The effect of barium on calcite {10(1)over-bar4} surfaces during growth

被引:55
作者
Astilleros, JM
Pina, CM
Fernández-Díaz, L
Putnis, A
机构
[1] Univ Munster, Inst Mineral, D-48149 Munster, Germany
[2] Univ Complutense, Dept Cristalog & Mineral, E-28040 Madrid, Spain
关键词
D O I
10.1016/S0016-7037(00)00405-1
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
In situ atomic force microscopy (AFM) experiments have provided information about the effect of Ba2+ on crystal growth of calcite {1014} surfaces. The microtopographic features observed have been interpreted by considering both the structural control that the calcite surfaces exert on the incorporation of divalent cations and the supersaturation state of the solution used. Pinning of the calcite growth steps occurs at low Ba concentrations, suggesting specific sites for Ba incorporation. When the Ba content of the solution is increased the advancement of monomolecular steps is observed. Although [(4) over bar 41](+) and [48 (1) over bar](+) steps advance showing characteristic jagged edges, the parallel steps (i.e., [(4) over bar 41](-) and [48 (1) over bar](-)) remain practically immobile. This fact can be explained by considering the nonsymmetrically related distribution of large and small sites along the calcite steps and the easier incorporation of barium on the former. The measured increase in the height of the newly grown steps is also consistent with such preferential incorporation of Ba in certain positions. A further increase in the Ba concentration of the solutions leads to the formation of bidimensional nuclei on the calcite {10 (1) over bar 4} surfaces. The nature of these nuclei is discussed taking into account the supersaturation of the solution with respect to two possible structures that can accommodate Pa. the calcite-type structure and the aragonite-type structure. Copyright (C) 2000 Elsevier Science Ltd.
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页码:2965 / 2972
页数:8
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