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 --) .