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TABLE IV
LEVELS OF Sr°°—yYAND Cs!” IN TERRESTRIAL SAMPLES IN AND NEAR THE
ENIWETOK TEST SITE

ee
Eniwetok Atoll*

Soil

Spi yea

|

dimije %

|

a

dry weight

Messerschmidia
Fimbristylis
Sandburrs

|

375

wet weight
wet weight
wet weight

OG
|
76
|
9.4

;

5.9

(C3137

d/m/g °%
242

11.9
2.0
7.9

|
|

667
3,303
100

|

|

3.8

83
86
86.8

Average
7.3
|
85
I

Rongelap Atoll

Seaevola leaves (March, 1958)**

|

(Average of 11 samples)
Pandanus fruit (August, 1958) **
Pandanus leaves

|
l

Pandanus trunk borings

aot

Kabelle Island (Rongelap Atoll) **
Pandanus fruit (August, 1958)
Pandanus leaves (August, 1958)

Pandanus stems (August, 1958)

Pandanus bark

(August, 1958)

|
|
|

!
|

|

26.7
4.6
3.1

33.7
95.4
3.5

71.4

28.6

6.5
0.37

|

5.4

|

32.4

92.6
1,2

|

49,2

|

4.6

!

|

Einiaetok Island (Rongelap Atoll) **
Pandanus fruit (August, 1958)
Pandanus leaves (August, 1958)
Average

|
|

7.0
1.6

!
i

77.0
1.4

15.9

:

38.7

* D.J. South, 1957 (unpublished)
** DJ. South manuscript

highest percentages of Sr®°—Y®° (71%), and Cs!37--Ba!3’m accounted for the
remaining 29%. Thus on land the radioisotopes of strontium and caesium
and their daughter products accounted for a significant fraction of the total
radioactivity in the plants. This is not the case in the sea, although these
isotopes have been considered to be also of primary importance in the contamination of marine organisms.
In a series of plankton samples collected at the Eniwetok Test Site in 1958
3 to 36 hours after contamination, the ratios of observed Sr® to expected

Sr®° based on the observed levels of Mo%®—Tc#9m, Tel32—[132, Zr95_Nb%,

Cel41__Pr!41, and Ba!4°—La}!4° were calculated. The results are shown in

Table V.
In the plankton collected three hours after contamination, no Sr® was
detected in the large plankton. The level of Sr® in the nannoplankton was,
on the average, 0.43 of that expected on the basis of the levels of the abovenamed isotopes. In plankton collected later, no detectable difference in ratios
of radioisotopes existed between the large and the small plankton. At 21
hours, Sr® existed at a level 0.06 of that expected, and at 36 hours 0.03 of
130

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