Mossbauer characterization of iron oxides and (oxy)hydroxides : the present state of the art.
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2000
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Abstract
M¨ossbauer spectroscopy is a powerful direct technique for the identification and quantification
of iron oxides and (oxy)hydroxides in soils and sediments. However, further
characterization with respect to structural properties such as crystallinity, Al substitution,
stoichiometry, water content, etc. is rather limited. With some examples of synthetic and
natural goethite and hematite sample series it is illustrated that the hyperfine parameters depend
on much more structural features than the Al content and crystallinity alone. Neither
the Morin transition in hematite nor the Verwey transition in magnetite is directly applicable
for analytical purposes in natural samples.
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VANDENBERGHE, R. E. et al. Mossbauer characterization of iron oxides and (oxy)hydroxides: the present state of the art. Hyperfine Interactions, v. 126, n.1-4, p. 247-259, 2000. Disponível em: <https://link.springer.com/article/10.1023/A:1012603603203>. Acesso em: 20 abr. 2017.