Iron Mineralogy in Sediments. a Mössbauer Study

Author

J. Hilton
Gary J. Long, Missouri University of Science and TechnologyFollow
J. S. Chapman
J. P. Lishman

Abstract

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.

Recommended Citation

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

Department(s)

Chemistry

International Standard Serial Number (ISSN)

0016-7037

Document Type

Article - Journal

Document Version

Citation

File Type

text

Language(s)

English

Rights

© 1986 Elsevier, All rights reserved.

Publication Date

01 Jan 1986