Crystal structure of Rb2Mn3(H2O)2[P2O7]2, a new representative of the family of hydrated diphosphates
- Авторлар: Kiriukhina G.V.1, Yakubovich O.V.1,2, Dimitrova O.V.1, Volkov A.S.1
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Мекемелер:
- Faculty of Geology
- Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Biochemistry
- Шығарылым: Том 61, № 5 (2016)
- Беттер: 796-804
- Бөлім: Structure of Inorganic Compounds
- URL: https://journals.rcsi.science/1063-7745/article/view/190287
- DOI: https://doi.org/10.1134/S1063774516050084
- ID: 190287
Дәйексөз келтіру
Аннотация
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.
Авторлар туралы
G. Kiriukhina
Faculty of Geology
Хат алмасуға жауапты Автор.
Email: g-biralo@yandex.ru
Ресей, Moscow, 119992
O. Yakubovich
Faculty of Geology; Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Biochemistry
Email: g-biralo@yandex.ru
Ресей, Moscow, 119992; Staromonetnyi per. 35, Moscow, 119017
O. Dimitrova
Faculty of Geology
Email: g-biralo@yandex.ru
Ресей, Moscow, 119992
A. Volkov
Faculty of Geology
Email: g-biralo@yandex.ru
Ресей, Moscow, 119992
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