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Composite backfill materials for radioactive waste isolation by deep burial in salt

Conference ·
OSTI ID:6932789
Bentonite and hectorite were found to sorb Pu(IV) and Am(III) from concentrated brines with distribution coefficients K/sub d/ > 3000 ml/g. The permeability of bentonite to brine was less than 1 microdarcy at a confining pressure of 18 MPa, the expected lithostatic pressure at the 800 m level in a salt repository. Getters for sorption of TcO/sub 4//sup -/ (K/sub d/ approx. 300 ml/g), I/sup -/ (K/sub d/ greater than or equal to 30 ml/g), Cs (K/sub d/ greater than or equal to 30 ml/g) and Sr (K/sub d/ greater than or equal to approx. 100 ml/g) from brines were identified. Their sorption properties are presented. Thermal conductivity results (>0.5 W/mK) and evidence for bentonite stability in brines at hydrothermal conditions are also given. It is shown by calculated estimates that a 3-ft-thick mixture of bentonite with other getter materials could retain Pu, Am, and TcO/sub 4//sup -/ for >10/sup 4/ years and I/sup -/ for > 10/sup 3/ years. Another tailored mixture could retain Cs for approx. 600 years, Sr for approx. 700 years, TcO/sub 4/ for approx. 4000 years and I/sup -/ for approx. 400 years. The backfill can offer a significant contribution to the isolation capability of a waste package system.
Research Organization:
Sandia National Labs., Albuquerque, NM (USA)
DOE Contract Number:
AC04-76DP00789
OSTI ID:
6932789
Report Number(s):
SAND-80-1377C; CONF-801124-6
Country of Publication:
United States
Language:
English