diameter throughout the study period.
More studies are required to
address these problems and to find the specific causes responsible for
the large plutonium concentration variations at GZ site.

ACKNOWLEDGMENTS

The author would like to express his appreciation to E. M. Karlen, L. M.
Martinez, K. V. Bostick, and T. E. Hakonson of LASL for data collection
and sample processing efforts.

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