ML23292A206

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1 to Updated Final Safety Analysis Report, Questions and Responses 372.1 Through 372.28
ML23292A206
Person / Time
Site: Susquehanna  Talen Energy icon.png
Issue date: 10/12/2023
From:
Susquehanna
To:
Office of Nuclear Reactor Regulation
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ML23291A105 List: ... further results
References
PLA-8081
Download: ML23292A206 (1)


Text

SSES~FSAR

QUESTION 372.1 Provide any revisions to the extreme meteorological values presented in the Susquehanna Safety Analysis Report that may be necessary as a result of meteorological events occurring subsequent to 1974.

RESPONSE

Tables 2.3-17 and 2.3-33 have been revised to include this information.

Rev. 46, 06/93 372.1-1

SSES-FSAR

QUESTION 372.2 Tables 2.3-50 through 2.3-62 provide a precipitation wind rose for the Susquehanna site. During the winter months, the occurrence of invalid observations is quite frequent (e.g.,

January & February - 22%, December - 46%). To what may these invalidations be attributed? Provide a list of the periods of significant outage, including the cause, and discuss the effect of these outages on the monthly data summaries.

RESPONSE

The frequency of invalid observations during the winter months is due to the freezing of the weighing rain gage, and/or the anemometer or wind vane. The following difficulties were noted:

November 1973 - Freezing of anemometer & wind vane December 1973 - Freezing of anemometer & wind vane January 1974 - Freezing of anemometer & wind vane February 1974 - Freezing of anemometer & wind vane December 1974 - Freezing of rain gage; freezing of anemometer & wind vane December 1976 - Freezing of rain gage.

These outages result in a smaller data sample for the monthly summaries.

Rev. 46, 06/93 372.2-1 SSES-FSAR

QUESTION 372.3

presented for a four year period concurrent with the onsite Information from Avoca, Penna. on the occurrence of fog was

meteorological program. Provide long-term data (e.g., 30 years) for this meteorological phenomena.

RESPONSE

The response to this question is provided in Subsection 2.3.2.1.4.

Rev. 46~ 06/93 372.3-1 SSES-FSAR

QUESTION 372.4 Atmospheric stability data are provided for Avoca based on STAR data for the period 1971-1975. Explain the rationale for selection of this 5 year period and the representativeness of this period to long-term meteorological conditions (e.g., 30 years). Describe the seasonal occurrence of Pasquill E and F stability categories which were noted to occur 24\\ of the year.

RESPONSE

The response to this question is provided in Subsection 2.3.2.1.5.

Rev. 46, 06/93 372.4-1 SSES-FSAR

QUESTION 372.5 Calendar year 1976 meteorological data were inputs to the natural draft cooling tower impact assessment model. Explain the rationale for selection of this year of data and its representativeness with respect to long-term atmospheric conditions.

RESPONSE

The response to this question is provided in Subsection 2.3.2.2.

Rev. 46, 06/93 372.5-1

SSES-FSAR

QUESTION 372.6 Cite references for the cooling tower impact assessment model which was used.

RESPONSE

The response to this question is provided in Subsection 2.3.2.2.

Rev. 46, 06/93 372.6-1 SSES-FSAR

QUESTION 372.7

For each parameter, provide the height of meteorological measurement inputs to the model used to assess the impact of the proposed Susquehanna natural draft cooling towers.

RESPONSE

The response to this question is provided in Subsection 2.3.2.2.

Rev. 46, 06/93 372.7-1 SSES-FSAR

QUESTION 372.8 What is the minimum distance from the onsite meteorological tower to the "deciduous trees in a gully to the south?" How tall are these trees?

RESPONSE

The response to this question is provided in Subsection 2.3.3.1.

Rev. 46, 06/93 372.8-1 SSES-FSAR

QUESTION 372.9 Regulatory Guide 1.23 identifies recommended accuracies of the entire meteorological data collection and reduction system; however, the specifications provided in Section 2. 3. 3. 3 pertain only to the sensors. Provide the system accuracies for each parameter and compare these with the recommendations of Regulatory Guide 1.23.

RESPONSE

PP&L believes that the accuracy for sensors was only identified in Regulatory Guide 1.23. Instrumentation accuracies have been presented in the FSAR.

Rev. 46, 06/93 372.9-1 SSES-FSAR

QUESTION 372.10

Are the temperature accuracies presented in Section 2.3.3.3 of the FSAR instantaneous or time-averaged values?

RESPONSE

The response to this question is provided in Subsection 2.3.3.3.

Rev. 46, 06/93 372.10-1 SSES~FSAR

QUESTION 372.11 On FSAR page 2.3-18, full scale on the wind sensor is listed as 25 mph.

Describe the impact on plant operation and safety of your inability to record occurrences of wind speeds greater than 25 mph.

