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STAT 8 0F RH0DE ISLED AND PROVIDENCE PfaNTAT10HS j | |||
Attention: Division of Liconemg and Regulatica Gentiamens The Rhode Is1cnd Atcmic Energy Consission (RIAEC) herab7 submits for approval of the U. S. Atcaic Energy Ccmnocion (USA 20) infornticn to establish an ataoophoric dilution factor of 10 se:/ | \\ | ||
the rcactor building ventilatien natcs and the systems for removal of anbient atmosphere undarcoins neutrca batted 2ent, in ths beam ports, dry grm= facility, and allied racctor experinatal facMities,, hys been described provicualy (1,2,3)3 This exhaust syste::) will niao be und for the ruoval of various flauhing gases, t | ATO'310 D4EROY COW ISSION Docket Wo. 50-193 April 16, 1963 Chaire.an U. S. Atocic Worgy Coc:misalon Washington 25, D. C. | ||
Attention: Division of Liconemg and Regulatica Gentiamens The Rhode Is1cnd Atcmic Energy Consission (RIAEC) herab7 submits for approval of the U. S. Atcaic Energy Ccmnocion (USA 20) infornticn to establish an 3 | |||
ataoophoric dilution factor of 10 se:/n for determining the permissible average concentration of radiotetivu offluent from the reacter effluent diuposal stack which is 22 inches in diaator and 11$ foot hi; hor than the surrounding t | |||
terrain. Such a dilution factor &pplicd to the disposal of cirborne radioutin c:sterLd is eufficient to enaure tJ st the yccr3y eversge concentration of such i | |||
n:aterials at all points in unrestricted aron around tho stack, whica cuald be cccupied by individush will not cxceed the mxinam permissible, non. occupational concentrations estub]iched by the USAE04 The inforation which fo11cma 2dicates that dispceal of airborno radioactive 3 | |||
ut,orial from a stack which pr<nidce a dilution factor of 10 sec/m can to actoly permittod. Tuis factor vill be rogarded as a limit and gases will bc L | |||
releauad at a atniuum lovel aft,or c rcib1 monitoring. | |||
the rcactor building ventilatien natcs and the systems for removal of anbient atmosphere undarcoins neutrca batted 2ent, in ths beam ports, dry grm= facility, and allied racctor experinatal facMities,, hys been described provicualy (1,2,3)3 This exhaust syste::) will niao be und for the ruoval of various flauhing gases, t | |||
s | |||
: 1..- | |||
o | |||
' ;7' L | |||
alnfer:mtion Supplied in Rt,spenn to Q:cstiene Ccepiled by the USAEC Regarding the Rhodo Isl nd Atcuiu Energy Ocxaaission Reactor", answere A-3 and A-h, unbmitted to USt.EC on June 29, 1962. | |||
2. | |||
"InfcInstion Supplied by the Rhode Island Atenic Energy Coemission to Quostions Cor. piled by the 0.0a Atec.ic Enerry Commiartion", answers item l | |||
11 and attac.eJ non chn.t, ILm 13, cubnitted to USAEC un thy 2,1962., | |||
3. | |||
87afor.utier. Supplied iy do Op.e s1 dwtric Co,rtpany in !sspunce N Qucsticas 5:W LJ by N "S.M hwcJmg the E%do ktond Atra.ta ! Meg,y Ccudssion Reactc. ", cuuvers lj, % aubchted to USAEC on Wy 2,1962, 8808150377 88080s PDR ADOCK 05000193 P | |||
PDC | |||
) | |||
f | f | ||
'. : rich us holium requir?A in cetati caporinontal est upa in the ganeral reosarch progrn. hoac gaces. ill to colleevad in a usnifold and after coroful monitoring exhaustad to the exterior of the building through particulata filtors. | |||
These s/ stems will cxht.uot thrcugh a sta<2k 115 foot cbove the currounling terrain by maana of a 4000 cfn bicucro All building venti htica intakes are fittssi with louvers to close them off nutoanticony in the evont of tho necessity of using the building clean-up systor fonc71::3 a reactor incidcat. | These s/ stems will cxht.uot thrcugh a sta<2k 115 foot cbove the currounling terrain by maana of a 4000 cfn bicucro All building venti htica intakes are fittssi with louvers to close them off nutoanticony in the evont of tho necessity of using the building clean-up systor fonc71::3 a reactor incidcat. | ||
In relsasing gaseous cctivity to tho atsoaphoro, the RIAf C realizes ths necccsity of pret3cting inhabitsute of unrostricted t.?cca nur ^he rasctor site fr(c owr c:poeurs due to the stsch offluont. Hovowr, due to diffusion in the atsoaphore and variations in wind opcc. end ditcetion, ernuent concentrations of radioactive gasos in excess of ths kPC cca be aufoly dischersd frow the etzck. It is the purpose of the remaindor of this tn.r.aa.ihl to rovi<u the reactor locatica, the appropriate oparating proc:durcs, cr.d the applicable tactoorologiesi diffusion thoery in crder to justify thio statment. | In relsasing gaseous cctivity to tho atsoaphoro, the RIAf C realizes ths necccsity of pret3cting inhabitsute of unrostricted t.?cca nur ^he rasctor site fr(c owr c:poeurs due to the stsch offluont. Hovowr, due to diffusion in the atsoaphore and variations in wind opcc. end ditcetion, ernuent concentrations of radioactive gasos in excess of ths kPC cca be aufoly dischersd frow the etzck. It is the purpose of the remaindor of this tn.r.aa.ihl to rovi<u the reactor locatica, the appropriate oparating proc:durcs, cr.d the applicable tactoorologiesi diffusion thoery in crder to justify thio statment. | ||
