.EG. e.8968E=05 11 10 77.ve9 () FROM ~ ' - - ' 2.732 - 79.781 e.~5968E=0570 LT.OR.EQ. 5;3652E=05 -~
- - ~~
~11 3.005 ~'- " ~ 8 2 .7 5 7 ~ ~- -
F ROM' 5.3e52E=05 Tu LT.OR.EQ. 5.87e3E=05 16 e.372 e7.158 t) FKOM 5.8783E=u5 TU LT.04.tQ. 6.ee05E=05 16 4.372 91.530 FROM 6 ee05E=05 70 LT.OR.EQ. 7.0565E=05 8 2.186 93.710
~~~
FC04 7.0565E=05 lu LT.UR.EQ. 7.7318E=05 14 3.825 FIUM 97.541 t) 7.731eE=05 TO LT.ON.EG. 8.8708E=05 e 1.093 98.63e FROF8.e708E=05 - TO ~LT.OR.EQ. 9;2810E=05 1 .273 9 8.9 0 7 ' ~ - From 9.2810E=05 TO LT.OR.EQ. 1.0169E=0e 1 273 99.180 s; FRum 1.0169E=0e 10 LT.ON.Eu. 1.1181E=ce 0 0.0v0 99.1e0 F UM 1.1141E=0e TO LT.UW.EW. 1.2207E=ce .273 FIOn 1 99.eSe 1.2207E=0e Tu LT.UR.EO. 1.3374E=ce 0 0.000 99.uSe ss FC04 1.337eE=0e TO LT.OR.EW. 1.456eE=0e 2 .546 100.000 _ . . _ IUTAL 366 s NUMBER OF ZERU ENTRIES 5128 MIN NUMBER OF VALID OBSERVATION 3 PER AVERAG1hG INTENVAL a 1 v ~' ~~ 50.00 PENCENI Pu1NT 1.95dt=u5 55.00 PLMCENI PUINI 2.11eE=o5 60.00 PERCENT POTNT 2.3eet=05 e5.00 PEMCENT POINT 2.93eE=05 --- 70.00 P E R C E 'w i POINI 3.507t=05 75.00 PEMCLN1 POINT 4.215E=o5 s 80.00 PERCENT PUINT 5.luet=05 85.00 PENCENI PuldT 5.oo9E=u5 90.00 PLRCENT POINT 6.3elt=05 95.00 PENCENT PUINT 7.292E=05 J 86.08 PthCENT Pu1NT 5.628t=05 (NHL TELMNical PU31110N = RELAT1vt CONCtNiWAT1UN PMU$ad1LIIT)
..... ... u e..uorneniL u t s*t a diu's FUk ueA Ebstenflow3) =
vahatE ATOMIC ELECTWIC Cu mv 1977 12 1*0D 03. u?/de/Tel 11sdepto Pabt 40 MONTMS = ENUON0= LEVEL hELEa5E = vaklaeLE3 NEPLeCEDANta = EXCLUSION b 00:N=IND SECTOR #83 DEtta-T STAHILITY MoDEL
~
f.ROUND=LEvtl CMI/u 15EC/M3) = PRU8a81LITY DISTN!sOIIUNa 0iME7EN81 a " 610.0 ~ ~ PLUME CLNTERLINE VALUES =
!=H00N AWERAGES
_ 's !
~
_ t FRE90ENCY DISTRIBUTION RANGE NUm8ER OF e! DBSLRVA TION 8 PLNCENT OF CuMULATIVt ~ ~ - i TUTAL 085
~FCO3 5.8034E=06 TU LT.UR.EG.
PtHCENT [ FRum 6.63U3E=06 ~ ~ GD t-6.6303E=06 TU LT.ON.EU. 7 575DE*06 1
.568 .5e8
~'
FRua 0 7.5750E=06 TO LT.ON.EQ. 8.65e3E=06 0.000 .568 FCom 8.6543E=06 TO LT.0R.EO. 1 568 FCOM 9.s87eE=06 0 1.136 9 ! 9.5e74E=06 To LT.UR.EU. 1.1296E=05 0.000 I FCOM 1,1296E=05 70 LT,0R.EO 0 1.136 ^
~
FROM 1.2906E=05 0 0.000 1.136 ; 1.2906E=05 TO LT.UR.EO. 1.47e5E=05 ._ 0.000 ,1,13e C) ; FRun 1.4145E=05 TU LT.UR.EU. 1.68e eE=05 0 FCOM U.000 1.136 ! 1.6846E=05 70 LT.ON.EW. 1.9246E=05 0 0.000 1.136 j.
~ PCom ~ 1.9246E=05 TO LT.UN.EQ. 2.1988E=05 0 0.000 C) -
FCOM 2.1988E=05 TU LT.OR.EO. 2.5121E=05 0 1.13e 0.000 1.130
. FCOM 2.5121E=05 70 LT.UR.EG,~~2.8700E=05 -0 0.000 ~FROM ~
2.8700E=05 TU LT.OR.EW. 3.2790E=05~ -2 1.136 FN04
~
e
~ ~
~ 1.136 2.273 C) 3.2790E=05 fu LT.ON.EO. 3.7462E=05 2.273 PROM 3.7462E=05 70 L1.UN.EG. e.2799E=05 6 3.409 a.5e5 ' ~ ~ ~
~ FCOs 7.955 FCOM 4.2799E=05 to LT.ON.EO. e.8898E=05 16 2 1.136 9.091 ()
4.8898E=05 fu LT.ON.EG. 5.5665E=u5 9.091 FIUm 5,5845t=05 70 LT.OR.to 23 18.182 ~ ~ ~ ~
~FR06t 6.3825E=05 13.068 ft.250 PCOM 6.3825E=05-~TO ~LT.0R.f e,~7.291*E=05 ' ' '~ ~ 29 16 ~ 16.477 47.727 ()
7.2919E=05 Tu LT.OR.E9 8.3309E*05 9.091 ~ ~ -~ ~ 56.818 '- FCOM 8.330*E=05 Tu LT.ON.E9 9 9.5179E*05 5 5.114 61.932
~ FROM' Ff 01 9.5179E=05 Tu LT.OR.EG. 1.0874E=0e 9 2.841 6e.773 Q ,
1.9874E=ce Tu LT.ON.EG. 1.2e23E=0e 5.11e , FCOM 1,282)E=04 10 LT.UN.EW. 1.e194E=0e 9 e9.886 ~
~FROM 5 5.11e 75.000 ;
FCOM 1. H 4 e E = 0 s -~~TO~ E T. 0R . E Q .~~~1.'6 216 E = 0 4- '8
~ 2.841 77.841 C) '
FROM 1.6216E=ce TU LT.ON.EU. 1.852eE=04 4 e.545- ~ ~ ~ ' ' 82.366 ~ ~ ~ ~" I
~~ FRO 3-~~ 1.8526E De 70 L T.ON.EG. 2.I!6eE=ce 2 2.213 84.659 FCOM 2.1166E=0e 'To LT.OR.EG. 2.o182E=os 0 1.136 85.795 () . FCOM 2.e182E=ce 10 LT.OR.EO. 2.762sE=0e 0 0.000 85.795 -~~
2.7628E=0e 70 LT.ON.EU. 3.1564E=0e 0 0.000 65.795 FFCO2 3 ; 156 e E 40 e70 TT . O R . E G .~~3.~6 062 E = 04-~ 0.ovo %) FCO3 3.6062E=ce 3
~ ~' ~ 65.795 FCOM TO LT.OR.EO. e.1200E=0e 9 1.705 ~ ~ ~ ~
87.500 - ~ 4.1200E=04 70 LT.OR.ED. e.7070E=0e 5.11e 2 92.614 3 i FCOM FCO3 ~ 4.7070E=0e TO Lt OR.EQ. 5.377TE=ce 1.136 93.750 %) 2 1.136 5.3777t=04 70 LT.OR.EU. 6.le39E=04 3 94.886 ~ ~ dE.OM ,6.1439E =04_TU L T.ON.E G. 6.9573E=0e 1.705 96.591 6 3.409 %> 100.000 lufal 176 NUMBER OF ZENO ENTRIES 631e v 50.00 PERCENT PUINT MIN NuMBEN tsF WALID Us3ERVATIums PEN aVENaGinG INTENVAL s. 1 ' ~ ~ ~ ~ - ~ 4.672t=05 40.00 PENCEN T PUINT 7.66st=u5 55.00 PEhCLNT POINT 1.08sE=n5 J 70.00 PERCENT PUINT 1.139t=ue e5.u0 PEWCENT POINT 9.552t-US 80.00 PtHCENT POINT 1.5uet-ce 75.00 PLNCtN1 PO1=T 1.d65E=ue 90.00 PENCENT PUINT 3.9eet-ce M5.00 PtWCENT 90lNI 1.930t=ue . 95.uu PEHLEN1 Pu1NT 5.632E=ue __ 71.06 PLNCENT POINT j.le9t=ue (hkC IECMMICal PUSITION = NLLATIvt CONCthlRATION PNUBAu1LIFf)
. . . ~
ime
I . ,
. SKICUN (ATMOSPMERIC DISPERSION FOR dea EVALUATIONS) = vahnEE ATOMIC ELECTRIC CU (MG0 03, 07/2e/76) 11/2e/7e PAGL 41
)
' (
. MT 1977 12 MONTM3 = GROUND LEVEL NELEASE = VARIABLES MEPLACED = EkCLUSION Ante DLLT&=T STA61LI1Y MODEL
)- D0nNMIND SEC10R 484 GAMMA CHI /G (SEC/m3) = PRugABILITY DISIRIBUTIONS { D(METEN8F s 610.0 - SECTUA~ AVERAGE VALuE8 = 1=MOUN AVERAGES ) ( FRE0utNCY DISTRIBUTION RANGE NUMBER OF PERCENT OF CUMULATIVE
~ ' ~ ~
) 083ENVATION8 TOTAL 085 PERCENT (
-~
FROM 5.6218E=06 TO LT.OR.EO. 6.0869E=06 1 568 568
' ~~~
) FROM 6.0869E=o6 TO LT.OR.EG. 6.5904E=06 6 3.4u9 3.977 (
~~
FROM 6.5904E=06 70 LT.UR.EW. 7.1356t=06 5 2.8e1 6.818 FROM 7.1356E=06 70 LT.04.EQ. 7.7259E=06 6 3.e09 10.227
- -~
) FROM 7.7259E=06 TU LT.ON.EU. 8.3650E=06 8 4.5e5 18.773 ( FROM 8.3650E=06 70 LT,0R.EU. 9.0570E=U6 1 568 15.341 3.977' F R 0d-~~ 9. 0 57 0 E = 0 6 TO'fT.04.EQ.~ 9.~8062E=o6 ^7 19.318
) FROM 9.8062E=06 70 LT.0M.EQ. 1 0617E=05 14 7.955 -27.273 (
~ - ~
FRUM 1.0617E=05 70 LT.uu.Eu. 1.teveE=05 8 4.545 31.e18 FROM 1.1496E=05 TO LT.OR.EO. 1.24e7E=05 9 5.114 36.932
'~"'
) FROM 1.2447E=05 TO LT.OR.EO. 1.3eF6E=05 12 6.818 43.750 t FROM 't.3476E=05 70 LT.UR.EG. 1.4591E=05 7 3.977 - 47.727 FROM l'.~4591E=05 TO LT;0R.EO.' 1.579BE=05 3 1.705 #9.432
- ^-~
) FROM 1.5798E=05 TO Li.OR.EW. 1.7105E=05 5 2.841 52.273 'd
- ~
FROM 1.7105E=05 TO LT.04.EU. 1.8520E=05 5 2.841 55.114 FROM 1.8520E=05 TO LT.OR.EG. 2.0052E=05 4 2.273 57.366
- -~ ) FROM 2.0052E=05 70 LT.OR.EO. 2.1711E=05 7 3.977 61.364- -
FRUM 2.1711E=05 TO LT.0R.E9 2.35U7E=05 2 1.136 62.500 FROM 2;3507E=05 7 0 IT.OR.EG. 2;5451E=05- 3 1.705 64.205
'~
,D FROM 2.5451E=05 10 LT.OR.EO. 2.755FE=05 4 2.273 66.877 - FROM 2.7557E=05 TO LT.ON.EG. 2.963eE=05 5 2.841 69.318
- -- - FROM 2.9836E=05 TU LT.OR.EQ. 3.2305E=05 5 2.841 72.159
~ ~~ ~
D FROM 3.2305E=05 10 LT.OR.EG. 3.4977E=05 2 1.136 73.295 ( FROM 3.4977E=05 TO LT.0R.E9 3.7870E=05 9 5.11e 78.409 FRO O p870E=05- TO~LT.0R.EG. 4;1003E=05 ~ ~ ~ 6-~
~~ 3.409 ~ ~
~
81.818 -
' ~ ~- ~
9 FROM e.1003E=05 TO LT.UR.EG. 4.e395E=05 3- 1.705 83.523 ( FROM e.806eE=05 e 2.273 85.795
~~~
-FROM ~4.8068E=05 4.e395E=05 70 TO LT.OR.EG.
