Behavior of Catapleiite under Heating and Crystal Structure of its High-Temperature Transformation Product, a New Phase Na6Zr3[Si9O27] with Nine-membered Rings of SiO4 Tetrahedra
- Авторы: Ksenofontov D.A.1, Grebenev V.V.2, Zubkova N.V.1, Pekov I.V.1,3, Kabalov Y.K.1, Chukanov N.V.4, Pushcharovsky D.Y.1, Artamonova A.A.1
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Учреждения:
- Geological Faculty, Moscow State University
- Institute of Crystallography of Federal Research Center “Crystallography and Photonics”
- Institute of Geochemistry and Analytical Chemistry, Russian Academy of Sciences
- Institute of Problems of Chemical Physics, Russian Academy of Sciences
- Выпуск: Том 61, № 7 (2019)
- Страницы: 696-705
- Раздел: Mineral Crystallography
- URL: https://journal-vniispk.ru/1075-7015/article/view/215578
- DOI: https://doi.org/10.1134/S1075701519070080
- ID: 215578
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Аннотация
Thermal behavior of catapleiite, ideally Na2ZrSi3O9 ⋅ 2H2O, has been investigated with the X-ray diffraction, electroconductivity measurements using impedance spectroscopy, dynamic scanning calorimetry, thermal gravimetry, and infrared spectroscopy. The high-temperature transformation product of catapleiite obtained after annealing of catapleiite at 1000°C has been studied. This is a new microporous zirconosilicate, ideally Na6Zr3[Si9O27], representing a new structural type. It is hexagonal, P63/mcm, a = 11.5901(9), c = 9.9546(9) Å, V = 1158.05(16) Å3. Its crystal structure model has been obtained using single-crystal X-ray diffraction data and refined by the Rietveld method on the basis of the powder X-ray diffraction data (R = 3.87%). The structure is based on the heteropolyhedral framework, which substantially differs from that of catapleiite and is built by nine-member rings Si9O27 formed by SiO4 tetrahedra linked with isolated ZrO6 octahedra. Extraframework Na cations are located in broad channels of the framework and between the tetrahedral Si9O27 rings.
Об авторах
D. Ksenofontov
Geological Faculty, Moscow State University
Автор, ответственный за переписку.
Email: ksen53@gmail.com
Россия, Moscow, 119991
V. Grebenev
Institute of Crystallography of Federal Research Center “Crystallography and Photonics”
Email: igorpekov@mail.ru
Россия, Moscow, 119333
N. Zubkova
Geological Faculty, Moscow State University
Email: igorpekov@mail.ru
Россия, Moscow, 119991
I. Pekov
Geological Faculty, Moscow State University; Institute of Geochemistry and Analytical Chemistry, Russian Academy of Sciences
Автор, ответственный за переписку.
Email: igorpekov@mail.ru
Россия, Moscow, 119991; Moscow, 117975
Yu. Kabalov
Geological Faculty, Moscow State University
Email: igorpekov@mail.ru
Россия, Moscow, 119991
N. Chukanov
Institute of Problems of Chemical Physics, Russian Academy of Sciences
Email: igorpekov@mail.ru
Россия, Chernogolovka, Moscow oblast, 142432
D. Pushcharovsky
Geological Faculty, Moscow State University
Email: igorpekov@mail.ru
Россия, Moscow, 119991
A. Artamonova
Geological Faculty, Moscow State University
Email: igorpekov@mail.ru
Россия, Moscow, 119991
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