vere
-
.
”
eshey
1S arent a — ttaIGEAeterna eos =:
—
Sr cae
.
ewe
-
soe
eee
a
oa
.
- woe
see
’
rn
a iRaaliering ok + mona Fea Apialinen =~
|
~ are +
=ate
enn en
eMme ae ee
.
ee
eeeeeae WA atte EItenn
_
03)
isomer (2.9 y) of rhodium which we have designated ?°?#™Rh,
Peaks from *555u, *5?8u, #41Am,
.
:
oe
1**Ce, ?9?tRh and 5*lm are
Te
aiso clearly identifiable.
Sem
Several seaks in this spectrum
have not yet been definitely identified. —
—
"ew
»
.
se
ee
Ly.
.
.
oy
oe
°
ie
a
.
r
The composition of the radiation field on ‘Lukoj, ac
-
we
Cr
heavy fallout area, is indicated by the Ge (Li) spectrumshown”,
in Figure 4.
ma.
This densely vecucated island exhibited
Apyoroximately 60%
FL
74 re ween
:
a
k
Again the relatively large °°Co and +*5sb activities
wr‘
?
*25Sb and 1°?MRh and the remainder principally from +37¢s.
de
ON eh
exposure rate interior of the island was from ®°Co, 30% from
{
j
~
relative to 37Cs contrast with the Bikini Island situation.
The peaks characteristic of }°*®™ph are quite prominent in
- Fig. 4along with the ®°Co, 175Sb and *+37Cs peaks.
. Cn eng
Also
easily identifiable are peaks from ®41Am, *55Eu, 1°?Rh, 2°°Rh,
—_ 2m
|
+
144Ce, and *®Zn.
” ‘- ns
-
are
i
nat
es
.
.
i= :.
“ *
: =
a
*
come
-
*
‘
a
. -
. -
n
-
.
-
fo
so s <
oy
me
‘
,
-
fe Mera oY
tee
:
a a
.
-
.
;
:
a
be
Ce dae eg.
“os
sg 8.
se
in additionto the isotopes identified in Figs.
i.”
=e,
ae
oe
a
.
ee.
* aaa
oe ye
.
3 and ae
aos
~
a tees
detected aor Bit in:a| soil sample from the Bravo crater
4 we ree
Foe
a
LE eggs Bae
$
-
5
Mage
eT el
Be Soy
-
-
cee
SUR
BO
+
.
ape empene s
ve
mote
cle em eel Are a ol me NR tees ee
.
Se Pewee thm
ae em ne
a
vo
sie
ee apeta -
2
enc
uF
Pe
eo
,
he a ee
toe
~*:aewobee
ute wey #*,“Tae oe
S005 749 =.see
ees 7
PANE
= haere
nf
2
-
8
An
Wee
rs
teBt
a
a, caves
-
7
he =o
En erager es
at
:
diA bereTE a
etnaary
re eee
as
tor
paee tL
pene
$F Ae ee te
~~,
~
ce cee
oeee
ee
v
a
Oo
it
Ye
ee=
ie to Teeter wnimmmmnagneme «+1 ie ene a ae llr oe <aere
te eaeeesSen oe nein tee,
i" natn ee wae
-
wee ae
ef
penieny sharee 0
a ee
of the exposure rate at the soil sampling site in the high
8
‘
at ” tye =a:
;
exposure rates cf from 60 to 200 ur/hr.
a