“a

ei ££ he

anne

TA

2

NC

3

restricted ae
The COG Le
OLS 2
Atomic Ensigy ACKO
€-iinec she

i

+b

,

Sane

mL

,

le ve oe

.

*
a”
i. y ee oe

a)

ACA LLby

H. 0. Waipple, M. Do» Health Division
QUERMNT RADIATION LEVELS af WWETOK 5).

ee

h

ee meen oiiecting the
dervaoet
oem os LCS.
eam
ee ciscles cre of ics contents in
Repent cee ieee COT 48 prohibited
ms Laeaseoacebdewt
reaper
penaitées ander

—"

.

s

eral [BWR

Measurements of activity at Bniwstek Atoll during the early part of

:

February, 1949, agree in the main with the findings of Br. ghlaer, |

dn Octobder, 1945. Levels of activity at the present tine are between
1/2 and 2/3 ef the values feunt by hia. For exemple, on Ingedi the

Cte Leas OOD CS? LZa7.

date)
(Signature of pergon making the changa and

presen¥-activity at Sero is 30-00 ar/hr (Gemma), and the maxizum

(Person authorizing change in c

oy

Dp a RIS_H, DUNNING

s

Ce

Clacsification changed to

by authority of the U.S. ERDA

lassification and date) 8-00 Ft,

he we

a

-

z

activity fount by us in the *hot® sone about 300 yards out was 75 ar/hr
(Senna). The corresponding values reported by Dr. Shiaer are 60 ar/hr

and 100-150 ar/hr, respectively.
The general >

the area of int

und activity over the entire island, exclusive of
rp eontemination, which is believed to be due to

fall-out from the Yoke shot, has however decreased to a value of from

0.1 to 0.2 ar/hr, as compared with the October level of 0.4% to 0.6.

Film studies shoved the activity to be due to a fairly dense distri-

bation of particulate radioactive material on the ground mrface.

Bunit alone is presumably free, in the main, of such a gm eral ised
particnlate hasard. Further film studies will clarify this point in
the near future,
The ground surface at the present time is wind-stabilised; that is,

all the finest material has been blown out of the superficial layer

of soil, and as a result the islands are singularly free of dust.
Although we did not have facilities for collecting and counting dust
samples, the group concurred in the opinion that mao respiratory hasard

eurrently existed. It wae also almost painfully obvious that any
aisturbaace of the ground surface immediately resolted in producing
voluses of dust and an undoubtedly serious respiratory hasard,

The levele of activity are such that little if any restriction ss

|

working time in the Shet® areas will be necessary, as far as remaining
within permissible linits of external radiation exposure is soneerned.

Past, Rovever, reproseste an entirely different probdlen, ead it is net

pessible te specify a permissible level af aetivity in the respired air

when Shis activity is in the form of finely @ivided insoluble parti cies.

. A fraction ef och saterial will Be retained in the lung and pulmonary
G_Svnph nodes for leng periods of time; the dosage level in body celis
sijecent to such particles are extremely high even though the total
activity of the particles is relatively low; and it isc believed that

QO

ou

iw
a

UNGLASS

to conduct operations in such a seiF
FOLDER

wa

these circumstances are markedly increased.
BOY No

o

Ee

the statistical chances of eventual development of lung cancer under

COLLECTION

>
aa

é
4,20

aren 11, vol

SS

os

se
fig

LZ

LASSIFIED |

Alvin Graves, d-Division Leader

>°

}

Je ras

It therefore behooves us

.

he respiratory exposure of

mid

Select target paragraph3