Published online by Cambridge University Press: 03 September 2012
The logical place for the US Federal government to site a permanentrepository for its massive accumulation of cold-war reprocessing radwastewould be at its primary cold-war nuclear device testing reservation, theNevada Test Site(1). Regardless of whether it eventually choosesto implement that repository by drilling lateral “drifts” into consolidatedrock (e.g. its proposed Yucca Mountain facility) or by augeringmoderately-deep boreholes into unwelded alluvium beds (e.g. the “GreaterConfinement Disposal (GCD) repository implemented at Frenchman Flats in 1984 (2), zeolitic hydroceramic materials would be more stable thanwould glasses. The thermodynamic rationale for this is that in such regions,soil solutions and soil gasses both tend to “weather” buried natural glassesto zeolitic materials(3). It has also been demonstrated that thesame type of phases form when properly designed cementitious “grouts” arecured under mild hydrothermal conditions(4,5) - precisely thoseconditions assumed by DOE's repository modelers for “failed” (i.e. flooded)repositories and under which radwaste-type glasses rapidly decompose to formcrystalline zeolitic phases(6,7).