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xNEtouncON
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the
presen0t
has be
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datCm
t theemamlea
for ansy twanty yasre ad gratdually Itost
people adnation tCs evWy portian Ot tin eartnea
bmn ewoed a
ot the ear.
the problems at allot* ad rcioactiv
ctions.
reSObly
Well
eContfl
le in a OCIeaM
ng ad delopmat of
the t
cntenItion tvm Sa* f
any ad extonsiv
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OU the Othaer ha4
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substae en#be
e(xpea
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ptae
s are na-
caftainly, a
of veeareh on thn
eatann-
extnt aid Offect of radioactive fallout that haft been done a"
ly
t
as a stratoM
t
his
of tfear, alto
nme Aat
aet ame itae
thouaht
tive abstae
We the wave me of a radin4
tracer MWay cae
onts 4
ton dcbaevast
11=h 4isom
jeatitted4 404 0""9ssayo
The dtonatiol tmay be eteotLee
wideroits,
r hurnts, inrfc* bWlt*
as
and sea Wrarts. ft this paper, only the st"n
burat will be craidfrm
ancmt iof eneary to rapi4ly rveal
tL heat adc 15%Us ntUcIrO
oofts oaun,
ulea
na,
mcan
s d Of th
radiatifon. the
at the time of the fttontir,
s the atao peg
about SS%
anlasd ainr
westar
rad0atIon tO 4at
SS
ray ad the
tg 10%
iivtial radiation ame n
ifn2atd
initial radiation eonaisti* Mnanly of gan
rnwidual radiation. thi beat eovad
a large
while the residtal radi ti(A
L disparsed
the atfcts of resldal radation ay be tlt
hours
ot the
after the detonatmO and at large distens** trn the position
biut.
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callo
"I Ied tbin
tuhl*
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a
As 00*114 QOQcUn, th
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4 IA the ftoflbe
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bWSH t,, th
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attamaet ta
t"e flnbef IVs
bft awl
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t1 parttclSoil vof~"*4
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In
&44theerth, the rafte
te particics fA the CId dnantfly tal
Of tal be"iE .)epa
latt"
f 4 the
s. As4theytall thv we &oo
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byte
tCoe wctt *'o
t im to do so than Otbnre
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be tssfttto4ut
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of the oath. ***a t
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allout Ua 4al1e
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all of tba pottascM
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up tuto the
earte
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fallot n
o the SOrad,
flM141 the pocttcl 0 es
1thI&PWWy
Lted. oil the
40Tf (sott't
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tpa
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Wift r XIS1t. By far the jna'rtuf 'Prot~;Orradtacti%v t
the 4tato
srvd
UthM ItAtwzn two tin tin at
reache0
tnt
tacovo
n
ad vitbtu a few tbaoasit
tvttou*Vwotye
of
o t the locality ot deo.
actmo
axe by far tbe a1n;,pln to stagy, adA
will be the only type of valant oonia$4d to this ps~v ,OW
acitpttot ia batid tox teoerom
mra Our..
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(3)# (4),
above 4am
ftef
to t
by
the
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s
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the
unly.
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deto-
the tauonet stJbt"a noqutro pOWAttim o Ow qu*tas
for the pwed ot tivn tldve4. "0 vWposO of this Stady to to pmov&4
a
thd for .atitI
the fatllout dtstwthatta fwm m
steoewod or predicted $O wb adt Etose
s*u
of the mo4tttajtioi produced by preipttation at
datonation can alsoe be ad. fro the o4els.
3.
based o
y tim
or place after
tthe dttl*
n*
i.actal wlx$ fioeldsw
a nm
theamw4$Aodt
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tb
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t tl
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t bho
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o cete
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the tea
40
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iat
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tares * selpla en, e
ttis t4
aotuntdts
4i
off nwt
aestatlnz
f
t
11*1*. U ass
ht~BEs
to
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se
VWr=a 1 *U OWSA
Uttw (2) weet. t*an04
toa me
a
-V
tar sp*e of- both sisu of bwrsty won
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s
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.t4a
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anpr UAtatr
l la~
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ho V
1
aft
m (1sW), ats4
10 kilotos
to snauteat
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h ostrvatteioo
a atto% *mplAw tm
Of thtp b"V
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be~ peopation14al0
to~~a3
m
s
to bo p,
pt st41e fAa
e
Mwe
wA
to b
ot O*Iiao tt o partielas Uee sem
wear
tas2~C
4tet ages at
s.Stitod,* wanf
t
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t 0h
radiso~isp4 afa
to
anet
t
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W),
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wift r414 of Is
a. *lPwtwo*
is
Soweo 41~l
to
o"
n.'apot ),4 of then total
*ipaticle
Mom 0 d 0to0000000000001
LEPk:douviYty
vtloy
dio tabti
of, raF
#4 bS.
Ss4$caatflt
fti
volvi",amn0
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5%rn amt$n
t,
4a4
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t44 tio wi
i
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tWO.
(1) M4
to the ""to of
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p414.. s
stem
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particle 9t gal stas
thst
4
at..v*4u400Vits
tag ttoa*ttoml
aB
.
weft
tK- pattlea von
I m stes v Is 14.
w 40lF
t
A
%
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*Lonl
layers
t"0"0
4salt,
La *#All*r
IALnvM~t
of Of ndvatte
total0. 0000*
LOV113044
U
asmood to outmd vwl,*.~C
W" to,
or tho to XT0,datmatiou
mobromt%4U"Oft
** CW
ow
ticaily &oft I4-00
wat
-500 ft
at to 2%
od was tv14a lo
with 500 toot tzttcnalso beta .ltn..** S ta 10no0f~
to
ly re 200 tn"t baby orn4 UIte
o 4vL44tato aota
And
to 14%
v~ora, with IMO tet tat
"Is
ot
Matwss
sitne, *
l6WlW
4Vtc Of hVt4 tWn wagEs balm.
