Absorption line shape of electron spin resonance in metals

1975 ◽  
Author(s):  
H. S. Jarrett ◽  
J. E. Gulley ◽  
P. C. Hoell
Clay Minerals ◽  
1985 ◽  
Vol 20 (3) ◽  
pp. 281-290 ◽  
Author(s):  
C. Crăciun ◽  
Aurelia Meghea

AbstractSixteen montmorillonites (8 normal and 8 abnormal using DTA dehydroxylation criteria) from the Gurasada bentonite deposits, Romania, were investigated by ESR. The spectra showed two features: a g = 4·3 signal attributed to isolated Fe3+ ions and a broad resonance with g ∼ 2·0 which was interpreted as arising from exchange interactions between clusters of Fe3+ ions. Additional experiments suggested that the latter resonance could have a structural component. The line-shape of the two resonances varied between normal and abnormal montmorillonites, indicating that the distribution of the Fe3+ ions between internal phase (montmorillonite lattice) and external phase (montmorillonite surface) was different for the two varieties.


1977 ◽  
Vol 40 (1) ◽  
pp. K53-K55 ◽  
Author(s):  
G. O. Berim ◽  
F. G. Cherkasov ◽  
E. G. Kharakhashyan ◽  
Y. I. Talanov

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