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Abstract

The ability to determine the time since forming of seized nuclear material would provide crucial data to be used in its investigation. The time dependent processes of diffusion relevant to this need are examined; to include grain boundary diffusion, and discontinuous precipitation, and an assessment is performed of the utility of examination of impurity and alloying element concentration profiles for use as a pre-detonation nuclear forensics tool for determining the age of a metal sample. Several examples illustrate the effects of time on both binary alloys and multi-component systems. Parallels are drawn from studies of diffusion in mineral samples under geologic time and proposes modifications to that approach in order to determine the time since a metal sample was cast or formed.

DOI

10.7290/V7RF5RZ3

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This work is licensed under a Creative Commons Attribution 4.0 License.

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