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RADIATION ECOLOGY
Radiation Ecology or Radioecology is a term that came into
common usage in 1956 to denote that area of the broad field
of ecology concerned with the assessment of radioactivity
in the environment. More specifically, radiation ecology has
come to be recognized as that area of ecology concerned
with radioactive substances, radiation and the environment.
The development and subsequent expansion of nuclear
energy for military and peaceful purposes has been accom-
panied by environmental problems, some of which are typi-
cal of other facets of industrialization and some unique to
atomic energy. The unique problems primarily concern the
fate and ecological effects of radionuclides released into
the environment.
The major environmental problems introduced by the
Atomic Age may be grouped into several areas of scien-
tific and public concern. Underlying each of these is the
worry about the effects of ionizing radiation—on man, his
domesticated plants and animals, and on the environment
and its living components, Fallout from weapons testing,
reactor radioactive waste effluents, radioactive waste dis-
posal, nuclear war, and use of nuclear explosives for major
engineering and related technological projects of large scale
comprise the activities which have concerned society and
which, because of potential impact on the environment and
man, have stimulated the development of radiation ecology.
Understanding the manner in which our ecological systems
(ecosystems) distribute, assimilate, and affect the environ-
mental behavior of radioactive substances, and the effects of
radiations emitted from those substances, are the concern of
the radioecologist.
RADIONUCLIDES OF ECOLOGICAL IMPORTANCE
Radionuclides which are of interest to the ecologist are
listed in Table 1. These radioactive elements represent the
major naturally-occurring and man-made sources of radia-
tion in the environment. Principal sources of exposure from
background (natural) radiation are represented by the ura-
nium, thorium and actinium decay series. Internal exposure
to man results primarily from^40 K,^14 C,^226 Ra, and^228 Ra and
their daughter products that are deposited in the body.
Radionuclides such as^222 Rn and^220 Rn and their daughter
products represents sources of internal radiation exposure to
man from inhalation.
Radionuclides produced by the fissioning of uranium
(fission products) are of the greatest current concern. These
man-made isotopes are not essential to organisms, but they
constitute the major sources of radiation in the environment
whether it be from fallout or waste disposal from reactor
operations. All of these radionuclides may enter ecosystems
where they become part of the flux of systems that are being
circulated within and between systems.
Some of the fission products which are chemically simi-
lar to biologically essential elements are of special inter-
est. They vary greatly in their physical half-life and in the
extent to which they participate in metabolic processes of
living organisms. The most important radionuclides affecting
plants and animals on land are strontium-90, cesium-137, and
iodine-131.
Strontium-90 remains in the environment for a long
time. Its half-life is 28 years. Strontium is chemically similar
to calcium, and it can enter living organisms as a replace-
ment for calcium. In weapons fallout strontium-90 is usually
deposited in the root systems of plants. the amount of^90 Sr
that a plant absorbs from soils depends on several factors,
particularly on the quantity of calcium in the soil, the relative
quantities of calcium and strontium at the depth where the
roots are located, and the ability of the plant to discriminate
between the two elements. The plant is the base for^90 Sr to
enter the human food chain. This chain is a short and simple
one consisting of plants, cows, and man, with cow’s milk
being the chief source of entry into man. There is consider-
able discrimination against the transfer of strontium at each
step in this food chain, but the small amount that is trans-
ported to man tends to concentrate in bone tissue. It remains
there, undergoing radioactive decay and emitting its radia-
tion. Its danger is related to the fact that bone contains blood
forming (erythropoetic) tissue. In sufficient quantities the
radiation can cause leukaemia and bone cancer.
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