1986
DOI: 10.1016/0304-8853(86)90844-9
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Effect of stoichiometry changes on electrical properties of magnetite

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Cited by 63 publications
(24 citation statements)
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“…The latter orbital is characterized by a very strong anisotropy of the charge and spin distribution, with the angular part stretched along the hexagonal c axis. This is 57 Fe, which is negatively proportional to the increase in the s-electron density at the Fe nucleus, usually follows a volume reduction (see Ref. [34]).…”
Section: A Case Of a Mott Transition Driven By An Increasing Crystal-mentioning
confidence: 99%
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“…The latter orbital is characterized by a very strong anisotropy of the charge and spin distribution, with the angular part stretched along the hexagonal c axis. This is 57 Fe, which is negatively proportional to the increase in the s-electron density at the Fe nucleus, usually follows a volume reduction (see Ref. [34]).…”
Section: A Case Of a Mott Transition Driven By An Increasing Crystal-mentioning
confidence: 99%
“…At ambient pressure the spins are highly frustrated between neighboring layers as well as within layers [39]. The combined high-pressure studies of CuFeO 2 using X-ray diffraction, along with 57 Fe Mössbauer and Fe and CuK-edge XAFS spectroscopy methods [40], reveal a sequence of intricate structural/electronic-magnetic pressure-induced transitions. At 18 GPa a structural transition takes place to a more isotropic C2/c structure (HP1) with the O-Cu 1þ S¼0 -O axis tilted 28°from the c axis (Fig.…”
Section: A Case Of Pressure-induced Intervalence Charge Transfermentioning
confidence: 99%
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“…The Verwey transition temperature (T V ) was found to be (122 ± 1) K [46]. Stoichiometric magnetite is expected to have a T V of around 120 K [47]. As magnetite becomes cation deficient T V decreases, and the transition eventually disappears.…”
Section: Methodsmentioning
confidence: 99%