The vibrational structure in electron detachment spectra is calculated using a formalism recently developed. In this formalism only data from the molecule are used; no data of the ion are required. The vibrational structure in the photoelectron (PE) spectrum of Hz0 is well reproduced using only the
On the use of koopmans' theorem to estimate negative electron affinities
β Scribed by N. Heinrich; W. Koch; G. Frenking
- Publisher
- Elsevier Science
- Year
- 1986
- Tongue
- English
- Weight
- 430 KB
- Volume
- 124
- Category
- Article
- ISSN
- 0009-2614
No coin nor oath required. For personal study only.
β¦ Synopsis
For 26 molecules the experimentally determined negative electron affinities resulting from electron transmission spectroscopy are compared to the theoretically determined eigenvalues of the lowest unoccupied molecular orbitals ( eLUMo) of the neutral compounds, and to the eigenvalues of the highest occupied molecular orbitals (c "oMo) of the respective anion. With the 3-21G and 6-31G* basis sets, the eLUMo values are found to give qualitatively correct correlations in most, but not all, cases for molecules with similar structures. The eHoMo data of the anions show a much poorer agreement with experimentally established trends. The inclusion of diffuse functions in the 6-31+G* basis set leads to a complete breakdown in the correlation of experimental and theoretical data.
π SIMILAR VOLUMES
## Abstract Genomeβwide association studies may be necessary to identify genes underlying certain complex diseases. Because such studies can be extremely expensive, DNA pooling has been introduced, as it may greatly reduce the genotyping burden. Parallel to DNA pooling developments, the importance
## Publio He& h 'The negative binomial distribution (N.B.) was previously proposed ( B E N N E ~, 1981) in the estimation of and testa of significance for the relative risk ( y ) in proepective studies in epidemiology. This paper discusses the application of the N.B. model in combining estimates o
The estimation of erosion and sediment delivery rates in tropical mountain watersheds is dicult and most of the methods widely used for estimating soil erosion over large areas have serious limitations. The 137 Cs approach has potential for quantifying soil erosion because it can provide retrospecti