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Dissolution kinetics and mechanisms at dolomite-water interfaces: effects of electrolyte specific ionic strength
Man Xu1, Katie Sullivan, Garrett Vanness
1Department of Chemistry, Wright State University, 3640 Colonel Glenn Highway, Dayton, Ohio 45435, United States.
Background electrolytes significantly impact dolomite dissolution rates, with higher ionic strength and lower pH accelerating the process. Sodium chloride showed stronger effects than tetramethylammonium chloride.
Area of Science:
- Geochemistry
- Environmental Science
- Materials Science
Background:
- Understanding carbonate mineral-water interactions is crucial for environmental processes like CO2 sequestration.
- Dolomite (CaMg(CO3)2) dissolution is a key reaction in many geochemical systems.
Purpose of the Study:
- To investigate the influence of background electrolytes on dolomite dissolution kinetics.
- To elucidate the mechanisms governing dolomite reactivity at mineral-water interfaces.
Main Methods:
- In situ hydrothermal atomic force microscopy (HAFM) was used to measure step dissolution rates.
- Dolomite surfaces were exposed to NaCl and TMACl solutions at varying ionic strengths (0-0.77 m) and pH (4 and 9) at 90 °C.
Main Results:
- Dolomite step retreat rates increased with increasing ionic strength and decreasing pH.
- Anisotropy in step speeds ([481] vs. [441]) became more pronounced with higher ionic strength.
- NaCl exhibited stronger effects on step speeds than TMACl at equivalent ionic strengths.
Conclusions:
- Dissolution rates are sensitive to ionic strength, pH, and the type of electrolyte.
- A proposed mechanism involves orientation-dependent ion adsorption affecting edge free energy.
- These findings advance the understanding of dolomite reactivity in geological CO2 sequestration.
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