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Perspective on sum frequency generation spectroscopy of ice surfaces and interfaces

机译:浅谈冰曲面和界面的频率产生光谱

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摘要

This perspective is focused on surfaces and interfaces of crystalline ice studied with sum frequency generation (SFG) spectroscopy by several research groups within these twenty years. The intrinsic interface selectivity of SFG has already enabled one to determine structural aspects of the ice surfaces and interfaces through vibrational signatures of the OH stretch. Here we describe why SFG is suitable for ice surface science and how SFG has revealed the structure and dynamics of dangling bonds, quasi-liquid layer, hydrogen-bond network, and ordered protons at the ice surfaces, ice/substrate interfaces, and ice films on metal surfaces. In particular, we compare SFG spectra of ice reported by different groups to examine consistency between their experiments. We elaborate current controversies on a few SFG studies of ice before presenting future outlook for ice surface science by SFG. Additionally in the appendix we briefly explain some technical issues that may help us resolve conflicts and make progress in the right way.
机译:该观点集中在本20年内在几个研究组中使用若干研究组研究的结晶冰的表面和界面。 SFG的内在界面选择性已经使能够通过OH拉伸的振动签名来确定冰表面和界面的结构方面。在这里,我们描述了为什么SFG适用于冰面科学以及SFG如何揭示悬空粘合,准液体层,氢键网络的结构和动力学,并在冰表面,冰/基板接口和冰膜上有订购的质子在金属表面上。特别是,我们比较不同群体报告的冰的SFG光谱来检查其实验之间的一致性。在通过SFG提出未来的冰面科学前景之前,我们详细说明了对冰的几个SFG研究的争议。此外,在附录中,我们简要解释了一些可能有助于我们解决冲突并以正确的方式取得进展的一些技术问题。

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