*Jun KAWANO1, Hiroshi SAKUMA2, Takaya NAGAI3
(1.CRIS, Hokkaido Univ., 2.NIMS, 3.Grad. School of Science, Hokkaido Univ.)
Keywords:calcium carbonate, impurity, crystal growh
Formation process of calcium carbonate polymorphs, calcite, aragonite and vaterite has been extensively investigated, and impurity effect has been proposed as controlling phenomena in order to account for the formation of a particular polymorph. For example, it has been reported that an addition of Mg2+ in a solution inhibits calcite formation and promotes aragonite formation, however incorporation mechanism of this kind of impurities is poorly understood.In general, smaller divalent cations than Ca2+, like Mg2+, cannot form solid solution with aragonite. However, the structure of a crystal surface or small cluster forming at an initial stage of crystal growth can be different from the bulk crystal because of its flexibility, and it can act as the site for incorporation of ions which is unstable in the bulk structure. In the present study, the stability of divalent cations, especially Mg2+, (1) on hydrated aragonite surface and (2) in the cluster forming in an early stage of nucleation was investigated by quantum-chemical calculations, and the impurity effects on the formation of polymorphs were discussed.The calculation results show that Mg2+ is easier to be incorporated into a small cluster, while the hydration energy of Mg2+ is higher than that of other divalent cations. This indicates that Mg2+ is difficult to be released from hydration shell, however, once released, it is easy to incorporate into the cluster. Atomic arrangement of these clusters including Mg2+ is different from that of additive-free CaCO3 clusters. Furthermore, Mg2+ on the aragonite surface considerably affects the surface structure and has an influence on the stability of aragonite. Thus, incorporation of Mg2+ into the clusters and surfaces sites should play an important role on the formation of the crystalline nuclei and the consequent crystal growth.