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首页> 外文期刊>Geochimica et Cosmochimica Acta: Journal of the Geochemical Society and the Meteoritical Society >The effect of barium on calcite {10(1)over-bar4} surfaces during growth
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The effect of barium on calcite {10(1)over-bar4} surfaces during growth

机译:生长期间钡对方解石{10(1)over-bar4}表面的影响

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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. [References: 38]
机译:原位原子力显微镜(AFM)实验提供了有关Ba2 +对方解石{1014}表面晶体生长的影响的信息。观察到的微观形貌特征已经通过考虑方解石表面对二价阳离子的掺入施加的结构控制和所用溶液的过饱和状态来解释。方解石生长步骤的钉扎发生在低Ba浓度下,表明Ba掺入的特定位点。当溶液中Ba含量增加时,观察到单分子步骤的进行。尽管[[41]上的[4]和[48]上的[1]]步长显示出特征的锯齿状边缘,但平行步长(即[41的[4]上] [-]和[ [](-)上方的48(1)几乎保持静止。可以通过考虑方解石台阶上大,小部位的非对称相关分布以及钡在前者中的掺入更容易来解释这一事实。所测量的新生长台阶的高度增加也与在某些位置优先掺入Ba相一致。溶液中Ba浓度的进一步增加导致方解石{10(1)在bar 4}表面上形成二维核。讨论了这些原子核的性质,并考虑了溶液相对于可以容纳Pa(方解石型结构和文石型结构)的两种可能结构的过饱和。版权所有(C)2000 Elsevier ScienceLtd。[参考:38]

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