The ra2cter facility enriron.azt lus bean douctibed in prior transmittala to the Civi.sica of licencing and Rg.Gatica (b,$,6,7). A nun.aly of this information follona. | The ra2cter facility enriron.azt lus bean douctibed in prior transmittala to the Civi.sica of licencing and Rg.Gatica (b,$,6,7). A nun.aly of this information follona. | ||
l~ | l~ | ||
There 10 a ssparttion of abcut 600 feet bots:Ocn theso facilitieu. In addition the U. S. Public Ilo60th Serv 3co io prosently constructing the Northeast Shellfish Research laboratory and will econ construct n folluted Wtter IAboratory adjacent to tho 27 cero of to. The Jr.nd -urrounding the reactor is essentially contro11od by the Stste of hacdv Ic3..nd themch the University of Rhode Island. Tha distance frca the reactor building to thu boarAry of the thrco ucree of reactor inad is h., | The reactor is located or. threo c:rea of Isad ca a 27 scre cbandoned milit:ry reservation formerly en11cd Wrt Darnsy. The re:ervatica iu in the Town of Narrtpasott, R. I, en the wst choro of Narragsnsctt Bay approxitnately 22 miles acuth of Providence, R.1. | ||
x.d spprer.b.mtely 6 miles north of the entrance to the Day froa the Atlantic Ccean. Iocated on thia 27 acre site are the R. I. Huc1 car Scienca Center (the ructer) cnd tho Univorc$ty of lihedo Island Marine Imboratory. | |||
There 10 a ssparttion of abcut 600 feet bots:Ocn theso facilitieu. In addition the U. S. Public Ilo60th Serv 3co io prosently constructing the Northeast Shellfish Research laboratory and will econ construct n folluted Wtter IAboratory adjacent to tho 27 cero of to. The Jr.nd -urrounding the reactor is essentially contro11od by the Stste of hacdv Ic3..nd themch the University of Rhode Island. Tha distance frca the reactor building to thu boarAry of the thrco ucree of reactor inad is h., | |||
e, | Intter, Arthur b Quirk to USAIC, dated August 3,1962. | ||
5. | |||
Intter and enclosurcs, Arthur L quirk to USAEC dated Vay 2,1962. | |||
6. | |||
Intter, Arthur L Quirk to b3AEC dated Janunry 19, 1962,, | |||
,e, 7. | |||
Technical ipocificaticos to b: auM.it%! to UJrd:. | |||
2 | 2 | ||
lf | lf | ||
.<S O fcet. This boundary is to tha east of the building toward tha sh:re of | |||
S O fcet. This boundary is to tha east of the building toward tha sh:re of | ~ | ||
Narregensett Bay. The cloasst off site structure is the Old Ferry Church | Narregensett Bay. The cloasst off site structure is the Old Ferry Church (Old Nstragansett Church) at cheut 1300 feet. The clossat private dwelling is 100 feet frem the facility. | ||
(Old Nstragansett Church) at cheut 1300 feet. The clossat private dwelling is 100 feet frem the facility. | No gaseous effluent will be releasod frcan the stack without the knowledge of the reactor operating staff and without t.ppropriate monitoring. Prior to the conduct of any exporiconta, tha cporating staff, the scientists involve.h and the Reactor Utilisation Committee analyze potentini ha.zards. connected with the cxperiment, including studies of the c:: cunts of any rtdioactive gases to be evolved. rzporimenta involving tha reloaco of such gas are then fitted with appropriato moniterco After monitoriag, the Bos would be discharged through the stack providing the stack dilution factor is sufficient to result in concentraticas bohf WC for unrsstricted nrease, The uximun arcund concentratien of gaseous offluents from a stcck is calculated using the Sutton diffucien relation (8) 1,, ; = 33 - | ||
No gaseous effluent will be releasod frcan the stack without the knowledge of | |||
the reactor operating staff and without t.ppropriate monitoring. Prior to the conduct of any exporiconta, tha cporating staff, the scientists involve.h and the Reactor Utilisation Committee analyze potentini ha.zards. connected with the cxperiment, including studies of the c:: cunts of any rtdioactive gases to be evolved. rzporimenta involving tha reloaco of such gas are then fitted with appropriato moniterco After monitoriag, the Bos would be discharged through the stack providing the stack dilution factor is sufficient to result in concentraticas bohf WC for unrsstricted nrease, The uximun arcund concentratien of gaseous offluents from a stcck is calculated using the Sutton diffucien relation (8) 1,, ; = 33 - | |||
p | p | ||
(_ | (_ | ||
F#h Y | |||
where | |||
'Q ~ concentration (jt c/ce) at ground level fr.r the poeition of u.uimum concentration dernwind from the stack k | |||
In Table I, Column 1and 2 are procented tho (/Q for a stack 115 feet in he$ght and for various wind speode., lho rice of tho exhaust plume above the , | Q =emissionratoofrdiosctiveges(curies / soc) h - hoight of stack (matera) wind volocity (notora/ soc) u a | ||
cf | |||
- = the ratio of the vortice.* c,o horizontel atmoapheric diffusion | |||
*y coefficiento, which f u r.hrays lece than unity. | |||
