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利用高速调频原子力显微镜研究方解石生长台阶边缘的原子尺度结构和动力学。

Atomic-scale structures and dynamics at the growing calcite step edge investigated by high-speed frequency modulation atomic force microscopy.

机构信息

Nano Life Science Institute (WPI-NanoLSI), Kanazawa University, Kakuma-machi, Kanazawa 920-1192, Japan.

Division of Electrical Engineering and Computer Science, Kanazawa University, Kakuma-machi, Kanazawa 920-1192, Japan.

出版信息

Faraday Discuss. 2022 Jul 14;235(0):551-561. doi: 10.1039/d1fd00084e.

DOI:10.1039/d1fd00084e
PMID:35383345
Abstract

We have investigated the calcite growth mechanism by directly imaging atomic-scale structural changes at the growing step edges with high-speed frequency modulation atomic force microscopy (HS-FM-AFM). We compared the results with those previously obtained during dissolution, where a transition region (TR) consisting of a Ca(OH) monolayer was found to be formed along the step edges as an intermediate state. We found that the TR is created not only during dissolution but also during the growth process. Steps with and without a TR coexist with a ratio of 7 : 3 in both dissolution and growth, implying that their primary reaction pathways should involve TR formation. While all the dissolving steps show a linear shape, the growing steps additionally present a complex non-linear shape with many kinks. The TRs formed along the linear steps present a fixed and uniform width, while those along the complex steps present a non-uniform and dynamically varying width. The acute and obtuse steps show similar TR formation probability, TR width, and step velocity during growth, while a TR is preferentially formed along an acute step during dissolution. For both step types, TRs during growth are wider than those during dissolution. Based on these findings, we present possible reaction pathways triggered by the adsorption of either CO or HCO for the elementary steps in calcite growth.

摘要

我们通过高速调频原子力显微镜(HS-FM-AFM)直接观察生长台阶边缘的原子尺度结构变化,研究了方解石的生长机制。我们将结果与溶解过程中的结果进行了比较,在溶解过程中,发现作为中间状态的沿台阶边缘形成了由 Ca(OH)单层组成的过渡区(TR)。我们发现,TR 不仅在溶解过程中形成,而且在生长过程中也形成。在溶解和生长过程中,具有和不具有 TR 的台阶共存的比例为 7:3,这表明它们的主要反应途径应该涉及 TR 的形成。虽然所有的溶解台阶都呈现线性形状,但生长台阶还呈现出许多拐点的复杂非线性形状。沿线性台阶形成的 TR 呈现固定且均匀的宽度,而沿复杂台阶形成的 TR 呈现非均匀且动态变化的宽度。在生长过程中,锐角和钝角台阶显示出相似的 TR 形成概率、TR 宽度和台阶速度,而在溶解过程中,TR 优先沿锐角台阶形成。对于这两种台阶类型,生长过程中的 TR 比溶解过程中的 TR 宽。基于这些发现,我们提出了方解石生长中基本步骤可能由 CO 或 HCO 的吸附引发的反应途径。

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引用本文的文献

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