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- W2019579505 abstract "Previous experiments on the effect of a fluid phase in deforming rock and rock analogue systems have failed to differentiate between the relative roles of stress and permanent strain in controlling preferential dissolution at fluid—grain boundary interfaces. Experiments are described here in which halite single crystals were loaded under dry conditions, followed by removal of load and immersion of the crystals in brine. A correlation between net dissolution rate and plastic strain of the adjacent crystalline material was then observed at free crystal surfaces. Calculation of the increase in free energy of the solid phase due to deformation indicates that plastic strain should play a greater part in controlling dissolution than elastic strain in the experimental design reported here. Although pressure gradients or differences in normal stress may dominate over strain energy terms in producing solution transfer or diffusion through disordered phases in natural rock systems, these halite-water experiments demonstrate that caution must be used in interpreting mechanisms from petrographic and other observations of the phenomena now commonly referred to as “pressure solution”." @default.
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- W2019579505 title "Strain-induced preferential dissolution of halite" @default.
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- W2019579505 doi "https://doi.org/10.1016/0040-1951(81)90026-3" @default.
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