Mössbauer Spectroscopy Applied to Magnetism and Materials Science 1996
DOI: 10.1007/978-1-4899-1763-8_9
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Mössbauer Spectral Studies of Natural Substituted Spinels

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Cited by 11 publications
(2 citation statements)
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“…FeAl2O4 is a mixed oxide normal spinel, where one eighth of the tetrahedral sites is occupied by Fe 2+ cations and one half of the octahedral sites are occupied by Al 3+ cations. Sometimes, depending on the synthetic process, the Fe 2+ cations can also occupy octahedral sites [21].…”
Section: Introductionmentioning
confidence: 99%
“…FeAl2O4 is a mixed oxide normal spinel, where one eighth of the tetrahedral sites is occupied by Fe 2+ cations and one half of the octahedral sites are occupied by Al 3+ cations. Sometimes, depending on the synthetic process, the Fe 2+ cations can also occupy octahedral sites [21].…”
Section: Introductionmentioning
confidence: 99%
“…This formula describes the spinel compound with normal cation distribution which means that all the divalent cations occupy tetrahedral sites (T d ), whereas all the trivalent cations are located in the octahedral environment (O h ) [1]. However, the intersite exchange of the cations is possible, for example hercynite crystal lattice commonly contains Fe 3+ cations in the O h sites as a result of the formation process [2][3][4]. Furthermore, Al 3+ ion occurrence in T d sites is also feasible.…”
Section: Introductionmentioning
confidence: 99%