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首页> 外文期刊>The journal of physical chemistry, A. Molecules, spectroscopy, kinetics, environment, & general theory >Molecular Orbital Calculations of Water Clusters on Counterpoise-Corrected Potential Energy Surfaces
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Molecular Orbital Calculations of Water Clusters on Counterpoise-Corrected Potential Energy Surfaces

机译:平衡态势能面上水团簇的分子轨道计算

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摘要

Water dimer and the cyclic trimer and tetramer are calculated using the Hartree-Fock(HF),second-order M011er-Plesset(MP2),and two density functional theory(DFT)methods,B3PW91 and B3LYP for a wide variety of different basis sets.The interaction energies and O...O distances as calculated on the normal and counterpoise(CP)corrected potential energy surfaces(PES)are compared as a function of basis set quality(as measured by the energies for optimized water monomer)for each of the four methods.The HF and DFT procedures lead to reasonably rapid conversion to the large basis set values for both interaction energies and O...O distances.Even moderate basis sets can be used to obtain results similar to the extrapolated values when optimizations are performed on the CP-corrected PES's.For MP2,these energies and distances converge to the extrapolated values much more slowly.Basis set superposition error(BSSE)remains significant even for the best basis sets used(aug-cc-pVQz and aug-cc-pVTZ).Nevertheless,the extrapolated MP2 interaction energies could also be reproduced with moderate sized basis sets on the CP-corrected PES,although the calculated O...O distances were less well reproduced with moderate sized basis sets.We calculated the CP using the procedure where each fragment is calculated in the basis if the entire aggregate.The results show this procedure to be well-behaved,as the normal and CP-optimized calculations converged systematically to the same values as the basis set improved for all four methods used.The advantages of this practice over a proposed hierarchical procedure for calculating the CP are discussed.A misconception about the supposed superiority of the latter procedure is remedied.
机译:使用Hartree-Fock(HF),二阶M011er-Plesset(MP2)和两种密度泛函理论(DFT)方法B3PW91和B3LYP计算水二聚体以及三聚体和四聚体比较每个在正态和反平衡(CP)校正的势能面(PES)上计算出的相互作用能和O ... O距离,作为基础质量的函数(以最佳水单体的能量测量)四种方法中的HF和DFT程序都可以合理地快速转换为相互作用能和O ... O距离的大基集值。即使是适度基集也可以用于获得与优化时外推值相似的结果在CP校正的PES上执行。对于MP2,这些能量和距离收敛到外推值的速度要慢得多。即使对于使用的最佳基准集(aug-cc-pVQz和aug- cc-pVTZ)。甚至,在CP校正的PES上,也可以在中等大小的基础集上复制外推的MP2交互作用能量,尽管在中等大小的基础集上所计算出的O ... O距离再现性较差。每个片段都以整个聚集为基础进行计算。结果表明,此过程是正确的,因为常规和CP优化的计算系统地收敛到与所使用的所有四种方法改进的基础集相同的值。讨论了此实践对提议的用于计算CP的分层过程的影响。纠正了对后者过程假定的优越性的误解。

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