LT.OR.EG. 5.20e#E=05 1 .568 86.364
~~ ~
p FROM 5.20eeE=05 fu LT.UR.EW. 5.63e9E=05 1 568- 86.932 ( FROM 5.6349E=05 10 LT,0R.EG. 4 1011E=05 5 2.841 ~ ~ ~ - - 89.773 FROM~ 6;1011E=05 7 0 LT.OR.EU.~~6.6058E=05 7 3.977
~
93.750
~ '- -
9 FNOM 6.605eE=05 To LT.uN.EQ. 7.1522E=05 2 1.136 9a 866 t FNOM 7.1522E=05 Tu LT.OR.tu. 7.7439E=D5 e 2.273 97.159 FROM 7.7439E=05 TU LT.0W.ED. R.38e5E=u5 1 568 97.727 g FROM 8.30a5E=05 IU LT.ON.EW. 9.0761E=U5 3 1.705 99.432 e FNOM 9.0781E=05 fu LT.0W.Lu. 9.7771E=05 -- 1 5e8 100.000
, TUTAL 176 C NUMBER OF ZENU ENTHIES 6314 MIN NUMBER OF WALID OBSENWATIONS PEN AVLhAGING INTENVAL a g a
t 50.00 PtWCENT PUINT 1.tu5t=ub 55.00 PEWCLNI PUINT 1.765E=05 60.00 PERCENT POINT 2.113E=05 65.0u PENCENT POINT 2.555E=05 s 70.00 PENCENT PHINT 3.100t=u5 75.u0 PERCLNT PUINI 3.527t=n3 i 80.00 PEwtENT PulNT 3.926L=05 85.00 PENCLMI PUINT 4.eVoE=05' 90.00 PLHCENT PUINT 6.330t=05 95.00 PERCLNi PDINT 7.275t=U5 s 71.06 PtHCENT POINT 3.197t=ub thWC IECHNIL AL POSIlluN = RELATIVE CUNCLNINaTION PRuemeILITY) .- m__ _ .. . _ _. . . _ _ _ . . _ . . _ _ . _ _ _ _ _ _ . . ~ _ . . - . _ _ . - . . _ . m -_ _ _ . - - - - - - - -- - - - - - - - -
- 8%ICO:s ( ATMO5PHEMTC UIsPERSION F02 DUA Ev&LUATION5) = YANREE AluMIC LLECTRIC Cu (muu v3. 07/2e/783 11/2e/18 PAGE 42 MY 1977 12 MUNTH3 = GhuuhD= LEVEL NELEASE = v4RIABLES NEPLACEO = taCLUSION AREA utLIA=T 51AeILITY MuDEL _
DowNm!ND SECTOR w GROUND
- LEVEL CMI/O (8EC/M3) PRO 8As!LITY DISTN18UTIONS
=
( D(METERS) a 610.0 PLUME CENTERLINE VALUES =
!=HUUN AVERAlE5
~~
I l ~~ FREWEkCY DIST*I UTIUb RANGE NUM8ER OF PENCENT OF CUMULATIVE
~ - - - -
ue5ERWaTIUh3 TOTAL 085 PERCENT ( FROM 1.0109E=05 fu LT.OR.EW. 1.1483E=05 2 1.042
~~
FROM 1.0a2 1.1483E=05 TO LT.UR.EG. 1.30eeE=05 0 0.000 1.0e2 0
~ ~ PROM 1,304eE=05 TU LT.ON.EG. 1.4817E=05 0 0.000 1.ce2 FROM ~'t.481TE*05 TO LT.UR.EQ. 1.6832E=US 0 0.000 1.042
~ ~
FROM 1.6832E=05 TU LT.OR.EQ. 1.9119E=05 FROM _ 1,9119E=05 _TU LT.uN.EG,_ 2.1718E=05 2 1 521 1.563 ( 1.042 2.60s FROM 2.1718E=05 TO LT.UR.EQ. 2.4671E=05 5 2.604 5.208 FROM 2.4671E=05 To LT.ON.EQ. 2.802eE=05 2 1.042 6.250 ~ FNOM 2.8024E=05 TO LT.ON.Eu. 3.183eE=05 6 3.125 9.375 FROM 3.183eE=05 Tu LT.OR.EQ. 3.6161E=05 6 3.125 12.500
~ ~ ~ ~-~
FROM 3.6161E=05 TO LT.OR.EQ. 4.1076E=05 7.292 le 19.792 Ci FROM e,1076E=05 _TO LT,0R.EQ ue.6660E=05_ 11 5.729 25.521 FRUM e.6660E=05 70 LT.UR.EQ. 5.3002E=05 12 6.250 31.771 FROM 5.3002E=05 TU LT.ON.EQ. 6.0207E=05 13 6.771 36.582 ( FMUM 6.0207E=05 TO LT.OR.EU. 6.8391E=05 13 6.7T1 e5.313 FROM 6.8391E=05 TO LT.OR.EU. 7.7688E=05 19 9.896 55.208
~~ ~
FROM 7.7688E=05 lU LT.OR.EQ. 8.8288E=05 6 3.125 58.333 C. FROM 8,82e8E=05 Tu LT,0R,EQ, 1.00deE=0e
~
12 ~' -6.250 66.583 FROM 1,0024E=0s~ TU LT.ON.EQ. 1.1387E=Us ~ 8 e.167
~~ ~~ '
66.750 -
~ ^ ' -
FROM 1.1387E=ce Tu LT.OR.EG. 1 2935E=0e 13 6.771 75.521 ( PROM ~ 1.2935E=0a TO LT.UN.EQ. 1.a693E=04 5 2.60s 78.125
--~ ~ 'FROM 1.4693E=08 TO LT.OR.EG. 1.~6690E=0s a 2.083 80.208
' ---~
FROM 1.6690E=0e TO LT.ON.EQ. 1.s959E=0e 8 a.167 84.375 E FROM 1.8959E=0e 70 LT.OR.EG. 2.1536E=0e ~~ ~ ~ ~ ~ a
~4.167 88.542 FROM 2.1$36E=0e70 LT.ON.EQ. 2.446eE=0e ~3 ~ - ~ ~ ~ ~ 1.563 - -~~ ~ ~ 90.104'- ~ ~ ~ ~ ~~
FRUM 2.4864E=04 Tu LT.ON.EQ. 2.778vE=0e 5 2.604 92.708 L: FRUM 2.7789E=0e TU LT.uk.EQ. 3.1567E=0e 0 0.000 92.708
- ~ FROM 3.1567E=0e TO LT.UR.EO. 3 5857E=0e 1 .521 93.229
~~-
FNOM 3.5857E=0e Tu LT.ON.EQ. 4.0732E=0e 7 3.646 96.875 (; FROM 8.073?f=0e TO LT.OR EQ. E.6268E=O4 3 1.563 98.437 FROF4.6268E=0s- TO LT.OR,EQ. . 5.2558E=ce' 0'- - - ~ - ~0.000~~ 98.437 - FRum 5.2558E=04 Tu LT.OR.EQ. 5.9702E=0e 1 521 98.958 s FNOM 5.9702E=0e 10 LT.ON.EG. 6.7817E=0e .521 FROM 6.7817t=08- TO LT.OR.EQ.' 7.7036E=04 1
'~ 99.e79 ~ ~
0 0.000 FROM 99.e79 7.7036E=04 TO LT.OR.EQ. 8.7507E=04 0 0.000 99.479 A. FROM 8.7507E=ce TO LT,0R,EQ. 9.8561E=0e 1 521 100.000 TOTAL 192 L-
- ~ ~ ~
NUM8ER OF ZERO ENTRIES 8298 MIN NUM8ER OF VALID OBSERVATIONS PEN AVERAGING INTENVAL = 1
' - ~ ~ -
L 50.00 PENCENT Pu1NT 7.e251-05 - 55.00 PENCENT POINT 7.690E=05 60.~00 PERCENT PUINT ~ 9.857E=05 65.00 PERCENT POINT 1.0 00E=0 4 - 70.00 PEHCENT PUINT 1.le2E=0e 75.00 PENCENT POINT 1.236E=De 80.00 PERCENT POINT 1.eetE=ce s:
~ - ~ ~ - ~ 85.00 PERCENT PUINT 1.935E=0e 90.00 PERCENT POINT 2.341E=04 95.00 PERCENT POINT 3.612E=0e
' - " ~ - ~ ~
73.47 PERCENT PUINT 1.183E=ce (NRC TECHNICAL PU8IIION = RELATIVE CONCENTRATION PRUBABILITV)
^
t Sn!"0N (ATMU3PMENIC DISPER5 tun Fue 0*JA E%ALUATIONS) = YANAEE ATOMIC ELEC1 HIC Cu IMUD v3, 07/24/78) 11/24/78 PAGE 63 _,___, NY 1977 12 =ONTM5 = bNUUND= LEVEL MELEASE = VARIABLES NEPLACED = EXCLu31UN AkEA
. DttTA=T STABILITY ecoEL. _ ) 00mWWIND SECTOR m GAMMA CHI /u (SEC/M3) =
PNU8ASILITY DISTRIBUTIONS ( D(METERS) s s10;0 SECTUR AVENAGE VALUES = '-leMOUR AVERAGES ~~ ' ' ' ~ ~
~ ~
~ - ~ ~ " -~' ~ ~ -"--
) i
- ---' ~
-" FREGUENCY DISTRIBUTION' R ANGE NUMBER OF PERCENT OF CUMULATIVE
' ~-
) OBSERVATIONS TOTAL UUS. PERCENT FR093.85e7EiO 67 dTY.OR. E W.~s.2431E=06' 3 1.56 3 - ~ ~ ~ - ' ~ 1.563
~^ ~ --- -
) FROM e.2831E=06 Tu LT.04.ED. e.6707E=06 2 1.042 2.6ea PROM e.6707E=06 TU LT.OR.EU. 5.1413E=o6 3 1.563 4.167 PROM ~ 5.le13E=06 TO LT.0H.EG. 5.6593E=ot 0 0.000 a.167
-~
) FROM 5.6593E=06 Tu LT.0R.EG. 6.2295E=06 5 2.604 6.771 FROM 6,2295E=06 TO LT,0R.EQ. 6.8572E=06~-~ ~ - 4 -2.083 8.854 FROM 6.8572E=06~~TU'LT.OR.EQ.~ 7.5481E=06 '#-
- ~ ~
2.o83
~ - -
10.938
) FROM 7.5481E=06 Tu LT.04.EG. 5 3086E=06 18 9.375 20.313 FROM 8.3086E=06 Tu LT.ON.EO. 9.te57E=n6 11 5.729 26.942
~~ FROM 9.1457E=06 TO LT.OR.EQ. 140967E=05 9 e.688 30.729
)- FROM FROM 1.0067E=05 fu LT.ud.EG. 1.1082E=05 1.1082E=05 10 LT.OR.EU 1.2198E=05 14 6 7.292 38.021 1 FROM--~1.2198E405 7 0 LT.04.EQ.,~1;3e27E=05 ~ 3.125 41.146
'7
- ~
- 3. 6 4 6---~ - 44;792
-~ ----
PROM 1.3427E=05 TU LT.OR.EO. 1.e78cE=05 3 1.563 e6.35e FNOM 1.4780E=05 Tu LT.OR.EQ. 1.6269E=05 7 3.6#6 50.0C0
' FROM 1.6269E=05 70 LT.OR.EQ. 1.7908E=05 3 1.563 51.562 -
