Intermediate-coupling approach in the induced covalent bond theory of chemisorption

1981 ◽  
Vol 14 (11) ◽  
pp. 1693-1711 ◽  
Author(s):  
S Sawada
1967 ◽  
Vol 93 (2) ◽  
pp. 300-320 ◽  
Author(s):  
D.C. Choudhury ◽  
T.F. O'Dwyer

1969 ◽  
Vol 125 (1) ◽  
pp. 140-160 ◽  
Author(s):  
D.C. Choudhury ◽  
J.T. Clemens

1974 ◽  
Vol 27 (2) ◽  
pp. 289 ◽  
Author(s):  
Woon-Hyuk Chung

In recent years the nucleus 51 Y has been extensively studied, both experimentally by Horoshko et al. (1970), using the 48Ti(oc, py)51y reaction, and theoretically in terms of shell model calculations by many authors (McCullen et al. 1964; Horoshko et al. 1970; Lips and McEllistrem 1970). Mixed configuration shell model calculations by Lips and McEllistrem, in particular, have successfully reproduced the low-lying energy levels of5ly. However, strong coupling rotational model calculations by Malik and Scholz (1966) did not give satisfactory results. In the present work, the intermediate coupling unified model (Bohr and Mottelson 1953; Choudhury 1954) is applied to Sly. The purpose of this work is to show that the intermediate coupling model can successfully predict the low-lying energy levels of Sly.


Minerals ◽  
2021 ◽  
Vol 11 (11) ◽  
pp. 1215
Author(s):  
Maria Czaja ◽  
Radosław Lisiecki ◽  
Rafał Juroszek ◽  
Tomasz Krzykawski

The cause of the split of 4A4E(4G) Mn2+ excited level measured on minerals spectra is discussed. It is our view that ∆E = |4E(4G) − 4A(4G)| should be considered an important spectroscopic parameter. Among the possible reasons for the energy levels splitting taken under consideration, such as the covalent bond theory, the geometric deformation of the coordination polyhedron and the lattice site’s symmetry, the first one was found to be inappropriate. Two studied willemite samples showed that the impurities occur in one of the two available lattice sites differently in both crystals. Moreover, it was revealed that the calculated crystal field Dq parameter can indicate which of the two non-equivalent lattice sites positions in the willemite crystal structure was occupied by Mn2+. The above conclusions were confirmed by X-ray structure measurements. Significant differences were also noted in the Raman spectra of these willemites.


2012 ◽  
Vol 4 (2) ◽  
Author(s):  
Marconi B. S. Costa ◽  
Karina A. Barros
Keyword(s):  

1971 ◽  
Vol 49 (12) ◽  
pp. 1582-1588 ◽  
Author(s):  
M. Csürös ◽  
J. A. Cameron ◽  
Z. Zámori

The results of a calculation based upon the intermediate coupling approach of the unified model are presented for the low energy nuclear properties of the 53Cr isotope.


Following the formal work of the preceding paper, a method is proposed to evaluate the functional integral which has been derived for the Green function of one nucleon interacting with a pseudoscalar meson field. The method is basically that of stationary phase taken to its second approximation, and since this approximation where applicable is accurate in the limits of strong and weak coupling constants, it is assumed good in general. There are several difficulties involved in the evaluation, and as far as possible these are isolated and discussed with the aid of models each showing one difficulty alone. Combining these separate points, the evaluation of the functional integral is thereby expressed in terms of the solution of a set of coupled equations which provide a basis for a covariant intermediate coupling approach to the problem. The solution of these equations is not attempted in this paper.


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