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TABLE 5.

Radioactive isotope ratios in soil and aerosols at a stabilized bare
field on Bikini Island
238PU

Soil
FSD*

Aerosols (HV)
.
FSD*

*Fractional

241AM

137CS

90cjp

239+240pu

239+24Cpu

239+240pu

0.0013

0.556

9.80

9.15

0.56

0.55

0.48

0.52

0.050

0.439

0.64

0.34

Standard Deviations

61.4

23g+240Pu

12.8
0.51

0.32

[

239+240pu

(pCi g-l)
15.3
0.57

*

>

12.6
0.35

(s/~)

view volume about 5 cm depth and the exponential decrease of isotope concentration
with depth gives lower mean values. After correction by a factor 1.44, the ISG
method was the primary method for mapping 2u1Am as a tracer for the source of
suspended plutonium isotopes. The horizontal variations in soil isotope concentrations (ISG data) were small enough so that one could justify mean values as
local regional values for soil. For example, on the one-hectare, bare field,
it was determined that plutonium in surface soil had the mean value 15.3 pCi g-l
with an observed range of 2.3 to 28, and a fractional standard deviation (s/X)
of 0.57. There was no apparent pattern to the soil concentrations and they
exhibit approximately normal, random variation perhaps due to previous tilling and
(The data did not fit a log-normal distribution any better. )
blading locally.

,-.,
.( ...

In the context of this surface soil contamination, personal dosimeters (PD)
provided information about inhalation exposure of individuals relative to the
It was found that the fraction of dust in the total
reference HV monitors.
aerosol collected by the PD was greatest for workers exposed during heavy tilling
but was also high for workers exposed in and around houses (Table 6) partly
because of-a lowered fraction of sea spray in both cases.
In this and prior
studies, we found that the ratio of PD Dust/HV Dust has a value of approximately
0.5 where both PD and HV are sampling the same aerosol cloud of this size
particles (2.5 urn MAD) because of the cyclone particle-discriminator on the PD.
Therefore, the enhancement of inhalation exposure by a worker’s own actions where
the PD and HV are ~
sampling the same cloud can be estimated by a personal
—-----,cIo~jrne~&ra-e-nha
ncement. (PDE):
PDE = 2x (PD Dust/HV Dust)

.

[4]

Values so computed show significant enhancement (PDE) of inhalation exposure
(2.64) during heavy work outdoors by persons) sitting or kneeling while digging
or using tools on the ground (Table 6). The second highest enhancement (1.86)
came from persons with duties in and arou,nd the houses. Other work, including

.

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