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A theoretical study of the hydration of Rb~+ by Monte Carlo simulations with refined ab initio-based model potentials

机译:Rb〜+水合的理论研究,基于蒙特卡洛模拟,具有基于从头算的精细模型势

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An infinitely diluted aqueous solution of Rb was studied using ab initio-based model potentials in classical Monte Carlo simulations to describe its structural and thermodynamic features. An existing flexible and polarizable model [Saint-Martin et al. in J Chem Phys 113(24) 10899, 2000] was used for water-water interactions, and the parameters of the Rb~+-water potential were fitted to reproduce the polarizability of the cation and a sample of ab initio pair interaction energies. It was necessary to calibrate the basis set to be employed as a reference, which resulted in a new determination of the complete basis set (CBS) limit energy of the optimal Rb~+-OH2 configuration. Good agreement was found for the values produced by the model with ab initio calculations of three- and four-body nonadditive contributions to the energy, as well as with ab initio and experimental data for the energies, the enthalpies and the geometric parameters of Rb~+(H2O)_n clusters, with n =1, 2,..., 8. Thus validated, the potential was used for simulations of the aqueous solution with three versions of the MCDHO water model; this allowed to assess the relative importance of including flexibility and polarizability in the molecular model. In agreement with experimental data, the Rb~+-O radial distribution function (RDF) showed three maxima, and hence three hydration shells. The average coordination number was found to be 6.9, with a broad distribution from 4 to 12. The dipole moment of the water molecules in the first hydration shell was tilted to 55° with respect to the ion's electric field and had a lower value than the average in bulk water; this latter value was recovered at the second shell. The use of the nonpolarizable version of the MCDHO water model resulted in an enhanced alignment to the ion's electric field, not only in the first, but also in the second hydration shell. The hydration enthalpy was determined from the numerical simulation, taking into account corrections to the interfacial potential and to the spurious effects due to the periodicity imposed by the Ewald sums; the resulting value lied within the range of the various different experimental data. An analysis of the interaction energies between the ion and the water molecules in the different hydration shells and the bulk showed the same partition of the hydration enthalpy as for K~+. The reason for this similarity is that at distances longer than 3 A, the ion-water interaction is dominated by the charge-enhanced) dipole term. Thus, it was concluded that starting at K~+, the hydration properties of the heavier alkali metal cations should be very similar.
机译:在经典的蒙特卡洛模拟中,使用从头算的模型势研究了无限稀释的Rb水溶液,以描述其结构和热力学特征。现有的灵活且可极化的模型[Saint-Martin等。 [J Chem Phys 113(24)10899,2000]中的Rb +水势的参数被拟合以再现阳离子的极化率和从头算对相互作用的能量样品。有必要校准要用作参考的基础集,这需要重新确定最佳Rb〜+ -OH2构型的完整基础集(CBS)极限能量。该模型产生的值与三体和四体非可加性对能量的从头算计算,以及能量,焓和Rb〜的从头算和实验数据之间发现了很好的一致性。 +(H2O)_n团簇,其中n = 1、2,...,8。这样就验证了这一潜力,它可以用三种版本的MCDHO水模型模拟水溶液。这可以评估在分子模型中包括柔韧性和极化性的相对重要性。与实验数据一致,Rb〜+ -O径向分布函数(RDF)显示了三个最大值,因此显示了三个水化壳。发现平均配位数为6.9,分布范围为4至12。第一个水化壳中水分子的偶极矩相对于离子电场倾斜至55°,并且其值低于离子的电场值。平均散装水;后一个值在第二个shell中恢复。 MCDHO水模型的非极化版本的使用不仅在第一个水合壳中,而且在第二个水合壳中都增强了与离子电场的对准。通过数值模拟确定水合焓,并考虑到对界面势和因Ewald和强加的周期性而产生的杂散效应的校正;结果值在各种不同的实验数据的范围内。对不同水化壳和主体中离子与水分子之间相互作用能的分析表明,水合焓的分配与K〜+相同。这种相似性的原因是,距离大于3 A时,离子-水相互作用主要由电荷增强的偶极子项决定。因此,可以得出结论,从K +开始,较重的碱金属阳离子的水合性质应非常相似。

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