In Table I, Column 1and 2 are procented tho (/Q for a stack 115 feet in he$ght and for various wind speode., lho rice of tho exhaust plume above the, | |||
stack because of tho cnhaust velocity (17 mph) has been included in the calculation. | stack because of tho cnhaust velocity (17 mph) has been included in the calculation. | ||
~- | |||
8. | |||
U.S. D2partzeat of Ccacerco "Yeterology and Atcutic F.norgy", AEClk 3066 July 1935, p h9. | |||
3 | 3 | ||
.I f | |||
Table 1, Column 3, preaanto tha percontage frequency of the various wind speeds for the location. The data ia taken frca Reference 9. | |||
Table I, Column 14, preaants the product of % /Q and frequency of wind oc. | Table I, Column 14, preaants the product of % /Q and frequency of wind oc. | ||
'Ihe ataospheric dilutica fcctor X /Q avoreged over wind speed and currence. | |||
From the tsble it 10 scen that tha wind direction 1e quito variable but that the most frequent dircetica, rofctred to tha sixtecn co2 pass points occurs no tnote then 10.$ porcont of the titco and occura frora either the sout'l went or north wast directicc. Thore* ore, the year round 7./Q averaged over wind spai and adjusted for trind direction 16 (5.35 x 10 ) (.105) or 5.6 x 10 | fmquency is the cum cf the last colum of Table I and la 5 35 x 10-5,,,f,3, Table II presents the percontogo frequency of wind direction based on 16 compass points and an ersual averago. The data is tuken from Roferenco 9. | ||
ace /m . | From the tsble it 10 scen that tha wind direction 1e quito variable but that the most frequent dircetica, rofctred to tha sixtecn co2 pass points occurs no tnote then 10.$ porcont of the titco and occura frora either the sout'l went or north wast directicc. Thore* ore, the year round 7./Q averaged over wind | ||
~0 spai and adjusted for trind direction 16 (5.35 x 10 ) (.105) or 5.6 x 10 3 | |||
ace /m. | |||
The distances dmntaind frcm the stsc!: uhore these maximum concentrations occw cro comput(d frots tho valutjon (0) | The distances dmntaind frcm the stsc!: uhore these maximum concentrations occw cro comput(d frots tho valutjon (0) | ||
( | ( | ||
_1 _ _ _ _- | _1 _ _ _ _- | ||
2 | 2 d | ||
h | |||
. 2-n | |||
,u :. - | |||
,p c' | |||
where | where | ||
( | ( | ||
d | |||
, distenco (arato 3) cf isxir.cn concantration from the stack ha effective stack hsight (rotors) na Sutton stability paremator c = generalized diffusion coefficient. | |||
9. | |||
"C11aatography of the United 2tr.tsa lh 30-37, Sraw.nry of Heurly Observaticas, Providence, R I.", U. S. Department of Comerco Weather Eureau. | |||
s h | s h | ||
I I | I I | ||
( | ( | ||
Table III presents the d, for an 115 foot stack and for various choices of the stability parotnoter. The diffusion coefficients appropriate far the particuler stack height, wind velocity, and motocrological conditions are obtained from Tables III and VII of ILO 12005 (10). | Table III presents the d, for an 115 foot stack and for various choices of the stability parotnoter. The diffusion coefficients appropriate far the particuler stack height, wind velocity, and motocrological conditions are obtained from Tables III and VII of ILO 12005 (10). | ||
'Ihis cciculation is concervativo fer the following reasons: | |||
0,/0 is assumed equal to la 1. | |||
7 2. | |||
The radioactiva decay of the gaseous effluents is ignored. This factor can become important for the dispercal of a gas cf relative 3y short half lifo under the condition of lw wind speed - eago for lo8 horar Argomh1 which io ascus:ed to be the major radioactivo constituont of the baxn port atmospheric con *Anto 3. | |||
The dilution facter calculated ic for the position on the grourd i.hsre the rty.iram concentratica occurs. The extent of this ponitice is licited. | |||
Tho c.bove calculatites chou that tho evorego dilution fcctor X /Q is at least yo6 x 10-0 sec/ | In the croso mind direction the concentratica in '2e exhaust plume is gcuacien in cbcpc end its value falls off rap:tdly | ||
( | |||
as distance fron tha plume centerline increacec. It can bo shown that the average concentration in the cross wind directica is. 57 of the mxisn of ths gaussion when 97'/. of the gaussian is includado h, | |||
iho offluent cena, especia137 under inversico conditions, is limited in cross wind sine end its effcctivo cross wir.d diameter ocpecially under invarcion cceditieto is often small cocpared with the distance L | |||
interceptedbythe221/2*rindacetoroverwhichaveragesweremads for wind direction.. | |||
Tho c.bove calculatites chou that tho evorego dilution fcctor X /Q is at least yo6 x 10-0 sec/n at the locatics of rax3can ground cencontrations therefora, 3 | |||
it 10 roquested that the USAEC parrit the TtIrdC to utilize an atmospherie 10 "Workbook in Atacophoric Diffucion Calculations, O. A. DeMarrais, IDO-12005, February 1959, p. h9. | |||
k 5 | k 5 | ||
3 dilution factor of 10 | 3 dilution factor of 10 cer:/m for the releaso of radioactive gases free its atack. | ||
Vory;truly yours, | Vory;truly yours, s | ||
