BATTELLE
Dr.

Rudolf J.

3.

Engelmann

NORTHWEST
-5-

March 12,

1971

The resuspension factors for <3 um diameter and high

density

(10 g/cc)

238Pu05 particles are desired.

A

direct answer is not known since we do not know if
the tracer would retain its identity, or if it would
attach to a host soil particle.
In addition the reSuspension factor would be a function of the surface
type as well as airborne loading of soil passing over
the contaminated area,
‘Consequently, we have to conclude that the plausible
estimate of the experimental resuspension factor is

still 6 x 1079 to 1077 m-! or greater.

However,

Fuquay's model in the SNAP-27 review does predict re-

suspension factors as high as 0.3 m1 for 1.5 ym

diameter particles at a wind speed of 10m/sec.

It is anticipated but unproven that charged 238pu05

particles would coagulate faster than uncharged particles

with natural dust particles.
The electrical forces
are present to cause the increased coagulation, but
the coagulation would depend upon the relative proximity

of particulates.

The hypothesized mechanisms for increased coagulation

is as follows:
Radiation from the particle would electrically ionize the surrounding air.
If subsequently
the particles became oppositely charged, an electrical
attraction between particles would increase the coagulation rate.

This increased coagulation rate is the case of coagula-

tion in a bipolar ion source.
The theory for ionic
equilibrium has been developed in the literature.
How-

ever, we are not talking about an equilibrium condition
in time, space, and concentration.
For these nonequilibrium conditions, a definite possibility exists
that coagulation would be enhanced.
Indeed, we propose
within to determine the importance of this non-equilibrium
charge distribution on enhanced coagulation.
We cannot predict the post-impact weathering half-life
or factor associated with the Pioneer capsule and plutonic molybdenum cermet fuel

as

respirable particles of 238pud>.

opposed to the <

3

um

Select target paragraph3