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- W98302016 abstract "Results of the synthesis of SYNROC C from both high surface area (16m/sup 2//g) and low surface area (4m/sup 2//g) powders at low and high oxygen fugacities indicate variations in radionuclide distribution. These results are most striking for the partitioning of uranium between perovskite and zirconolite. In highly active powders, the formation of a pyrochlore precursor ensures that equilibrium partitioning is approached. In less active powders, no low temperature pyrochlore is formed. As a result, the uranium partitioning is a function of nucleation processes. At high oxygen fugacities, uranium is rejected from perovskite and an additional uranium rich phase is formed precluding the synthesis of SYNROC C in air." @default.
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- W98302016 date "1981-10-16" @default.
- W98302016 modified "2023-09-24" @default.
- W98302016 title "SYNROC C: preparation and radwaste distribution" @default.
- W98302016 hasPublicationYear "1981" @default.
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