A new form of \(\mathrm{Cu}_{3} \mathrm{Fe}_{4}\left(\mathrm{VO}_{4}\right)_{6}\), different from the mineral lyonsite, has been isolated. It is triclinic (S.G. \(\overline{P 1} ; a=6.600(3) \AA\), \(b=8.048(4) \AA, c=9.759(5) \AA, \alpha=106.08(3)^{\circ}, \beta=103.72(3)^{\circ}\), \(\left.\gamma=
Phase Formation in Cu3+1.5xR4−x(VO4)6 (R=Fe and Cr) Systems: Crystal Structure of Cu2.5Fe4.333(VO4)6, Cu4Fe3.333(VO4)6, and Cu4.05Cr3.3(VO4)6
✍ Scribed by A.A. Belik; A.P. Malakho; K.V. Pokholok; B.I. Lazoryak
- Publisher
- Elsevier Science
- Year
- 2001
- Tongue
- English
- Weight
- 320 KB
- Volume
- 156
- Category
- Article
- ISSN
- 0022-4596
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✦ Synopsis
Phase formation in the Cu 3؉1.5x R 4؊x (VO 4 ) 6 (R ؍ Fe and Cr) systems was studied at 6703C by powder X-ray di4raction. In the Cu 3؉1.5x Fe 4؊x (VO 4 ) 6 system there are two compounds having homogeneity ranges with formula Cu 3؉1.5x Fe 4؊x (VO 4 ) 6 (0.6674 x(0.778) and Cu 3؉1.5x Fe 4؊x (VO 4 ) 6 (؊0.3334x4؊0.167) with structures of mineral lyonsite and mineral howardevansite (or Fe 7 (PO 4 ) 6 ), respectively. The structures of Cu 2.5 Fe 4.333 (VO 4 ) 6 and Cu 4 Fe 3.333 (VO 4 ) 6 were re5ned by Rietveld method: space group P1 ,
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