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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Published in | Chemical geology Vol. 540; no. C |
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Main Authors | , , , , , |
Format | Journal Article |
Language | English |
Published |
Netherlands
Elsevier
01.05.2020
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Subjects | |
Online Access | Get full text |
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