1981 Volume 30 Issue 336 Pages 856-860
The precipitation conditions for obtaining spherical particles of one-phase vaterite have been determined, and the effects of additives during precipitation and transition on the transition isotherms have been studied with the spherical powders obtained with different precipitants such as Na2CO3 and (NH4)2CO3.
The transition from vaterite to calcite in water media is characterized by abrupt appearance of calcite particles having well-developed crystal habits. Summarizing the experimental data, it is proposed that the dissolution-precipitation mechanism is operative in the transition, in which dissolution process is probably a rate-determining step.