Treatment of core electrons is controlled by N_FROZEN_CORE. Starting from Q-Chem version 5.0, the core electrons are frozen by default in most post-Hartree–Fock calculations. Selected virtual orbitals can also be frozen by using N_FROZEN_VIRTUAL keyword (the default for this is zero).
The number of core electrons in an atom is relatively well-defined, and
consists of certain atomic shells. (Note that ECPs are available in both
“small-core” and “large-core” varieties; see Chapter 8.9.)
For example, in phosphorus the core consists of 1, 2,
and 2 shells, for a total of ten electrons. In molecular systems, the core
electrons are usually chosen as those occupying the lowest energy
orbitals, where is the number of core electrons in the constituent atoms.
In some cases, particularly in the lower parts of the periodic table, this
definition is inappropriate and can lead to significant errors in the
correlation energy. Vitaly Rassolov has implemented an alternative definition
of core electrons within Q-Chem which is based on a Mulliken population
analysis, and which addresses this problem.
Chem. Phys. Lett.
(2001), 350, pp. 573.
The current implementation is restricted to n-kl type basis sets such as 3-21 or 6-31, and related bases such as 6-31+G(d). There are essentially two cases to consider, the outermost 6G functions (or 3G in the case of the 3-21G basis set) for Na, Mg, K and Ca, and the 3d functions for the elements Ga—Kr. Whether or not these are treated as core or valence is determined by the CORE_CHARACTER $rem, as summarized in Table 6.1.
|CORE_CHARACTER||Outermost 6G (3G)||3d (Ga–Kr)|
|for Na, Mg, K, Ca|
Note: The default setting (N_FROZEN_CORE=FC) does not work correctly in QM/MM calculations. One should specify the number of frozen core orbitals explicitly.