Ferenczy György G, Adams William H
Department of Inorganic and Analytical Chemistry, Budapest University of Technology and Economics, H-1111 Budapest, Hungary.
J Chem Phys. 2009 Apr 7;130(13):134108. doi: 10.1063/1.3096690.
We derive a local basis equation which may be used to determine the orbitals of a group of electrons in a system when the orbitals of that group are represented by a group basis set, i.e., not the basis set one would normally use but a subset suited to a specific electronic group. The group orbitals determined by the local basis equation minimize the energy of a system when a group basis set is used and the orbitals of other groups are frozen. In contrast, under the constraint of a group basis set, the group orbitals satisfying the Huzinaga equation do not minimize the energy. In a test of the local basis equation on HCl, the group basis set included only 12 of the 21 functions in a basis set one might ordinarily use, but the calculated active orbital energies were within 0.001 hartree of the values obtained by solving the Hartree-Fock-Roothaan (HFR) equation using all 21 basis functions. The total energy found was just 0.003 hartree higher than the HFR value. The errors with the group basis set approximation to the Huzinaga equation were larger by over two orders of magnitude. Similar results were obtained for PCl(3) with the group basis approximation. Retaining more basis functions allows an even higher accuracy as shown by the perfect reproduction of the HFR energy of HCl with 16 out of 21 basis functions in the valence basis set. When the core basis set was also truncated then no additional error was introduced in the calculations performed for HCl with various basis sets. The same calculations with fixed core orbitals taken from isolated heavy atoms added a small error of about 10(-4) hartree. This offers a practical way to calculate wave functions with predetermined fixed core and reduced base valence orbitals at reduced computational costs. The local basis equation can also be used to combine the above approximations with the assignment of local basis sets to groups of localized valence molecular orbitals and to derive a priori localized orbitals. An appropriately chosen localization and basis set assignment allowed a reproduction of the energy of n-hexane with an error of 10(-5) hartree, while the energy difference between its two conformers was reproduced with a similar accuracy for several combinations of localizations and basis set assignments. These calculations include localized orbitals extending to 4-5 heavy atoms and thus they require to solve reduced dimension secular equations. The dimensions are not expected to increase with increasing system size and thus the local basis equation may find use in linear scaling electronic structure calculations.
我们推导了一个局部基方程,当一组电子的轨道由群基集表示时,该方程可用于确定系统中这组电子的轨道,即不是通常使用的基集,而是适合特定电子基团的子集。当使用群基集且其他基团的轨道被冻结时,由局部基方程确定的群轨道使系统能量最小化。相比之下,在群基集的约束下,满足胡齐纳加方程的群轨道并不能使能量最小化。在对HCl进行的局部基方程测试中,群基集在通常可能使用的基集中的21个函数中只包含了12个,但计算得到的活性轨道能量与使用所有21个基函数求解哈特里 - 福克 - 罗特汉(HFR)方程得到的值相差在0.001哈特里以内。得到的总能量仅比HFR值高0.003哈特里。群基集近似胡齐纳加方程时的误差要大两个数量级以上。对于PCl(3)采用群基近似也得到了类似的结果。保留更多的基函数可以实现更高的精度,如使用价基集中21个基函数中的16个就能完美重现HCl的HFR能量所示。当核心基集也被截断时,对HCl使用各种基集进行的计算中不会引入额外的误差。对从孤立重原子获取的固定核心轨道进行相同的计算会增加约10^(-4)哈特里的小误差。这提供了一种以降低的计算成本计算具有预定固定核心和简化价轨道的波函数的实用方法。局部基方程还可用于将上述近似与将局部基集分配给局部化价分子轨道组相结合,并推导先验局部化轨道。适当选择的局部化和基集分配能够以10^(-5)哈特里的误差重现正己烷的能量,同时对于几种局部化和基集分配的组合,其两种构象之间的能量差也能以类似的精度重现。这些计算包括延伸到4 - 5个重原子的局部化轨道,因此需要求解降维久期方程。预计维度不会随着系统尺寸的增加而增加,因此局部基方程可能在线性缩放电子结构计算中有用。