FROM 1.7938E=05 Tu LT.OR.EO. 1.9713E=05 3 1.563 53.125 i FROM 1.9713E=05 70 LT.OR.EG. 2.1699E*c5 6 3.125 --- 56.250 FROM 2.1699E=05- TU LT;0R.EQ;- 243885E=05~ ~ ~~ 9 ~-- - ~ ~ ~ -~ 4 ; 6 8 8 -~ -- - 60.937 FROM 2.3885E=05 Tu LT.uR.EQ. 2.6292E=05 5 2.60s 63.542 , - --"- ' F N O M 2.6292E=05 TO LT.0M.EG. 2.8941E=05 e 2.083 65.625 9 i FROM -~ 2.8941E=05 TO LT.0R.EQ. 3;1857E=05 5 2.604 68.229
- - - ~ ~
) FROM FROM 3.1857E=05 TO LT.OR.EG. 3.5067E=05 TU LT.OR.EG. 3.8600E=05 3.5067E=05 3 1.563 69.792 Q l 17 8.854 78.6e6 3;8600E=05 TO UT.OR;EQ.-~~44 2a90E=05 - - - - - - - -'a [ FROM "
- -~~~ 2.083'
~
- 80;729 - ~ ~ ~
) PROM 4.2e90E=05 TO LT.Lw.EU. 4.6FFIE=05 5 2.604 83.333 j ---- FROM FROM 4.6771E=05 To LT.ON.E9 5.1483E=05 - T0 1;T.OR.E9 5.1453E=05 5;667pE=05 8 4.167 87.500 e
FROM 6 3.125 90.625
--~ -- --- ~
D 5.6670E=05 70 LT.OR.E9 6 23BcE=05 5 2.604 93.229 q FROM 6.2380E=05 TU LT.OR.EO. 6.8666E=05 8 4.167 FR04---~6;8666E=05 TU ET;UR;EG.-~7.5584E=05 - -- "~ 97.396 2-- ---t.042~~ 98.437 - --
) FROM 7.558aE=05 Tu LT.OR.EQ. 8.3200E=05 1 521 98.958 t PROM 8.3200E=05 TO LT.OR.EG. 9.1543E=05 1 521 99.479 FROM 9.1583E=05 TO LT.OR.EG;' 1.00stE=04 0 0.000
~~99.479
-- '~ '---
!. FROM 1.8081E=04 TO LT.ON.EG. 1.1097E=ce 0 0.000 99.479 9 l FROM 1.1997E=44 To LT.OR.EG. 1.2137E=04 1 521 100.000 5 TOTAL 192 , C
-" ~NUMSER'0F ZERG ENTRIES 8295 MIN NUMBER DF VALID OBSERVATIONS PER AVERAGING INTERVAL e 1
~ ~ ~ ~
? 50.00 PERCENT POINT 1.669E=05 55.UU PENCENT PUINT 2.112E=05 60.00 PERCENT' POINT 2.349E=05 65.00 PENCENT POINT 2.6a5E=05
~ ~ ~ ~ ~ ~
p 70.00 PENCENT PulNT 3.508E=05 75.00 PENCENT POINT 3.738E=05 4
-- ~ ~
80.00 PEWCENT POINT e.077E=05 85.00 PERCENT PUINT 4.90eE=05 90.00 PERCENT PUINT 5.609E=05 95.00 PERCENT POINT 6.351E=05 ' - ~ - - - ) G 7 3.622E=05 (NRC TECHNICAL PuSITION = __3_.47 _ PERCENT Pu!NT MELATIVL CONCENTRATION PMu8 ABILITY) _ _ _ . __ __.._____m__- _ _ _ _ _ _ - - __ . _ - _ _ _ _ __ - __ e -9*-
- _-'t'* + _ _ _ e_. '-P er ___-__--i m-
. SAICON (ATM08PMLHIC ut3PEH510N FON 0:e EVALua110=3) = VENAEE 410 MIL ELEC1h1C Cu ta00 v3e 07/24/76) 11/2e/78 PAbE GC t
, 8E f 1977 12 EON 1M3 = GWuuhD= LEVEL MELEa5E = vaHlanLLs NEFLACEu = EACLu51uw awEA utLTA=T STau1LITV MoutL _
00mhw1ND SECTON mM4 GRuum0= LEVEL CHI /W (3EC/M3) = PRusa81LITY 015fdIsuTIuks < D(METERS) e 610.0 PLOMt CENTERLINE WALUE8 = !=MuuR AVERAGE 8
~-
FREWUENCY DISTRIBUTION MANGt NuM8tR OF PENCENT OF CumuLAT1vE UWSEMVATIONS TUTal 088 PENCtNT
~~
FROM 1.2053E=05 Tu LT.ON.E3 1.3eF2E=05 1 535 535 FNOM 1.3472E=05 TU LT.OR.EQ. 1 505eE=05 0 0.000 535
~ ~ ' ' FNOM 1,5058E=05 fu L1.ON.EQ. l.h930E=05 0 0.000 535 ~-
FROM 1.6870E=05 70 LT.OR.EU. 1.8811E*05 0 0.000 535 FROM t.8811E=05 fu LT.ON.EU. 2.tud5E=05 0 0.000 535 FRUM _ 2,t025E=05 _70 f.T.OR.EU. 2.3500E=05 0 0.000 535 - PROM 2.3500E=05 fu LT.ON tu. 2.6205E*05 0 0.000 535 FROM 2.6265E=05 TU LT.uM.E9 2.9357E=05 2 1.070 1.60s FROM ~ 2.9357Ea05 70 LT.UR.EU. 3.2612E=05 a 2.139 3.743 ~~~ ~ FROM 3.2812E=05 10 LT.OR.EG. 3.667eE=05 e 2.139 5.882 FROM 3.e67eE=05 TU LT.ud.EU. e.099tE=05 7 3.7e3 9.62e . FROM 4.5516E=05 e 099tE=05-~ Tu LT.UR.EG,~ 5.lfveE*05 7 3.743 13.369 frROM ~ ,5816E=05
~ ' ~ ~
- e. TO'LT.OR.EU. e 2.139 15.508 FROM 5.1208E=05 To LT.04.EO. 5.7236E=05 6 3.209 18.717 FROM Tu LT.uR.LW. 6.3972E=05 9 a.813 23.529
~~ ' FNUM ~ 5.7236E=05 6.3972E=05 TU LT.ON.EQ. 7.1502E=05 17 9.091 32.620
~ ~~
PROM 7.1502E=05 70 LT.ON.EU. 7.9918E=05 24 12.834 e5.e55 PROM 7 8,9918t=05 Tu LT.OR.tu. 8.g32eE=05 8 a.278 ~~' '~ 49.753 ~~ FROM 932eE=05 10~LT.ON.EO. '9.983eE=05 26 13.908 63.636 " ' FROM 9.9838E=05 TO LT.ON.EU. 1.1159E=0e 8 4.278 67.914 FNOM 1.1159E=0e Tu LT.OR.EU. 1.2472E=0e a 4.278 72.193
- ~ ~ FROM
-~~~
't.2472E=0e TU LT.0W.EW. 1.3980E=04 1 535 72.727 FROM 1.3940E=0s 10 LT.OR.f0 1.55etE=0e 7 3.783 76.471 FROM 1.558tE=0e 70 LT.UW.to. 1.7el5E=0e 8 ~~ -
5.276 ~~ 80.749 ' ~ ~ - - - ~~ ~ FROM G7e15t=0470 ~LT.OR.tG. 1.9ee5E=0e' ~-' -~ ~ 6" 3.204 83.957 ~ ^ PROM 1.9465E=ce Tu LT.UW.to. 2.tF56E=ce 6 3.209 b7.166 FNum 2,1756E=0e 10 LT.uw.tu. 2.e317E=ce e 2.139 e9.395 ~~~-
~^ FROM '- 2.e317E=ce TO LT.OR.EQ. 2.7179E=ce 6 3.209 92.513 FRum 2.7179E=0e TO LT.ON.EU. 3.0378E=ce 3 1.6os 9e.11s FROM 3.0378E=0e TO LT.OR.EG. 3.3953E=0e ~
a - 2.139 96.257 ~ ~ FROM--~3.3953E=08 70 LT.04.EQ."~ 3.'7950E=0e ~e T 139 ^ 98.396 FNUM 3.7950E=ce 10 LT.uM.E9 e.2416E=04 1 535 98.930 FNum 4.2ej6E=0e TO Lt.UN tu, e,7eV9E=Um u 0.000 98.930 - FNOM e.7409E=0e Tu LT.uw.tu. 5.2939E=ce 0 0.000 9P.930 FROM 5.2989E=0e fu LT.UR.EW. 5.92deE=os 0 0.000 98.939 PROM 5.9226E=ce fu LT.OR.EG. 6.5798E=ce 2 1.070 100.000 TUTAL 187 Numb [W OF 2ENu ENTRIE S 63v3 alH NuMHER UF WAL10 OsSLRValluh3 PtN aVLHAGING INTENWaL e 1
~
50.00 PENCENT Pu1NT 9.U16L-05 55.00 PEhCLNI PulN1 9.9 21E =0 5 "" 60.00 PERCENT PulNT 9.957E=u5 e5.00 PENCENT POINT 1.otlE=0e 70.00 PEdCENT POINT t tabt-ce 75.uu PEwCLN1 PO1HT 1.485E=0m eu."o PtNCENT PO[wi 1.783t=9e 55.00 PEkCENT Pu1N1 2.015E=ce 90.00 PERCENT Puthi 2.se0E=U* 95.00 PEMCEN1 Pu1NT 3.160E=ue 72.76 PENCENT Pulhi 1.e26t=Um (Nhc IELMNltaL POSIlluN = NELa11vt ConCLNIR411bN PkOda5]LIIT) __
+
ii) <- IT SMICON (ATMuSPMERIC UISPERSION Fu3 D6A EVALUATIUN8) = YANMEE aiumIC ELECTHIL Cu tmOD 03, U7/28/78) 11/2e/78 PatiE 45 my 1977 12 m0NIN3 = GROUND = LEVEL NELEa3E = vaRIsulES NEPLaCED - E*CluS10N area O' . , OLLia=T stab!LITY MODEL O o0=N=INo SECTOR =NN samaa Caire teECea3) = PNu8a#1LITv 018tN18uTIO=8 O(METERS)'s 610.0 ~ SECTOR avENaGE VALUE8
~ ~ ~
= l-M0um AVERAGES O
" ~ ~ ~
; FREWUENCY DISTRI8UTIuN RaNbE NUMBER OF PENCENT OF COMULATIVL
~~
,O 088ENVST10N8 TuTal 088 PEaCtN
'i 2~
-~ ~'
F#0M e 59e2E=06~ TO LT.04.EG; e.985aE=06 ~ ' - ' - ~ ~ 1.070 ~ 1.070
~
() FROM e.985eE=06 10 LT.ON.Eu. 5.eU99E=06 3 1.60s 2.67e 4 ' - ' ~ FROM 5.4099E=06 TO LT.ON.EG. 5.8795E=06 0 0.000 2.6Te j FROM 5.8705E=06 TU L1.UR.EU. 6.379&E=06 2 1.070 3.743
~' ' ~ ~ ,() FNum 6.370eE=06 TU LT.ON.EW. 6.9128F=06 2 1.070 4.813
- PROM 6.9128E=06 TU LT.ON.EG. 7.5014E=06 0 - '
0.000 e.813
~~~ 5.348 FROW ~~7.50tet=06 TO LT.OR.EO.~ '8.teu2C=06 535 ~
d) FROM 8.teO2E=06 fu LT.ON.EW. 8.8333E=06 11 5.862 11.230 3 ~ ' FNOM 8.8333E=06 TO LT.UM.EU. 9.58S4E=U6 8 2.139 13.369 FROM '9.5854E=06 To LT.OR.EG.' 1.ce02E=05 5 2.67e 16.0=3
- - ' - - - ~
