Na2Ca2(P2O7)F-2, the first diphosphate of the cuspidine family

Citation
A. Piotrowski et al., Na2Ca2(P2O7)F-2, the first diphosphate of the cuspidine family, AM MINERAL, 85(10), 2000, pp. 1534-1539
Citations number
14
Categorie Soggetti
Earth Sciences
Journal title
AMERICAN MINERALOGIST
ISSN journal
0003004X → ACNP
Volume
85
Issue
10
Year of publication
2000
Pages
1534 - 1539
Database
ISI
SICI code
0003-004X(200010)85:10<1534:NTFDOT>2.0.ZU;2-D
Abstract
The crystal structure of synthetic Na2Ca2(P2O7)F-2 was solved from single c rystal X-ray diffraction data and refined to R = 4.31% for 1234 independent reflections [I>2 sigma(I)]. The compound is monoclinic with space group sy mmetry P2(l)/n, a = 10.8730(21) Angstrom, b = 10.5516(25) Angstrom, c = 7.4 287(13) Angstrom, and beta = 109.74(2)degrees and twinned by pseudo-merohed ry with m((100)) as the plane of twinning which was accounted for in the re finement calculations. The crystal belongs to the structure family of the m ineral cuspidine and represents the first phosphate member of this group. T he structure is characterized by ribbons of four MX6-octahedra (M = Na,Ca; X = O,F) running parallel to c. Within a single ribbon the octahedra are li nked by edge-sharing, whereas two adjacent ribbons are connected via common corners. Further linkage results from the diphosphate groups, sharing each of the six equatorial oxygen atoms with adjacent octahedral ribbons. Using the modular description usually applied for the classification of cuspidin e type structures the present compound belongs to the so called type 5 and is the first representative of this class.