Dolomite dissolution kinetics in aqueous solutions in the presence of organic and inorganic additives at 25 °C and pCO2 ~ 1 atm

The steady-state dissolution rate of dolomite was studied at 25 °C and 1 atm CO2 total pressure in deionised water in the absence (control) and presence of twenty seven different organic and inorganic additives at low concentration (1 mM). These additives are most likely present at low concentrations (