WtttlQ
the attn4. pnbte4
U
1wV4 to 47,000 teat. flt*
"wneOso that 0 tint
of tbwn vters ten *t t06
to fly. waters, itt bortmatot beu40u
64,mdant
4,0
atM#S
Its
.ltt t* %tat
13.00
waft"
40 no
cost
*170M
u um
tVWatt*14
A
MC&AAfWPWaA
airX
Oasn
Lav~
inablo
wares L tnl
tt4
0
to fte WaOaSettS At t0he*VLOVS O **
log to t&w ItwIS O tinWSho
2 at
3.
tb
the vatoncttvtty should be 4ttrt$*$OV*OW
in ntty,
vatr. 'Ta tin
nel
priLitt a dttrtbtto
ortaLaate At tbon aOU
w~l
40 1*
atW
v~mttvtty ditiaUttm
In
be
as
n"0e.ad the -49itore
taO
nm
tuat 41 pw)atteU4
ton"U
the
got lead to Sorioa
m
Matr
valtc
of the v~ will
ea
thn
a a p14 at 340000WW
tbe10 Ttsad th*Il f MUf
ela~y 9500 teatt 0O 100,000 tooat, natwtay.
we app
in
tn*prin,4toQttstu,
10
V vto
*o
tw
LonlUMtotOWM*f
to be
o
twad wrafly
to roacto
tti
v.ts.
mwnww
to
4 v 44s4inw
to 730M0 ftet,
20
4Mtp#2,00Z4
tt
4wa
I Xfl
$T ub~
viam 4L$Aad L1400
$tx0$
a
S.tA000A
0 Wt"
JAOw Sqatiat
va a ula
l
f"
'tgll*otM4k
W*IUg
2)v is the unbtn 40Pte'a
am. ("u
#A'
adwaly
All
LA each watew L& tEored Lto A£ 5
rs4dloative mt rtil
of tn
ufIlt*
oqmms (teUAn) vhieh to at tta ceantra Poat of the wtur. A ZrIA oono
over al stw
was td
was tealpoat to aUk optim use of this
100 Sil bwr Uwe%, "Th*04
.co44be twod tnetote1r, '4bat
oti, -so that te rda 44
En
"sefor
ti
pi*$0 to the astie lmt* S
lefs
uatiou.
t
t
gad points to
thn dad4 date whAkh ap-
tsat
i
a
thre
SaM
at
"tWtte,
the level at the iontts or a givep lape coste
the attn lpm.
toot Oaw
terila to *a
mod thm Is 3000 fSoot
ale frm 10,000 to 20,000 tnti
eratw
diotributtmi,
to 10,00* teot; in 200
in the rage %fwsthe onet
to
protftm
U.S. rob data wids are given for 1000 toot i$tew.
t the sttwor
wval
to 1et the 0n
tis
aus,
to tn omlq wos ssipned to the catrl
ta
1/13 of the
teala the print o0ad
%an to
tanins Z, eqs w
daeUo
o nd for tin 10 t
tens waf
taksa at 1000 toot tatearalo tom smmd to
10,00 tnt, thn at 200* toot Iaterwt, tro 10,000 toot to 20,000
fet in t0 0e o tOfaoe eMlXI
dets e~ea
sixtaee
to 73,000 fet, t e
tu
W4
4OW4t
w tale
wan we4
uri10 K
loels wewo the soe as ths frhe
ulg teVt,
%MA tbe
tos 20,sOM toot to 70000 toot, won
at
tir-
ienttn, Iho
aemto ,00*
tay4vtlss
loot
To order t6 soadnt a stvay that would be 9404val M010 fto apiAY
to
pot
.1 sitation, a pla borsotsat ge
was
aods in
t Wray aWd #4
sgive
ta the
ataUILawg sats
pi
aw' potau waft pCstottSd it, a
at Ltervals of 200
lntWO cst bess"a 1ep"tora
s, tack pt
(~ pair ofks
point at
P
sadt)
oesttug 4tirectto e4
4 c* 4 twy vm at
at
I *5 Ta
tmfs,.e, ai
levels of the
vuti
*
ou14 nosnut lo
tia boflhntal
variatione A the 41440 at the vaVXan irat.
Lowtiag ncbiam to gaiclM htaf*tUk dot
In oder to Us. a
requires
tatio
vs ofa
tdie
40ppa
1
ilmepatto**et
taminm
t
ap
Lai. A SAt
tLe tn
t
,tin, it Is ueesar to a
lwfty s th4 tocgt aZ the tin #ep. fl odan to statF
tin varees
nsalreeite thi tin
owas** that wosd be ApparULa tO thi
*tog*
wU*d be *ta
uttwt
gStrVa cseie
mad thon
cowotate tu
to five
avi*".
or t
to
%waftms a tstua
th=401
tint
tom
weas0ary
tt was
)a
petadm
Lo tbo 006M 0,l-W,
ot WasOMMOMMUNP
f1*sta y.
Atfn
in R
M
tiA
a
I 1Cu-
0'41
0
a to
OAS 4t *be stAM messsm I'm goo 101
aetotn
t thusm
to A pwrod
Unorer to tocttatat* the
I's t the tota "nOXIS 010exeprseat
w-01 1-W
oft $%a0TQC
tqm
ctna
no
nasestt wn fta
n
e esp wasd
S
&iA
S durtwig
ot
*xtfoas Cetr mw tial
ta ial d dat IA this pa
tW0 *da l.
uXat
i0 fal as to 1ld
Wlm,but # *
mt
that adequddY alph
fl
ad to be MattcLAnUy aII
Oteps
I
I as
,
t
t
ho
.
".9
diatethettaa ot
ain a
lb
"wtt*
ttnats at stone *
and tin
ad VttAd,
bove tbi
(S) wa
aS
inr3 iflflo
4uraig
a typieM naS
$00 b tlowl a viUW distratmtin aZ fZod to V"00004
as"do pit"* 3 was t akef t
the
bovn pubiatt.
ltate veois
Sta
o
adreetonaft th9.
v adeoui
0too, bowew it
10
So
futlly "o tuntwa.
o 30W0 teat, the top of ti
te
b
obtavw by a wee
h
et"a
t*A*
300 Wb
set b t00
t
*
apponowtely wmntmasts tb* esos
$00 ti@ed.
dimaton of tba Satn.y,
twnztn twae
0"a
thn 3S
Sigg"uwas platt# tor winds of 20, W0, 60, ad ao umatate
tent, so
m of
of WO$* viaW VAhIS
the 4teti
ipnd
to
ft to be 0 kts,
frwas
tiErAlaon.
09 a 600 z 400 OM
a coastaut $0) t WifAl For SeVIttty the c-ea4
arItan ansted to
thin
n t
vae ooavatmfta
4d
thits, a hate
ttafs
e0a
I
d I MW
I10 &
W as
lttan
nftolS
e4
ttwsf
*tmly to to investtgata M
aft 0th
he Impeo
the $0
as* betWee
sfWlydil
*L And t nta
abtw
-
* I
ad
then
ab
tsts
iok
3004
to a be
frieatte UapV# vwimS MaV OWMPOe
i
wu
spe4 and direttka of the wie
ftlow te 3000 togt ntl Us the trittio
tseeAder the geesett
etta
t s "Oftl t.
ata is 2/3 of tat
at 3MO ft, nd that ft t=W 20 t.
akdtfl 4tea4tco.
