0
tT
40
7?
50
7
60
T
70
zWO/9W
NI
JONVY
ASLVINDIVS
TO
UT
UT
UT
T
cE
Uc Ed
170 180 190 200 210
3° SPECTRUM ANALYSIS (PCi/G)
}{/0 120 130 140 150 160
Dependance of the mean rance of the alpha radiations on the
composition (total activity) of Bikini surface sediments.
oT
—~NMAON OPrOARO-N
o< AND
T
90 100
17% +9
Appendix Figure 3.
T
80
&
*
TOTAL ACTIVITY FROM
30
TTT
20
i0
A
°o
en
rn
N an
Nw =
' ri
|
OMNAYY ao ana
_
1 $-16
6 5-8
7
143