Historical review descriptions of diffusive mass transfer accompanying deformation

Historical review descriptions of diffusive mass transfer accompanying deformation 

A permeable elastic host and low-viscosity fluid (Terzaghi 1925, Biot 1941). 

A mass of grains, each wetted by a boundary layer of fluid the material of any grain can dissolve in the fluid and diffuse away to be precipitated at another location, the fluid itself remaining stationary throughout (Fletcher 1982). 

An amorphous stiff fluid mixture with atoms of two species A and B (Stephenson 1988). 

At times intermediate between first loading and stagnation, the stress state will be intermediate also. It is described by means of a local average stress state in the elastic host that is nonhydrostatic, and a local average stress state in the fluid that is hydrostatic the fluid pressure varies from point to point in the same sinusoidal manner as at the first moment but with diminished amplitude. 

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