Time-dependent shapes of a dissolving mineral grain: Comparisons of simulations with microfluidic experiments

Experimental observations of the dissolution of calcium sulfate by flowing water have been used to investigate the assumptions underlying pore-scale models of reactive transport. Microfluidic experiments were designed to observe changes in size and shape as cylindrical disks (radius 10 mm) of gypsum...

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Veröffentlicht in:Chemical geology 2020-05, Vol.540 (C)
Hauptverfasser: Dutka, Filip, Starchenko, Vitaliy, Osselin, Florian, Magni, Silvana, Szymczak, Piotr, Ladd, Anthony J. C.
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Sprache:eng
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