* 10 *
aepie
the
a3
petab
fe*
i to w
at tOo
s bel w 3000 ft a tuat its et
Sthat the win
lu the *otte
asmto
ocal
lazar, Il wAlit
&Vs
awnuea
shaar
4Oft
oi
tunatcnt.
ct
ooputatLu
;on$
Ue %ad* 4At
ftrictla lavor La oz'4r to tlM4 Ow 4a t
ta
0014 L4 tdsix layer on the
tUlttmst
The 30W0 toot tinde uove nlert
esnttnv
4"Ulw
ot the vWa
st e
so that a sstttcteat ma0hr of
"*AlU
typkaltrio
a
Idos covtrtq41-"
tLot* Ext t0#fl'ate Ustitu~es wold be avaUal,
toot
Ot1ow M
LaW*i
di-strLboiO
b Wxi %A# the3
IAJ mx all, in fte mwinatta Cpf4
40* 10, 2a#, aud
to~ the $X0 tb u4s4. alaa
oot wuai* A& am$4a h.4 M)0( SO
120 kmts W"an0 sel-at.4 two Via4
-Alw
l
tW
k*AM).*V'4U
V
to tbs $0 ut* viw&. ta4"UW
49".
*.U
1
s1~9
5 OF
it
*a layn owtretf
at the amnasvb*.
aVen
540, 104-15, ad 15-20 thaund feet.
Ga*S
Zn as to a t
"nn obtaa
purte4t 244, ad 6 hount afte
"o
f
after
-eafto an wo"e g
nm4ete AU4
ret boE
as I
A CoMlatSO
the atmosp
ea
wraftes by 2 hbe
e
0"'.
to. aa out" .00 %" sEo
0*ted.
at tb dtariatoU at aelov
at a giva layw 1A
* tor a gva in4 tt44, would aspet that the 4 WA4 6
her patrem
wOWd
patton expedby
uterl *"ate 40*o
a Otral Shape as th 2 bOl
rely banV the
*ia
Lactor o * c$r
nt
.4h,. ly
se4 meompe
oo"te*1
e
coeiarattes of the
pzvwth elo
s total
mault*,
an *wotieOS of WtI fl0octty -04 to osly
*"mt.* with*a teth 1
S)v
toW wdel wi*$ flades
molts of te tit
e radioattvity we distributed An a0t4apt
1
od that a l
a* a tow
deviatins in the 04000 toot layer end on the grod
stt
aWW 'en never greater them tn
activity kwaved tms smail s
planed agast Aacea
oil$* anw the
at thee dtstwibvSttms
ntG 41 b4
for the 2 bow 4tertRioa toA r a gion
laears.
m 4or
pA
reslts. or the 4 awl 6 bow ditrbuto
Ptte
Oash
ase
h with tb* distance *eats entracted by
o* 2 avd $3
deviL
1em 1%U puvwages of raoetIty
asume to be La a statt
vePS
ftematLons
tin *"*-steWOUtest
tee,
s at 1 tb eta patalas won taud to teeth tu
Is
r
bae
e
Callot Mustratan
Pot each wtu4 t.d
face, sad for tevts
E10 OftEBA
pfttbay (Mgar
4# t
- 12 *
t
teton
e1se t eu" nwm aneml
paral tl tea Te 4 and 6 trw aurv es wre thn nlttplit
at radtoattvtty ix
fetor ttet was the ratto at the total pewee
the layW at feh ot
t"
te
ing
by a neaOL
(OW owa
tatio of the tias .0aene
pia by 4/2)v the rstefting aun
falal 'wnd fSeld
S thea
WW Lavnifltoa. A
wtndtt(g
he 4eUt.t
ta
tsoe
7)nw
41Wps.
0,
adtbtc
Mtw
Itnati
ti
*U.*~
o le
Sona
ot te%
c4 (2) A Sp44
14t OVv
t*1)
ant O-
as f trt
tcmpwas nWtt*
a
seo, the maits
1O
*advIM
-
41e
pl*ated vs
t atiton peakette
.r!Isr~~
e valw
*a, *a9i
apposia~
akj
Inktas
iarit .t5*
tOEA .
by tae ttn
tril
to the
Se 15,40 thoutaSd COOt lmr
OtAg
that vat
of
saltE oe
0als S stes wVta anatedr
tM
by a nma.
not p4ne
OiAerhta
1 414
LtstatAo 1tsa elb alrWs
,sotwoa
tb
dtrbutbt*
OZ the 2 bou patte
fth aS pedta
sach odwa
pdfat
be
W t* pttewn *SW
"scaletostor, Whe location
by watIrpi
to
406 sut,
4 4 bwns
Lmte that wita
2 hrar Camn ftr the ans s4
wattplytja ta
in
tod
wac
In sehb 14pr (flSgjn $). "do "a"t
41momloW
fn t"e lowe
IPO "ae pnvw*n
at 2 %our#div"Ma
ta
w
tvtv t
how oetrn wae sultipliM by tbo t**a ptatles
weapute prg
Canste0a
A
t
e
opsen
etwvS awar tb pantes having Lath velocitica Ian then 040 tI/n.,
~be
tiSens
a'g
w
falls 4h"nut
h"44 in
Pe l3-Z
1th10 act
layer in 2 hours. Figure 8 clearly shows the results of this computation: the skewness was artificially introduced by the computational
scheme used in the model (the stepwise continuomse wind field). Tae curves
- 13 -
am
pcolaU4
tve b*
abn&4
to each
attape at best flU teaWg the 44A
aot, tha anaVes uswa
4) aWO bettewA Ao OOOM p9WtaniY be
(ipfgts
pWots, Sma sit
tzd flal*4 up1oy4 ad the
a
4~se Of thsag
A* ptt.
lOatm
at
nAtt
at
awing of pawtios at pattoulr 41
An
inat#na th oanlluAttoWe
fa.1Eof oai% thi typ of *mo4e.
asso~etat the finl rests,
at *alolt
a* swum tadovtt distreabtiwn sysaonts tbe anu
theken, 0t
t0a M ad Us centtn.
aS
af
IMdd Oter
that
aoeeava"is wt anl temble at the orwf.