RESPONSE

The inability to record occurrences of wind speeds greg1ter than 25 mph has no impact on plant operation and safety.

Rev. 46, 06/93 372.11-1 SSES-FSAR

  • QUESTION 372.12 Are the digital data recorded onto magnetic tape instantaneous
  • or integrated one-minute time ave~ages?

RESPONSE

Instantaneous values are recorded on the magnetic tape.

Rev. 46, 06/93 372.12-1 SSES-FSAR

QUESTION 372.13 Discuss the results of the calibration findings including adjustments and/or replacements of components in the data collection and recording system.

RESPONSE

During the inspection and calibration of the equipment at the Susquehanna SES meteorological tower, all wind speed and wind direction sensors are replaced with pre-calibrated sensors.

The dewcell is retreated at least semi-annually.

The translator cards and chart recorders are checked and calibrated as necessary.

As a result of the calibration, the only data which had to be corrected was the wind direction. This correction was due to the meteorological tower being straightened. All other data has not needed correction after the calibration and inspection.

Rev. 46, 06/93 372.13-1 SSES-FSAR

QUESTION 372.14 Provide the dates and times of significant instrument outage, the causes of the outage, and the corrective action taken.

RESPONSE

The following are the dates and times of significant instrument outage (more than 5 days), the causes of the outage, and the corrective action taken:

0:>rrective Date and time Cause of action Instrument of outage outage taken Wind speed 12/32/73-8 AM System power Power 30' level to failure restored 12/26/73 10 AM

1/2/74-11 AM Frozen None to bearings 1/14/74-11 AM

1/18/74-6 AM Frozen and Sensor to dirty replaced 2/25/74-10 AM bearings

12/7/74-8 AM Frozen and Sensor to dirty replaced 12/11/74-9 AM bearings

6/11/75-11 AM Dirty Sensor to bearings replaced 6/17/75-10 AM

6/2/76-3 AM Dirty Sensor to bearings replaced 6/7/76-11 AM

12/3/76-1 AM Frozen sensor None to due to 12/10/76-11 PM storm Wind Speed 1/6/73-4 AM Frozen None 300' level to bearings 1/15/73-11 AM due to precipitation

Rev. 46, 06/93 372~14-1 SSES-FSAR

2/8/73-6 PM Frozen None to bearings 2/14/73-4 PM due to precipitation

5/16/73-10 PM Dirty Sensor to bearings replaced 5/23/73-11 AM

12/21/73-8 AM System Power to power restored 10/26/73-10 AM failure

11/29/76-6 AM Frozen and Sensor to dirty replaced 12/10/76-8 PM bearings Wind 12/21/73-8 AM System Power Direction to power restored 30' level 12/26/73-10 AM failure

1/2/74-11 AM Frozen None to and dirty 1/14/74-11 AM bearings

1/18/74-6 AM Frozen and Sensor to dirty replaced 2/25/74-10 PM bearings

12/7/74-8 AM Frozen and Sensor to dirty replaced 12/11/74-9 AM bearings

6/11/75-11 AM Dirty Sensor to bearings replaced 6/21/75-10 AM

6/2/76-3 AM Dirty Sensor to bearings replaced 6/7/76-11 AM

Wind 1/6/73-4 AM Frozen None Direction to bearings 300' level 1/15/73-11 AM 2/8/73-6 PM Frozen None to bearings 2/14/73-4 PM

Rev. 46, 06/93 372.14-2 SSES-FSAR

5/16/73-10 PM Dirty Sensor to bearings replaced 5/23/73-11 AM 12/21/73-8 AM System Power to power restored 12/26/73-10 AM failure

12/3/76-1 AM Frozen and Sensor to dirty replaced 12/10/76-11. PM bearings Dry bulb 12/21/73-8 AM System Power Temperature to power restored 30' level 12/26/73-10 AM failure Wet bulb 10/13/73-9 PM Sensor Sensor Temperature to failure replaced

30' level 10/25/73-7 AM 12/21/73-8 AM System Power to power restored 12/26/73-10 AM failure Delta 6/8/73-midnight Sensor Sensor Temperature to failure replaced 100'-30' 6/14/73-11 PM levels 6/27/73-midnight Sensor Sensor to failure replaced 7/3/73-10 AM

12/21/73-8 AM System Power to power restored 12/26/73-10 AM failure 1/2/74-11 AM Sensor Sensor to failure replaced

1/14/74-11 AM

1/18/74-6 AM Sensor Sensor to failure replaced 2/26/74-11 AM

Delta 1/1/73-midnight Sensor Sensor Temperature to failure replaced 300'-30' 2/23/73-11 AM levels