Arthur L, Quirk, Chairasn Subecribed and Sworn to before ao this_ // | |||
Notary Public | day of M __ | ||
1963 P | |||
/4A _ _. | |||
Notary Public | |||
) | |||
Lty can.iosion a:tpires 4_ j nt/ | |||
L Encle (1) Tabis I (2) Tabla II (3) Table III L | L Encle (1) Tabis I (2) Tabla II (3) Table III L | ||
6 | 6 | ||
m l | m l | ||
Wind Speed | TABIE I L | ||
Sec/m | Wind Speed Fr uency of occurrence I #* | ||
Designated Tiind Speed | [X/c)xr fr m | ||
3 Sec/m Designated Tiind Speed | |||
( | ( | ||
f 41 | f | ||
-5 41 117 x lo-o05 oo585 x 10 1-3 12.h x 10-5 | |||
,o93 3,3g, 30-5 | |||
h-7 | -5 | ||
23 - 18 | ~ | ||
19 - 2h | h-7 6.9 x 10 a25 17 x 10 8 - 12 h | ||
x lo'I | |||
.298 1.19 x 10-5 | |||
-5 23 - 18 2.7 x 10 | |||
TOTAL | .238 o.6h x 10-5 | ||
L. | -5 | ||
-5 19 - 2h 2 | |||
x 10 | |||
,og o,1 | |||
,30 | |||
-5 | |||
> 214 | |||
.18 x 20 | |||
.o13 o.002 x lo-5 TOTAL 5 35 x 10 sec/m | |||
~ | |||
L L. | |||
l l | l l | ||
l | l Enc 1 (1) to RIAEC ltr Dated: April, 16, 1963 | ||
-l TABLE il PERCENTAGE FREQUENCY OF WIND DIRECTION JAN FEB MAR APR MAY JUNE JULY AUG SEPT OCT NOV DE-C SLN SUM /12 N | |||
9 9 | |||
7 6 | |||
8 3 | |||
4 5 | |||
6 7 | |||
6 5 | |||
75 6.25 ffE 7 | |||
6 6 | |||
8 8 | |||
4 3 | |||
5 6 | |||
8 5 | |||
3 69 5.75 PE 3 | |||
4 5 | |||
4 7 | |||
4 3 | |||
4 5 | |||
6 4 | |||
4 53 4.42 EM 1 | |||
1 2 | |||
1 2 | |||
2 1 | |||
1 1 | |||
1 2 | |||
1 16 1.33 E | |||
1 1 | |||
2 2 | |||
1 1 | |||
1 1 | |||
1 1 | |||
1 13 1.08 ESE 1 | |||
1 2 | |||
1 2 | |||
1 1 | |||
2 1 | |||
1 1 | |||
1 15 1.25 SE 4 | |||
3 7 | |||
8 12 7 | |||
7 7 | |||
4 4 | |||
3 4 | |||
70 5.83 SSE 4 | |||
4 4 | |||
6 8 | |||
8 5 | |||
4 5 | |||
4 4 | |||
3 59 4.92 S | |||
4 5 | |||
4 7 | |||
5 7 | |||
7 7 | |||
7 6 | |||
6 4 | |||
69 5.75 SSW 8 | |||
4 6 | |||
8 6 | |||
12 12 12 11 7 | |||
8 7 | |||
101 8.42 SW 10 7 | |||
5 10 6 | |||
14 16 13 13 12 10 10 126 10.50 WSW 7 | |||
5 4 | |||
6 4 | |||
6 8 | |||
7 5 | |||
6 8 | |||
11 77 6.42 W | |||
7 6 | |||
6 6 | |||
5 7 | |||
8 6 | |||
6 6 | |||
9 10 82 6.83 WNW 11 16 15 8 | |||
7 8 | |||
7 6 | |||
7 7 | |||
9 13 114 9.50 NW 13 14 13 10 8 | |||
8 7 | |||
8 9 | |||
9 13 13 125 10.42 fMN 7 | |||
11 9 | |||
6 6 | |||
4 4 | |||
6 6 | |||
8 7 | |||
7 81 6.75 CALM 5 | |||
4 3 | |||
3 5 | |||
4 6 | |||
7 7 | |||
6 5 | |||
3 l | |||
t | |||
TABIE III Stability Parameter | TABIE III Stability Parameter Wind Velocity iff. Coef. | ||
saax n | |||
uph C | |||
miles | |||
.2 (superadiabatic) 1 39 0.21 5 | |||
34 0.12 10 | |||
.31 (L12 | |||
.25 (adiabatic to 1 | |||
.2 0.56 isothermal) 5 | |||
.16 0433 10 | |||
.15 0 362 | |||
.33 (Isother:nal and 1 | |||
.1 1.7 alight inversion) 5 | |||
.08 1.M 10 | |||
.M 1.25 | |||
-L | |||
.5 (strong invorsion) 1 | |||
.05 0.11 5 | |||
.03 | |||
%1 10 | |||
.02h 0 11 C | |||
t l | t l | ||
[ | [ | ||
I l | I l | ||
C Enci (III) to RIAEC ltr Dated: | C Enci (III) to RIAEC ltr Dated: | ||
April 36, 1963 | |||
t. | |||
EF ST HT 14000 DAVID A | s EF ST HT 14000 DAVID A | ||
2 4 | B 1 | ||
_8 | C D | ||
l E | |||
18 19 | F G | ||
20 | H 1 | ||
21 | 2 4 | ||
delta H H + delta H 5 | |||
26.95/COLC COL D^1.4 dxCOLE COL F + 35 COL G - 14.6 6 | |||
EFFECTIVE EFFECTIVE 7 | |||
WIND SPEED U | |||
W/U STACK STACK HGT- | |||
_8 AVG. WIND HEIGHT HGTOFBLOG 9 | |||
MILES / HR METERS /SEC METERS /SEC METERS METERS 10 1 | |||
0.447 0.45 60.29 310.71 173.62 208.67 194.04 11 1 TO 3 | |||
.44 TO 1.32 0.89 30.28 118.48i 66.21 101.26 86.63 12 4 TO 7 1.76 TO 3.08 2.45 11.00 28.70 16.04 51.09 36.46 13 8 TO 12 3.52 TO 5.28 4.47 6.03 12.37 6.91 41.96 27.33 14 13 TO 18 5072 TO 7.92 6.93 3.89 6.70 3.74 38.79 24.16 15 19 TO 24 8.36 TO 10.56 9.61 2.80 4.24 2.37 37.42 22.79 16__ | |||
> 24 | |||
> 10.56 10.56 2.55 3.71 2.07 37.12 22.49 t | |||
17 18 19 W - STA.CK DRAFT - 26.95 METERS PER SECOND 20 CACS BLDG HGT - 48 FEET = 14.6 METERS [ | |||
~ | |||
21 d - DIAMETER OF STACK - 22 IN.5588 METERS Spreadsheet 1 | |||
s | w s | ||
~ | |||
. CV. | |||
EF ST HT 14000 BOSANOUET A | |||
EF ST HT 14000 BOSANOUET A | B l | ||
C D | |||
E F | |||
G 1 | |||
2 3 | 2 3 | ||
4 | 4 delta H 5 | ||
E AVERAGE | E AVERAGE W/U (W/U)^2 | ||
10 | .615/ COL D 1.31 - COL E COL FxCOLEx 7 | ||
WIND SPEED 3.14y.5588 8 | |||
METERS /SEC 9 | |||
10 0.447 60.29 3634.98 60.30 0.01 1.30 137.50 11 0.89 30.28 916.93 30.29 0.02 1.29 68.52 12 2.45 11.00 121.00 11.03 0.06 1.25 24.21 13 4.47 6.03 36.35 6.08 0.10 1.21 12.79 14 6.93 3.89 15.12 3.96 0.16 1.15 7.88 15 9.61 2.80 7.86 2.90 0.21 1.10 5.40 16 10.56 2.55 6.51 2.66 0.23 1.08 4.83 Spreadsheet 2 | |||
EF ST HT 14000 HOLL A | EF ST HT 14000 HOLL A | ||
B C | |||
_4 U | D E | ||
6 | 1 2 | ||
8 | 26.95/ COL A 1.5x.5588xCOL B COL C + 35 3 | ||
10 | _4 U | ||
W/U 5 | |||
WIND delta H H + delta H Heff - | |||
6 SPEED BLDG HT 7 | |||
8 METERS / SEC 9 | |||
10 0.447 60.29 50.54 85.59 70.96 11 0.89 30.28 25.38 60.43 45.80 12 2.45 11.00 9.22 44.27 29.64 13 4.47 6.03 5.05 40.10 25.47 14 6.93 3.89 3.26 38.31 23.68 15 9.61 2.80 2.35 37.40 22.77 16 10.56 2.55 2.14 37.19 22.56 17 18 19 20 delta H = 1.5dW/ava u Spreadsheet 3 | |||
