good.

Not.sme NRL-operated instrument failed; at the LASL end 57 oscil-

loscope chani®™ recorded out of a possible 61, and Bowen spectrograph
¢

ls operated.

The total thermal radiation recorded on Orange was
The time-interval measurement
encountered similar difficulties as on feak, except that they were more
severe. Both primary and secondary signals were recorded, but because of
scattering in the deep cloud layer the time smear of the primary light pre_ vented the initial sharp rise required for a valid measurement. However
unfolding of the otherwise well-written records should yield a useful number,
The majority of the spectrographs and cameras registered either weak
signals or none. However, three instruments (two NRL, one LASL) recorded
relatively late time information which appears valuable. Also many photoelectric channels wrote a readable signal. These data describe qualitatively

the fireball behavior from approximately 1 msec on.

Aljlthough information

for earlier times ia not entirely absent, it is very sketchy. Nevertheless
there is a fair chance that one will arrive at a useful qualitative picture of

Orange fireball development, especially if the spectroscopic data analysis

can be supplemented by analysis of the EG&G high speed photographic records
taken from airplanes.

Program 11, Radiochemistry
The objectives of Program 11 were (1) to determine the fission yield
of the device, (2) to ascertain when possible what nuclear reactions take
place in the device, (3) to study specific aspecta of the reactions by radiochemical tracers placed within the device, and (4) to determine the production of specific activities in certain areas of the devices arising from mate-

rials included in them by design necessity or by intent.
Samples of radioactive material from the cloud were obtained by manned

aircraft equipped with specially designed sampling tanks, Radiochemical analyses were made at LASL to determine the fraction of the bomb included in
the sample and the number of fission events. The fission yield was determined from these data. Analyses were made to determine the production of
various radioisotopes of interest from the bomb materials or from detector
samples placed in or near the device.
The results of measurements of fission yields by various methods are

included in Table 2.1.

An investigation of water samples taken from the

lagoon shortly after Walnut shot showed marked fractionation, indicating that
such samples were not an adequate replacement for aircraft sampling.
Program 12, External Neutron Measurements

Program 12 was designed to determine the configuration of the active

material of certain devices during the nuclear reactions by the Pinex tech-

nique, whereby a neutron collimating "pinhole" is placed between the device
and detector. A pinhole camera image of the device is formed on the detector, which is a sandwich of various materials to be activated by the neutrons. The sample may be cut into segments and counted on a scintlilation

counter or placed against a photographic film to produce an autoradiographic
image.

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