The dissolution of calcite under conditions of high pH (8.0-9.0) is shown to be strongly inhibited by the presence of magnesium (Mg2+) cations. Channel flow cell measurements are used to deduce the appropriate rate law for dissolution and it is demonstrated that the inhibition arises from competitive Langmuirian adsorption of Mg2+ and Ca2+ ions on the calcite surface
The concentrations of magnesium (Mg) and calcium (Ca) in natural aqueous environments are controlled...
Magnesium (Mg2+) is one of the most common impurities in calcite and is known to have a non‐linear i...
The effect of Mg++ ion on the solubility of calcium carbonate was determined using P. K. Weyls carb...
Magnesium and sulfate are each known to affect calcite growth and dissolution, but little is known a...
The rate of dissolution of surface-treated calcite crystals in aqueous acidic solution has been stud...
The effects of maleic and fumaric acids and their mono- and di-anions on the dissolution of calcite ...
We have measured the surface controlled dissolution rates of natural calcium carbonate minerals (lim...
Abstract--Fol lowing Shiraki and Brantley (1995), who found different growth mechanisms for calcite ...
The channel-flow cell method is used to establish the dissolution/precipitation kinetics of calcite ...
The kinetics of proton-induced calcite dissolution in aqueous solution in the presence of humic acid...
The effects of the dianions (A2-) of d-, I- and meso-tartaric acids on the dissolution reaction whic...
The kinetics of calcite dissolution in aqueous acidic solution following various surface treatments ...
An understanding of the factors controlling calcite dissolution is important for modeling geochemica...
The dissolution kinetics of surface-pretreated and weathered calcite was investigated in dilute acid...
CaCO3 particles grow excessively upon chemical precipitation in the absence of impurities or growth ...
The concentrations of magnesium (Mg) and calcium (Ca) in natural aqueous environments are controlled...
Magnesium (Mg2+) is one of the most common impurities in calcite and is known to have a non‐linear i...
The effect of Mg++ ion on the solubility of calcium carbonate was determined using P. K. Weyls carb...
Magnesium and sulfate are each known to affect calcite growth and dissolution, but little is known a...
The rate of dissolution of surface-treated calcite crystals in aqueous acidic solution has been stud...
The effects of maleic and fumaric acids and their mono- and di-anions on the dissolution of calcite ...
We have measured the surface controlled dissolution rates of natural calcium carbonate minerals (lim...
Abstract--Fol lowing Shiraki and Brantley (1995), who found different growth mechanisms for calcite ...
The channel-flow cell method is used to establish the dissolution/precipitation kinetics of calcite ...
The kinetics of proton-induced calcite dissolution in aqueous solution in the presence of humic acid...
The effects of the dianions (A2-) of d-, I- and meso-tartaric acids on the dissolution reaction whic...
The kinetics of calcite dissolution in aqueous acidic solution following various surface treatments ...
An understanding of the factors controlling calcite dissolution is important for modeling geochemica...
The dissolution kinetics of surface-pretreated and weathered calcite was investigated in dilute acid...
CaCO3 particles grow excessively upon chemical precipitation in the absence of impurities or growth ...
The concentrations of magnesium (Mg) and calcium (Ca) in natural aqueous environments are controlled...
Magnesium (Mg2+) is one of the most common impurities in calcite and is known to have a non‐linear i...
The effect of Mg++ ion on the solubility of calcium carbonate was determined using P. K. Weyls carb...
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