a. | a. | ||
L!NE SOURCE 14000 HOLL | L!NE SOURCE 14000 HOLL A | ||
B i | |||
3 4 | C l | ||
D l | |||
25 | E l | ||
F i | |||
G l | |||
H I | |||
i J | |||
i K | |||
1 | |||
.12/ COL A COL B/.01 COL Cx3.7EXP 07 COL E SHEET 3 COL Of4COf. E COL F/400 COL "3x1000 COL HxCOLI - | |||
COL Jr.1 2 | |||
3 4 | |||
U 5 | |||
AVERAGE UNE SOURCE UNE SOURCE DISTANCE FLUX AT DOSE RATE DOSE RATE FHDUENCY DOSE RATE DOSE RATE 6 | |||
WIND SPEED STRENGTH STRENGTH UNE TO ECEPTOR MICROR/HR OF WIND COMECTEDFOR COR CTED 7 | |||
Nim SPEED Wito SPEED FOR 8 | |||
METERS /SEC mci / METER mci /CM D/SEC.CM 04 PHOTONSPER MR/HR DIRECTION 9 | |||
SO CM-SEC MICRO R/HR MICRO R/Mt y | |||
0.447 0.27 0.00268456 99328.86 7096 3.50 0.00874867 8.75 0.05 0.44 y | |||
0.89 0.13 0.00134831 49887.64 4580 2.72 0.00680781 6.81 0.093 0.63 12 2.45 0.05 0.0004898 18122.45 2964 1.53 0.00382i37 3.82 0.25 0.96 13 4.47 0.03 0.00026846 9932.89 2547 0.97 0.0024374 2.44 0.0298 0.07 14 6.93 0.02 0.00017316 6406.93 2368 0.68 0.00169102 1.69 0.238 0.40 15 9.61 0.0 : 0.00012487 4620.19 2277 0.51 0.00126817 1.27 0.05 0.06 16 10.56 0.01 0.00011364 4204.55 2256 0.47 0.00116482 1.16 0.013 0.02 17 18 THIS UNE SOURCE CALCULATION IS TAKEN FROM LAMARSH,PAGE 462 2.58 0.26 19 AND CALCULATES THE PHOTON FLUX AT A RECEP's OR X CM 20 FROM AN INFINITE UNE SOURCE. THE PHOTON FLUX IS THEN CONVERTED 21 TO DOSE RATE IGNORING ATTENUATION DUE TO AIR SCATTERING 22 AND ABSORPTION AND IGNORING BUILD-UP 23 l | |||
l l | |||
24 GAMMASSO CM SEC - GAMMAS /CM-SECDNIDED BY 4 TIMES SOdRCE TO RECEPTOR DISTANCE IN CM. | |||
25 l | |||
l l | |||
26 IT TAKES 400 GAMMAS /SO CM-SEC TO PRODUCE IMR/HR 27 FOR 1.3 MEV GAMMAS. | |||
l | |||
} | |||
Spreadsheet 4 | Spreadsheet 4 | ||
*~ | |||
PLUME DOSE 140@ HOLL | PLUME DOSE 140@ HOLL C | ||
l D | |||
l E | |||
2 | l F | ||
l G | |||
l H | |||
10 | f I | ||
4.47 | l J | ||
23 | l K | ||
A I | |||
B 1 | |||
2 U | |||
S pS 3 | |||
AVERAGE PLUME ISUB1 ISUB2 kl SUB 2 ISUB1+ | |||
COL G TIMES COL H f | |||
DOSE RATE 4 | |||
WIND SPEED CENTERLINE k i SUB 2 F19 DIVIDED BY FREO OF PER UNIT 5 | |||
TO RECEPTOR.0073XS WIND SPEED WIND SPEED EMISSION 6 | |||
DISTANCE RATE 7 | |||
DavoU/O D/O Dav9/O 8 | |||
METERS /SEC METERS 9 | |||
10 0.447 70.96 0.52 0.65 0.46 0.506 1.156 6.0276E-06 1.3485E-05 0.05 6.7423E-07 11 0.89 45.8 0.33 1.6 0.82 0.902 2.502 1.3046E-05 1.4658E-05 0.093 1.3632E-06 12 2.45 29.64 0.22 2.4 1 | |||
1.1 3.5 1.825E-05 7.4488E-06 0.25 1.8622E-06 13 4.47 25.47 0.19 2.6 1 | |||
1.1 3.7 1.9292E-05 4.316E-06 0.0298 1.2862E-07 14 6.93 23.68 0.17 2.7 1 | |||
1.1 3.8 1.9814E-05 2.8591 E-06 0.238 6.8048E-07 15 9.61 22.77 0.17 2.7 1 | |||
1.1 3.8 1.9814E-05 2.0618E-06 0.05 1.0309E-07 16 10.56 22.56 0.16 2.7 1 | |||
1.1 3.8 1.9814E-05 1.8763E-06 0.013 2.4392E-08 17 18 TOTAL 4.8362E-06 19 0.1616 0.0073 0.0034 1.3 5.2142E-06 20 21 DIRECTON 22 DavnO X FREQUENCY X O X | |||
sects 23 4.83624E-06 0.1 0.00012 3600 2.0893E-07 RAD /HR 0.00020893 mR/HR Assume pay =.0073 because o = 1 c | |||
=c 0 | |||
= | |||
x y | |||
pa =.0034 k = buildup factor = 1.1 7 = 1.3 MEV for Argon-41, E p =.0073 Y | |||
receptor - (.1616ppah) O(Il + kI2)!11 avg where Il and 12 are from pages 341 and 342 of Meteorology and Atomic Energy, 1968 Spreadsheet 5 | receptor - (.1616ppah) O(Il + kI2)!11 avg where Il and 12 are from pages 341 and 342 of Meteorology and Atomic Energy, 1968 Spreadsheet 5 | ||
MAX GRD CONC 14000 HOLL A | MAX GRD CONC 14000 HOLL A | ||
B C | |||
D E | |||
10 | F 1 | ||
18 | C=B/A E=D/C 2 | ||
21 | 3 f | ||
CORRECTED 4 | |||
AVERAGE FROM PAGE FREQUENCY FOR WIND 5 | |||
WIND 410 OF WIND SPEED AND 6 | |||
SPEED PASQUILL A SPEED FREQUENCY 7 | |||
METERS /SEC 8 | |||
U Y U/Q y/Q Yavg/Q 9 | |||
10 0.447 0.000052 0.00011633 0.05 5.81655E-06 11 0.89 0.0001 0.00011236 0.093 1.04494E-05 12 2.45 0.00018 7.3469E-05 0.25 1.83673E-05 13 4.47 0.00025 5.5928E-05 0.0298 1.66667E-06 14 6.93 0.00027 3.8961 E-05 0 238 9.27273E-06 15 9.61 0.00035 3.642E-05 0.05 1.82102E-06 16 10.56 0.00035 3.3144E-05 0.013 4.30871 E-07 17 18 TOTAL 4.78246E-05 19 20 Yavg/Q X DIRECTION X O | |||
= | |||
21 4.782462E-05 0.1 0.00012 5.73895E-10 CURIES PER 22 METER CUBED 23 UNRESTRICTED MPC FOR ARGON-41 IS 0.00000004 MICROCURIES / CC 24 262000 5.738955E-10 0.000001 1.3 1.95469E-10 R/SEC 25 7.03688E-07 R/HR 26 0.000703688 mR/HR 5 | |||
X = 2.62 x 10 9E R/sec, Lamarsh page 568 where 9is C1/cm3 E is MEV Spreadsheet 6 | |||
.}} | |||
Latest revision as of 22:08, 6 December 2024
| ML20207D528 | |
| Person / Time | |
|---|---|
| Site: | Rhode Island Atomic Energy Commission |
| Issue date: | 04/16/1963 |
| From: | Quirk A RHODE ISLAND, STATE OF |
| To: | US ATOMIC ENERGY COMMISSION (AEC) |
| Shared Package | |
| ML20151U912 | List: |
| References | |
| NUDOCS 8808150377 | |
| Download: ML20207D528 (15) | |
Text
,
m I
STAT 8 0F RH0DE ISLED AND PROVIDENCE PfaNTAT10HS j
\\
ATO'310 D4EROY COW ISSION Docket Wo. 50-193 April 16, 1963 Chaire.an U. S. Atocic Worgy Coc:misalon Washington 25, D. C.
