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Thermoluminescence for Self-Dosimetry in Climax Stock Quartz Monzonite

Richard C. Carlson

Nuclear Technology / Volume 60 / Number 2 / February 1983 / Pages 244-252

Technical Paper / Radiation Effects and Their Relationship to Geological Repository / Radioactive Waste Management / dx.doi.org/10.13182/NT83-A33079

An examination has been made of the feasibility of using thermoluminescence (TL) for the self-dosimetry of the rock surrounding a canister of nuclear waste. The rock investigated was quartz monzonite from the Climax Stock, a granite intrusive at the Nevada Test Site. Samples of the rock were irradiated by 60Co to doses of 103 to 109 rads, then ground to a fine powder and read for TL response at a heating rate of 1°C/s. The procedures are described in detail to allow their duplication by others. Effects of total dose, thermal history after irradiation, grinding to a powder after irradiation, mineral composition, and powder grain size were investigated. Although all of these factors were found to be important, the use of TL in this manner appears promising.