t w
An asrt
prnetcnw, tin y
ahe
te
hero
w
ksv
tas
tar *A
4ta
* at *, ho
fby the apesetoeft
41Am" at tem
awe taken at te o-ofa
rs
of au-ty
es
posiita.- 00
iMonate
tS
d aac
*4 *a.a
tins at time. otter than t
bis
yer (le
m i
ao
4t
Eto
a k to aa
ta
*e0 wit ba
b
7)MlI.
io th tin.
will bo wItplt*e4 WY twn faWcts
pa
St
totSIe b te pet
-toa
to.pattcl4la*#at
seaste
o lk
a
Dbta
by /2 sst
As ine4 aa* besf
,teullt 4
tie pawt4
tuVst
the b
m
attn
tncldtug tho poittoac will he atLpta
yv aus
1t0d1t
dfor
lO sptawltr the p
ue ttacos
tmap
1aav
tor all
ttcaO .pnnswA"
alkUtab
to
m
amct0
a
oat a Mito
to
aeaom a t bo *46%hs VUIe
t-ltUtott
sti a* v M
I bealo
t
dA*
ke
3iii
~~~Lw t03a
UU"Sm
apt*S
wvt
*"thatqtn.
by thi
axobc4±o nil on be:
fDP~ll
is stiL~K~1
pSl4bto*Llbt ot
distrbLntLa
HatMs botoro ehtcls t
~Mu
at. PO
t" Wwrtou trtta Ova limit. got tlo to IV?
bermcn got-nias, 1-4 aUae.daoal
uutfm
17*~m
(Ka" 9).0*e
prox
tL
siamba9 e
dotU4 nd actor w#iLt alt a the
*l
tin.to b
t b"d suait*
* bmamb
a
ted%to.W.
094rto
at
@am
n
wa
t"
t
ama
soflrVn
0 eatat of0 * ofittM nutrt
4v*
aw1o
the
WOPtt
!LuSt
e beat
V 4
for
pt*t*CO
patawe
urf
Ati
re
3000o
4a
tAtth
tb vper tqe* Svo ma4*Z# 104 ago I5w
so bfwt
09t
i
mt
t
e CMttan(tsv
-
a
Itm
b o
10-fl).
La This
s uuptm $LVM
tamAt
s~t~bsn~flbst$O*1a4
Ew.' AUW# it W40m
Op IS *
$(fta
.sl*.0*
Awt s; 'a
was bqworJw s in
tL44 v"
eusaa
z J dtrectien flauly9 the
b~t4c
at
aoletuos A"rdtl
at anu sfl tet
WA V
tbqr nirni~hl a a ood basis for anwaatatlxn.~ Tht~'ar~w,
tv
Uxe
uS vtt
I
l
wom altced by son totov, a,
jtU
txde tatMw P
the s
dtreetoa t. a -0.4
et,a*
t4a
Lat voij
~
~
W#waOnln
t
In a
t4r
by7# EltW
notittna parttch dointl vould he c*W
nun~
a
$ow (or
patttw ucatttw be
t~t3
t.
1*
dtstributtoaf wn4 hott bo a trts -s tar tlrm the
that the
ti
rad *.
tbs abwn owit2osE shoxgd be OUn
it
4
OWg. Z naflUty
t4 6
for icarSqas ofi
to
at
indtwo
the tnmaltaE ptttfWQUI b
te
mv
4imteats woid be hao by the factor, u*
SThnb
edA the 4ncstty ;tiud be chamge4 bry a &atort1tt.
A ItuM PpttlO by *W* 4cto, a, the nOilt inz4
W"4tltftl
=toay be Mo OsefliattoS $A.tin vw
0
"el
be ecrnftdw*ty mine sdltftMlt tu 4"70-lyfl
4bo~
ypZ~U oneve
by tba oseiflattone1 wnit @Att to tbut
~~
~
h4VIUM"
a ~ so ~
i~
4ft-~ ~
0nnZWe.otl
dolt
Impid-oa
at
is to
La
wfi
aLO
tto trtetNVO
4.~tf
with
my tins that fthe wI-a lts"t
tho wA4NO
thetn
w
Si
ZRv
tarms
OMh tin WA)t $4,
**16 *0
C"04tin
w
*
t aa*
Ift And t~
lll
abt felt M
"
tt
WUI
~;a ba
tow0%*
aw24
~unbtbskndaavw,
*
O.
WM
loft.
baro
w Os~
?s am
tu aeetw .44
4 a
f Sto
"twWtOU#*4b
vtth na~a*IS
l*
t
f Romatt bttae
44tni
doo
wen-vo
.1pu
b*%
14Mdo
bs
rad
wfa-4a
urns wi asc~
tf"asO tantol
for pawtte
fit.
"Preses"
C01MI410901Y Sita
Of
O0096tM-M0
aane 40,000 toot, am tr
000 C t
weawe o
"clureii0migim
tbI
EW
4a
prinatos tarn IA S z Sas equane.
ft thet"ft Of the 10 WflttwitI
044h vA9or 4o1"d Ut Itot A S S
tLetutaemsoofthe1I
oton
20,000 at 40#00
0000 teot) ta"
tnldistribttoue). **
tv
atoeaft O
attt the ndkaativtty tI". S r I wile
pOlt Of the 'wa9494 it W"
4104a0t to tu nt%
to 4tWm*the raded
amws i
00 call wl4tlsa
3a4d22,am4$afUKl*.
a4 amegStnniJA
no
*AI
to
it Vas
thtaom
0 at
b
(em
atctatima toy
a 4if
IMit Wa*
* Of
~M.,V,0~ OLM*,o W~t
at wlo0CLttn, m. wrsfs
ow tn fldr4 ftr-tiamc
1*4
tho UP
m 140,000 to 73#000 90
t
tt
otr 2,*000
atef nay
Wtitj %bU~
ly gnatome4%..
of "aseL
, 446 41M
-theut
w
I
tba
sit* 4 4taft ~tomo
IV
qw
aVtOfm
vtty 0WO Oft APMrcwMLae AXd VOn nALatt
ltatrated Lu I~a 2. Al00, ft w Uom mt apdtt
- 10,1000 toot tq"r ditr*
ftfm 4V
ii~la. irttisftt
b"Usup tft
the 4t9*,
a tAM tbow 20,000 toot i*kwUt
-
18 .
