The dissolution into water of anhydrite and gypsum was studied at 25°C using a rotating disc of polycrystalline material, and the kinetics were followed with a calcium selective electrode. The dissolution rate of gypsum was transport controlled while that of anhydrite was intermediate between chemical and transport control.
A. F. M. Barton and N. M. Wilde, Trans. Faraday Soc., 1971, 67, 3590 DOI: 10.1039/TF9716703590
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