STRUCTURE DETERMINATION OF CA3HFSI2O9 AND CA3ZRSI2O9 FROM POWDER DIFFRACTION

Citation
Jr. Plaisier et al., STRUCTURE DETERMINATION OF CA3HFSI2O9 AND CA3ZRSI2O9 FROM POWDER DIFFRACTION, Journal of solid state chemistry, 115(2), 1995, pp. 464-468
Citations number
20
Categorie Soggetti
Chemistry Inorganic & Nuclear","Chemistry Physical
ISSN journal
00224596
Volume
115
Issue
2
Year of publication
1995
Pages
464 - 468
Database
ISI
SICI code
0022-4596(1995)115:2<464:SDOCAC>2.0.ZU;2-I
Abstract
The crystal structure of Ca3HfSi2O9 has been determined from X-ray pow der diffraction data using a recently developed software package in or der to find individual intensities from overlapping reflections. The H f atoms were found from the Patterson map, while Ca atoms were found i n a subsequent heavy atom Fourier map. The other atoms were determined by trial and error using the Rietveld method. The atomic parameters f or Ca3ZrSi2O9 were determined from neutron powder diffraction data wit h the structure of Ca3HfSi2O9 use as the trial model. Ca3HfSi2O9, a = 7.3517(4) Angstrom, b = 10.1489(11) Angstrom, c = 10.4319(12) Angstrom , beta = 91.084(7)degrees, P2(1)/c, and Z = 4; Ca3ZrSi2O9, a = 7.3603( 1) Angstrom, b = 10.1766(3) Angstrom, c = 10.4514(3) Angstrom, beta = 90.875(2)degrees, P2(1)/c, and Z = 4. The structure contains ribbons o f edge-sharing octahedra parallel to [100]. The structure of these com pounds is nearly the same as that of BeY2O4, substituting Si2O groups for 2 Be and doubling the a-axis. The mineral cuspidine (Ca4Si2O7(F,OH )(2)) has a very similar structure as well. (C) 1995 Academic Press, I nc.