Abstract Examining carbonate dissolution kinetics at mineral-water interface is crucial to understand numerous environmental and geochemical processes, including global carbon cycling, CO2 sequestration in deep geological reservoirs, and trace elements release in terrestrial and aquatic environments. Here we explored the effect of circumneutral to alkaline pH solutions (pH 6–11) on dissolution kinetics of pure dolomite and Ca and Mg release stoichiometry in flow-through reactor experiments at 25 ± 1 °C. Results revealed that the dolomite dissolution rates obtained from effluent Ca and Mg concentrations (RCa and RMg in mol/cm2/s) were dependent on input solution pH and HCO3 − log activity. The pH dependence of dissolution rates showed two distinct trends, i.e., at circumneutral pH ranging between 6 and 8, the dissolution rate decreased with increasing pH, with minimum rate at pH 8. While in the highly alkaline pH range (pH 9–11), the dolomite dissolution rate increased with an increasing pH. Irrespective of the input pH, the dolomite dissolution rates indicated a reverse relationship with HCO3 − log activity, with the lowest dissolution rate (RCa = 3.80 × 10–12 mol/cm2/s) at pH 8 where HCO3 − log activity attained the highest value (− 3.957). The lower RCa and RMg obtained at pH 8 compared to all the other pH could possibly be attributed to an inhibition caused by high HCO3 − log activity in solution at this pH. Dolomite dissolution rates were non-stoichiometric at all the experimental pH values, showing higher preferential Ca over Mg release (RCa > RMg) whereas an opposite trend was observed at pH 8, with RCa < RMg at the steady state. Saturation index values calculated using geochemical speciation modelling were positive for Mg-bearing minerals (brucite, dolomite, artinite) at alkaline pH of 10–11, indicating favourable conditions for their precipitation under studied conditions. This study provides insights on the significance of log ion activities of HCO3 − and Me-OH+ under varying pH for elucidating the dissolution mechanism of dolomite in circumneutral to alkaline aqueous environments.
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