The structure of reyerite, (Na,K)2Ca14Si22Al2O58(OH)8.6H2O
- 1 April 1988
- journal article
- Published by Mineralogical Society in Mineralogical Magazine
- Vol. 52 (365) , 247-255
- https://doi.org/10.1180/minmag.1988.052.365.12
Abstract
The crystal structure of reyerite, (Na,K)2Ca14Si22Al2O58(OH)8.6H2O, Z = 1, was refined in the space group P, a = 9.765, c = 19.067Å, to R = 0.064 for 1540 reflections. The structure is composed of the following structural units: (a) tetrahedral sheets S1, with composition (Si8O20)8−, characterized by six-membered rings of tetrahedra; (b) tetrahedral sheets S2, characterized by six-membered rings of tetrahedra, with six tetrahedra pointing in one direction and two pointing in the other direction—the apical oxygens of these two tetrahedra connect two inversion-related S2 sheets to build double sheets, with composition (Si14Al2O38)14− and ordered distribution of aluminum cations; (c) sheets O of edge-sharing calcium octahedra. The various structural units are connected through corner sharing according to the schematic sequence ……; the corresponding composition is [Ca14Si22Al2O58(OH)8]2−. The charge balance is restored by alkali cations which are placed, together with water molecules, in the cavities of the structure at the level of the double tetrahedral sheet.Keywords
This publication has 4 references indexed in Scilit:
- Truscottite: composition and ionic substitutionsMineralogical Magazine, 1979
- Recent developments in analytical electron microscopyJournal of Microscopy, 1973
- New Tetrahedral Sheets in ReyeriteNature Physical Science, 1972
- Calcium-phyllosilikateThe Science of Nature, 1958