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Tke maszin vody, af Sec, 2.6 conprises 2 report
conctusions outlined in Sec. 2.6.11 were not ac, on fall-out that was completed just before Kem
cepted as fully established by all interested
shot. Certain observations on particle size of
parties. The third point was discussed at a
Item shot fall-out were added to this report in
meeting, held several days after Dog shot, at
4, Sec. 2.6.18. There was nothing in these observa- which all professionally interested individuals
tions to alter the earlier conclusions.
were invited to present their views. It appeared
that, at the root of the skepticism expressed
2.6.2 Summary Account
about the large-particle conclusion, there lay
the fact that no such large active particles had
Before going into details, subsequent develbeen observed among those isolated from the
opments are summarized under the following
cloud samples drawn from previous shots.
three subheadings.
Considerable emphasis was also given to certain differences between the physical and chem2.6.2.1 Immediate Action
Within a very short time, substantial evidence
was brought forth that most of the activity was
carried on large particles.
A study of the wind soundings in the neighborhood of the shot time showed no westerly components below 20,000 ft. It was known that the
fall-out started about 2 hr after the shot. The
rate of fall of the particles must therefore have

exceeded 10,000 ft/hr, and, by using Stokes’

law, the size was computed to be 100 microns
or greater. Earth samples were collected from

Parry and other islands of the Atoll; a considerable number of particles were isolated by
nonselective methods; and the sizes were measured under a microscope. All particles were

found to be large (details are given in Sec. 2.6.5).

A record of the radiation intensity versus time
was made. The general character of this record
suggested the settling of a cloud oflarge particles rather than the blowing by of a cloud of
small particles of which a small proportion
would be expected to settle out.
2.6.2.2 Supporting Action

Interest in the Dog shot fall-out was naturally
widespread, and investigations were made both
inside and outside the original scope of the
TG 3.1 program by many individuals and projects. The following summary is confined to
those investigations that were made by or at the
request of CTU 3.1.5. Subject investigations
were motivated by three primary considerations. In the first place, it was obviously desirable to support physical observations and calculations by biological investigations. Second,
it was clear that more data were needed on the
fall-out phenomenonto facilitate decisions con-

ical properties of the particles isolated on

Parry (Sec. 2.6.5) and the characteristics of
particles isolated from previous cloud samples.
The suggestion that such negative evidence was
invalid, on account of the relatively smal] number of particles needed to account for Dog shot
fall-out, was apparently too tenuous a counterargument to be convincing.
Many other arguments were presented on
both sides. It appeared desirable to seek, at
subsequent shots, further evidence bearing on
the presence or absence of heavy active particles in the cloud at high altitudes immediately
after the shot. Direct cloud sampling with
available equipment was inapplicable since it
had provided no pertinent information in the
past. It appeared that the best that could be
done was to attempt to catch particles immedi-

ately before they reached the surface. It was
planned to attempt to do this where fall-out
similar to the Dog shot fall-out on Parry was
expected to occur, as predicted by the meteorologists. Particles so caught could not be suspected of having becomeattached to larger
particles after contact with the soil. The findings of fall-out in the predicted area would, it
was hoped, give convincing verification of the
meteorological data and methodsof prediction.
2.6.2.3 Reconsideration of Past Information

It is frankly admitted that the Dog shot fallout in the neighborhood of Parry came as a
complete surprise, regarding both the early
hour of arrival and the intensity of the radioactivity. It is necessary in assessing the state
of current knowledge to inquire whether any
earlier information had been neglected or mis-

Select target paragraph3