Yu Lan

Computational Methods in Organometallic Catalysis


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which each atomic orbital is represented by a single mathematical function. The atomic orbitals used in this procedure are represented by what is known as the basis set. Following this idea, the mathematical form of atomic orbitals should be considered, when it is used to be linear combinations for the construction of molecular orbitals. One choice would be to simply use the hydrogenic wavefunctions adapted for other atoms, which is called a Slater-type orbital (STO). These wavefunctions have radial forms possessing terms such as rn−1e−ζr (ζ = Z/n), whose function form has clear physical meaning (Scheme 2.3a). However, it is very difficult to evaluate the complex two‐electron integrals.

Schematic illustration of the combination of Gaussian-type orbitals for the construction of Slater-type orbital. (a) STO. (b) GTO. (c) The combination of GTOs.

      The minimum basis set has one basis function for every formally occupied or partially occupied orbital in the atom, which is referred to as a single‐zeta (SZ) basis set. The use of the term zeta here reflects that each basis function mimics a single STO, which is defined by its exponent, zeta (ζ). The minimum basis set is usually inadequate, failing to allow the core electrons to get close enough to the nucleus and the valence electrons to delocalize. An obvious solution is to double the size of the basis set, creating a double‐zeta (DZ) basis. Further improvement can be had by choosing a triple‐zeta (TZ) or even larger basis set [68].

      2.3.2 Pople's Basis Sets

      As most of chemistry focuses on the action of the valence electrons, Pople developed the split‐valence basis sets, single zeta in the core and double zeta in the valence region, which won him the 1998 Nobel prize in chemistry. A double‐zeta split‐valence basis set for carbon has three s basis functions and two p basis functions for a total of nine functions, a triple‐zeta split valence basis set has four s basis functions and three p functions for a total of 13 functions, and so on.

      For the vast majority of basis sets, including the split‐valence sets, the basis functions are not made up of a single Gaussian‐type function. Rather, a group of Gaussian‐type functions are contracted together to form a single basis function. An example is split‐valence basis set 6‐31G, which is popular in computational organic chemistry. In this basis set, the left value means that each core basis function comprises six Gaussian functions. Meanwhile, the valence space is split into two basis functions, which referred to the inner and outer parts of valence space. The inner basis function is composed of three contracted Gaussian‐type functions, and each outer basis function is a single Gaussian‐type function. Thus, for carbon, the core region is a single s basis function made up of six s‐GTOs. The carbon valence space has two s and two p basis functions. The inner basis functions are made up of three Gaussians, and the outer basis functions are each composed of a single Gaussian‐type function. Therefore, the carbon 6‐31G basis set has nine basis functions made up of 22 Gaussian‐type functions. This type of split‐valence basis sets involves 3‐21G, 4‐31G, 6‐31G, 6‐311G, etc. [69–72]. The accuracy of those basis sets depends mainly on the number of basis functions, and secondly on the number of Gaussians. However, the time consumed in calculation increases accordingly with the improvement of accuracy.

      A critical problem with a simple split‐valence basis set, such as 6‐31G, is that the flexibility of wavefunctions is insufficient to distort to the actual shape. Extending the basis set by including a set of functions that mimic the atomic orbitals with angular momentum one greater than in the valence space greatly improves the basis flexibility. These added basis functions are called polarization functions. For second and third periodic elements, adding polarization functions means adding a set of d GTOs; therefore, a basis set involving polarization functions for heavy atoms can be written as 6‐31G(d) or 6‐31G*. For hydrogen, polarization functions are a set of p functions. Therefore, a basis set involving polarization functions for all atoms can be written as 6‐31G(d,p) or 6‐31G**. As adding multiple sets of polarization functions has become broadly implemented, the use of asterisks has been abandoned in favor of explicit indication of the number of polarization functions within parentheses, that is, 6‐311G(2df,2p) means that two sets of d functions and a set of f functions are added to heavy atoms and two sets of p functions are added to the hydrogen atoms. The polarization functions are simply mathematical tools that allow to give the basis set more flexibility, and thus produce a better calculation.

      2.3.4 Diffuse Functions

      For anions or molecules with many adjacent lone pairs, the basis set must be augmented with diffuse functions to allow the electron density to expand into a larger volume. For split‐valence basis sets, this is designated by “+” as in 6‐31+G(d). The diffuse functions added are a full set of additional functions of the same type as are present in the valence space. So, for carbon, the diffuse functions would be an added s basis function and a set of p basis functions. If a molecule involving hydride, diffuse functions for hydrogen atom is necessary, which would be an added s basis function, the corresponding split‐valence basis set can be written as 6‐31++G(d).

      2.3.5 Correlation‐Consistent Basis Sets

      2.3.6 Pseudo