Crystal structure of Rb2Mn3(H2O)2[P2O7]2, a new representative of the family of hydrated diphosphates
- Authors: Kiriukhina G.V.1, Yakubovich O.V.1,2, Dimitrova O.V.1, Volkov A.S.1
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Affiliations:
- Faculty of Geology
- Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Biochemistry
- Issue: Vol 61, No 5 (2016)
- Pages: 796-804
- Section: Structure of Inorganic Compounds
- URL: https://journals.rcsi.science/1063-7745/article/view/190287
- DOI: https://doi.org/10.1134/S1063774516050084
- ID: 190287
Cite item
Abstract
The crystal structure of Rb2Mn3(H2O)2[P2O7]2, a new phase obtained in the form of single crystals under hydrothermal conditions in the MnCl2–Rb3PO4–H2O system, is determined by X-ray diffraction (Xcalibur-S-CCD diffractometer, R = 0.0270): a = 9.374(2), b = 8.367(2), c = 9.437(2) Å, ß = 99.12(2)°, space group P21/c, Z = 2, Dx = 3.27 g/cm3. A correlation between the unit-cell parameters and the size of cations forming the crystal structures of isostructural A2M3(H2O)2[P2O7]2 diphosphates (A = K, NH4, Rb, or Na; M = Mn, Fe, Co, or Ni) is revealed. It is shown that, due to the topological similarity, the structures of diphosphates and orthophosphates of the farringtonite structural type can undergo mutual transformations.
About the authors
G. V. Kiriukhina
Faculty of Geology
Author for correspondence.
Email: g-biralo@yandex.ru
Russian Federation, Moscow, 119992
O. V. Yakubovich
Faculty of Geology; Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Biochemistry
Email: g-biralo@yandex.ru
Russian Federation, Moscow, 119992; Staromonetnyi per. 35, Moscow, 119017
O. V. Dimitrova
Faculty of Geology
Email: g-biralo@yandex.ru
Russian Federation, Moscow, 119992
A. S. Volkov
Faculty of Geology
Email: g-biralo@yandex.ru
Russian Federation, Moscow, 119992
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