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利用高速调频原子力显微镜和模拟技术研究方解石台阶边缘在水中的溶解过程。

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

机构信息

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

COMP Centre of Excellence, Department of Applied Physics, Aalto University , Helsinki FI-00076, Finland.

出版信息

Nano Lett. 2017 Jul 12;17(7):4083-4089. doi: 10.1021/acs.nanolett.7b00757. Epub 2017 Jun 29.

DOI:10.1021/acs.nanolett.7b00757
PMID:28650174
Abstract

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) 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.

摘要

通过原子力显微镜(AFM)、光学干涉测量和 X 射线显微镜直接对纳米级台阶流进行成像,极大地推动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事件之一,即台阶边缘的原子事件,尚未得到很好的理解。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),并能够在液体中以约 1 s/帧的速度实现真正的原子分辨率成像,比传统的 FM-AFM 快约 50 倍。通过开发的 AFM,我们直接观察到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。获得的图像表明,沿着台阶边缘形成了典型宽度为几个纳米的过渡区。基于先前研究的深入了解,我们的模拟表明,该过渡区很可能是溶解过程中的中间状态形成的 Ca(OH)单层。基于这一发现,我们提高了对方解石在水中的原子溶解模型的理解。这些结果为高速 FM-AFM 在具有真正原子分辨率的固液界面各种动态过程的研究中的广泛应用开辟了道路。

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