, () FROM 1.0402E=05 10 LT.OR.EG. 3.12eFE=05 e 2.139 18.182 FROM 1.1287E=05 70 LT.ON,EW, 1.2248E*05 ~~5e 2.67e '~ 20.856
FROM ~ 1.2248E=05 ~Td LT;0R.EO"~1.3291E=05 2.139 22.995
~ ~ ' '
.O FRON 1.329tE=05 70 LT.ON.EG. 1.ae23E=05 6 3.209 26.203 1.se23E=05 70 LT.OR.EU. 1.56SIE=0S PROM 8 4.278 30.e81
~ ' FROM 1,5651E=05 Tu LT.OR.EG. 1.690eE=05 6 3.209 33.690
,O PROM 1.698eE=05 Tu LT.OR.EG. 1.843cE=05 7 3.743 37.433 PROM 138430E=05 To LT.ON.EG. 1.9999E=05 9 a.813 42.2e6 j FROM~~'1'.9999E = 05 ~TO LT.OR.EQ s 2;17 02E=05 ' ~~~ ~ ' ~ ' ~ 15 ' ~ " ' ~ ~ ~ ~ 8 ; 0 2 8 ~ -- ~ - 5 0.267 ' -~ ~
" ' ' ~
'Q FNOM 2.1702E=05 Tu LT.ON.EO. 2.355UE=05 11 5.882 56.150 FROM 2.3550E=05 T0 LT.ON.EG. 2.5555E=05 3 1.604 57.75e
~~ PROM ~ '2.5555E=05 TO LT.OR.EG. 2.7731E=05 11 5.882 63.636
"~7
() FRom 2.7731E=05 fu LT.UN.Ew. 3.0092E=05 6 3.209 66.845 FROM 3.009dE=05 70 LT.ON.EO. 3.26SeE=05 5 2.674 69.519 FROM 6265ef=05 7 0 LT;0R.EO. 3.5435E=05' ~ ~5 ~ ~~ ~ -'^2.674 ~ ~ ~ ~ - ~7 2.19 3 ^ - ~ ~ ~ ' ' ' ' Q FROM 3.543SE=05 To LT.uM.EU. 3.8eS2E=05 7 3.743 75.936 FROM 3.8e52E=05 70 LT.ON.Eu, e.17d6E=05 e 2.139 78.075
~ ~ ' FNON 4.1726E=05 TO LT.OR.E9 4.5279E=05 e 2.139 80.214
~~ ~ ' -
g) PROM e.5279E=05 fu LT.ON.EU., e.913eE=05 7 3.743 83.957 ; FROM e.913eE=05 Tu LT.04.EG. 5.3318E=05 7 3.743 87.701 FROR ~ 5;1318E=05 TO LT;0R;Eo;-'~5.7857E=05 " - ~~--"~~6~-- ~ ~ ' ~ ~ 3.209 - ~ ~ 90.909 ~ ~ ^
- ~ ~ ~
() FROM 5.7857E=05 10 LT.OR.EG. 6 2784F=05 6 3.209 94.118 FROM 6.278eE=05 T0 LT.ON.EG. 6.8130E=05 e 2.139 ' ~ ~ 96.257 FROM-' 6.8130E=05 ~TO~LT.04.E0 ~7.393tE=05 1 535 '96.791
~ ~ ~ " '
C3 FROM 7.3931E=05 70 LT.04.Ee. 8.0226E=05 2 1.070 97.861 FROM 8,8226t=05 TO LT.OR,E9 8.6S8eE=05 4 2.139 100.000 CD TOTAL 187
~~- ' MUM 8ER OP ZERD ENTRIE8 8303 NIN NUNSER OF VALID DSSERVATIONS PER AVERASING INTENVAL e 1
~~
O 50.00 PERCENT PUINT 2.167E=05 55.00 PERCENT POINT 2.3e8E=05 60.00~PE# CENT ~ POINT 2.620E=05 65.00 PENCENT POINT 2.815E=05
' ~
, C 70.00 PENCENT PutkT 3.509E=05 75.00 PENCENT POINT 3.758E=05
~
80.00 PERCENT POINT e.397E=US 85.00 PENCENT PUINT 5.046E=05 "90.00 PERCENT Pu!NT 5.609E=0S 95.00 PENCENT Pu1NT 6.602E=05
~ ' ~ ' ~
O 72,74 PENCENT POINT
'3.642E=05 (NRC TECHNICAL POSITION
- RELATIVE ComCENTRaTION PROSA81LITV) ,,,
U -
O _ _. SM1 Da (CTMO5PMERIC DI5 PENSION FOR D::A EVALUATIONS) = v w it ATOMIC ELECINIC CU MD v3 u7/24/7M) 11/ds/Fo PaGE GO
, NY 1977 12 MONTM3 = GRUUND*LEvtL MELLA3E =
VARIABLES NEPLACEu = EXCLUSION AWEA DLLTA=T Sis?ILITY puoEL _ , [] 00ahmIND BECTOR Nw 4RuuMD= LEVEL CMI/G (SEC/M3) = PROBABILITY DISTWIeuTIUNS ctMETERS) e 610.0 PLUME CENTENLINE VALUES = 1*MuuR AVERAGES ]
- ' ~ ~
FREQUENCY DISTRIBUTION MANGE NUMBER OF PENCENT OF CUMULATIVE [) . 083ENVATIONS TOTAL 0b8 PERCENT
~ ~
FROM 1.0109E=05 70 LT.OR.EQ. 1 143eE=05~ 1~ 340 340 f.) FROM 1.te3eE=05 Tu LT.0W.E9 1.2933E=u5 0 0.000 3eo FROM 1.2933E=05 70 LT.UM.EQ. 1.codeE=n5 0 0.000 3eo
- ~~ FROM 1.et28E=05 Tu LT.OR.EW. 1.65e5E=05 0 0.000 3eo
~~-
D FROM 1.6545E=05 TO LT.OR.EQ. 1.871eE=05 0 0.000 3eo FROM _ 1,871eE=05_TO LT,0R,Eu,_ 2.1167E=05 ___ 0 0.000 340 2.1167E=05 70 LT.OR.EQ. 2.39etE=u5 FROM 1 3e0 680 C) FROM 2.39 ele =05 fu LT.uk.EW. 2.7079E=u5 0 0.000 .e80 FROM 2.7079E=05 TO LT.OR.EG. 3.062eE=05 0 0.000 680
~~~FROM 3.0628E=05 TO LT.OR.EQ. 3.4ee2E=05 6 2.041 2.721
~ -
C) FROM 3.ute2E=05 TU LT.0R.EQ. 3.9153E=05 10 3.401 6.122 FNOM 3.9183E=05 TO LT.OR.EW. e.e319E=u5 ~
~ ~ ~
6 ~ ~~~ 2.oet 8.103 ~ e 4314E=05 10 L T.OR.EG. 5.0127E=05
- ~ ~ ~ ~~
FROM 15 ~ 5.102~~~ ~1 3.205 C) FROM 5.0127E=05 Tu LT 0h.EW. 5.6697E=05 le e.762 18.027 FhuM 5.0697E=05 TO LT.OR.EQ. 6.4129E=o5 6 2.0e1 20.066
~ ~FROM~ 6.e129E=05 TO LT.OR.EQ. 7.253eE=05 26 8.844 28.912 3 FROM 7.253eE=05 Tu LT.04.EQ. 8.2041E=05 17 5.782 34.694 FROM 8.2041E=05 TO LT 9.279eE=05 ~~--'- 5 1.701 36.395 FROM 9.2794E=05 TO~LT,Ud.EQ0R.EQ.t_ 1.'0496E=ce 50.000 -~
~ '-
'- 40 13.605 ~ ~
C) PROM 1.0e9eE=04 70 LT.04.EW. 1.1871E=0e 28 8.163 58.163 FNOM fu LT.0M.EG. 1.3e27E=0e 11 3.7e1 61.9u5
~~~ FROM -1.3e27E=0e 1.1871E=0e TO LT.ON.EQ. 1.5187E=0e 20 6.803 68.707
- ~ ~ ' ~ ~
C) FRUM 1.5187E=0e TO LT.0R.EQ. 1.7178E=0e 9 3.061 71.769 FROM FROM 13 7178E=04 TO LT.OR.EG. 1.9e29E=04-1.9429E=0#7U LT.OR.EQ. 2.1976E=04
- ~~ ~-- 21 ~--- 7.1e3 ~~ 78.912 - ~ ~~
11 ~~3.7e1 ~-~ 82.e53 C) FROM 2.197eE=0e 70 LT.OR.EQ. 2.eu56E=ce le e.762 87.415
~
FROM 2.e85et-ce Tu LT.ON.EQ. 2.8114E=0e 11 3.7e1 91.156 FROM'-~ ~ 2.811 e E=0 e TO LT.OR.EW. 3.1799E=04 11 3.741 94.898 C) FROM 3.1799E=0e 70 LT.OR.EG. ,3.5907E=04 e 1.361 96.259 FROM 3.5967E=0e TU LT.OR.EG. e.0681E=0e~~ ~ -~ ~ 3 1.020 -97.279-
~0.000
~ ~ ~ ^
FROM e.0681E=0e 7 0~C.ON.EQ. e.6013E=04 C -~
~ ' - -
97.279 ~~~ () FROM e.6013E=04 70 LT.OR.EU. 5.20eeE=0e 1 3e0 97.619 FROM 5.20eeE=04 fu LT UH.EU. 5.8865E=ue 1 .3eo 97.959 5.8865E=0e TO LT.uR.EG. 6.6581E=04 FROM 3 1.02u 98.950 g FROM 6.6581E=ce Tu LT.uM.EG. 7.5301E=De 0 U.000 98.980 FkUM _ 7.5307E=0e_ Tu LT.uN.EQ. 8.e481E=04 3 1.020 100.000 _ , TOTAL 294 NUMBER OF ZEku ENTHIEs d19o MIN mundEN OF WALID 08bEdv4110NS PER AVERAGING INTERVAL = 1 50.00 PLNCENT PulNT 1.05^t-ce 55.00 PLNCtNT Pu!NT 3.13dE=ce 60.00 PEktENT Pu1NT
~~~
1.27dt=ue 65.30 PERCENI PulNT 1.43eE=04 70.00 PEHCENT PUINT 1.595E=0* 75.00 PEWCENT PUINI 1.851F=0e 60.00 PEkCENT Pulaf 2.018t=ou e5.uo PENCENT Pu1NT 2.d34E=0m 90.00 PERCENT PUINT 2.631t=ue 95.00 PEhCENT Pu1NT 3.29eE=Us 82.67 PENCENT Pu1NT 2.216t=ue thWC TECHNICAL POSIIION = HELATIVE CONCENIHATION PRue AB ILI T Y) _ ._ ~
-8KICUM (ATMOSPMENIC U18PERSION FON DBA EVALUATIONS) = YANAEE AIDMIC ELECTRIC Cu (m00 03. 07/2e/76) 11/24/7e P a t.E 47
,_ MY 1977 12 MUNTHS = GROUND LEVEL NELEASE = WARIABLES MEPLACEu = EXCLUSION ANEA (
DElla=T 31481LITY MODEL DOWNw!ND SECTOM Nm GAMMA CHI /O (SEC/M3) = PRumA61LITY DIS 1NIBUTIONS ( 0(MtTER8F's 610.0- -~ SECTuR AvgAAGE VALUES =
~
^ !=MUUN' AVERAGE 8
~ ~ ~ ~ -
~~~
r FREGUENCY DISTRIBUTION RANGE NUM8ER OF PENCENT OF CUMULATIVE
~ '~
088EkVATION8 TOTAL 063 PENCENT F10M e.729eE=06 TuTT.ON.E3 5.1567E=06 3 ~
~ ~ ~
F004 1.020 1.020
~ ' ' '