Rev. 46, 06/93 372.14-3 SSES-FSAR

6/8/73-midnight Sensor Sensor to 7/20/73-11 PM failure replaced

12/21/73-8 AM System Power to power restored 12/2~/73 failure

1/2/74-11 AM Sensor Sensor to failure replaced 1/14/74-10. AM

1/18/74-6 AM Sensor Sensor to failure replaced 2/26/74-11 AM Precipitation 12/21/73-8 AM System Power to power restored

12/26/73-10 AM failure

12/6/74-11 AM Ice in Ioe rem:,/00 to weighing from 12/27/74-5 PM mechanism mechanism 12/1/76-midnight Ice in Ice rem:,/00 to weighing from 12/31/76-11 PM mechanism mechanism

Rev. 46, 06/93 372.14-4 SSES-FSAR

QUESTION 372.15

Identify the fraction of meteorological data recorded digitally that was lost and supplemented by strip chart records.

RESPONSE

The response to this question is provided in Subsection 2.3.3.4.

Rev. 46, 06/93 372.15-1 SSES-FSAR

QUESTION 372.16 Provide an estimate of the root mean square and largest differences found in the comparison of strip chart and digital data for each meteorological parameter measured.

RESPONSE

The response to this question is provided in Subsection 2.3.3.4.

Rev. 46, 06/93 372.16-1 SSES-FSAR

QUESTION 372.17 FSAR page 2.3-21 states that if the wind speed is non-calm and the wind direction is zero, implying a calm, then the wind direction for that observation is set to north. Does this was recorded were grouped into the north direction category? statement mean that all non-calm winds for which no direction What was the frequency of occurrence of this phenomena and what impact does this have on the data summaries which were used in making relative concentration estimates?

RESPONSE

with that observation because the wind direction for a calm If the wind speed is calm there can be no direction associated must be distributed in proportion to the wind direction frequency of the lowest non-calm wind speed class by stability class. Therefore, it was decided to identify all calm wind directions with a zero. If, however, the wind direction for an observation with a non-calm wind speed was determined to be 0°,

indicating calm, this would be an error. So, for all non-calm wind speeds with a wind direction of 0° the wind direction was changed to 360° in order to avoid counting the observation as a calm. For all observations which no wind direction was recorded or was determined to be invalid the direction was"--" indicating missing or invalid data. We do not know the whatsoever on the relative concentration estimates. frequency of occurrence of this phenomena but it has no impact

Rev. 46, 06/93 372.17-1 SSES-FSAR

QUESTION 372.18 A description of the method used to calculate hourly wind directions is provided. What are the bases for selecting the modal direction for wind speeds between calm and 3 mph? How are multi-modal occurrences of the same magnitude within the same hour treated? For wind speeds of about 3 mph, what are the differences in the resultant wind direction selected using the modal technique versus the vector analysis technique?

RESPONSE

The text of the FSAR has been corrected to reflect the fact that all non-calm wind directions are determined by vector analysis. For calm conditions wind directions are determined by the frequency distribution of the lowest non-calm wind speed class by stability class.

Rev. 46, 06/93 372.18-1 SSES-FSAR

QUESTION 372.19 directional dependent model. This is to inform you that there To calculate short-term diffusion estimates, you have used a are two models which may be used to evaluate atmospheric transport conditions for analysis of accidents.

Attached are a copy of our Interim Branch Technical Position concerning a model which considers horizontal plume meander and the directional dependence of dispersion conditions, air flow, and exclusion area boundaries, and a copy of our DRAFT Regulatory Guide 1. Potential Accident Consequence Assessments at Nuclear Power XXX, "Atmospheric Dispersion Models for Plants," 9/23/77. The model was approved for interim use by the Regulatory Requirements Review Committee on May 2, 1978.

If you choose to revise your estimates based on this position, the Susquehanna Units 1 & 2 FSAR should be updated to reflect this change. To facilitate our review we request that you provide the 16 exclusion area boundary distances as described in Section C.2 of Regulatory Guide l.XXX, if you wish to revise your exclusion area so that it is no longer circular.

RESPONSE

PP&L does not plan on revising the Susquehanna SES exclusion area.

r

Rev. 46, 06/93 372.19-1 SSES-FSAR

QUESTION 372.20 How were periods of missing data handled when making running average {e.g., 8 hour9.259259e-5 days <br />0.00222 hours <br />1.322751e-5 weeks <br />3.044e-6 months <br />) estimates of relative concentration?

RESPONSE

The response to this question is provided in Subsection 2.3.4.2.

Rev. 46, 06/93 372.20-1 SSES-FSAR

QUESTION 372.21

Section 2.3.4.4 of the FSAR states that "the percentile calculations were performed using the total concentration distribution (independent of sector), 11 yet FSAR Tables 2.3-93 through 2.3-117 list cumulative percentile by direction.

