quantitative determinations from a few profiles.
Gamma-ray
spectra of equal amounts of soil from different depths were
compared directly te arrive at
(1) a qualitative evaluation
of the vertical distribution of the radionuclides and (2) a
Semiquantitative estimate of relative amounts of radionuclides
at different depths.
Gamma-ray spectra were made with a system
which included a 3-inch by 3-inch solid, thallium-activated,
sodium Lodide crystal 2:1 a 256-channel analyzer.
In addition,
selected samples were taken for analyses of the pure beta.
emitter, sr? ,
¢
RESULTS AND DISCUSSION
Vertical distribution in relation to soil type is made by
comparing young and old soils.
young soil,
Examples are Kabelle Sand, a
(Fig. 2) and Gogan Gravelly Sandy Loam (Fig. 3) and
Lomuilal Sand (Fig. 4), old soils.
Their characteristics are
given in Tables I and III.
The young soil has little organic material except that in
an algal surface crust about 1 cm thick.
Hermit crabs, Coeno-
bita perlatus, at the base of a few shrubs, the borrowing ghost
crab, Ocypede ceratopthaimia, and ants are the main animals
present.
Litter accumulation is found only at the bases of
the acattered shrubs and is a minor part of this soil system.
ney
Iu