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The kinetic dissolution of Flagstaff Hill chlorite (CCa-2 from Clay Minerals Society), (Mg4.55Al1.23Fe0.12)(Al1.04Si2.96)O10(OH)8, was investigated using a well-mixed flow-through reactor at 100°C, pH values ranging from 3.0 to 7.5, and variable saturation states. The objective was to measure the dependence of chlorite dissolution rate on pH as well as on degree of undersaturation under conditions...
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