Abstract
Environmental protection by isolation of
radionuclides escaped from High-Level Radioactive Waste stored underground in
crystalline rock can be achieved by surrounding the metal canisters by smectite
clay, which provides hindrance of radionuclides to migrate into the
surroundings, and ductile embedment of them for absorbing seismic and tectonic
displacements in the host rock. The waste-isolating capacity of the expansive
clay is explained by its high hydrophilic capacity and large specific surface
area giving low porosity and limited interconnectivity of the voids, which both
makes such clay low-permeable and gives it a very low through-diffusion rate of
anionic species like iodine, and of some cationic radionuclides. The
expandability of such clay means that it can swell and undergo self-healing in
case of microstructural contraction caused by heating. The mechanisms involved
in permeation and ion exchange are described based on conceptual
microstructural models and their theoretical analogies. Stress/strain phenomena
involved in saturation with fluids, desiccation, shearing under deviatoric
conditions, and creep strain under stable conditions or at failure are
described as well. Longevity matters, which have been richly treated in the
literature, is given limited space.
Keywords: Smectite clay, montmorillonite,
microscopy, clay microstructure.