5.1567E=06 To LT.OR.EQ. 5.622eE=u6 1 3a0 1.361 FNOM TO LT.ON.EG. 6.1399E=06 FROM~'4.1309E=06 5.6228E=06TO LT.OR.EG. 6.6850E*06 0 0.000 1.361 4 1.361 2.721 FNOM 6.6850E=06 Tu LT.ON.EU. 7.2891E=o6 8 2.721 5.442 FEOM 7 TU LT.OR.EU. 7.9478E=06 7 2.381 ~ FROM 7.,2891E=06--~T0 9478E=06 l f.OR.EQ. 4.6661 E=06 ~
~
7.623 FKUM '8.6661E=06 Tu LT.ON.EG. 9.4e92E=06 13 4.422 12.245
~ ^
'~~
1 340 12.565 - FROM 9.4492E=06 70 LT.OR.EQ. 1.0393E=05
~ ~ FROM 9 3.u61 15.646 F;0M 1.0303E=05 To LT.ON.EQ. 1;125aE=05 7 2.381 18.027 ~-~ ~ ~
1.1234E=05 Tu LT.ON.EG. 1.2250E=05 5 1.701 19.728 FROM 1,2250E=05 70 LT.ON.EG. 1.3357E=05 5 1.701 21.829 FROM 1.3357E=05 Tu TT;UR.E W ~1;a56eE=05 ~ ~ ~~ 6 2.041 ~ ~23.869 FROM 1.4564E=05 TO LT.ON.EW. 1 5880E=05 8 2.721 26.199 ^ F UM 1.5880E=05 Tu LT.UN.E9 1.7315E=05 8
~ ' ~ ~ ~ FROM 2.721 28,912
't.7315E=05 70 LT.OR.EG. 1 8880E=05 18 6.122 35.034 ' ' ~ ~ ~ -
PROM 1.8880E=05 TO LT.OR.EQ. 2.0586E=05 6 2.041 37.075 ; FCOM 2.0586E=05 10 LT.OR.EU. 2.2446E=05 15 FROM 2;2486E=05- To LT.OR.EQ. 2;4475E=05 - ' to' 5.102 ~ ~ - ~ _-- e2.177
3.401 45.578
*~ --
FROM 2.ee75E=05 fu LT.ON.EO. 2.6086E=05 8 2.721 48.299 i ^ FEDM 2.6686E=05 To LT.OR.EG. 2.9098E=05 18 6.122 54.422
~ FROM ' -^ 249 094E=05 TO LT.OR.EO. 3.1728E=05 7 2.381 56.803
'~
FEOM 3.1728E=05 fu LT.ON.EG. 3.a595E=05 F"UM 3.4595E=05 10 LT.OR.EG. 3.7721E=05 to 18 3.401 6.122 60.20e ( FIDM 67721E=05 7 0 ET;0R;EG.~ 4;1130E=05- ' ~ ~ - ~ ~ 66.327 9 ~3.061- ' 69.388 - ---
~ ~ ' - ~
FROM 4.1130E=05 TU LT.ON.EG. 4.8847E=05 9 3.061 72.aag FNOM a.48e7E=05 70 LT.ON.Eu, s.8900E=05 ( 17 5.782 78.231
~ ~ FKOM a.8900E=05 'TO LT.0R.EG. 5.3319E=05 17 5.782 84.014 FROM 5.3319E=05 ~~ LT.UR.EU. 5.8138E=05 19 FROM 6.a63 90.476 s 5.8138E=05 10 LT.ON.EG. 6.3392E=05 6 2.041 92.517 rROF6;3392E=0570 LT;0R.EU;-~T.9121E=05 - ~ ~ ~ ~ ~ ~7" ~
~ ~ ~ 2.381 ' 9 4. 8 9 8 ~~ ~--- -
FKUM 6.9121E=05 70 LT.0W.EO. 7 5367E=05 e FnUM 3.061 97.959 s 7.5367E=05 TU LT.OR.E9 8.2178E=05 1 340 98.299 FROM--- 8;2178E=05 70' LT.OR.EU; 8.9605E=05 ~1 340 98.639
'- ~
F2OM 8.9605E=05 TU LT.OR.Ee. 9.77o2E=05 2 680 99.320 t FCOM 9.7702E=05 TD LT.OR,EG. 1.0592E=04 2 650 100.000 TOTAL 294 (
~ ~ ' ~ - NUMBER OF ZERD EN7RIE8 8196 MIN NUMBER OF VALID 088ERv4TIUN3 PER AVERAGING INTERVAL e 1
~~
L 50.00 PENCENT POINT 2.815E=05 55.00 PENCENT POINT 2.975E=05 60.00~ PERCENT POINT 3.a17E=05 65.00 PERCENT POINT- 3.760E=05 '~- 70.00 PENCENT Pu!NT 4.175t=05 75.00 PENCENT POINT 4.609E=o5 80.00 PENCENT POINT t
~
4.915t-US 85.00 PENCENT POINT 5.347E=05
.90.00 PENCENT POINT 3.765E=05 95.00 PERCENT POINT 7.039E=05-
~
L 82.67_PENCENT PUINT 5.271t=05 (NNC TECHNICAL'PuSITION = RELATIVE CONCENTRATION PR00s51LITY) _ k
. 8AIMON (ATMOSPHENIC DISPEN31uw FUw osa EVALuaT1uns) -
VAnnEE ATOMIC ELECTRIC CO (MOD v3. 07/24/76)
' . 11/2a/7s PAut .40 ,
My 1977 12 EUNIM5 = GNuumD= LEVEL NELEASE = VARIACLES NEPLACED - EkCLUSION AMEA DELTA =i STAWILIlv MOOLL __
). 00mhw!ND SECTOR NMW GNuUND*LEVLL CHI /O (SEC/m3) =
PRQ8 ABILITY DISTNieUTIUNS O(METERS)~s-610. 0'~ " PLUME CENTERLIhE VALUEin = t= HOUR AVERAGES
~ ~ ~
s
~ ~~~
FRE90ENCY DISTRI80 TION WANGL NUNHE9 OF PERCENT OF CUMULATIVE
~ ~ ~ ~
3 088tRVAT10NS TOTAL Des. PENCENT
~
FNOM-7.2840E=06 T U'L T'.UR . E Q . ~ 8.3040E=06 1 .15e 154
~
FRUM 8.30e0E=06 70 LT.OR.EG. 9.4616E=06 1 15e FROM .308
- 9.a616E=06 TU LT.UN.EO. 1.07BIE=05 0 0.000 308-
~ ~ ~ ~-PROM 1.0781E=05 70 LT.OR.EG. 1.2283E=05 0 0.0vo ~ ~ ~ ~ ~
FROM .308 1.2283E=05 TO LT.ON.EO. 1.3996E=05 1 154 462 FROM 1,3996E=05~Tu LT.ON.te, 1.5947E=05 0 0.000 462 FROM~~'t. 59a7E = 05 10 LT.uN.EG. 1.8170E=05 1' 154 ' .615 ' PROM 1.8170E=05 TU LT.OR.EG. 2.0703E=05 1 15e 769 FROM 2.0703E=05 Tu LT.OR.EO. 2.3589E=05 1 .154 923
~~ FROM -'2.3589E=05 70 LT.OR.EG. 2.6877E=05 4 415 1.536
~~~
FRUM 2.6477E=05 TU LT.uR.EG. 3.042eE=05 5 769 2.308 i 3.0624E=05 TO LT.UR.EG. 3.8893E=05 9 1.355 3.692 PROM-3.4893E=05^~ TO L T.ON.EG.~ FR04 3.975eE=05'
~ ~
15 ~ 2.308 '~ ~ ~ ~ ~ 6.000'
~
FNUM 3.9758E=05 TU LT.OR.EU. 4.53u0E*05 20- 3.077 9.077 FNOM 4.5300E=05 Tu LT.04.Eu, 5.1615E=05 23 3.538 12.615' FROM 5.1615E=05 70 LT oR.EO. 5.8811E=05 26 a 000 16.615-
~~~
FROM 5.8811E=05' TO LT.ON.Eu. 6.7009E=u5 52 FNON 8.000 24.615 6.7009E=05 Tu LT.OR.EO. 7.6351E=05 79 12.154 36.769 FROM 7.6351E=05 TO'LT.0R.EQ.~ 4.699eE=05~ ~~
~ 3a
~
~ '5.231' - 42.000 '~~ -' - "~
, FROM 8.699eE=05 Tu LT.ON.EW. 9.9122E=05 3e 5.231 47.231 FROM TU LT.ON.EG. 1.229eE=04 136 FROM~9.9122E=05 20.923 68.154 1.129eE=ce TO LT.OR.E9 1.2868E=ce 47 7.231 75.385
~~~
- FROM 1.2868E=04 TO LT.UN.EQ. 1.4662E=0a 19 2.923 78.308 FROM 1.46e2E=0a 70 LT.ON.E9 1.6706E=ce 23 FROM-3.538 --'~ 81.est 1.6706E=04 7 0'LT 04.EG. 1.9035E=0e ' - ~ ~ 23 - - ~ . ~ ~ ~ ' ' 3. 5 3 8 ~ ~ 45.385~~~ -
'FROM 1.9035E=04 TU LT.04.EW. 2.16e9E=0e FNOM 18 -2.769 88.154 2.1689E=ce TO LT.uN.EQ. '2.4712E=ce 22 3.355 91.538
- ~ ' ' ~ ' 'FROM~ 2.4712E=ce TO LT.OR.EO. 2.8157E=04 FROM 7 1.077 92.615
~ ~ ~ ~-
2.8157E=0a fu LT.ON.EO. .3.20e3E=0e 14 2.15e 94.769 l FROM 3.2083E=04 TU LT.OR.EG. 3.6555E=ce ~~ ~ 3 462
~ ~ - ' ~. 95.231 FROM~3.6555E=6a- TO'CT.OR.EG.- 4.'1651E=ce
~
FROM e.1651E=0e 70 LT.ON.Eu, e.7457E-04 5 9 769~ ~~ 96.000~~ ~ ~ ~ FNOM 1.355 97.385 a.7457E=0a Tu LT.UR.EW. .5.a073E=04
- 615 98.000 FRUM 5.4073E=04 10 LT.UN.EQ. 6.1611E=04 2 308 98,30s ~~
FROM 6.1611E=0s TO LT.ON.EG. 7.02c0E=U4 7 1.077 99.385 FROM 7.0200E=04 _Tu LT.uN.EE. 7.929eE=04 4 .t15 100.000 _ _ _ _ . . _ TOTAL 650 i NUMBER OF ZERO LNik1ES 78eo MIN nuMdEN OF WALID ObbERvATION3 PEN AVENAEING 14fEhWAL = 1 6 50.00 PERCENT POINI 9.927L=US 55.00 PENCt NT POINT 9.955E=u5 60.00 PENCENT Pu!NT 9.es2E=05 65.uu PEHCENT POINT 1.056E=04 ' ~ ~ ~ ~ 70.00 PLWCENT PUINT 1.162t*04 75.00 WEkCEN1'PulN1 1.27aE=0e 80.00 PtNCENT Pului 1.5e2t=04 e5.99 PEhtt N T 90141 1.85ut=ce 90.00 PERCENT PulNT 2.337teve 95.00 PEhttN1 POINT 3.600E=0e 92.16 PtkCEnt pu1NT 2.628t=U4 (NMC IECMm1 CAL PUSIlluN __ = RtL&llWL Cu%CtklNATIum FNuua8ILiff) .-
-9 % -
g ,- a
+m'- V
- y s
.a ae a
)
, , 8KI%N (ATMusPHEh!C UISPENSION FOR DDa EVALUATIONS) = YAnxEE A10MIC ELECINIC CU (mud 03. 07/24/763 11/24/Fe PAGE 49
~
)
ny 1977 12 MUNips - GNUUNO-LEVEL MELEASE = WARIABLES kEPLACED = EXCLusIUN ANEA DELTA =T SIABILITY MODEL r . _ .
