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Competing quantum effects in the dynamics of a flexible water model

机译:灵活的水模型动力学中的竞争量子效应

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Numerous studies have identified large quantum mechanical effects in the dynamics of liquid water. In this paper, we suggest that these effects may have been overestimated due to the use of rigid water models and flexible models in which the intramolecular interactions were described using simple harmonic functions. To demonstrate this, we introduce a new simple point charge model for liquid water, q-TIP4P/F, in which the O–H stretches are described by Morse-type functions. We have parametrized this model to give the correct liquid structure, diffusion coefficient, and infrared absorption frequencies in quantum (path integral-based) simulations. The model also reproduces the experimental temperature variation of the liquid density and affords reasonable agreement with the experimental melting temperature of hexagonal ice at atmospheric pressure. By comparing classical and quantum simulations of the liquid, we find that quantum mechanical fluctuations increase the rates of translational diffusion and orientational relaxation in our model by a factor of around 1.15. This effect is much smaller than that observed in all previous simulations of empirical water models, which have found a quantum effect of at least 1.4 regardless of the quantum simulation method or the water model employed. The small quantum effect in our model is a result of two competing phenomena. Intermolecular zero point energy and tunneling effects destabilize the hydrogen-bonding network, leading to a less viscous liquid with a larger diffusion coefficient. However, this is offset by intramolecular zero point motion, which changes the average water monomer geometry resulting in a larger dipole moment, stronger intermolecular interactions, And a slower diffusion. We end by suggesting, on the basis of simulations of other potential energy models, that the small quantum effect we find in the diffusion coefficient is associated with the ability of our model to produce a single broad O–H stretching band in the infrared absorption spectrum.
机译:许多研究已经确定了液态水动力学中的大量子力学效应。在本文中,我们建议这些作用可能由于使用刚性水模型和柔性模型而被高估了,在刚性模型和柔性模型中,使用简单谐波函数描述了分子内的相互作用。为了证明这一点,我们引入了一种新的简单的点电荷模型q-TIP4P / F,用于液态水,其中O–H拉伸由莫尔斯类型函数描述。我们对这个模型进行了参数设置,以在量子(基于路径积分)模拟中给出正确的液体结构,扩散系数和红外吸收频率。该模型还再现了液体密度的实验温度变化,并与大气压下六角形冰的实验融化温度合理地吻合。通过比较液体的经典模拟和量子模拟,我们发现量子机械波动将模型中的平移扩散和定向弛豫速率提高了约1.15倍。该效果远小于在所有先前的经验水模型仿真中观察到的效果,后者发现至少有1.4的量子效应,而与所使用的量子仿真方法或水模型无关。我们模型中的小量子效应是两个相互竞争的现象的结果。分子间零点能量和隧穿效应使氢键网络不稳定,从而导致粘度较低的液体具有较大的扩散系数。但是,这被分子内零点运动所抵消,该运动改变了水单体的平均几何形状,从而导致更大的偶极矩,更强的分子间相互作用以及更慢的扩散。最后,根据其他势能模型的模拟,我们建议在扩散系数中发现的小量子效应与我们的模型在红外吸收光谱中产生单个宽O–H拉伸带的能力有关。

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