Various aspects of the ERI evaluation problem are described in the following subsections.
The fundamental ERI , which is
the basis of all ERI algorithms, is usually represented as
420
Adv. Quantum Chem.
(1994),
25,
pp. 141.
Link
(A.3) |
which can be reduced to a one-dimensional integral of the form
(A.4) |
and can be efficiently computed using a modified Chebyshev interpolation
scheme.
415
Int. J. Quantum Chem.
(1991),
40,
pp. 745.
Link
Equation (A.4) can also be adapted for the
general case integrals required for most calculations.
Following the fundamental ERI, building up to the full bra-ket ERI (or
intermediary matrix elements, see later) are the problems of angular momentum
and contraction.
Note: Square brackets denote primitive integrals and parentheses denote fully-contracted integrals.
The fundamental integral is essentially an integral without angular momentum
(i.e., it is an integral of the type ). Angular momentum,
usually depicted by , has been problematic for efficient ERI formation,
evident in the above time line. Initially, angular momentum was calculated by
taking derivatives of the fundamental ERI with respect to one of the Cartesian
coordinates of the nuclear center. This is an extremely inefficient route, but
it works and was appropriate in the early development of ERI methods. Recursion
relations
937
J. Chem. Phys.
(1986),
84,
pp. 3963.
Link
,
938
J. Chem. Phys.
(1988),
89,
pp. 1540.
Link
and the tensor
equations
22
J. Chem. Phys.
(1997),
107,
pp. 124.
Link
are the basis for the modern approaches.
The contraction problem may be described by considering a general contracted ERI of -type functions derived from the STO-3G basis set. Each basis function has degree of contraction . Thus, the ERI may be written
(A.5) |
and requires 81 primitive integrals for the single ERI. The problem escalates dramatically for more highly contracted sets (STO-6G, 6-311G) and has been the motivation for the development of techniques for shell-pair modeling, in which a second shell-pair is constructed with fewer primitives that the first, but introduces no extra error relative to the integral threshold sought.