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oxide, calcium hydroxide and calcium carbonate formed by the decarbonation, hydration and recarbonation processes going on in the firebafl
and subsequently,

The majority of them were white or transparent but

some were yellow or brown,

Many of the flaky aggregates were observed

to disintegrate spontaneously into smaller particles within a few hours
after collection,

In addition to these primary types, a fourth kind was noted consisting of small black spheres of calcium iron oxide (2CaO- Fe, 03).

These were usually observed adhering to the surfaces of the large grains

but occasionally were found isolated (Reference 12),
For detonations over ocean surfaces the fallout collected consisted

of droplets of salt slurry 50-300 microns in diameter,
about 80% salt,

These contained

18% water and 2% insoluble solids by volume,

The major

part of the radioactivity was found in the insoluble solids portion,
The fallout deposited at more distant points has not been as well

characterized, but is believed to be composed of minute spheres formed
by condensation of the environmental material from the vapor plus a very
fine, unfused dust swept up into the cloud from the area around the shot

point (Reference 14),

The availability of the radioactivity in the fallout for assimilation
into the biosphere depends to a large extent on its solubility in aqueous
18

22,

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