Journal article
Non-stoichiometric magnetite and maghemite in the mature teeth of the chiton Acanthopleura hirtosa
Hyperfine Interactions, Vol.71(1-4), pp.1275-1278
1992
Abstract
Mature radula pieces from the chiton Acanthopleura hirtosa were studied using Mössbauer spectroscopy. The magnetite present in the radulae was found to have a distribution of Verwey transition temperatures in the range 85-100K. It was deduced that the magnetite was non-stoichiometric with an average formula Fe 2.98O 3. About 10% of the Fe in the radulae was in the form of maghemite and about 19% was in the form of paramagnetic or superparamagnetic phases.
Details
- Title
- Non-stoichiometric magnetite and maghemite in the mature teeth of the chiton Acanthopleura hirtosa
- Authors/Creators
- T.G. St Pierre (Author/Creator)L.A. Evans (Author/Creator) - Murdoch UniversityJ. Webb (Author/Creator) - Murdoch University
- Publication Details
- Hyperfine Interactions, Vol.71(1-4), pp.1275-1278
- Publisher
- Kluwer Academic Publishers
- Identifiers
- 991005545068607891
- Copyright
- © 1992 J.C. Baltzer A.G., Scientific Publishing Company
- Murdoch Affiliation
- School of Mathematical and Physical Sciences
- Language
- English
- Resource Type
- Journal article
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