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) |
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