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• W2019907634 abstract "A new model has been developed for the deformation of granular material such as porous rock, based on a mechanism of relative movement of grains (granular flow) controlled by the rate of solution transfer involved in accommodating intergranular interferences. Distinction is made between control of the strain rate by: (1) the rate of diffusion of the dissolved granular substance in the pore fluid (fluid diffusion control); (2) the rate of dissolution or precipitation at the sources or sinks in the solution transfer process (reaction control); and (3) the rate of diffusion within the “islands” of the assumed “island and channel” structure of the grain interface (source/sink diffusion control). Using an analogy with particulate flow in soil mechanics to derive a flow equation for constant-volume flow and combining this with calculation of the rate of porosity reduction, general flow laws are derived for axisymmetric non-hydrostatic conditions. Application to the cases of quartz and rocksalt porous aggregates, with water as the pore fluid, suggest that, under geological conditions, source/sink diffusion control will tend to predominate where granular flow occurs." @default.
• W2019907634 created "2016-06-24" @default.
• W2019907634 creator A5052939994 @default.
• W2019907634 date "1995-05-01" @default.
• W2019907634 modified "2023-10-01" @default.
• W2019907634 title "A theory for granular flow accommodated by material transfer via an intergranular fluid" @default.
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• W2019907634 doi "https://doi.org/10.1016/0040-1951(94)00231-w" @default.
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