In a nuclear reactor, quartz alters gradually to an amorphous form. Some of the property changes observed are ( a ) decreases in density, refractive indices, rotatory power, and birefringence, ( b ) disappearance of the α‐β transition, and ( c ) changes in the absorption spectrum. The properties of vitreous silica also alter in a nuclear reactor, the density and refractive index increasing somewhat. On heating the irradiated solids the properties alter in a complex manner.
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Primak et al. (1955) studied this question.
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