WVWK
* 17 14** 4*
pAsf4 At 0
20#O000e by wm *t the
of variAe 4Lnttao w- *pa*4 Oma beo
vita ttautsap layod tot the 10 Wt ftr
cMlea
was whed Wow 20.00 ft In all ttwtlnr t W tridaw tt
datd
that my utzitcat*variation ct the
for
stb
mm
the socma cloiad406400
an Atiocted
IS at swprttg
4aWU. tie
by vadr4Mjat i tt tbin"
Ina aftlo
aws
tm paviods
saids t c0Onstaeby Iit
to n
#1
%WM ti1
aot20,000 tnt,
wdwp
t-o-00
Wolw 20,000 tnt ad mII1 *ato
attn the ms.4t54 difttbo
sm
Ovms
a
vswa simply *hat
4t4mW*
%.
tthetefl .
mata-tt"n-tbtp
i
tile
~
l"tt *t tbafe tias
to
souf vMWWLtfl4.
to. tnt tba enacts-
n~ft ol u
0tinnft
twn tbq an to tue lower sas
v to Odtatl
ufl
seto
tiom trat the bat ptol
be enS to O
-0u14
oW a
t
t$
t44,
vW d"a awe "affleat,
~~do~
at3r~sj
-e~
t
lts
at
l Ia*t
i
to itit
,se
tnOat
toin0%"t tin uaft
it i
o
nbita
09
tbe
*o
tbo
t4mn
ttb
s ism.tx$a 941 !AV
Jost"*
$600*,VOa basic
the wts a
ipop"
ens.
t4UtAbtlttv at VOW
the udoe to tbne
&VIit
ipil
b ara cQ3ejitt~~ s~s~~is~
I's.1
OW
h2m tnfts
L irs
ndntlvt
a
n00t
atW
h Lstglto
MOO**Awe dtv
MOO
I
Or
bw
t A .
teWIs
ni
20 al" ft.a01"0
ft* t.
little,
howov"w
n
23w24, IMa our"
1%t alo. tiVtI4ntcaM
pea
0
a"n-
to 10
I stw
on0 *ow
pinrn
ott4, *fle
~r ftvi g6t U* Isi
Ot ftftftft to tb~Fafatat tb" a -*.-af~bi~ ~8~ fld.OPAV.o
ofe
lI
S In
$4 eath Uwt.
is ti tile
oEwratatvt
Ge1~
as~ to tban
fluelcasor
"i
Crai Ia tin
ZaS*t
ad
iae
#Amm
I *a&~
at caral
bt theifr
tin
4*o"
t 'Itctla'sw
#aa
. Wmit
a".ftbe~
atool~i.
o omwU
~ W,^4
t,"
14110
a the~
~ IfW
ill ~43tW*
flom*
ttu1sat
#~tto~nIeW
alow
prsfi.Ioft ~10i..3
tba hew
is bottm of in
ast
I O1t1 aWnQ
ft
It~ obattothe,
E mac
t;iad oatnWer
tnI~n~
ff tie
0*bM
ttQ
~alirs). Ite
pef ftthel
S.Paa
Ad dtead acelwy bat a "atomth ehttatty at A0,000 ENW
y
th..
tte
00
orNoI
tapor
..
1*e4n
4at
C
o1 ta
aEAfaof
tm
s
t tin0E1
**apn enthue i4.4 *1*14 *o4e help ia c-nn Wwt
~9,~ ~i
~
IrA"-nalliA o8-out- b p ft- vm90-
#an,
tset
fs#
oo
vaowr*
VOMA*. wi na.
Kzw
9sd
questla of appiMfbfttr Of tin railt4 Mat be
ti
4o4414 both to tnnM*toa
WWI
amda
tot
soeume .tu
te ni00 at the wmOdl41
muite ad to f
*bn
waif
aa
1
W0d
nSW uttaf
t04
dttrU**J*t
ant t4 VOnnM
ikevOVtdO
n*4 4
o.
*AtV*lfr
*V
'that theft
Aft
meet
ina
at
aGnsil
oatint
ano aeece
dtvflts
0WiNW
V**44"
V9444da4ta wp ft 2000 bat,
Sta~a"
ftte 0
rt44. aAras
ttfso the wu* dau ta
a tbe teats UNA to
'4w at eadi of. as au. -peotiso a-~
trfl
UIe
*Nt
tifatad
ip-K.
itoil
wban4b
s1t 4w
that 0-M
e4at adnt the poticaes
a ocs
£M
dly A follow below* ftr tab
t
'4th 4itttt.
"petdao0socuotse
atawt
aLtv~~
Ae$m n40tted tinb aftm
"U
set
- tinhele Wt6"1
a.
byaSL
Pie
trf~~L~"~
pl~Iglt~~~~
to :M- a0
the"ocm
I~~g
oba
Wl (101 9). %Ui
tno wes
or 00
UU4
mity bema
s-las et
th moe*
mn e
Mn
abng ot 4ppMAsaske
no amt
IAW Ode Ohme
W4
M
attn vlzd 4tatr butio
tIat -t
rtasbe Ciften
as
3000
SM fAtte a
SW0 *a
4iftftIM beUm*
fa
4
t
, 4 a#
w
a4
Ot
the MUM
Wu)l&A.ot
*4s
siatartian
teeter Wits
t
U
Vmiattms
utd
L
Ie
a detnatemz at the PO W (0,
radicattsn patktas ftp
taft b 3tss
4nott0l at
whCh WnA1d att
$as
irate (this is two of theo
Lu t
t
e"d te0
1 nl Pee
LA the -04s
t*tlr Smaler ta-e tIm
43 defta
nftociaty 41AtUtto
tAct that the rOot
is tb
*e4ams
0 "
tt
4iStribUdfl
t
tn eat at
ar
trale the wtM t*144 at 1646 6, 19$
PM Ot
resits o the afd4.
"antatyq a pxedtatJ-AS bees -UPC the go* 1-6 M.4 300W-
e
w
sawho amt
WLa for tit
itt".pei
w Po
tin wtwa avs 11*, the iaAtWal %Aats at thn
wiaed sendI (a
witud'
at
09
%u
as*
we lts,
Mm4 aW*dt.1
tiA
fl4Wa for th awtive 4 omw powads 4 *)
nasem
at 30Mn
o thi sfltal,
i to 01or
r 4
d.
acte p
t
to apy ar
nase
W*Nft W&O'
1;t
a (1$, S
ft (M00 13 tvh
saw
aspte
otlay
this
Wse
t
aIttnl a
tscn a boe
tuf
oa
Oahf
atas1ato cmpte ti
oa
ast
%fe
e lato."
UAtWI2t .
