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- W2069098786 abstract "The Mossbauer spectra of the cubic spinel FeV2O4 at 298 and 193K in the paramagnetic state have been resolved into a pair of two quadrupole split sub-spectra of unequal intensities. The results have been interpreted as evidence of a partially inverse cation distribution in FeV2O4 and not as arising from a mixture of a normal and a completely inverse spinel as suggested by du Plessis (1971). The degree of inversion has been determined from the relative areas under the two sub-spectra to be 10+or-3% at 298K. This is in good agreement with the value of 8% determined from the intensities of the X-ray diffraction pattern." @default.
- W2069098786 created "2016-06-24" @default.
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- W2069098786 date "1975-02-07" @default.
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- W2069098786 title "The cation distribution in the ferrite FeV<sub>2</sub>O<sub>4</sub>:Mossbauer and X-ray diffraction studies" @default.
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- W2069098786 doi "https://doi.org/10.1088/0022-3719/8/3/015" @default.
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