Attention: Division of Liconemg and Regulatica Gentiamens The Rhode Is1cnd Atcmic Energy Consission (RIAEC) herab7 submits for approval of the U. S. Atcaic Energy Ccmnocion (USA 20) infornticn to establish an 3
ataoophoric dilution factor of 10 se:/n for determining the permissible average concentration of radiotetivu offluent from the reacter effluent diuposal stack which is 22 inches in diaator and 11$ foot hi; hor than the surrounding t
terrain. Such a dilution factor &pplicd to the disposal of cirborne radioutin c:sterLd is eufficient to enaure tJ st the yccr3y eversge concentration of such i
n:aterials at all points in unrestricted aron around tho stack, whica cuald be cccupied by individush will not cxceed the mxinam permissible, non. occupational concentrations estub]iched by the USAE04 The inforation which fo11cma 2dicates that dispceal of airborno radioactive 3
ut,orial from a stack which pr<nidce a dilution factor of 10 sec/m can to actoly permittod. Tuis factor vill be rogarded as a limit and gases will bc L
releauad at a atniuum lovel aft,or c rcib1 monitoring.
the rcactor building ventilatien natcs and the systems for removal of anbient atmosphere undarcoins neutrca batted 2ent, in ths beam ports, dry grm= facility, and allied racctor experinatal facMities,, hys been described provicualy (1,2,3)3 This exhaust syste::) will niao be und for the ruoval of various flauhing gases, t
s
- 1..-
o
' ;7' L
alnfer:mtion Supplied in Rt,spenn to Q:cstiene Ccepiled by the USAEC Regarding the Rhodo Isl nd Atcuiu Energy Ocxaaission Reactor", answere A-3 and A-h, unbmitted to USt.EC on June 29, 1962.
2.
"InfcInstion Supplied by the Rhode Island Atenic Energy Coemission to Quostions Cor. piled by the 0.0a Atec.ic Enerry Commiartion", answers item l
11 and attac.eJ non chn.t, ILm 13, cubnitted to USAEC un thy 2,1962.,
3.
87afor.utier. Supplied iy do Op.e s1 dwtric Co,rtpany in !sspunce N Qucsticas 5:W LJ by N "S.M hwcJmg the E%do ktond Atra.ta ! Meg,y Ccudssion Reactc. ", cuuvers lj, % aubchted to USAEC on Wy 2,1962, 8808150377 88080s PDR ADOCK 05000193 P
)
f
'. : rich us holium requir?A in cetati caporinontal est upa in the ganeral reosarch progrn. hoac gaces. ill to colleevad in a usnifold and after coroful monitoring exhaustad to the exterior of the building through particulata filtors.
These s/ stems will cxht.uot thrcugh a sta<2k 115 foot cbove the currounling terrain by maana of a 4000 cfn bicucro All building venti htica intakes are fittssi with louvers to close them off nutoanticony in the evont of tho necessity of using the building clean-up systor fonc71::3 a reactor incidcat.
In relsasing gaseous cctivity to tho atsoaphoro, the RIAf C realizes ths necccsity of pret3cting inhabitsute of unrostricted t.?cca nur ^he rasctor site fr(c owr c:poeurs due to the stsch offluont. Hovowr, due to diffusion in the atsoaphore and variations in wind opcc. end ditcetion, ernuent concentrations of radioactive gasos in excess of ths kPC cca be aufoly dischersd frow the etzck. It is the purpose of the remaindor of this tn.r.aa.ihl to rovi<u the reactor locatica, the appropriate oparating proc:durcs, cr.d the applicable tactoorologiesi diffusion thoery in crder to justify thio statment.
The ra2cter facility enriron.azt lus bean douctibed in prior transmittala to the Civi.sica of licencing and Rg.Gatica (b,$,6,7). A nun.aly of this information follona.
l~
The reactor is located or. threo c:rea of Isad ca a 27 scre cbandoned milit:ry reservation formerly en11cd Wrt Darnsy. The re:ervatica iu in the Town of Narrtpasott, R. I, en the wst choro of Narragsnsctt Bay approxitnately 22 miles acuth of Providence, R.1.
x.d spprer.b.mtely 6 miles north of the entrance to the Day froa the Atlantic Ccean. Iocated on thia 27 acre site are the R. I. Huc1 car Scienca Center (the ructer) cnd tho Univorc$ty of lihedo Island Marine Imboratory.
