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Radiation-Induced Sodium-Metal-Colloid Formation in Natural Rock Salt from Different Geological Localities

机译:不同地质环境中天然岩盐中辐射诱导的钠金属胶体形成

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Radiation damage has been studied in natural rock salt from various localities, including potential repository sites. In the 100 to 300 C range the damage consists of point defects, primarily F-centers, and colloidal metal sodium particles. With increasing dose the F-centers grow to a saturation level, reached at 10 exp 7 to 10 exp 8 rad, that decreases with increasing temperature to a negligible level at 300 C. Colloid concentration vs. irradiation-time curves follow nucleation and growth curves accurately described by C t/sup n/, or C(dose)/sup n/, relations at large irradiation times. For fourteen samples, n = 1.85 +- 0.18 but the values of C vary by a factor of more than 10 exp 3 . The constant C is related to the sample strain, the impurity and void content, dose rate, and possibly other factors. The currently available data indicate that rock salt adjacent to radioactive waste canisters, at a temperature of 150 C, will contain between 0.01 and 10 mole percent of sodium metal when the total dose reaches 10 exp 10 rad. (ERA citation 07:003359)

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