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A sped up 14 C launch rate at tiny mass losses is observed, a sign of a 14 C-enriched surface region with a depleting concentration slope into the material, and the source terms and complexities linked with anticipating where the 14 C developed from are talked about. This work demonstrates a method for identifying the distribution of 14 C between near-surface areas and the bulk material in varying sources of irradiated graphite, and gives data on behalf of making an educated assessment for the fostering of reduced temperature level thermal treatment and isotopic decrease of irradiated graphite wastes.
Source link: https://www.osti.gov/biblio/1819518
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