The morphology of calcite crystals grown in a porous medium doped with divalent cations

被引:69
作者
Fernández-Díaz, L [1 ]
Astilleros, JM [1 ]
Pina, CM [1 ]
机构
[1] Univ Complutense Madrid, Dpto Cristalog & Mineral, E-28040 Madrid, Spain
关键词
calcite; crystal morphology; gel crystal growth method; impurities;
D O I
10.1016/j.chemgeo.2005.08.024
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
Calcite crystals were grown in the presence of small concentrations (50, 200, and 600 ppm) of divalent cations (Ba2+, Sr2+, Co2+ and Mn2+) in a silica hydrogel medium. The calcite crystals grown in the presence of cations larger than Ca2+ (Ba2+ or Sr2+) developed rhombohedral habits defined by {1014} form, similar to the morphology of calcite grown in a pure gel. SEM images show that growth on {1014} occurs by lateral advancement of layers bounded by macroscopic dendritic or jagged steps. In the case of calcite crystals grown in a gel doped with cations smaller than Ca2+ (Co2+ or Mn2+), a variety of morphologies was obtained, ranging from blocky crystals (at lower concentrations: 50 and 200 ppm) to peanut-like aggregates, spheres and spherulites (at 600 ppm). The macroscopic morphological characteristics of such doped calcite crystals reflect closely the growth behaviour of calcite {1014} surface at a nanoscale, reported by previous AFM studies. Morphological features have been interpreted on the basis of the modification of growing steps characteristics as a consequence of asymmetrical cation incorporation. The use of such morphologies as a criterion of biological activity is, therefore, unreliable. (c) 2005 Elsevier B.V. All rights reserved.
引用
收藏
页码:314 / 321
页数:8
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