)- 00nNMIND SECTOR NNN GAMMA CHI /W (SEC/M3) = PNuBASILITY DISTRIBUTIONS D(METER 8)~~s-610.0 '8ECTOR AVENAGE VALUE5 - !=HOUN AVERACES
~ ~ -
)
~ ~~ ~
FREQUENCY DI8TRIBUTION RANGE NUM8ER OF PERCENT OF CUMULATIVE
- --~
08SERVATIONS TUTAL 085 PENCENT FRO F 3.6072E=06 3.9831E=06 TU LT.OR.EQ.
-' ~
'2 308 .308
~~
FROM 3.9831E=06 TO LT.ON.EO. 4.3952F=06 1 154 462 FROM 4.3982E=06 TU LT.ON.EW. 4.8565E=ob 2 308 769
~FROM 4.8565E=06 TO LT.ON.EQ. 5.3626E=u6 3 462 1.231 FROM 5.3626E=06 TU LT.ON.EU. 5.9214E=06 11 1.692 2.923 FROM 5.9214E=06 TU LT.ON.EG. 6.5385E=06 7 1.077 4.000 6.5385E=06 70 'LT.OR.EQ.-- 7.2199E=06
~
FROM 6 923 4.923
- '~
FROM 7.2199E=06 TU LT.OR.EG. 7.9722E=o6 11 1.692 o.615 FNUM 7.9722E=06 TU LT.OR.Eu. 8.8030E=06 15 2.308 8.923 FROM' ~8.8030E=06 fu LT.OR.EQ. 9.7204E=06 16 2.462 11.365 FROM 9.7204E=06 TO LT.bR.EG. 1.0733E=u5 27 4.154 15.538 FROM 1.0733E=05 TO LT.UR.EQ. 1.1852E=05 ' 21 ~ 3.231 18.769 FROM 1.1852E=05-~TO LT.OR.EQ. 1.3087E=05
~
22 ~~ ~ ~ 3.385 ~ ~ '22.154 FROM 1.3087E=05 TO LT.OR.EQ. l.4451E=05 38 5.846 28.000 FROM 1.4451E=05 TU LT.ON.EU. 1.5957E=u5 43 6.615 34.615
~~~ ~ FROM 1.5957E=05 TO LT.OR.EQ. 1.7619E=05 36 5.538 40.154
~ ~ " - -
PROM 1.7619E=05 TO LT.OR.EU. 1.9456E=05 33 5.077 45.231 FROM 1.9456E=05 TU LT.ON.EU. 2.1483E=05 31 4.769 50.000 FROM 2.1483E=05--TO IT.OR.EQ. "2;3722E=05 ~~ 40 ~~ ~ 6.154 ~ ~ - - ~ ~ ~ ~ ~56.154
~ '~
FROM 2.3722E=05 70 LT.OR.EW. 2.6194E=05 37 5.692 61.846 FROM 2.6194E=05 TO LT.0R.E9 2.8924E=05 44 6.769 68.615
~ FROM 2.8924E=05 TO LT.OR.EQ. 3.1938E=05 29 4.462 73.077
~ - - ~ ~
FROM 3.193eE=05 TU LT.ON.EQ. 3.526eE=05 34 5.231 78.308 FROM 3.5266E=05 TO LT.ON.EG. 3.8941E=05 23 3.538 FROH
~
3.8941E=05 TO LT.OR.EQ.- 4;2999E=05 ~ 17 - -- ~
~~
~~~2.615~ - ~'~ ~~ 84.462 81.846 -~'--"-~
FROM 4.2999E=05 70 LT.OR.EU. 4.745UE=05 23 3.538 88.000
~~ ~
FROM 4.7480E=05 TO LT.UN.EW. 5.2428E=05 15 2.308 90.308 FROM 5.2428E=05' TO LT.OR.EG. 5.7891E=05 17 2.615 92.923
~ ~ ~ ~ ' ~ ~ - -
FROM 5.7891E=05 10 LT.ON.EQ. ,6.3924E=05 17 2.615 95.535 FROM 6.3924E=05 70 LT.OR.EG. 7.0555E=05 6 923 96.462 FROM r a 0585E=05 TD~LT.OR.EG.-- 7.7941E=05
~
~7 ~-~ ~ - -~ ~ 1. 0 7 7 -~~ ~' 9 7 . 5 3 8 ~ -~ -- - ' - ~ - ~ ~
FROM 7.7941E=05 TU LT.ON.EG. 8.6063E=05 9 1.385 98.923 FROM 8.6063E=05 - TU LT.ON.EU. 9.5032E=05 5 769 99.692 FROM -^9.5032E=05 TO LT;0R.EQ;~ 1.0494E=04 0 0.000 '99.692
~~ ~ -----
FROM 1.0494E=04 TO LT.ON.EG. 1.1587E=04 1 154 99.846 FROM 1,1587E=04 70 LT.OR.EG. 1.2710E=04 1 .154 100.000 TOTAL 650
- - ' ~ ' ' NUM8ER OF ZERO ENTRIE8 7840 MIN NUMBER OF VALID OBSERVATIONS PER AVERAGING INTERVAL u 1
' - ~ ~ ~ -
50.00 PERCENT POINT 2.148E=05 55.00 PENCENT POINT 2.345E=05 60.00' PERCENT POINT ~ ~2.551E=05 65.00 PERCENT PDINT 2.749E=05
~~ ~~
70.00 PENCENT PUINT 2.967E=b5 75.00 PENCENT POINT 3.303E=05 80.00 PENCENT PUIhi 3.759E=ob 85.00 PERCENT PUINT 4.348E=05 90.00 PERCENT PUINT 5.117E=u5 95.00 PENCENT Po!NT 6.263E=05 ~ - - ~ ~ ~ _92.16 PERCENT POINT 5.620E=05 (NRC TECHNICAL PO8ITION = NELATIVE CONCENTRATION PRueABILITT)
SKICOM (ATKOSPPERIC UISPERSIUM fur D3A EVALUATIONS) = YANMEE ATOMIC ELECTRIC Cu (*UD u3 U7/24/75) 11/24/76 PAGE 50 NY 1977 12 MONTM3 = GROUND = LEVEL NELEASE = var!a8LES MEPLaCED = EXCLUSION area DELla=T Sta81LIrY MODEL
) D0mhWIND SECTOR aLL GRuuND= LEVEL CNI/Q (SEC/M3) = PRu8a81LITY DISTRI8utIONs
~~ ~
OlMETERS) -s 0.0 ~~ PLUME CENTERLINE VALUES = !=HOUM AVERAGES
)
~ ~ ~ ~
FREkufhCY DISTMISU11UN RANEE NUM8Ed 0F PERCENT OF CUMULATIVE
) OBSERVATIONS TOTAL OJS. PERCENT
~
6'~
- ~ ~
FROM t 7507E=06-~TOTT .OR . E Q .~ - ~2.098eE=06' ~~ 071 ~-~ 071
) FROM 2.0988E=06 Tu LT.OR.EG. 2.5160E=06 1 ,012 082 FROM ~~ 2.5160E=06 Tu LT.ON.EG. 3.0162E=06 0 0.000 082 3.0162E=06 TO LT.ON.EG. 3.615vE=06
~ ~ ~ - - - - -
FROM 3 035 118
) FRom 3.4159E=06 Tu LT.OR.EO. 4.3347E=06 0 0.000 .118 FROM--~4.3347E=06--TO LT.ON,EW,~ ~ 5.1965E=06 6 071 188 ~~
FROM 5.1965E=06 Tu LT.OR.EO. 6.2296E=06 18 212 .eu0
) FNOM 6.2296E=06 TU LT.0R.EG. 7,4680E=06 12 141 542
- ~ ~
FRom 7.e680E=06 TU LT.ON.EO. 8.9527E=06 7 082 624
~FROM ~~ 8.9527E=06 TO LT.OR.EO. 1.0732E=05
~- - ~ ~ ~ ~ -
2e 283 907
) FRom 1.0732E=US TO LT.OR.EG. 1.2866E=05 24 283 1.190 FROM 1 TO LT.OR.EQ 32 .377 1.567 FROM -- f,2866E=055424t=05- TO LT.OR;EQ.t__1.5edeE=05 l iR 4 9 0 E = 0 5 - ---- ~~ ~ s o ~
~~ ~~~~~ -
4 71 ~~ ~ - ~ ~ ~~ "-~~ ~ 2. 0 3 8 - ~ ~
) FROM 1.8490E=05 10 ST.OR.EG. 2.2166E=05 71 836 2.874 FROM 2.2166E=05 TO LT.OR.EG. 2.6573E*05 110 1.296 4.170
. -~~~ '-~FROM 2.6573E=05 To LT.OR.EQ. 3.1856E=05 215 2.032 6.702
~ ~'
D FNOM 3.1856E=05 70 LT.OR.EW. 3.8189E=05 401 4.723 11.425 FNOM 3 8189E=05 70 LT.OR.EO. 4.5781E=05 528 6.219 17.64= FROFe,5781 . E=05 TO~ LT.OR.EQ;-- 5;4 8 82E=05 ~~-~ ~ -- 586
~
'6.902'--~ '- ~ 24.547
~' -- --
U- FRum 5.4882E=05 Tu LT.0M.EG. 6 5792E=05 868 10.224 34.770
----- - FNOM 6.5792E=05 TU LT.04.EW. 7.8572E=o5 886 19.e36 e5.206 FROM' 7.8872E=05 TO LT.OR.EQ. 9.4552E=05
~- -
#11 4.841 50.0e7 D FROM 9.4552E=05 TO LT.0R.E9 1.1335E=04 1539 18.127 68.174 FROM 131335E=04 TO LT.OR.EU. 1.3588E=04 402 4.735 72.909
~ - ~~~- 3.1 10 ' ~~ -- -- " 7 6. 019 ' -
~ ~ ~ ~ ~
FROM 1.3588E=04~ To CT.OR.EQ. 1. 6 2 9 0 E = 0 4 ~ ~ -~~ - ~~- ~ 2 6 4- - ~ U FRUM t.6290E=04 TO LT.ON.EG. 1.9528E=04 389 4.582 80.601 FRuM 1.9528E=04 TO LT.OR.Eu, 3.3410E=0e -305 3.592 84.193 ' - ~ ~ ~ ~ " ~ ~
