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expected to pass to man via the marine food pathway, verification is
required.

We will

first sample mullet again from the same islands

sampled in 1976 during a different season.

The fish will be dissected

into tissues as before and analyzed for plutonium and other radionuclides
to assess any changes in concentration that might have occurred during

the intervening years.

At two islands where fish are plentiful, a

large variety of reef fish will be caught for analysis to insure that

concentrations in mullet are representative of other edible species. As
stated previously, it is impossible to analyze samples of the 600
species of fish in. the Marshall tslands from al! islands of the atolls.
Thus we must restrict our evaluation to data generated from analysis of.
the most representative species available.
In addition, 24lam levels

will be evaluated carefully to provide a complete transuranic assessment

in marine food products.

We will continue experiments to evaluate the generation of marine
plutonium-labelled organic particulates resuspended by wind and wave
action on the ocean-side reef at the atolls. Although no data were
available for evaluation during a recent private conversation with a
knowledgeable DOE representative, it was not at all encouraging to learn
that a similar resuspension process might be generating small quantities
of airborne marine plutonium aerosols at some coastal regions near
Windscale. Because there are few regions in the world contaminated with
levels of plutonium sufficiently high to be measured precisely, a
continuation of this study in the Marshal! Islands is essential. Any
positive results will require carefule evaluation.
We have terminated sampling at some of the groundwater sites on
Enewetak but, at the same time, are redirecting our efforts toward a
more detailed assessment of the groundwater processes at our remaining
sites. These include wells and locations containing usable freshwater
as well as sites related to the agricultural experiments on Janet Island.
This spring, storms permitting, we will drill additional test wells on

Janet to perform hydrologic tests and measurements on the wells including

dynamic pump tests, tidal response measurements, dye injections, and
detailed sampling in these.and our other wells for chemical and

radionuclide analysis. Soil from the well sites will be separated into
size fractions and equilibrated with water to determine the distribution
coefficients for plutonium and other radionuclides between the solid
and solution phases. The purpose of these latter experiments is to
evaluate the amount of plutonium that is selectively mobilized to
solution from different soil types.
:
When ship support is available for Bikini, we will continue the
studies begun in FY 1978. We also hope to initiate similar groundwater

studies at Rongelap if ship support is available.

Dye studies provided

an estimate of the rate of groundwater movement that varies throughout
the island and changes with season. Radionuclide groundwater

concentrations are more variable at Bikini, but the reasons for these
variations are not yet understood.
Additional temporal experiments are
needed to evaluate the radionuclide dynamics in the water.

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