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Crystal structures of potassium-exchanged forms of catapleiite and hilairite

Journal Article · · Crystallography Reports
; ;  [1]; ;  [2];  [3]
  1. Moscow State University, Faculty of Geology (Russian Federation)
  2. University of Pisa, Department of Earth Sciences (Italy)
  3. Russian Academy of Sciences, Institute of Problems of Chemical Physics (Russian Federation)

The crystal structures of potassium-exchanged forms of catapleiite and hilairite of the compositions (K{sub 0.49}Ca{sub 0.42}Na{sub 0.26})ZrSi{sub 3}O{sub 9} . 2[(H{sub 2}O){sub 0.8}(H{sub 3}O){sub 0.2}] and K{sub 0.51}ZrSi{sub 3}O{sub 9} . 3[(H{sub 2}O){sub 0.5}K{sub 0.27}(H{sub 3}O){sub 0.23}], respectively, were studied by X-ray diffraction and IR spectroscopy. Both structures retain the heteropolyhedral frameworks of the parent minerals formed by Zr octahedra and Si tetrahedra. The K cations occupy different positions in these minerals. In K-exchanged catapleiite, K cations are located only in the position occupied by Na in the structure of the parent mineral. In the K-exchanged form of hilairite, K cations are not only involved in the Na position but also partially occupy the H{sub 2}O position.

OSTI ID:
21091393
Journal Information:
Crystallography Reports, Journal Name: Crystallography Reports Journal Issue: 1 Vol. 52; ISSN 1063-7745; ISSN CYSTE3
Country of Publication:
United States
Language:
English