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Investigation of the hydrogen bonding in ice Ih by first-principles density function methods

机译:用第一性原理密度函数法研究冰Ih中的氢键

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It is a well recognized difficult task to simulate the vibrational dynamics of ices using the density functional theory (DFT), and there has thus been rather limited success in modelling the inelastic neutron scattering (INS) spectra for even the simplest structure of ice, ice Ih, particularly in the translational region below 400 cm~(-1). The reason is partly due to the complex nature of hydrogen bonding (H-bond) among water-water molecules which require considerable improvement of the quantum mechanical simulation methods, and partly owing to the randomness of protons in ice structures which often requires simulation of large super-lattices. In this report, we present the first series of successful simulation results for ice Ih using DFT methods. On the basis of the recent advancement in the DFT programs, we have achieved for the first time theoretical outcomes that not only reproduce the rotational frequencies between 500 to 1200 cm~(-1) for ice Ih, but also the two optic peaks at ~240 and 320 cm~(-1) in the translational region of the INS spectra [J. C. Li, J. Chem. Phys 105, 6733 (1996)]. Besides, we have also investigated the impact of pairwise configurations of H2O molecules on the H-bond and found that different proton arrangements of pairwise H_2O in the ice Ih crystal lattice could not alter the nature of H-bond as significantly as suggested in an early paper [J. C. Li and D. K. Ross, Nature (London) 365, 327 (1993)], i.e., reproducing the two experimental optic peaks do not need to invoke the two H-bonds as proposed in the previous model which led to considerable debates. The results of this work suggest that the observed optic peaks may be attributed to the coupling between the two bands of H-O stretching modes in H_2O. The current computational work is expected to shed new light on the nature of the H-bonds in water, and in addition to offer a new approach towards probing the interaction between water and biomaterials for which H-bond is essential.
机译:使用密度泛函理论(DFT)来模拟冰的振动动力学是一项公认的艰巨任务,因此,即使对于最简单的冰,冰结构,对非弹性中子散射(INS)光谱建模的成功也相当有限。 Ih,尤其是在400 cm〜(-1)以下的平移区域。原因部分是由于水-水分子之间氢键(H键)的复杂性,需要对量子力学模拟方法进行相当大的改进,部分是由于冰结构中质子的随机性,通常需要对大分子进行模拟超晶格。在本报告中,我们介绍了使用DFT方法对冰Ih成功进行模拟的第一系列结果。在DFT程序的最新进展的基础上,我们首次获得了理论成果,不仅再现了冰Ih的旋转频率在500至1200 cm〜(-1)之间,而且还再现了〜处的两个光学峰。在INS光谱的平移区域中有240和320 cm〜(-1)[J. C.Li,J.Chem。 Phys 105,6733(1996)]。此外,我们还研究了H2O分子的成对构型对氢键的影响,发现冰Ih晶格中成对的H_2O的不同质子排列不能像早期那样显着改变氢键的性质。纸张[J. C.Li和D.K.Ross,Nature(London)365,327(1993)],即,再现两个实验光学峰不需要像先前模型中所提出的那样引起两个H键,这引起了很多争论。这项工作的结果表明,观察到的光学峰可能归因于H_2O中H-O拉伸模式的两个谱带之间的耦合。预计当前的计算工作将为水中氢键的性质提供新的思路,并为探测水与氢键至关重要的生物材料之间的相互作用提供新的方法。

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