Next: 3.2 Potential Energy Surfaces
Up: 3. Results and Discussion
Previous: 3. Results and Discussion
3.1 Single-point Calculations
Using the methods described in Section 2, single-point calculations
were done for various diatomic systems in the vicinity of the equilibrium
geometry using basis sets of varying sizes. In the table below we compare the
relative quality of full core and frozen core results with the validity of
criterion (8) averaged over the different basis sets.
For each molecule except Hydrogen we refer to two tables, the first for full core
and the second for frozen core data.
System |
Table |
Criterion (8) |
Errors wrt. CCSD(T) |
B2 |
1, 2 |
not satisfied |
large |
BH |
3, 4 |
well satisfied |
small |
C2 |
5, 6 |
not satisfied |
large |
F2 |
7, 8 |
satisfied |
acceptable |
H2 |
9 |
well satified |
small |
HF |
10, 11 |
well satified |
small |
N2 |
12, 13 |
sometimes satisfied |
acceptable or large |
NH2 - |
14, 15 |
sometimes satisfied |
acceptable or large |
OH- |
16, 17 |
mostly satisfied |
small or acceptable |
From the data presented in these tables, the following conclusions may be drawn
- Criterion (8) gives good guidance, for which system and
with which basis set the perturbation-derived methods yield good or acceptable
errors wrt. to CCSD(T) calculations with the same basis set that are more expensive
than MP4 calculations. It
also seems to help to identify cases like
N2 for which single-reference
methods are problematic.
- The 2 estimator produces in many cases the best energies. This holds
especially for basis sets of double zeta and valence double zeta quality. Adding
polarization functions is not always improving the (relative) performance.
- For basis sets containing diffuse functions, the F4 estimator seems to be
preferable to the 2 estimator.
These conclusions seem to be valid for both frozen core
and full core calculations.
Next: 3.2 Potential Energy Surfaces
Up: 3. Results and Discussion
Previous: 3. Results and Discussion
Herbert H. H. Homeier (herbert.homeier@na-net.ornl.gov)