Ahe
r14
nd
itntd
*peed shears are linear between the two levels. It is not necessary to
- 23 -
knw t04 tSMd boloi M00 et pro$id" there an in
Mt
)* it
300w ft (as*1 Z3
43 IpfrJ
nit fl)'* (2*
C*4W
tttC anttoue for
to
waattosw fa
f"
s tMt
that a *Wuk lot.hOw
PatteIfw nnui~t*eMfr&0 tM- -t44 dWin "Inttdbe 4amost
t
0 sz xftct
I.r It LO 0- 10
"Mot~y eu amnan the ormato 09 th
Otstrnto
2M
togSlam& at fter"*Atat 04e1 0V(4ft
cpza~ttettny or qUWwttt&fttn47. A qu~ttttniCU8
OW be
fllw, the idsd~o4tvtno
4
fl00
flW
zrSettco
a{kpnt lel
~
a *xhttnoauo$
Mm
~ft$=W
4 0004~t
Cle4
Ar e
to chars b, "Slya
AUSU wtth the *4"v. 4 all the w$A44W
=4
t,
* C
to ttte
aeflcta
Ui*
wa
t
a
sic3
tin *ttflt
i~of
iso4 th.nedrteboL p~paaf4
o~~ilsk
~
$a tf~h
sf the
wloctyw the UM
taas have sur
Ithis l4"c themo
si
INs
*s laver by 1eyo wa*
*
aalve
M
pott-h ibis ntof
ath
41*f
bumtflw vatL*&tWr
mtc.
&;JtiVl4
"I, dim-at
to tbo
nlott
v9low*
4tw
Vt
-too$1~P
ato" sepap~rao
this
est
,
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4a~tba
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i~iXl~jJ~~~
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te
Ltal4i
ef~~~i
-KCZZI
Mushroom
Diameter
7-
Mlxshroom
Thickness
I
V_
lStem
Diameter
Figure 1.
Geometry of initial cloud.
Grid
Square
Wafer
Size
Figure 2.
Actual and assumed shape of 1 Mr wafers.
- 35 -
hei
t
(10
ft)
56
40
36
32
28
24
20
181
Figure 3.
I
I
I
I
r
I
Ir
L
Mean wind speed vs height above 500 ab (Reference)(5))
-
36 -
111
2 hours
3 -
4 hours
2 16 hours
.
10
20
30
miles
S0
20
30
miles
Figure 4. 'iypical curves of distribution of radioactivity Figure 5, Normalized curves of radioactivity vs distanct
vs distance in a 5000 ft layer for a 10 Kr detonation.
for a given layer.
Ordinates are % radioactivity in a 5x5 mile square,
percent
radioactivity
Figure 6.
Typical curves for the distribution of radioactivity in the
15-20l03d
ft layer for a 10 KT detonation.
- 38 -
height
(10
ft)
20-
10-
speed
s
0
I
20
Figure 7.
Linearly continuous and stepwise continuous wind distributions.
I
40
(knota)
0
20
40
percent radioactivity
1.0 Stepwise continuous
0.5 -
0Linearly
0
I
I
I
I
20
40
60
80
Distribution of radioactivity vs distance in the
Figure 8.
layer for stepwise and linearly continuous wind fields.
- 39 -
_
ft
percent,
radio-
50
100
150
miles
Surface distribution of %radioactivity vs downwind distance
Fiure 9.
for 10 KT detonatLons for model wind f£elds 1-4. Units are percent of
total radioactivity in 5x5 mile square*.
I
050
100
I
I
150
200
m
3
2
S10150
PLgure 9. (continued)
200
-41-
Rles
,
-, t*
AN 100,1b1
0 At0
gi1a
mo it
W U
at
ti
$
.
sah,
ant is
1*11W Awwl
Sol
aa
k $"IA
P"i a
to.w
Aft PSO14
It
ato tbn tw 10b It*
ZM.ta
00
06-t
-
42 -
*, 4
to Ca
Surface
ft
05x10
..
5-I10
3
ft
10-15x10 3 ft
0-1O
50
o
S.
,
15-20X103 ft
0
Figa r
10.
2 houar contours, model 5.
.- 43 -
10
d
I
Surface
5-10x10 3 ft
10-15x.10 3 ft
140
15-20x10 3 ft
Figure 11.
4 hour contours, model 5.
44 -
0
/o
2o
Surface
O-5xlO3 ft
5-1xlO3 ft
lIO
5-llo3 ft
0
35
210
10-15xl0 ft
.
2\0
15-2 Ox10 3 ft
Figure12
Figure 12.
6hourcontoursmodel
6 hour contours, model 5.
s
45 -
0
/0
30
Surface
0-5x10 3 ft
5-10x10
3
10-15x10
ft
3
ft
15-20x10 3 ftt
I
0
Figure 13,
2 hour contours, model 6.
-
46 -
e
I
/0
I
.2
20
Surface
0-5x10 3 ft
5-10X10 3 ft
105
10-1510 3 ft
15-20x10 3 ft
Figure 14.
4 hour contours, nodel 6.
- 47 -
L
0
4
10
W
.1.
IIYII
_i.li--~-^i~DY-
i^ iiii----il-_i~--liliY1~L
_~*
CI~~_Cll~a~i__l
_i (1I1
Surface
0-5xlo3 ft
5-1xlO3 ft
O-15xlO3 ft
o& /o
290
Figure 15.
6 hour contours, model 6.
- 48 -
20
-L
~L
L
II~--I~;ii;j___llll____l
i__~__~
X
Surface
0
~zz0
0-5x10 3 ft
5-10x10 3 ft
(0
10-15x10
3
ft
752
ontour
hour
odel 7
15-20x10 3 ft
Figure 16.
2 hour contours, model 7.
I
0
go 49 -
i
/O
I0
20
Surface
0-5x10 3 ft
90
5-I10x1
3
ft
10-15x10 3 ft
Sto
15
15-20x10 3 ft
Figure 17.
4 hour contours, model 7.
0
- 50 -
/0
20
Surface
Oo
190
10-15x103 ft
O
235
15-2.x210 3
ft
295
I
0
10
20
--
Surface
0-5x10 3 ft
.qI5
0
10
5-10Orx10 3 ft
65
10-15x10 3 ft
0
70
15-20X10
3
Figure 19.
ft
2 hour contours, model 8.
- 52 -
I
C
a_
a
10
a
ID
surface
0-5x10 3 ft
5-1010
3
ft
10-15x10 3 ft
15-.200
3
ft0
190
Figure 20.
,
4 hour contours, model 8.
- 53 -
0
/o
Z
Surface
O-SxlO3 ft
5-1xlO
ft
210
lO-15xL03 ft
i
ft
1.-2x10
0/
oo
5
.Sc
J
L,
I /0
2*
hei ht
(10 ft)
Figure 22.
