A magnetic and neutron diffraction study of the Fe2O3-V2O3 system∗

Cox, D. E.; Takei, W. J.; Miller, R. C.; Shirane, G.

doi:10.1016/0022-3697(62)90143-9

Cited by 59 publications

(21 citation statements)

References 26 publications

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“…Loffler and Mader, 2006), which has a hexagonal structure with space group R 3c (Cox et al, 1962). The oxygen ions are approximately in a hexagonal close-packing arrangement, where the Fe(III) ions are located between the O layers and octahedrally coordinated to six O atoms (Fig.…”

Section: Hematite A-fe 2 Omentioning

confidence: 99%

Surface simulation studies of the hydration of white rust Fe(OH)2, goethite α-FeO(OH) and hematite α-Fe2O3

Leeuw

Cooper

2007

Geochimica et Cosmochimica Acta

108

106

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Section: Hematite A-fe 2 Omentioning

confidence: 99%

Surface simulation studies of the hydration of white rust Fe(OH)2, goethite α-FeO(OH) and hematite α-Fe2O3

Leeuw

Cooper

2007

Geochimica et Cosmochimica Acta

108

106

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“…So we have calculated ECoN and MEFIR for a series of these and structurally related oxides. The values for Mn 2 0 3 [25], Sc 2 0 3 [26], Y 2 0 3 [2T] as well as for A1 2 0 3 [28] and Fe 2 0 3 [29] are collected in addition. In all cases ECoN (cation/Σ) is about 6.…”

Section: Oxides Of Rare Earth Elementsmentioning

confidence: 99%

Effective coordination numbers (ECoN) and mean fictive ionic radii (MEFIR)

Hoppe¹

1979

Zeitschrift Für Kristallographie - Crystalline Materials

218

143

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Proceeding from usual ionic radii by means of exponential averaging, Mean Fictive Ionic Radii (MEFIR) are reached and with these values Effective Coordination Numbers (ECoN) are calculated. In 'classical' cases, for example for closest-packed structures, the simple counted known values are obtained. Anion-anion-contacts and in the cases of cationrich compounds that have larger cations, contacts between cations, are also considered. Such calculations, applied only to parts of crystal structures, permit the detection and testing of structural relationships.

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“…In considering the possibility of Li + ion conduction in rock saltbased oxides, there are a number of materials that have rock salt superstructures and that contain other multivalent cations in addition to Li + , for example, Li 3 NbO 4 [5], Li 2 TiO 3 [6], LiFeO 2 [7] and Li 2 CuZrO 4 [8]. The main purpose of this work is to explore a sol-gel synthetic route for the preparation of single phase Li 3 NbO 4 oxides with a cubic structure [9].…”

Section: Introductionmentioning

confidence: 99%