After the construction of the spent nuclear fuel (SNF) repository, the initial ambient environment of the bentonite barrier is subject to residual radioactive decay heat. Subsequently, the elevated temperature conditions within the repository (40-70°C) can persist for >1,000 years. Furthermore, a temperature gradient can be generated from the center of SNF storage area to the surface of the host rock, as the boundary of the SNF is at natural groundwater temperature (18-30°C). Given that SNF repositories must remain stable for over 100,000 years, understanding how microbial activity responds to these temperature conditions is critical for long-term repository safety.
Park et al. (Fri,) studied this question.
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