Crystal structure of Rb2Mn3(H2O)2[P2O7]2, a new representative of the family of hydrated diphosphates
- 作者: Kiriukhina G.V.1, Yakubovich O.V.1,2, Dimitrova O.V.1, Volkov A.S.1
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隶属关系:
- Faculty of Geology
- Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Biochemistry
- 期: 卷 61, 编号 5 (2016)
- 页面: 796-804
- 栏目: Structure of Inorganic Compounds
- URL: https://journals.rcsi.science/1063-7745/article/view/190287
- DOI: https://doi.org/10.1134/S1063774516050084
- ID: 190287
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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.
作者简介
G. Kiriukhina
Faculty of Geology
编辑信件的主要联系方式.
Email: g-biralo@yandex.ru
俄罗斯联邦, Moscow, 119992
O. Yakubovich
Faculty of Geology; Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Biochemistry
Email: g-biralo@yandex.ru
俄罗斯联邦, Moscow, 119992; Staromonetnyi per. 35, Moscow, 119017
O. Dimitrova
Faculty of Geology
Email: g-biralo@yandex.ru
俄罗斯联邦, Moscow, 119992
A. Volkov
Faculty of Geology
Email: g-biralo@yandex.ru
俄罗斯联邦, Moscow, 119992
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