Explain further what the quoted statement means.

RESPONSE

Subsection 2.3.4.4. The response to this question is provided in

Rev. 46, 06/93 372.21--1 SSES-FSAR

QUESTION 372.22

FSAR Tables 2.3-115 lists a cumulative frequency totaling 138.21 percent in the SE sector. Correct this error.

RESPONSE

For response see Revised Table 2.3-115.

Rev. 46, 06/93 372.22-1 SSES-FSAR

QUESTION 372.23

The statement is made that "calculations were made after removing all zero values." What was the frequency of occurrence of such values and the impact of removing these values from the cumulative frequency?

RESPONSE

The response to this question is provided in Subsection 2.3.4.4.

Rev. 46, 06/93 372.23-1 SSES-FSAR

QUESTION 372.24 A puff advection model was used in your assessment of routine releases to derive a table (2.3-128} of terrain correction factor. Were the correction factors which were less than unity used to adjust the uncorrected straight line model?

RESPONSE

The response to this is provided in Subsection 2.3.5.1.4. question

Rev. 46, 06/93 372.24-1 SSES-FSAR

QUESTION 372.25 evaluation cited in Reference 2.3-18. Provide a copy of the Dames and Moore Susquehanna tornado

RESPONSE

The above referenced document is provided to you under separate cover.

Rev. 46, 06/93 372.25-1 SSES-FSAR

QUESTION 372.26 The hourly onsite meteorological data which you have submitted indicates that during part of the four year period, the 96m temperature reading exceeded the dew point reading by as much as 9°C during periods of precipitation. What fraction of the time did this occur? Under what conditions might this happen?

During a 56 consecutive hour period in 1973 the temperature and dew point readings were identical. To what may this be attributed?*

RESPONSE

We have reviewed the data and determined that during periods of precipitation there were 240 occurrences when the dry bulb temperature was greater than the wet bulb temperature by more months of April and September. A spot check of some than 3°C. These occurrences were noted primarily between the occurrences showed that the precipitation amount was very light

(.04) and isolated or it happened during the onset of a long period of precipitation. We feel that passing isolated light showers typical for the April - September period could explain the occurrences which fell into the first category. When the temperature-wet bulb differential is large and precipitation starts it will take some period of continuous precipitation until this differential becomes 3°C or less (Thus, the occurrences during the onset of a precipitation period).

we suspect that the 56-hour period when the temperature and wet bulb were identical was due to an equipment malfunction.

Rev. 46, 06/93 SSES-FSAR

QUESTION 372.27

What are the delta-T intervals used in each of the joint frequency distributions presented (e.g. Tables 2.3-75 through 2.3-81)? Describe the effect on the estimation of atmospheric stability of using an interval from 30.5 to 9.6 meters versus a deeper layer as described in Regulatory Guide 1.23.

RESPONSE

Refer to Question 372.28 for response.

Rev. 46, 06/93 372.27-1 SSES-FSAR

QUESTION 372.28 FSAR Tables 2.3-75 through 2.3-81 are joint frequency distribution summaries for winds measured at the 9. 6 meter delta-T interval from 30.5 to 9.6 meters from the hourly data level. We have compiled joint frequency distributions for a tape which you provided. For some stability classes there are significant differences. Therefore, provide a detailed description of the procedure used to derive the joint frequency distributions which appear in the Susquehanna FSAR. Were these distributions generated from a data tape identical to the tape which was supplied to us or were the data in some other form {e.g., more significant digits, different units)?

RESPONSE

As discussed in Subsection 2.3.3.6 of the FSAR, the primary delta-T interval was from 31.5 ft. to 300 ft. If these data were missing or invalid, data from the 31. 5 ft. to 100 ft interval were used. If both sets of data were missing or observation. The stability classifications used are as invalid, there was no stability classification for that follows:

Category ( °C/100 m) AT°C/270 ft. 6T~C/70 ft. Pasquill NRC REG 1. 23

A <-1.9 <-1.6 <-0.4 B -1. 9 to -1. 7 -1. 6 to -1.4 -o.4 C -1. 7 to -1.5 -1. 3 to -1. 2 -0.3 D -1.5 to -0.S -1.1 to -0.S -0.2 to -0.1 E -0.5 to 1.5 -0.4 to 1.2 0 to 0.3 F 1.5 to 4.0 1. 3 to 3.3 0.4 to 0.9 G >4.0 >3.3 >0.9

Since the interval between 30.5 and 9.6 meters is rather small the stability range is significantly compressed with 5 stability classes falling in a 1.3°C range. With so small a range one would expect to find more values at the ends of the stability classification scale if this were used as the primary delta-T interval.

Rev. 46, 06/93 372.28-1