- 38 In October 1955, the highest values in the marine algae were at Kabelle
and Labaredj Islands and the lowest in the shallow water of the lagoon at
Enibuk Island, Ailinginae Atoll.

|

The highest of all were the fresh-water

and brackish water algae from Rongelap Island which were collected in
locations where fission product material would tend to accumulate.

These

algae were collected from the bottom of a concrete cistern which was used
to collect rainwater and from the sides of a well which contained water originating from the fresh water lens.

In both of these locations the water

contained much more activity than the water in the lagoon (see Table 13).
Considering all the samples collected on this date, the ratio of the activity in
the soll to that in the algae varied from 1 to 15, an indication that the level
in the soil is not the primary factor in determining the level of activity in
the algae.
A comparision of the radioactivity in the algae collected in the shallow

water near the lagoon shore with that of those collected at the bottom of the
lagoon in deeper water shows that the latter were slightly more radioactive

at Enibuk Island and less radioactive at Rongelap Island.
The radioactivity in the algae at Rongelap Atoll igs declining at a rapid rate.
This is illustrated in Figure 11, a log-log plot of radioactivity in the algae
at Kabelle Island from March 26, 1954 to October 21, 1955.

The slope of

this line is -2.5, which ig steeper than that for beach sand (-1.5).

It ia also

steeper than that for the land plants (-1.25), which indicates that different
fission products were being absorbed by the two types of plants.

This differ-

ence in compoasitim of the radioactive material is also bore out bythe faster

Select target paragraph3