There 10 a ssparttion of abcut 600 feet bots:Ocn theso facilitieu. In addition the U. S. Public Ilo60th Serv 3co io prosently constructing the Northeast Shellfish Research laboratory and will econ construct n folluted Wtter IAboratory adjacent to tho 27 cero of to. The Jr.nd -urrounding the reactor is essentially contro11od by the Stste of hacdv Ic3..nd themch the University of Rhode Island. Tha distance frca the reactor building to thu boarAry of the thrco ucree of reactor inad is h.,
Intter, Arthur b Quirk to USAIC, dated August 3,1962.
5.
Intter and enclosurcs, Arthur L quirk to USAEC dated Vay 2,1962.
6.
Intter, Arthur L Quirk to b3AEC dated Janunry 19, 1962,,
,e, 7.
Technical ipocificaticos to b: auM.it%! to UJrd:.
2
lf
. 214
.18 x 20
.o13 o.002 x lo-5 TOTAL 5 35 x 10 sec/m
~
L L.
l l
l Enc 1 (1) to RIAEC ltr Dated: April, 16, 1963
-l TABLE il PERCENTAGE FREQUENCY OF WIND DIRECTION JAN FEB MAR APR MAY JUNE JULY AUG SEPT OCT NOV DE-C SLN SUM /12 N
9 9
7 6
8 3
4 5
6 7
6 5
75 6.25 ffE 7
6 6
8 8
4 3
5 6
8 5
3 69 5.75 PE 3
4 5
4 7
4 3
4 5
6 4
4 53 4.42 EM 1
1 2
1 2
2 1
1 1
1 2
1 16 1.33 E
1 1
2 2
1 1
1 1
1 1
1 13 1.08 ESE 1
1 2
1 2
1 1
2 1
1 1
1 15 1.25 SE 4
3 7
8 12 7
7 7
4 4
3 4
70 5.83 SSE 4
4 4
6 8
8 5
4 5
4 4
3 59 4.92 S
4 5
4 7
5 7
7 7
7 6
6 4
69 5.75 SSW 8
4 6
8 6
12 12 12 11 7
8 7
101 8.42 SW 10 7
5 10 6
14 16 13 13 12 10 10 126 10.50 WSW 7
5 4
6 4
6 8
7 5
6 8
11 77 6.42 W
7 6
6 6
5 7
8 6
6 6
9 10 82 6.83 WNW 11 16 15 8
7 8
7 6
7 7
9 13 114 9.50 NW 13 14 13 10 8
8 7
8 9
9 13 13 125 10.42 fMN 7
11 9
6 6
4 4
6 6
8 7
7 81 6.75 CALM 5
4 3
3 5
4 6
7 7
6 5
3 l
t
TABIE III Stability Parameter Wind Velocity iff. Coef.
saax n
uph C
miles
.2 (superadiabatic) 1 39 0.21 5
34 0.12 10
.31 (L12
.25 (adiabatic to 1
.2 0.56 isothermal) 5
.16 0433 10
.15 0 362
.33 (Isother:nal and 1
.1 1.7 alight inversion) 5
.08 1.M 10
.M 1.25
-L
.5 (strong invorsion) 1
.05 0.11 5
.03
%1 10
.02h 0 11 C
t l
[
I l
C Enci (III) to RIAEC ltr Dated:
April 36, 1963
t.
s EF ST HT 14000 DAVID A
B 1
C D
l E
F G
H 1
2 4
delta H H + delta H 5
26.95/COLC COL D^1.4 dxCOLE COL F + 35 COL G - 14.6 6
EFFECTIVE EFFECTIVE 7
WIND SPEED U
W/U STACK STACK HGT-
_8 AVG. WIND HEIGHT HGTOFBLOG 9
MILES / HR METERS /SEC METERS /SEC METERS METERS 10 1
0.447 0.45 60.29 310.71 173.62 208.67 194.04 11 1 TO 3
.44 TO 1.32 0.89 30.28 118.48i 66.21 101.26 86.63 12 4 TO 7 1.76 TO 3.08 2.45 11.00 28.70 16.04 51.09 36.46 13 8 TO 12 3.52 TO 5.28 4.47 6.03 12.37 6.91 41.96 27.33 14 13 TO 18 5072 TO 7.92 6.93 3.89 6.70 3.74 38.79 24.16 15 19 TO 24 8.36 TO 10.56 9.61 2.80 4.24 2.37 37.42 22.79 16__
> 24
> 10.56 10.56 2.55 3.71 2.07 37.12 22.49 t
17 18 19 W - STA.CK DRAFT - 26.95 METERS PER SECOND 20 CACS BLDG HGT - 48 FEET = 14.6 METERS [
~
21 d - DIAMETER OF STACK - 22 IN.5588 METERS Spreadsheet 1
w s
~
. CV.
EF ST HT 14000 BOSANOUET A
B l
C D
E F
G 1
2 3
4 delta H 5
E AVERAGE W/U (W/U)^2
.615/ COL D 1.31 - COL E COL FxCOLEx 7
WIND SPEED 3.14y.5588 8
METERS /SEC 9
10 0.447 60.29 3634.98 60.30 0.01 1.30 137.50 11 0.89 30.28 916.93 30.29 0.02 1.29 68.52 12 2.45 11.00 121.00 11.03 0.06 1.25 24.21 13 4.47 6.03 36.35 6.08 0.10 1.21 12.79 14 6.93 3.89 15.12 3.96 0.16 1.15 7.88 15 9.61 2.80 7.86 2.90 0.21 1.10 5.40 16 10.56 2.55 6.51 2.66 0.23 1.08 4.83 Spreadsheet 2
EF ST HT 14000 HOLL A
B C
D E
1 2
26.95/ COL A 1.5x.5588xCOL B COL C + 35 3
_4 U
W/U 5
WIND delta H H + delta H Heff -
6 SPEED BLDG HT 7
8 METERS / SEC 9
10 0.447 60.29 50.54 85.59 70.96 11 0.89 30.28 25.38 60.43 45.80 12 2.45 11.00 9.22 44.27 29.64 13 4.47 6.03 5.05 40.10 25.47 14 6.93 3.89 3.26 38.31 23.68 15 9.61 2.80 2.35 37.40 22.77 16 10.56 2.55 2.14 37.19 22.56 17 18 19 20 delta H = 1.5dW/ava u Spreadsheet 3
a.
