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ABSTRACT
Calcium carbonate precipitated in Ca- and Mg-saturated montmorillonite suspensions was more soluble than calcite added to these suspensions. The CaCO3 precipitated from a clay suspended in Ca(OH)2 had a greater solubility than when the CaCO3 was precipitated by the addition of CaCl2 and NaHCO3. The difference in solubility between the two directions of approach to equilibrium was related to the amount of soluble Mg in the system. When CaCO3 was precipitated from CaCl2 and NaHCO3 in clay suspensions with Mg-saturation as a variable, its solubility was related to the amount of Mg in solution with apparently no effect of the clay per se.
1 Contribution from the Department of Soils and Plant Nutrition, University of California, Riverside.
2 Former Graduate Research Assistant and Professor of Soil Science, respectively.
Received for publication March 7, 1968. Accepted for publication June 25, 1968.
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