-- FROM -~ 2.3 s 10 E=0 4 ~TO LT.OR.EG. 2 806eE=04 213 2.509 86.702 g FROM 2.806sE=04 10 LT.ON.EO. .3.3644E=04 216 2.544 89.2e6 FROM 3.364eE=04 TO LT.OR.EG. 4.0332E=0e- - ~ 28C 3.298 ~ 92.544 470332E40s-~TOTT.0 R ;E Q . e.835UE=0a ~ 2.See
~ ~
FROM ~ ~216 95.088'- - 9 FNOM 4.535uE=ce TO LT.OR.EW. 5.7963E=0e 168 1.979 97.067
~ ~ "
FNOM 5.7963E=0e Tu LT.ON.EO. 6.9456E=04 te4 1.696 98.763 6.9886E=ce TU LT.OR.EQ. 8.33voE=04
~
FROM 69 813 99.576 f FNum 8.3300E=04 Tu LT.UN.EG. 9.9860E=0e 26 .306 99.882 FROM 9.9860E=0e Tu LT.ON.EW. 1 1827E=03 to .118 100.0c0 TulaL 8490
~
NUM8ER OF ZEHu EN1 HIE 8 27u MIN NUMBEM OF VALID DeStHvallums PEN avEMaGING 1hitaWaL = 1 i ~ ~ ~ ~ ~ 50.00 PENCENT Pu1MT 9.a43E=ub 55.00 PENCENI POINT 9.956t=05 ~ ~ ~ ~ ~ ~ , 60.00 PERCENT PUINT 1.ovoE=ce 65.00 PENCENT Pd1NT t.006F=o4 70.0u PENCENT Pu1NT 1.193t-ce 75.00 PENCENI Pu!=t 1.5J6E = 0 e
~
90.00 PERCENT PO1Mi 1.93te=ue 85.u0 PENCENI POINT ~ 2.549t=ue ~ 90.00 PERCENT POIN1 3.579E=ue 95.00 PENCENT POINT 4.757f-ce ALL SECIURS CUMdTNED = CHECK PNEVIOUS PaGES Fud DISTANCES
6 8% IRON (ATMus?MERIC OISPENStum fun une EVALuaT!uNS) = YANALE ATOMIL ELECTNIC Cu (ebo c5 97/2e/75) 11/24/78 PAGE 51
-- MY 1977 12 MumTH3 = bMUUND= LEVEL MELLA3E = VARIAeLES NEPLACED = EXCluS10N AREA DELTA =T STABILITY MODEL _ ) 00nNw!ND SECTON ALL 6AMMA CHI /u (SEC/M3) =
PNuGAeILITY DISTR 18uTION5 0(METENs) e 0.0- " SECTUR AVENA 6E VALUES - 1=MuuN AVERAGE 3
~ ~ ~
~
FREWUENCY D14TRIBUTION RANGL NUMRER OF PERCENT OF CUMULATIVL
' ~ - - ~ ~
) Ud3ERVATIONS TOTAL 088 PENCENT
~
FROM 2.1386E=06 Tu LT.uR.EW.~~ 2.4051E=06 5 ~^ 059
~~
- ~ ~059
) FROM 2.4051E=04 10 LT.uM.Eu. 2.7de9E=06 2 024 082
~~ ~ FROM 2,70e9E=06 Tu LT.UR EQ, 3.0421E=u6 0 0.000 082 FROM 3.0421E=06 To LT.OR.EG. 3.4213E=06 6 071 153
~~
p FROM 3.e213E=06 70 LT.ON.EG. 3.84F7E=06 16 188 .3e2 FROM 3 .8e77E=06 Tu LT.UN.EW. e.3273E=06 41 .e83 824 FROM e.3273E=u6Tu'LT.OR.EG.- e.8667E=06' '69~~ 813 1.637
~~-
9 FROM 4.8667E=06 To Lt.OR.EQ. 5.e733E=0e 71 836 2.473 FNOW
- ~ ~ ~ 'FROM ~~ 6.1555E=06 5,4733E=06 TOTo LT.uw.Eu. 6.1555E=06 149 1.755 4.229 LT,0R.EQ. 6.9228E=06 207 2.438 6.667
~~ ~ ~ ~ '
3 FCOM 6.9228E=06 Tu LT.0M.EG. 7.*857E=ce 339 3.993 10.660 PROM 7.7857E=06 70 LT.UN.EG 8 '502E=06 426 5.016 15.677 FROM ~ 8.7562E=06- TO LT.OR.EO,. ~ .Re76E=u6
) FROM 9.8476Ea06 70 LT.ON.EU. 1.1075E=u5 425 453 5.006 -~ ~ - '~ 20.68 3 ~ ~ -
5.336 26.019
~
FNOM 1.lo75E=05 70 LT.0M.Eu. 1.2455t=05 497 5.85e 31.873 FROM ~1.2e55E=05 Tu LT.OR.EG. 1.eUO8F=05 475 5.595 37.e68
~~
) FROM 1,e008E=05 TU LT.ON.EG. 1.5758E=05 516 6.075 PROM 1,5754E=05 e3.545 70 LT.ON.EW. 1.7718E=05 485 5.713 e9.258 FROM l .7718E=0570' LT.OR.EQ. 1.9926E=05 ee8 5.277 54.535 ~
~ ~ ~
) FROM 1.9926E=05 TO LT.ON.EQ. 2.2410E=US 417 4.912 59.ee6 FNOM 2.2410E*05 To LT.ON.EG. 2.52u3E=05 415 e.888 64.335
~FROM 2.5203E=05 TO LT.ON.EQ. 2.8345E=v5 364 e.267 es.622
~~ ~~~~-
) FROM 2.8345E*05 To LT.ON.EO. 3.1878E=05 29e 3.803 72.085 FROM 3.1878E=05 Tu LT.ON.EU. 3.5851E=05 339 3.993 FROM- T.5851E=05 TGTT;0R.EW. 76.078 e.032uE=05 321 ~~ 3.781 - ~ ~~~'79.859"~~ ~~
~ ~ ~ ~ ~ "
) FROM e 0320E=05 TO LT.ud.EQ. s.53#5E=05 274 3.227 83.086 f-~' PROM FROM e 5345E=05 10 LT.ON.EQ. 5.0998E=05 303 3.569 86.655 5.0998E*05' TO LT.OR.EQ. 5.735eE=05 285 3.357 90.012
~ ~ ~ ~ ~
) FROM FROM 5.735eE=05 TO LT.ON.EG. .6.e503E=05 6.4503E=05 To LT.0R.E9 297 3.498 93.510 7.2543E=05 184 2.167 95.677' i FROM7;254 3E=057~LT.0R.EQ.~- 8.1585E=05 ~ 214 ~
^
- 2. 5 21 --- 98.198'
~
F90M 8.1585E=05 Tu LT.OR.EO. 9.1755E=05 74 872 99.069 FROM 9.1755E=05 70 LT.ON.EW. 1.0319E=0e 36 424 99.494
- FROM 714 0 319E=0e -~TO LT.OR.ED. 1.1605E=0e 23 271 '99.764 j
- ~~~
FROM 1.1605E=0e Tu LT.OR.EW. 1.3052E=0e 9 106 FROM 99.870 1.3052E=0e 70 LT.OR.EG. 1.456eE=ce 11 130 100.000 TUTAL Se90
~
l - NUMBER OF ZERO ENTRIE5 270 MIN NUMBER OF VALID 088ERVATIONS FEN AVERAGING INTENVAL a 1
~ - ~ ~
b l 50.00 PERCENT Pu!NT 1.799E=05 55.00 PENCENT POINT 2.021E=05 l 60.00 PERCENT PolNT 2.252E=05 e5.00 PENCENT POINT 2.560E=05 -- % 70.00 PERCENT PulNT 2.959E=u5 75.00 PENCENT POINT 3.505E=05 80.00 P1RCENT Pu!NT 4.072E=u5 85.00 PENCENT POINT 4.856E=n5 90.00 PERCENT Pu!NT 3.645E=05 95.00 *ENCENT Pu!NT 6.968E=05 --~ 9 ALL SECTORS CumdINED = CHECK PREVIOUS PAGES FOR DISTANCES-
O a I SAIRON ( AT8tOSPHEN{C UISPERSIUN FOR Dea EVALUailom3) = YANAEE ATOMIC ELECTHIC Cu (Milo v3e U7/2e/T8) 11/de/Te pat E 52 f NY 1977 12 PUNIHS = GRUUN0=LEvtt NELEa3E - VARIABLES NEPLaCED = EXCLUSION ARta DELTA =T siam 1LITV MuoEL
)
SUMMANY = ACCIDENT UILUTION FACTORS PER NRC IECHNICAL POSITION =
!= HOUR AVERAGES )
DISTANCE PENCENT GRQuND= LEVEL CHI /W (SEC/m3)
~ ~ " -
SECTOR (METER 8) GAMNA CHI /O (SEC/m3) PU1NT (PLUME CENTERLINE MODEL) "~ ~ (SECTOR AVERAGE MODEL) ) N 610,0 98.e5 4.4130E=0e 6.6663E=05 NME 610.0 ~ 92 55 3.5971E=04
~ ~ ~ ' ~~ ~~
6.u3e3t=05
~
) NE 610.0 87.81 2.7330t=04 5.3739E=05
~ ~ ENE 610.0 88.00 1.9399E=os e.2323t=u5 E 610.0 87.10 3.1747E=de 5.3836E=05
~
~ ~ ~ ~ ~
) ESE 610.0 92.63 3.9360E=04 5.9392E=05 BE _619,0 95.33 4,6529E=44 6.6412E=u5 410.0 _ _ _ SSE 93.64 5.1268E=04 8 410.0 7.0398t=c5
) 92.50 e.7123E=0e 6.5978E=u5
~-~
SSW 610.0 89.e3 5.1331E=ce' 6.61355 05
~ Sh 610.0 86.08 3.9404E=os 5.62esE=05 ~ ~ ~~ ~ ~
WSW 410.0 71.06 1.149tE=04 m 1.1974E=u5 610,0 . . _ . - . - 73.47..- 1.1834E=04
- - .--_- _ 3.6221E=05 ..
