Abstract
The reaction of the (101̄4) calcite surface during dissolution was studied as a function of pH (HCl) by liquid-cell Atomic Force Microscopy (AFM) under ambient conditions of both temperature (22 °C) and partial pressure of carbon dioxide (PCO2). A flow through AFM liquid reaction cell was used, and solutions were renewed at a controlled flow rate and sampled for chemical analysis.
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Schedule a callMore From: American Mineralogist: Journal of Earth and Planetary Materials
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