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Solution alteration of limestone depends on rate at which water entering rock becomes saturated; this rate is governed by rate of transport of solute away from solid liquid interface; for laminar flow in straight circular capillary of radius a, solution will be 90% saturated after penetrating distance 0.57va2/D, where v is average flow velocity of fluid and D is diffusion constant of solute in solution.
Solution alteration of limestone depends on rate at which water entering rock becomes saturated; this rate is governed by rate of transport of solute away from solid liquid interface; for laminar flow in straight circular capillary of radius a, solution will be 90% saturated after penetrating distance 0.57va2/D, where v is average flow velocity of fluid and D is diffusion constant of solute in solution.
Solution kinetics of calcite
J Geology
Weyl, P.K. (author)
Journal of Geology ; 66
1958
14 pages
Article (Journal)
English
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