ML092640168

From kanterella
Revision as of 23:15, 6 December 2019 by StriderTol (talk | contribs) (Created page by program invented by StriderTol)
Jump to navigation Jump to search
Diffusion Models
ML092640168
Person / Time
Site: Indian Point  Entergy icon.png
Issue date: 08/28/2009
From:
Atomic Safety and Licensing Board Panel
To:
SECY RAS
References
50-247-LR, 50-286-LR, ASLBP 07-858-03-LR-BD01, RAS 284
Download: ML092640168 (33)


Text

Rees of a aeilt niomn Certain volumeS Ceti rainciecocnrto Rees mixe wit ai du o0ubuec Rees inrese in voum Rees derae incnenrto derae asymptoticall

Li

- I0 S uS 0~

  • 0~ p- sio * *oS Gassa plm mode mos wiel use for esiatn diprso in dose prjcin

&Generally~ no-pta and no -tmoa stragh-ln " snpso SS Stlied Simle can be imlmne in han cacuaton V Ma o- erpeettiefragvnst Adane moel arvial

Mode:

Eseta condtion No-zr win see Wind dieto 0ostn ove tieaddwwn area Rees rat costn ove tim fo th duration0o0 th relas Atophrc tbiiycosan ve im n downwind area Becus ofteecodtos Gassanasesm n i asragh-in, 6snpso Gausia moe snotSeprlnopta

0o 0e Lf i 00 n I Inu paaetr 0an be mesue or prjce I an (7, vaya0ucin 0Jftedwwn ditac an atopei stblt class Vaus were deemie by correlaionst exeim na fil esrm ns Coreaton Sa by l an Gifor tyialyue

VVIJISJtI n5 VS bflWIfl~C ~WJSUUflhRtJ --

-- ---- P-- -~ -- --

-- -- -

-- w --

1w I*3 4

181 6 U E 4

I 4 3

I

  • 4 I

4 4

$

10.1 is, 101 2 102 .1 3 1 101 I ý ý ý jgi 3 I 43* ~o~ ~ I 41* j~3 23 31 4454 1 1F Dislarm from Source, m ~m Suew buw..m

rnliedi Concentratio ITh prcdn eqain ar o0.e0 restrucure tocluaenraie ibrecnetain or X /QS - . S *g Nomlie 00cetato diie - by0 Q~0 V whr aibon rainuld cocnrtin0.

Cim

  • 0. *iha.. . . s.

I Mos liitn asec of b si Gasiaodli inblt to evlut spta and te poa difrne in moe inputs.S --

Enane Gasinmdl a-drs hs ina iltis.

Puf m ~odelS Segmented*plume0models Enane Gassa moel geerll addre0

Divie th caclto doai intoeqa tmetp Assg meteroogca and relas dat toechtm the caclto eut Useofimestp allo modlt reflec tmpoa step Th in d veto asin the inita codtin fo tha time ste

Plm is aprxiae 0a by seie of staih-ln Gausia plm s each esiae ontepaaeervle aplcal to that time~ step Puf Model 000-Plum is aproimte by aeisofpfs the difuio an trnpr of eac i

Screen capture from MIDAStm software bv PLG. Inc.

Adane Models In many Gausia moe s,teri hegh is adrse onl indtriig h fetv plm height0 - ew .

The imato erano lm0rasoti o adrssed- 0 Staih-ln moel 0 ca 0uveno a plum aroun montin or foll0owu a rie vale Adane 0oel ca adrs teri0ipc

  • *~*S wa e S S a patcein0 In~~ PI)m dltewn fildi the- dimesional - 0.

Wind vetr hav x- co pnet win vetr S o ths cell - 0

1W 0*

Ms.-p o in Advnce Model In lie of Gassa fomlain PIC0 us models~ lrenmrs o ita patces, eac of whc ar tagdih

&Time ste ofijcininown il 51 Raioucid charateriatio W~hre-axs difuson ceffiien A.

gru of patce is crae fo ec time stp n-netdinotewn il

0.- S *n 00 Models I~

The~ patce disers thog the winfel Moemn deed ntreai*ifuincefcet n thre-xi win fiel vetos On enontrn a terai fae patile follo vecor into adjacen cels moin aroun or0 ovr h trri Paricl poiton ar perioicall reore and inertdoe tim IWhe dsesio is copee th integrate patclsi eac cel are covre to cocnrain an then dose0 0.- - 0404 In aaind s sin do l o p rilsi elly rajc n to ground0 the

ýcreen capture from MIDASun oftware by PLG, Inc.

Screen capture from MIDASu" software by PLG, Inc.

A - E S.- odels I~~ ~ Gasinmdlcngnrlyb

~ ~ ~ ~ A ~stagtln~ ~ ~ . rvnb5 sigl se of metoroogca data Non-tmoa- non spatia SWinfiel moel can ofte be drve bymutil meteorooia staion Te poa and spatial Im roe modeling in com le terrainS E A win fi l mo e drve by a e m t o o o i a

  • o e a no prv id reut an bete tha ths fro a staih-ln
  • 0l Gassa mode- 1 00 ~ S~ S

-eg h- eedn nsronigtranadmtoooia reg imesS -0 ~ ~

Addtina meerloia tower may be neesar to

0

HLH

(

.........-

PR ARY INSTRUMENTATION DIR SPO TEMP DELTA-Ti DIR SPD DIR deg mpIh deSF SC doug mph dog

,asmuninmmman Xumu*mmrnauuuuinMmMiNue.. Mi m mm qgumtb 164 1"ee 100 165. 1.5 66.3 6. 2.3 222. 3.5 263 21.15 Lh66. 2 6. 1, 9 235 264.

130 166. 2 66.5 6, Lt m. ;2, q272.

145 126. 1.2 65.6 6. 2 4 203, 1.8 287.

200 125. 1.2 6.4 6. 2.2 192. 2. 1 300.

215 169. 1.1 65.3 6. 24 190. 2.2 26.

230 154, 1.4 65.3 6. 1. 9 15, 3.s i34, 245 141, 1. e 65.3 6, 1.7 201. 3.6 217.

K 300 145. 2. 0 65. 1 6. 1. 9 202. 2. 3 213.

315 129. 0.11 44.9 6. 145 172, 1.4 242.

F~f

-1 0.9.65.0 6. 1. 341. 1. 4 .

345 174, 0.1 64.9 6. 1. 356. 0. 9.250.

400 153, 1.4 65,0 6. . 1.3 2771.

41.5. 't 1". 1.2 40.2 6. .i.1426 430 .179. 1.7 6p4. 9 6. .. 2 5.- 1. 61275..

451 NO0 I-P 166.

177 1. i 64. 9 5.

1.8 65.0 5. 0. 0.220,

ý 1.91272 1.6

4LZ