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ANO-R 基组。

The ANO-R Basis Set.

机构信息

Division of Theoretical Chemistry, Kemicentrum , Lund University , P.O. Box 124, SE-221 00 Lund , Sweden.

出版信息

J Chem Theory Comput. 2020 Jan 14;16(1):278-294. doi: 10.1021/acs.jctc.9b00873. Epub 2019 Dec 4.

Abstract

In this work, the new ANO-R basis set for all elements of the first six periods is introduced. The ANO-R basis set is an all-electron basis set that was constructed including scalar-relativistic effects of the exact-two component (X2C) Hamiltonian and modeling the atomic nucleus by a Gaussian charge distribution, which makes the basis set suitable for calculations of both light and heavy elements. For high accuracy, it takes advantage of the general contraction scheme and was developed at the CASSCF/CASPT2 level of theory. The distinguishing feature of the ANO-R basis set is its compactness in terms of both primitive and contracted basis functions, thus containing no superfluous functions for a given quality. An optimum number of primitive basis functions was selected based on studying the convergence toward the complete basis set limit for each element individually. The primitive basis sets were then contracted using the density-averaged atomic-natural-orbital (ANO) scheme, and suitable contraction levels were determined solely based on the natural orbital occupation numbers that describe the contribution of each natural orbital to the one-particle density matrix. Rather than following the common "split-valence -tuple zeta plus polarization functions" structure, the resulting basis sets ANO-R0 to ANO-R3 possess a unique composition for each element, ensuring that no unnecessary functions are included while the basis sets are still balanced across the first six periods (H-Rn).

摘要

在这项工作中,引入了用于前六周期所有元素的新的ANO-R 基组。ANO-R 基组是一个全电子基组,它包括精确双分量(X2C)哈密顿量的标量相对论效应,并通过高斯电荷分布来模拟原子核,这使得基组适合于轻元素和重元素的计算。为了获得高精度,它利用了通用收缩方案,并在 CASSCF/CASPT2 理论水平上进行了开发。ANO-R 基组的一个显著特点是其在原始和收缩基函数方面都很紧凑,因此对于给定的质量,没有多余的函数。根据每个元素的完全基组极限的收敛性研究,选择了最佳数量的原始基函数。然后使用密度平均原子自然轨道(ANO)方案对原始基组进行收缩,并仅根据描述每个自然轨道对单粒子密度矩阵的贡献的自然轨道占据数来确定合适的收缩水平。ANO-R0 到 ANO-R3 的基组没有遵循常见的“分裂价 - 元组 zeta 加极化函数”结构,而是为每个元素具有独特的组成,确保在基组仍然在第一到第六周期(H-Rn)之间保持平衡的同时,不会包含不必要的函数。

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