Crystal structure of Rb2Mn3(H2O)2[P2O7]2, a new representative of the family of hydrated diphosphates


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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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