L!NE SOURCE 14000 HOLL A
B i
C l
D l
E l
F i
G l
H I
i J
i K
1
.12/ COL A COL B/.01 COL Cx3.7EXP 07 COL E SHEET 3 COL Of4COf. E COL F/400 COL "3x1000 COL HxCOLI -
COL Jr.1 2
3 4
U 5
AVERAGE UNE SOURCE UNE SOURCE DISTANCE FLUX AT DOSE RATE DOSE RATE FHDUENCY DOSE RATE DOSE RATE 6
WIND SPEED STRENGTH STRENGTH UNE TO ECEPTOR MICROR/HR OF WIND COMECTEDFOR COR CTED 7
Nim SPEED Wito SPEED FOR 8
METERS /SEC mci / METER mci /CM D/SEC.CM 04 PHOTONSPER MR/HR DIRECTION 9
SO CM-SEC MICRO R/HR MICRO R/Mt y
0.447 0.27 0.00268456 99328.86 7096 3.50 0.00874867 8.75 0.05 0.44 y
0.89 0.13 0.00134831 49887.64 4580 2.72 0.00680781 6.81 0.093 0.63 12 2.45 0.05 0.0004898 18122.45 2964 1.53 0.00382i37 3.82 0.25 0.96 13 4.47 0.03 0.00026846 9932.89 2547 0.97 0.0024374 2.44 0.0298 0.07 14 6.93 0.02 0.00017316 6406.93 2368 0.68 0.00169102 1.69 0.238 0.40 15 9.61 0.0 : 0.00012487 4620.19 2277 0.51 0.00126817 1.27 0.05 0.06 16 10.56 0.01 0.00011364 4204.55 2256 0.47 0.00116482 1.16 0.013 0.02 17 18 THIS UNE SOURCE CALCULATION IS TAKEN FROM LAMARSH,PAGE 462 2.58 0.26 19 AND CALCULATES THE PHOTON FLUX AT A RECEP's OR X CM 20 FROM AN INFINITE UNE SOURCE. THE PHOTON FLUX IS THEN CONVERTED 21 TO DOSE RATE IGNORING ATTENUATION DUE TO AIR SCATTERING 22 AND ABSORPTION AND IGNORING BUILD-UP 23 l
l l
24 GAMMASSO CM SEC - GAMMAS /CM-SECDNIDED BY 4 TIMES SOdRCE TO RECEPTOR DISTANCE IN CM.
25 l
l l
26 IT TAKES 400 GAMMAS /SO CM-SEC TO PRODUCE IMR/HR 27 FOR 1.3 MEV GAMMAS.
l
}
Spreadsheet 4
- ~
PLUME DOSE 140@ HOLL C
l D
l E
l F
l G
l H
f I
l J
l K
A I
B 1
2 U
S pS 3
AVERAGE PLUME ISUB1 ISUB2 kl SUB 2 ISUB1+
DOSE RATE 4
WIND SPEED CENTERLINE k i SUB 2 F19 DIVIDED BY FREO OF PER UNIT 5
TO RECEPTOR.0073XS WIND SPEED WIND SPEED EMISSION 6
DISTANCE RATE 7
DavoU/O D/O Dav9/O 8
METERS /SEC METERS 9
10 0.447 70.96 0.52 0.65 0.46 0.506 1.156 6.0276E-06 1.3485E-05 0.05 6.7423E-07 11 0.89 45.8 0.33 1.6 0.82 0.902 2.502 1.3046E-05 1.4658E-05 0.093 1.3632E-06 12 2.45 29.64 0.22 2.4 1
1.1 3.5 1.825E-05 7.4488E-06 0.25 1.8622E-06 13 4.47 25.47 0.19 2.6 1
1.1 3.7 1.9292E-05 4.316E-06 0.0298 1.2862E-07 14 6.93 23.68 0.17 2.7 1
1.1 3.8 1.9814E-05 2.8591 E-06 0.238 6.8048E-07 15 9.61 22.77 0.17 2.7 1
1.1 3.8 1.9814E-05 2.0618E-06 0.05 1.0309E-07 16 10.56 22.56 0.16 2.7 1
1.1 3.8 1.9814E-05 1.8763E-06 0.013 2.4392E-08 17 18 TOTAL 4.8362E-06 19 0.1616 0.0073 0.0034 1.3 5.2142E-06 20 21 DIRECTON 22 DavnO X FREQUENCY X O X
sects 23 4.83624E-06 0.1 0.00012 3600 2.0893E-07 RAD /HR 0.00020893 mR/HR Assume pay =.0073 because o = 1 c
=c 0
=
x y
pa =.0034 k = buildup factor = 1.1 7 = 1.3 MEV for Argon-41, E p =.0073 Y
receptor - (.1616ppah) O(Il + kI2)!11 avg where Il and 12 are from pages 341 and 342 of Meteorology and Atomic Energy, 1968 Spreadsheet 5
MAX GRD CONC 14000 HOLL A
B C
D E
F 1
C=B/A E=D/C 2
3 f
CORRECTED 4
AVERAGE FROM PAGE FREQUENCY FOR WIND 5
WIND 410 OF WIND SPEED AND 6
SPEED PASQUILL A SPEED FREQUENCY 7
METERS /SEC 8
U Y U/Q y/Q Yavg/Q 9
10 0.447 0.000052 0.00011633 0.05 5.81655E-06 11 0.89 0.0001 0.00011236 0.093 1.04494E-05 12 2.45 0.00018 7.3469E-05 0.25 1.83673E-05 13 4.47 0.00025 5.5928E-05 0.0298 1.66667E-06 14 6.93 0.00027 3.8961 E-05 0 238 9.27273E-06 15 9.61 0.00035 3.642E-05 0.05 1.82102E-06 16 10.56 0.00035 3.3144E-05 0.013 4.30871 E-07 17 18 TOTAL 4.78246E-05 19 20 Yavg/Q X DIRECTION X O
=
21 4.782462E-05 0.1 0.00012 5.73895E-10 CURIES PER 22 METER CUBED 23 UNRESTRICTED MPC FOR ARGON-41 IS 0.00000004 MICROCURIES / CC 24 262000 5.738955E-10 0.000001 1.3 1.95469E-10 R/SEC 25 7.03688E-07 R/HR 26 0.000703688 mR/HR 5
X = 2.62 x 10 9E R/sec, Lamarsh page 568 where 9is C1/cm3 E is MEV Spreadsheet 6
.