Abstract
Some particular results of investigations employing Mossbauer spectroscopy are considered so as to show for the first time that it is necessary to take into account a broad class of physical factors for the correct interpretation of asymmetric shapes of lines in the spectra of model FeCl3-(FeCl3 · nH2O solution)-clay mineral systems used for the description of soil-mineral systems of the Earth and some soils of Mars. The proposed methods are effective in the study of physicochemical processes in multicomponent natural media.
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