Iron Mineralogy in Sediments. a Mössbauer Study
Sequential chemical extraction is used to show that the Mössbauer spectrum of a lacustrine sediment is deceptively simple. Only two pairs of doublets arise when at least four chemically distinct forms of Fe are present. Recognition of this effect increases the power of Mössbauer spectroscopy as a tool in studies of the redox chemistry of Fe in sediments. © 1986.
J. Hilton et al., "Iron Mineralogy in Sediments. a Mössbauer Study," Geochimica et Cosmochimica Acta, Elsevier, Jan 1986.
The definitive version is available at https://doi.org/10.1016/0016-7037(86)90069-4
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© 1986 Elsevier, All rights reserved.