Nu 610.0 82.67 2.2159E=ce 5.2712E=05 NNw 610.0 92 16 2.6278E=ce 5.6199E=05 g CRITICAL SECTOR 5.13 31 E = 041 7.0398E=05 . x '95 PERCENT VALUES 3 N 610.0 95.00 e.6500E=04 7.0185 Emu 5 NNE 610.0 ~95 00 - ' ~ ~ ~ ~ ~ ~ e.3869E=0e 7.0099E=05 NE 610.0 ~-~ ~ . 95.00 4.1885E=04 '- - ~ ~ ~ ~ ~ ~ ~~~ 7. 0 2 3 7 E = 0 5 ' '
~ - ~ ' ~
- ENE 610.0 95.00 2.8423E=0e 5.755cE=us E .
~ - - ' ~ 610.0 95.00 4.6657E=ce 7.2828E=05 E8E'~ 610.0 95.00 4.5311E=oe 6.5972E=05 ~ ~ " - ~
SE 610.0 , 95.00 4.3929E=04 6.3606t=U5 SSE 614,0 95.00 5.3909E=0e 7.2837E=05 5 6.5.6 95.00
"~
5.3940t=ce
-~ ~
7.2572E=05 SSW 410.0 95.00 5.9023E=0e 7.2964E=05 8m 610.0 95.00 5.9323E=0e
-m8of 610. 0 ~ --- ~ 95.00 ~ '~ 7.2920E=v5 5.6318E=04 7.274 5E=0 5 -~~
~~
w 610.0 95.00 3.6117E=0e 6.3508E=05 NNm 410.0 95.00 3.1602E=04 6.6017E=05 de 610.~0 95.00 '-- ~ 3.2942E=ce -- NNn 7.0388E=05 610.0 95.00 3.6003E=0e 6.2628E=05 .
~ CRITICAL ~ SECTOR ' 5.9323E=04 7.2984E=05
- -~
f alt. SECTORS CUMSINED 4.7573E=0e 6.9678h=05 s
.-.___._,__m_ _ _ _
, N4 n___..--_.-.__ __ m _ _ _ _ _ . . . _ _ _ - ~ - .2==,- .
r s- w ..e, .-, _.__..,,_y
1 Q Attachment 3: One hour EAB X/Q at 0.5% exceedance probability developed from Maine Yankee site meterological data , January - December, 1979 Contents as in attachment 2 : Results shown on page 52 t i p i i i
tutw0N (ATED$PMFett DisptkStow Fow n3A FwaluaffoNS) - van FF ATOMIC ELECTRIC CO tonu 03 12/05/78) 41/02/03. P&GE 1
- INPUT DATA LISTthG 2 3 4 5 6 7 0 Caeo 1 SEG. 1234567890123a567890123a5678901234567890123456789012345678901234567890123a567890 t '97 DME Moue ACCIDENT Cw!/o 1979 nata 610 METFe8-2 1 12 50 1 0 n 1 1 0 900.' n .' 45.00 0.0 400 280 0.0 a Iq1n, 10000e, 5 0.5 6 1.0 ,
7 (8u,F1,1,6W,F3,0,t6a,Fe,t,at,F4.1.23X,F3.2,2F2.0) a 2 e : 1- a 0 5 0 150 3 a88 9 S a.O . 90 90 15., 110. 50.6 In 1. 0.447 0.5556 =32. 1. 0.2235 0.2235 t 0 0 0 0 0 0 n 0 0 in Sn. 32 610.' 6tu'g 6to'g 6to'g 610E 6tu g 410, 610 610. 6t0. 610 610 610 i3 sto. 6to. 6to. o Og 0, 0 O. O. to o g og g 0 O. 6. O. 9 O. G. O. 15 ATTAC4 rwpr 3 - _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ . . . _ _ _ _ . . _ _m-__ _ _ _ __ _
is t hieu f 41*sinPHrp tr pt st*Festeev Fei# pHA F v at tla f f rintt) = V ars2 F F A llIM{r (( F.C Tii}C Cil ( =if tn n ), 17/pq/TR) _ ta g /pppn( pgqF g
>v t it- F Httlep a rr tfi[qi C W1/r3 go79 naT4 esin erfF99 4
Tsor -le ctst esp t i f'h ( I fiP T ) e t pt ee:.a s ed (1r Me th f >43 V PF f p f1pf tl InC]r et bErflatim atast v3FD a 12 taluf Csi*sivet trpf teep s- 50 es theis w traat vn t m rs't.ipeit s tP t Ifita (Inn) e I f fi% F r f 14 tet F ar igts t p g istas { {g F) e n SrarpFF yr eip tile: titr a) n FnHat ST glarm t o.1p un as pts pr tFe* (PFTFDS) a st . n n IsF Ptse seF t[P{TF.n MitfNf tAVFD ( PF I F 88 91 a 9n4,00 iT At w FutT vFe sici ty ("/*tri n 9,000n e n z iottet a n.t a r F N T kt'f t tilNs: kF i r.HT (MFIFPM) a 4 % , ti ts
' WF t F A *ll 64F I t'.64 i A Mitb F f;4 8 't **8t) (MFTEkSi's n,00 mas, FFFFCTivt etI"*F HF f t;pt altnwEn f*EffoS) s ann,no f A ttle 1F k t f r*PF se p itWF (ot GoF4 9 erFI WlHi a 2Rn,00
$ Tats FFFttirMt ut41 Cf1HTF t i trat#8Fr) e n, ni e l l, ti t iet, s co esq.sF r 1 T(1*I A[ Aora ( 9fJ.HF TF H S) a 3R30,un pl o t ti:CF $4F vitets kHirH 5ftILDIMC WSWF IS IGNfif Fft ,sn0nF406 r.4%M4 P4V F l*F Ql-fl 9 (PFW) p Hf) DEtaT{vF a nsatst)& NCF R Ff'O GAMMA CHI #4 seters.& w F t'F or Y A P ltNf14 k r F.
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- a= ccC CC E C a y, e e e* s e e T
*= 4 er J GGC GCO7 E 2 == ib a= > k F e *e e e- e e e e aC e of s as a a > CC C(C C c > e= 8 *=
0 W k e@ @ == V F F 2 5 J av K N C == ma # C V' F F *=e- C w *= e > w & C 4 Fm C Ee
> e O m e2 F.
E C Z L h C k e a **2 e C ** 2 e X Ekw e (> W .J E.* w F, *= > b .J e= T *= 6 (L e em M w e e e w C O > I w > ke C C
- ec 6CI
== e m 2 EL o= > kr ws en 2 I Ee h b b >7 C Pb % F, b
- 2 0 2 > W (L TC e 2 UC2 % EL F h O k O O U ; h> > e b *= 1VO C s E. m > 2 e s p= C> e C e K er e=
2 % 6
- b e == U C 2 C>% O e-O ei s > *= 2 g W F 4 .g g a .6 2 ,,) C2e
*= 2
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& I L k e6 2 5 . E 1 0C (L er b M == IL &
k' ** *= == m2m e b e6 *= 1 k eF E&m L 2 k kO>I F. > m h. k'> 2 ** C *= kF&CZ o= F. F %
- e Z U * * > : 7 .? == C O U2 Go % ~WO C
*= 0 > > 0& Oe E == 0 e Ci C uJ e= m e= k 2 i e, C
- e- 2 02
== e * == e 2 .J > >= > == ar e= u e= I 3 e e= p O W O C >3 k ke e > e *= 3 k e ee == k J ak e 3 a6 F L W 6 C (A C. k ** e O U L .L a a e= g. > C 2 CL *= C L
- e . k ? as %10 C > b T e6 0 h 6. C 2 2m;7C CFb
.1 e a .1 es >mIe 2 *= 3 0 e6 > CL as O2 0 k >>e ** E en & G L *= == EL e *= F 2 k : e= *= C. *A F. 1 a a b == C. e e 2 C & T *= e= 1 > F, 2 E & C>y = m. ==== > F, '.6 2 . 7S 4
CL C U M b baa2 3 E 6 e> .i D. 2a O U m 66 h > *= EL F 3 O C 46 &&k 6 4 0 e= C .6 C E. e. * * > E Ck& 4 5 O . 222 1. a= id 2 4 4==. a6 > a2 J e
- h 7 . = o= == 6 0 e
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= om is., m O.
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== w .
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==
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- 9. 177 wMm ta7 m 1At ut.h 796
*= tIse titeH R f3 7 9 *
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- to
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s e emwwwwwweemmme ,=wwmmemmmmmwe me A s wwwmmwwwwmwwwem CCCCCDCCCC SCC C COCC CCCC CC CCC CC Dw CCCCCC CCC CCCCC C eeeeeeeoeeeeoee e e e e e e e e e e e e e e. eeeeeeeeeeeeeee' erep opppoppp0 PO W. apppyoppepppeee eepappatepeO pp FCOF O pp D O ce@ cPP
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>> 9999999@@ @ ppp F 4 9 4 e e Op7p?FPPOPPDF99 2 %
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0 3h e= e everae o e e o 0ECA=PPNV e te eeee eeoe e e o 0-= eee eeeeeeee SAF G W > 2 m= 940 $ $ 8 0 wee p t 8 9 0 r= 9 0 0 O F C *C 4 6 SA t= 8 0 0 0 0 0- G t & 4 a F'
= C
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- i. ~
1079 nata Atn MFTFDS [ t IST fir H0 Holy METEnnotncical n4TA te00:q,7 MINO DtPFC u T Nf) TFMP afo WATFR S0t so n,' TEM Sic TH w!Nn ngo, pakcF spErn otFr SPEED DELT4 Y AIR,t w&T.Suor 80t_Ao v. SEspar SEO. TFw m,TrH RAD ClAMM ClaS9 Fle n* fM/SFC) (K/innet it) TFMP (C) (LY/"tN) IF GT,0 i 4 MONTH q ? 3 31A. 90,6 a.to . 4n 37.o 90{0 9.90 0 NNw t,83 ..sso 7,7m goe,nt 099.pt o
%1 on. 90.0 a.to . . an 37 o 90 go 9,00 D F 3.A7 . 87m 2,7m 090,03 909,c1 o
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- i tot._ 00,9 7.en .t,00 3t.n 99,o 9,00 0 F 3.31 -1, nom 1,A7 o90,nt 900,01 o I 751 793, 09.o te.tn .I.%o e7.n 90,0 o,90 C www 6.75 .t.6a7 m,5A co9,ut 999,01 o l'
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