Mössbauer spectroscopic studies of iron in organic material from natural sedimentary environments

Details Mössbauer spectroscopic studies of iron in organic material from natural sedimentary environments Mössbauer spectroscopic studies of iron in organic material from natural sedimentary environments

Sep 1979

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1979gecoa..43.1449d&link_type=abstract

Geochimica et Cosmochimica Acta, vol. 43, Issue 9, pp.1449-1453

Physics

3

Scientific paper

57 Fe Mössbauer spectra have been obtained from samples of humic acid, fulvic acid and kerogen and from the organic material extracted from bituminous chalk with benzene-methanol. The spectra indicate that iron occurs in a trivalent form in the silicate residue of the humic acid fraction, as hydrated ferrous ions associated with the fulvic acid fraction, as pyrite in kerogen and in a form not detectable by Mössbauer spectroscopy in the benzene-methanol extract.

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