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- W2029977583 abstract "It is shown that the Stanford University Mercury Cadmium Telluride process simulator (SUMerCad) is only in approximate agreement with published Hg self-diffusivity data at or near Hg saturation. The cation vacancy component involved in Hg self-diffusion according to SUMerCad is at least a factor too large. At all temperatures between 350 and there is a significant contribution to the Hg self-diffusivity which is independent of the Hg pressure and is not accounted for by SUMerCad. The relevant point defect concentrations predicted by Berding et al are considered in relation to the Hg self-diffusion data and to the SUMerCad defect concentrations." @default.
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- W2029977583 date "1997-06-01" @default.
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- W2029977583 title "Comment on the Stanford University Mercury Cadmium Telluride process simulator" @default.
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- W2029977583 doi "https://doi.org/10.1088/0268-1242/12/6/001" @default.
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