10

1.3

EFFECTS OF IONIZING

Superficial Doses of Radiation
From Beta and Soft Gamma
Radiation

Trrere Can Br no doubt that the doses of radintion to the surface and the first few millimeters
of the body were substantially higher than the
nud-line dose of gammaradiation asa result of

physical considerations of gamma energy and
depth dose. In addition, the clinical observations of the skin lesions (see Chap. IIT) force-

tuliy demonstrated that the dose to the skin

varied considerably between individuals and
over the surface of any given individual. As
will become evident in the following discussions
of surface dose, it is obvious that any numbers
presented are at best only estimates and repre-

sent an approximation of some minimal value.
In areas where lesions were severe the doses

must have been significantly higher than in nondamaged areas,
To arrive at some physical estimate of the

skin dose, an attempt must be made to add up
the contributions of the high energy gamma,

the very soft gcamma,andthe higher energybeta
radiation from the lavge planar source in which
the individuals were of necessity existing.

Flawever, as alluded to above and emphasized
in Chapter TIT, the largest component of skin
Irradiation resulted froin the spotty local de-

‘posits of fallout material on exposed surfaces
of the body. The dose from deposited material
is impossible to estimate: however, that from
the large planar source mav be roughly estimated as follows:

The beta dose rate in nir 3 feet above the
surface of an infinite plane contaminated with
mixed 24 hourold fission products is estimated
to be about three times the total air gamma dose.

The mid-line gamma dose is approximately 60
percent of the air dose remuining after excludIng that portion of the dose below 60 KY.

This port.on in turn is estimated to be 40 per-

cent of the ganima dose measured im air hythe
Mistrument. Thus the dose at the surface of 2
phantom exposed to mixed fission product
radiation from an external plane source night

500218

RADIATION

be expected to be 3/(0.6) (0.6) or about 8 times

the
the
hus
ous
the

mid-line dose, if both are taken at 3 feet off
ground. Such a depth dose measurement
in fact been made experimentallyat a previtest, using a phantom man exposed to both
initial and residual radiation (5). The

depth doses for each situation are shown in

Figure 1.5, with all data as percent
meter dose. With the diverging
tion from the point of explosion,
Was seen to be 63 percent of the 3

of the 3 centiinitial radiathe exit dose
cm. dose, but

with the diffuse residual field of fission products

providing a semi-infinite planar source, a surface dose some 8 times greater than the 3cm. and
deeper dose from the harder gamma components
was observed. This is seen to be of the same
order of magnitude as that estimated above.
At heights above and below the 3 foot level this
surface dose would become lower and higher
respectively, but since it is due to soft radiation
of short range, it probably would not exceed 50
times the 3 foot air gamma dose or 80 times the
midline dose, even in contact with the ground.
An estimate of skin dose due to ground contamination for the Rongelap case would result, for
exninple, in a figure of about 2,000 rep at the

level of the dorsum of the foot, 600 rep at the lip

level and 300 rep at the head 77 continuous ez-

posure with no shielding occurred. Unknown
variation in dose undoubtedly resulted from
shielding and movement. It thus seems probable that the external beta dose from loca} direct
skin contamination far outweighed that from
the ground in importance, since the latter was
not high enough to produce the observedlesions.
Clothing probably reduced the beta dose from
the ground by 10 to 20 percent.

1.4

Summary

Rapiation Doses from gamma rays originating
externally were calculated for the 267 individuals who were accidentally exposed to fallouc

following the nuclert detonation at the Pacitie
Proving Ground in the Spring of 1954. The

dose estimations were made using information

resulting from radiological safety surveys on

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