Abstract
The migration of groundwater equilibrated with cement from a deep geological disposal facility for radioactive wastes will perturb the chemical, minerological and physical properties of the geosphere in advance of the migration of radionuclides. Preliminary modelling of a simplified scenario has been conducted to assess these changes using appropriate data for mineral dissolution kinetics, the chemical composition of cement pore fluids, and the hydrogeological characteristics of fractured crystalline rock. Chemical exchanges between rock immediately adjacent to the engineered barriers of a waste disposal facility and pore fluids were evaluated using the speciation-reaction path code. EQ 3 6 which revealed rapid loss of Ca, and gains in Na and Si of the evolved fluids, with little change in pH. Secondary minerals show a sequence of calcium silicate hydrates, and zeolites. Precise definition of the overall mass balance is uncertain due to the absence of both thermodynamic data for many zeolites and kinetic data for the precipitation of feldspars. Modelling has demonstrated that reaction kinetics will be important in governing chemical exchanges for length scales up to 20 m. Radionuclide retardation will be enhanced by the growth of zeolites and calcium silicate hydrates.
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