Mean upper wind profile for 50 knot 500 mb wind and one
standard deviation to each side.
-
55 -
6
1
MT
2
0
4
1 MTMAX
0P
MTMI
50
1
100
150
200
250
300
350
miles
Figure 23. Surface distributions of radioactivity vs distance for one megaton detonations for
mean wind field (1MT), and mean wind field ± 1 standard deviation (IMTMAX and IMTMIN). Units
are 0.1% of total radioactivity.
eoq
-
LS w
a
eu*s@@g
wen
as
quaagem
*ws
gea
pt
*0eyepg
Oa;
4 "1
"MOMa
"0
*ntl"
5011moo
s
Wf
I
~'~I--
10.0
25,0
30 - 40
20.0
I 5.0
I 0,0
5,0
0
20
15.0
50 - 60
I
/
5,0
/.
0
Figure 24.
*
20
1 M2T.
- 58 -
*lpYI__
~XI~D-UI-C~Lrrl-I-L--L-L-*I*~U-I
;irr;Y
- ~ls~q~~*~ilP
~ri-~l~iLi~i-~l-Y~1I_____~_
15
.._1~1-.-~ii.
20-30
I
20
40
30-40
20
15
10 -
51
0.
20
Figure 25.
40
1 MMAX.
- 59 -
15-
10-
5-
0
20
50-60
20
15
10
5/
0/
20
Figure 25, (cont iied)
-
60 -
10
I
,/,\
0
,\
20
40
20-30
20
15
10
5
7
20
Figure 26.
40
1 EMIN.
- 61 -
40-50
25-
I
I
20
\
15
i
\
/
20
Figure 26,
,
60
40
(continued)
-
62 -
\
80
miles
15
I
/
10
20
Figure 26. (continued)
percent
radioactivity
10
Figure 27.
5
0
5
10 miles
Cross-wind distributLon of radioactivity from 1 MI detonations.
- 63 -
io
as
aS
ame
saeaa
trses
a s*tfto,
atas
t
0io
4Aname la atteSlg t~ as
-
-
ae
er~aes ias seektr
am t~a
UEsS
.1116
40.04
jam&
0-5x10 3 ft
5-10x10 3 ft
//o
10-15x10 3 ft
i
m
-
-
15-20x10 3 ft
Figure 28.
Distributions for trial #1 estimated from the entire wind
field.
- 65 -
Surface
0-5X10 3 ft
85 f
5-10x10 3. ft
10-15X10 3 ft
150(o
15.20103 ft
175
Figure 29.
I
0
I
10
I
I
20
Machine results for trial #1.
- 66 -
VP, I.
Surface
0-5x10 3 ft
29
5. 1xl
3
ft
33
40Z3X
10-15x10 3 ft
4ZOI
)
r I
I
10
20
D
15-20x10 3 ft
Figure 30.
Distributions for trial #2 estimated from the entire wiad
field.
-
67 -
Surface
I
0-5x10 3 ft
5-10100
3
0
I
10
I
I
20
15-20x103 ft
I0
ft
I
10
10-15x10 3 ft
104h~
aS
,4-20
Figure 31.
Machine results for trial #2.
- 68 -
~l~rr-r_~-_r;r-.-,_ly~L~
-----
Surface
0-5x10 3 ft
10~J
5-10X10 3 ft
9o
10-15x10 3 ft
I
0
I
I
a
10
20
15-20x10 3 ft
135
Figure 32,
of 2 and
our distribut
Average of 2 and 4 hour distributios
- 69 -
for model P7.
Surface
0-5xl0 3 ft
5-2.0x10 3 f t
1O-15xl03 ft
15-20xl03 ft
I
0
I
10
20
Surface
0-5x103 ft
90
5-i1010 3 ft
10-15x10 3 ft
J5
I1F1
0
1&.5
010
15-20x10 3 ft
Figure 34.
Machine results for trial #3.
-
71 -
/0
2
20
Surface
O-5x103 fft
5-loxlo3 f t
0.
10-2.5x103 ±ft
0
n
15-20x10 3 fft
pA
23J
P
20
Surface
0-5x10
3
ft
5-10r10 3 ft
9D
10-1510 3
I
0
38
a
Ir
/0
I
201
15-20x10 3 f
Figure 36.
Distributions for trial #4 estimated from the models.
- 73 -
Surface
0-5x10
3
ft
30'
SO
4130
10-15x10 3 ft
I
0
15-20o10 3 ft
Figure 37.
Machine results for trial #4*.
- 74 -
IO
10
ZoI
Z20
hei ht
(10 ft)
20
Figure 38,
40
60
80
100
mph
Profiles of model and trial wind speeds vs height for 1 MT
case.
- 75 -
5
0
15
10
5
0
15
10
5
0
Figure 39.
Machine results for 1 TMtrial case with comparison of
distribution estimated from models in 20-30x10 3 ft and
50-60x10 3 ft layers. Dashed curves represent estimates
from the models.
- 76 -
Figure 39
(continmd)
-. 77 .-
(of-1 it1,-
40-50
surface
0-10
CC~~L
~\
10-20
N
AID
50-60
20-30
- !- /
!
-
60-13
30..40
4e
-
I
I
!
I
I
I
_
160 miles 0
Figure 40.
p
I
80
I
I
160 miles
Positions of contours in various layers as estimated freo
the model (solid lines) and computed by machine (dotted
Ordinates are units of 10 miles.
lines) for 1 Mr trial.
.- 78 -
TABLI
1.
Man fall velocIties 14 (ft/see)
This table reprasents the mean Fall velocities (in 20,000 foot layers)
of the radioactive particles. W
represents the fall velocities above
40,000 feet. W 20 represents the
thousand feet. W
all velocities between tweaty and forty
represents the fall velocities between 0 and twenty
thousand feet.
