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Mechanism of fast proton transfer in ice:Potential enertgy surface and reaction coordinate analyses

机译:冰中质子快速转移的机理:势能面和反应坐标分析

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The mechanism of proton transfer in ice is invetigated theoretically by examining the potential energy surfaces and determining the reaction coordinates. It is found to be quite different from that in liquid water. As shown by many authors, proton transfer in liquid water is promoted by the structure fluctuation, creating three-coordinated water molecules in the hydrogen bond network rearrangement, and the excess proton makes transtions among these three-coordinated water molecules as forming a so-called Zundel structure,(H_5O_2)~+. This kind of large structuralrearrangement cannot take place in ice. Nevertheless, the proton transfer in ice can be very fast. It is found that the srtrong constraint on the molecular beometry in ie is the source of the facile proton transfer. This constraint reduces tha stabilization of the excess proton state in two ways:(1) as O-O cannot shrink freely, it canot form a stable Zundel structure in which two water molecules share the excess proton lo ating at the center of the shortened O-O bond, and (2) as the existence of the repulsive force, an Eigen structure cannot be cmuch stabilized. This repulsive force slso contributes to partially shorten the O-O distance and thus facilitating a proton transfer. As the result, the excess proton is not trapped in a deep energy minimum but makes the transfers on small energy barriers. The molecular geometry rela ation along the proton transfer is analyzed; it is found that O-O stretchings/shrinkages at the excess proton moiety are mutually coupled to assist the sequential proton transfers in a concerted fashionl. The energetics and geometrical changes along these reaction coordinates are analyzed .The potential energies are found to be fairly flat for different locations of the excess proton. The nature of the excess proton solvation from the surrounding water molecules are analyzed; it is shown that the solveation by even distant shells yields a significant contribution to the potential energy surface of the proton transfer
机译:通过检查势能面并确定反应坐标,从理论上研究了质子在冰中的转移机理。发现它与液态水有很大不同。正如许多作者所表明的那样,液态水的质子传递通过结构波动而促进,在氢键网络重排中产生三配位的水分子,而过量的质子使这三配位的水分子之间发生转变,形成所谓的Zundel结构,(H_5O_2)〜+。这种大的结构重新布置不可能在冰上进行。然而,质子在冰中的转移可能非常快。发现对分子等宽线的严格约束是容易质子转移的来源。这种限制通过两种方式降低了多余质子状态的稳定性:(1)由于OO无法自由收缩,因此无法形成稳定的Zundel结构,其中两个水分子在缩短的OO键的中心共享过量质子。 (2)由于排斥力的存在,本征结构不能得到稳定。该排斥力slso有助于部分缩短O-O距离,从而促进质子传递。结果,多余的质子不会被束缚在最小的深能量中,而是在较小的能垒上进行转移。分析了沿质子转移的分子几何关系;已经发现,在过量的质子部分的O-O伸展/收缩相互偶联,以帮助以协调一致的方式进行连续的质子转移。分析了沿着这些反应坐标的能量学和几何学变化。发现过量质子的不同位置的势能相当平坦。分析了周围水分子中过量质子溶剂化的性质;结果表明,即使是较远的壳层,也能对质子转移的势能面产生重大贡献。

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