The apatite-type compound, penta-strontium tris-[arsenate(V)] chloride, Sr(5)(AsO(4))(3)Cl, has been synthesized by ion exchange at high temperature from a synthetic sample of mimetite [Pb(5)(AsO(4))(3)Cl] with SrCO(3) as a by-product. The results of the Rietveld refinement, based on high resolution synchrotron X-ray powder diffraction data, show that the title compound crystallizes in the same structure as other halogenoapatites with general formula A(5)(YO(4))(3)X (A = divalent cation, Y = penta-valent cation, and X = F, Cl or Br) in the space group P6(3)/m. The structure consists of isolated tetra-hedral AsO(4) (3-) anions (the As atom and two O atoms have m symmetry), separated by two crystallographically independent Sr(2+) cations that are located on mirror planes and threefold rotation axes, respectively. One Sr atom is coordinated by nine O atoms and the other by six. The chloride anions (site symmetry ) are at the 2a sites and are located in the channels of the structure.
The apatite-type compound, penta-strontium tris-[arsenate(V)] chloride, Sr(5)(AsO(4))(3)Cl, has been synthesized by ion exchange at high temperature from a synthetic sample of mimetite [Pb(5)(AsO(4))(3)Cl] with SrCO(3)as a by-product. The results of the Rietveld refinement, based on high resolution synchrotron X-ray powder diffraction data, show that the title compound crystallizes in the same structure as other halogenoapatites with general formula A(5)(YO(4))(3)X (A = divalent cation, Y = penta-valent cation, and X = F, Cl or Br) in the space group P6(3)/m. The structure consists of isolated tetra-hedral AsO(4) (3-) anions (the As atom and two O atoms have m symmetry), separated by two crystallographically independent Sr(2+) cations that are located on mirror planes and threefold rotation axes, respectively. One Sr atom is coordinated by nine O atoms and the other by six. The chloride anions (site symmetry ) are at the 2a sites and are located in the channels of the structure.
For crystal chemistry of apatites, see: Mercier et al. (2005 ▶); White & ZhiLi (2003 ▶); Wu et al. (2003 ▶). For powder diffraction data on SrAs-apatite, see: Kreidler & Hummel (1970 ▶). Atomic coordinates as starting parameters for the Rietveld (Rietveld, 1969 ▶) refinement of the present phases were taken from Bell et al. (2008 ▶); Dai et al. (1991 ▶); de Villiers et al. (1971 ▶). For related Sr—Cl-apatites, see: Đordević et al. (2008 ▶); Sudarsanan & Young, (1974 ▶, 1980 ▶); Beck et al. (2006 ▶); Noetzold et al. (1995 ▶); Noetzold & Wulff (1996 ▶, 1997 ▶, 1998 ▶); Swafford & Holt (2002 ▶); Wardojo & Hwu (1996 ▶). For synthetic work, see: Baker (1966 ▶); Essington (1988 ▶); Harrison et al. (2002 ▶).
In-house design diffractometerSpecimen mounting: capillarySpecimen mounted in transmission modeScan method: stepAbsorption correction: fixed at 02θmin = 2, 2θmax = 60°Increment in 2θ = 0.01°
Refinement
R
p = 0.052R
wp = 0.066R
exp = 0.047R
B = 0.090S = 2.00Excluded region(s): 2-6° 2θProfile function: Pseudo Voigt225 reflections16 parametersPreferred orientation correction: noneData collection: local software; cell refinement: CELREF (Laugier & Bochu, 2003 ▶) and GSAS (Larson & Von Dreele (2004 ▶); data reduction: local software; method used to solve structure: coordinates taken from a related compound; program(s) used to refine structure: GSAS and EXPGUI (Toby, 2001 ▶); molecular graphics: VESTA (Momma & Izumi, 2008 ▶); software used to prepare material for publication: publCIF (Westrip, 2009 ▶).Crystal structure: contains datablocks global, I. DOI: 10.1107/S1600536809005054/br2096sup1.cifRietveld powder data: contains datablocks I. DOI: 10.1107/S1600536809005054/br2096Isup2.rtvAdditional supplementary materials: crystallographic information; 3D view; checkCIF report
Sr5(AsO4)3Cl
Dx = 4.510 (1) Mg m−3
Mr = 890.31
Synchrotron radiation, λ = 0.998043 Å
Hexagonal, P63/m
T = 298 K
a = 10.1969 (1) Å
Particle morphology: powder
c = 7.28108 (9) Å
white
V = 655.63 (2) Å3
cylinder, 40 × 0.7 mm
Z = 2
Specimen preparation: Prepared at 1258 K and 100 kPa
In-house design diffractometer
Data collection mode: transmission
Radiation source: Synchrotron
Scan method: step
Si(111) channel-cut crystal
2θmin = 6°, 2θmax = 60°, 2θstep = 0.01°
Specimen mounting: capillary
Rp = 0.052
Profile function: Pseudo Voigt
Rwp = 0.066
16 parameters
Rexp = 0.047
0 restraints
RBragg = 0.090
4 constraints
R(F2) = 0.33148
(Δ/σ)max = 0.001
χ2 = 3.992
Background function: Cosine Fourier Series
5801 data points
Preferred orientation correction: None
Excluded region(s): 2-6° 2θ
Experimental. Absorption correction fixed at zero, all attempts to refine this term in GSAS
were unsuccessful so this term was fixed at zero.
CELREF was used for initial lattice parameter determinations before Rietveld
refinement. Lattice parameters from GSAS refinement are quoted in the paper.
Authors: Patrick H J Mercier; Yvon Le Page; Pamela S Whitfield; Lyndon D Mitchell; Isobel J Davidson; T J White Journal: Acta Crystallogr B Date: 2005-11-14
Authors: Anthony M T Bell; C Michael B Henderson; Richard F Wendlandt; Wendy J Harrison Journal: Acta Crystallogr Sect E Struct Rep Online Date: 2008-08-23