Crystal structure of Na-4[Cu4O2(SO4)(4)]center dot MeCl (Me : Na, Cu, square) - the synthetic Na-analogue of piypite (caratiite)

Citation
V. Kahlenberg et al., Crystal structure of Na-4[Cu4O2(SO4)(4)]center dot MeCl (Me : Na, Cu, square) - the synthetic Na-analogue of piypite (caratiite), MINERAL MAG, 64(6), 2000, pp. 1099-1108
Citations number
15
Categorie Soggetti
Earth Sciences
Journal title
MINERALOGICAL MAGAZINE
ISSN journal
0026461X → ACNP
Volume
64
Issue
6
Year of publication
2000
Pages
1099 - 1108
Database
ISI
SICI code
0026-461X(200012)64:6<1099:CSONDM>2.0.ZU;2-J
Abstract
The crystal structure of Na-4[Cu4O2(SO4)(4)]. MeCl (Me: Na,Cu,square) has b een solved by direct methods and refined to R1 = 0.028 using 2466 independe nt reflections. The compound is tetragonal with space group P4/n, a = 18.45 1(1) Angstrom, c = 4.9520(2) Angstrom, Z = 4. The two main building units r unning parallel to the c-axis comprise: (1) slabs containing SO4 and OCu4 t etrahedra; and (2) chains of corner sharing Me(Cl,O)(6) octahedra. The disp lacement ellipsoids of the atoms occupying the Me sites and of the Cl ions indicate a short-range static disorder. Copper in the slabs exhibits a (4+1 ) coordination. Both elements form a tunnel structure in which additional N a atoms are incorporated for charge compensation. The structure is closely related to the mineral piypite (K4Cu4O2(SO4)(4). MeCl (Me: Na,Cu,square)): a approximate to root2.a(piy.); c approximate to c(piy.). Furthermore, the structure has a pronounced pseudo-translational symmetry: apart from some o f the oxygen sites, all of the nineteen crystallographically distinct posit ions are related by a pseudo F centring.