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INVESTIGACIONES SOBRE BIOLOGIA MARINA EN
LA ZONA DE ENSAYO DE ENIWETOK
Resumen

En la memoria se resumenlos resultados de las investigaciones sobre biologia
marina que se vienen realizando desde 1952 en la zona de ensayo de Eniwetok.
A consecuencia de los diversos ensayos nucleares efectuados desde esa fecha
se han introducido en el mar una serie de productos de fisidn y otros radioisétopos (237U, 23°Np, 54Mn, *5. 59Fe, 57, 58, 6800p, 65Zn y 185W). El autor indica

la concentracién de los radioisétopos en las muestras de plancton tomadas entre
cuatro dias y seis semanas despuésde la contaminacidn, asi comola distribucién
de la radiactividad entre el plancton y el agua. Los peces herbivoros contenian
65Zn, 55¥e, 57, 58.80C'o y 54Mn. Los peces carnivoros contenian principalmente
55Fe y Zn.

MARINE BIOLOGICAL INVESTIGATIONS
AT THE ENIWETOK TEST SITE
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Frank G. LowMan
LABORATORY OF RADIATION BioLocy, UNIVERSITY OF WASHINGTON
UNITED STATES OF AMERICA

The disposal of radioactive waste products in the sea is of primary interest
to maninsofar as it constitutes a potential hazard in his food materials derived
from marine sources. At the present time, the principal source of artificial
radioactive elements in the ocean is past weapons tests. In the future, however, the wastes from nuclear power development and the great volume of
associated contaminated materials will far surpass the present burden of
artificial radioactive elements in the sea.
Almost certainly, the radioactive wastes consigned to the sea in the future
will be deposited in chemical forms different in varying degrees from those in
fallout material. At first consideration comparison of the fates in the marine
biotic mass of radioisotopes derived from the two sources might appear to be
of limited use. However, investigations on the cycling of radioisotopes through
the marine food webs and thelevels of various isotopes in representative samples
have been conducted for the past eleven years at the Eniwetok Test Site in
areas contaminated by many different types of nuclear devices fired under a
wide variety of conditions. The transmission of given radioelements from
one organism to another follows similar paths whether the fallout is mixed
with calcium compoundsfrom pulverized coralline islands and reefs, or sodium
chloride from evaporated sea-water,or is essentially free of either of those nonradioactive materials. Indeed, groups of radioelements with similar chemical
characteristics tend to follow similar paths in marine organisms. The uptake
of radioisotopes from areas contaminated by fallout is controlled primarily
by two factors; the physical factors which determine the distribution of the
radioactive material in time and space, and the chemical factors which control
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