Abstract
The kinetics of the aragonite-calcite transformation were studied in aqueous solution to determine the factors involved in the process of calcite crystallization and the controlling diagenetic conditions for the aragonite-calcite transformation. The reaction involved the solution and equilibration of aragonite with the solution and the subsequent nucleation and growth of calcite. The extent of reaction was determined by X-ray diffraction. Data suggest that calcite nucleation occurs on aragonite surface, whereas growth occurs on point or line defects. Catalysis by CO 2 , CaCl 2 , and inhibition by KOH indicate a fundamental reaction involving Ca (super ++) and HCO 3 (super -) . Calcite crystallization is strongly inhibited by Mg (super ++) and less so by SO 4 (super --) .
Cite
CITATION STYLE
Bischoff, J. L., & Fyfe, W. S. (1968). Catalysis, inhibition, and the calcite-aragonite problem; [Part] 1, The aragonite-calcite transformation. American Journal of Science, 266(2), 65–79. https://doi.org/10.2475/ajs.266.2.65
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