Of
S%
Dianeters
20
Wotal
T
W-
1'
"IT Total
10
.13
.11
.10
1.0
43
1,91
1.68
1.54
11
.16
.14
.12
1.1
44
1.98
1.74
1.59
1.0
12
.19
.17
.15
1.2
45
2.05
1.80
1.64
1.0
13
14
IS
16
17
18
19
.22
.26
.30
.3
.38
.43
.48
.23
.27
.31
.35
.39
.44
.20
18
.21
.25
.29
,33
.37
.42
1.3
1.3
1.4
"49
46
47
48
50
51
52
2.13
2.21
2.29
2.37
2.45
253
2.61
1.86
1.92
1.98
2.04
2.10
2.17
2.24
1.69
1,74
1.79
1.84
1.89
1.95
2,01
1.0
0.9
"
"
0.9
0.8
20
.53
.49
.47
2.69
2.31
2.07
.50
.63
.68
.73
.78
.83
.88
.93
.98
.53
.57
.61
1
.65
.70
.75
.80
.85
.90
.51
.55
59
.63
.67
.71
.75
.79
.84
1.5
"
53
21
22
23
24
25
26
27
28
29
1
55
56
57
58
59
60
61
62
2.77
2.85
2
3.03
3.12
3.21
3.30
3.4
3.5
2.38
2.45
2.52
294
2.9
2.65
2.73
2.80
2.88
2.96
2.13
2.19
2.25
2.31
2.37
2.43
2.49
2.55
2.61
0.8
0.7
30
1.03
.95
.89
"
63
3.6
3.04
2.67
0.6
31
32
33
34
35
36
37
38
39
40
41
42
1.09
1.15
1.21
!.28
1.35
1.42
1.49
1.56
1.63
1.70
1.77
1,84
1.00
1.05
1.10
1.15
1.20
1.26
1.32
1.38
1.44
1.50
1.56
1.62
.94
.99
1.04
1.09
1.14
1.19
1.24
1.29
1.34
1.39
1.44
1.49
'
64
65
66
67
69
7
73
75
77
79
81
83
3.7
3.8
3.9
4.0
4.2
4.4
4.6
4.8
5.0
5.2
5.4
5.6
3.12
3,20
3.29
3.39
3.52
3.66
3.8
3.9
4.O
4.1
4.3
4.5
2.73
2.79
2.85
2.91
3.02
3.14
3.26
3.38
3.5
3,6
3.7
3.8
0.5
"
0.5
0.8
1.0
1.0
1.0
0.9
0.9
0.8
0.7
0.7
"
1.
"
"
1.5
1.4
"
1.4
1.3
1.3
1.2
1.2
1.2
1.1
1.1
-
79 -
1,i
"
0.7
0.6
"
"
"
TABLE 1.
t/
(continued)
40
85
5,8
87
6.0
90
93
96
6.3
99
7.2
7.5
7.8
102
105
108
112
116
120
124
128
132
136
140
144
149
154
159
164
169
114
179
184
190
196
203
211
220
229
6.6
6.9
8.2
8.6
9.0
9,14
9.8
10,3
10.8
11.3
11.8
12.3
12.9
13.5
14.1
14.8
15.5
16.2
16.9
17.6
18.4
19.3
20.2
21.2
22.2
23,3
239
24.4
249
255
20
4.7
4.9
5.1
5.3
5.5
5.7
5.9
6.1
6.3
6.6
6.96
7.2
7.5
7.8
8.1
8.4
8.8
9.2
9.6
10.0
10.4
10.8
11.2
11.6
12.0
12.5
13.0
13.5
14.0
14.6
15.2
15.8
16.5
17.2
% of
'0
1.
3.9
4.0
0.6
4.2
0.9
4.4
4.6
4.8
5.0
5.2
5.4
5.6
0.8
0.8
0.7
0.7
0.6
0.5
0.8
0.7
5.8 0.7
6.0 0.6
6.2
6.4
0,5
0.5
6.7 0.4
t1
7.0
7.3
It
7.6
7.9
8,2
8.5
0.43
8.8 0.3
n
9.1
9,4
9.7 0.3
10.1
10.5
10.9
11.4
11.9
12.4
13.0
13.6
14.2
0.2
I,
t
260
271
283
W2 0
26.8
17.9
14.8
28.1
18.7
19.5
414
29.5
31.0
32.5
34.1
35.8
37.6
39.5
41.4
43.4
45.5
15.4
16.0
16.6
432
47.7
451
50.0
29.6
30.8
472
495
520
550
52.4
32.0
54.9
57.6
33.3
60.5
36.0
585
63.6s
66.9
70.4
74.1
78.0
82.1
86.4
90.9
95.4
100.0
105.
110.
116.
122.
128.
295
308
321
335
349
3(4
380
397
620
660
700
7,50
800
850
900
950
1000
1060
1130
1210
1310
0.2
0.1
1440
W0
1440
- 80 -
20,3
21.2
22.1
23.0
24.0
25.0
26.1
27.2
28.4
34.6
17.3
18.0
15.7
19.4
20.2
21.0
21.6
22.6
23.5
24.4
25.3
26.2
27.2
28.2
37.6
29.3
39.3
30.5
31.7
41.1
143.0
45.0
32.9
51.3
53.6
34.1
35.3
36.6
38.9
39.2
55.9
58.2
41.8
47.0
49.1
60,6
63.0
43.2
66.0
70.0
46.3
44. 7
48.0
S of
Total
0.2
,)
0.1
ft
1i
It
I'
.02
TA"
2*
tu' X14dozo
t dfde
Sstrbutia
etatiLtiom
dowty vt*
1*0
2340
$4
54~
~x~~~991"
s
1.4~
25.3
$S0
503
5.5l~
2250
104
24$9
$1,'i~
5,7~j
14$so
14?Oig
1*0
40Y
10$
5.,~l
t,,
139
'sr
2*4~,
141~
'9J~
18~~j
'Iii~
14%C5,
'ar
.- 81 a
ItAm4 3,0
14
n ttyr 0strlbtti
otattstic$
It lt
S,
3
4.1
14$0
1
144
49CO
#7i
4$gf
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4.,~1F
109
400
4190
3*4
-
82 m
1-LA. 4,
10 Ir u-A
(1
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giiaMld~%;~~
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711,11W
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ind (ua~i"t)
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90.42
490
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5"4
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tate
o
(103
20453
VW$a dtnUntin (4)
n (3)
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9.%Di
24~i~
sw
*95
12
*4
a 83
-
TABLE 4,
(continued)
Awis diottbta
1*VI
(3)
altit
(t1O3at)
faratt
43
10-so
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1940
aso
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27
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284
210
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23
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300
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bi
340
30S
$21
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jb
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346
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59~
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300
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dsttUM
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- 86 -
wo
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saus
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-3
o
92 -
RIOLIOGRAM
(2) Fmti
Lrt
OC Pd'lo** tftet" 6V
1"* 3,12004 Vbdittaft~an
Jo In.kki
(S)'awSo Saw
aatbovIblool
WW4 190's 'WP
(6)ttvgd*AW 20*W 000ar 4 0,146
- 93 -
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