Mr. Church stated that the available
possible subterranean pockets.
data was not extensive enough to support a contention that other pockets
did not exist.
For purposes of certification there would have to be
additional data taken.
The same method of obtaining data for certification applies to all islands.
This consists of in-situ and surface
soil sample surveys, and investigation of suspected burial sites,
supplemented by selected soil profiling data.
Obviously, the greater
the density of soil sampling profile data, the lower the chance of being

surprised later in the cleanup.

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4

a.
After extensive discussion, the following was proposed and
accepted.
The norther half of the island will be gridded on a 50 meter

grid.

The "cool" area will be sampled first in order to characterize

the areas to be used for stockpiling of soil and debris from other islands.
Approximately 16 to 50 sample sites will be required, depending on initial
findings.
Areas are to be decided based on stockpile locations.
Sampling
transects should be cut through the mounds in this area to characterize
the contents thereof.
Characterization of the extent of subsurface pockets
can use an adaptation of the one half distance technique, working along

the 50 meter grid lines. Density of other sampling in the "hot" areas
can be decided on basis of data obtained from the "pocket" investigation.
b.

Use of the standard 50 meter grid will permit use of data obtained

during characterization for consideration for certification.
Although Runit
will be no different in method for certification, the history of the island
and available data do indicate a probable requirement for higher density
survey than may be required for other islands.
This led to a discussion
of the advantages and disadvantages of placing contaminated stockpiles on
relatively uncontaminated areas.
It would generally be better to put
contaminated stockpiles in areas known to be contaminated to similar or

higher levels. The "cool" area requires relatively few sampling sites and
to place the contaminated stockpile in the "hot" area may interfere with
the characterization effort.
15.

It was agreed that when resources permit it would be highly desirable

to use one IMP to further refine the area of surface contamination to be
removed,
These areas are defined, in the Fig/Quince area, by aerial survey
contours.
The Cactus crater area is not defined.
In-situ survey refine-

ment would assist considerably in refining the estimates of area, and
thus volume,

to be excised.

Mr. Church proposed to use the IMP only to

move in toward "hot" areas and define the periphery of those areas over
400 pCi/g. This would not be a full survey but would refine the area
boundries and would avoid risk of high contamination of the IMP.

There

was discussion of use of this "peripheral" technique as compared to a
full survey.

Nee

It was agreed that the peripheral technique would not totally

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