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Dissolution Processes at Step Edges of Calcite in Water Investigated by High-Speed Frequency Modulation Atomic Force Microscopy and Simulation

机译:高速调频原子力显微镜和模拟研究水中方解石阶梯的溶解过程

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摘要

The microscopic understanding of the crystal growth and dissolution processes have been greatly advanced by the direct imaging of nanoscale step flows by atomic force microscopy (AFM), optical interferometry, and X-ray microscopy. However, one of the most fundamental events that govern their kinetics, namely, atomistic events at the step edges, have not been well understood. In this study, we have developed high-speed frequency modulation AFM (FM-AFM) and enabled true atomic-resolution imaging in liquid at ∼1 s/frame, which is ∼50 times faster than the conventional FM-AFM. With the developed AFM, we have directly imaged subnanometer-scale surface structures around the moving step edges of calcite during its dissolution in water. The obtained images reveal that the transition region with typical width of a few nanometers is formed along the step edges. Building upon insight in previous studies, our simulations suggest that the transition region is most likely to be a Ca(OH)2 monolayer formed as an intermediate state in the dissolution process. On the basis of this finding, we improve our understanding of the atomistic dissolution model of calcite in water. These results open up a wide range of future applications of the high-speed FM-AFM to the studies on various dynamic processes at solid-liquid interfaces with true atomic resolution. © 2017 American Chemical Society.
机译:通过原子力显微镜(AFM),光学干涉仪和X射线显微镜对纳米级台阶流进行直接成像,大大提高了对晶体生长和溶解过程的微观理解。然而,控制其动力学的最基本的事件之一,即台阶边缘的原子事件,尚未被很好地理解。在这项研究中,我们开发了高速频率调制原子力显微镜(FM-AFM),并以约1 s /帧的速度在液体中实现了真实的原子分辨率成像,这比常规FM-AFM快约50倍。利用已开发的原子力显微镜,我们可以直接成像方解石在水中溶解过程中移动台阶边缘周围的亚纳米级表面结构。所获得的图像表明,沿着台阶边缘形成了典型宽度为几纳米的过渡区域。基于先前研究的见识,我们的模拟表明过渡区最可能是在溶解过程中形成为中间状态的Ca(OH)2单层。基于这一发现,我们加深了对方解石在水中原子溶解模型的理解。这些结果为高速FM-AFM在具有真实原子分辨率的固液界面上的各种动态过程研究中打开了广阔的未来应用前景。 ©2017美国化学学会。

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