inorganic compounds
Scheelite-type NaDy(WO4)2
aDepartment of Physics and Chemistry, Henan Polytechnic University, Jiaozuo, Henan 454000, People's Republic of China, and bState Key Laboratory of Structural Chemistry, Fujian Institute of Research on the Structure of Matter, Chinese Academy of Sciences, Fuzhou, Fujian 350002, People's Republic of China
*Correspondence e-mail: iamzd@hpu.edu.cn
The title compound sodium dysprosium(III) bis[tungstate(VI)], NaDy(WO4)2, has been synthesized under high temperature solution growth (HTSG) conditions in air. The compound crystallizes with the scheelite structure and is composed of isolated WO4 tetrahedra ( symmetry) with one set of bond lengths and distorted [(Na/Dy)O8] dodecahedra ( symmetry; occupancy ratio Na:Dy = 1:1) with two sets of bond lengths.
Related literature
For the structures, properties and applications of alkali rare-earth bis-tungstates with general formula ARE(WO4)2 (A = alkali metal, RE = rare-earth metal), see: Perets et al. (2007); Han et al. (2002); Huang et al. (2006); Li et al. (1990). For the scheelite (CaWO4) structure, see: Sillen & Nylander (1943).
Experimental
Crystal data
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Refinement
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Data collection: CrystalClear (Rigaku, 2000); cell CrystalClear; data reduction: CrystalClear; program(s) used to solve structure: SHELXS97 (Sheldrick, 2008); program(s) used to refine structure: SHELXL97 (Sheldrick, 2008); molecular graphics: DIAMOND (Brandenburg, 2004); software used to prepare material for publication: SHELXTL (Sheldrick, 2008).
Supporting information
10.1107/S1600536809052271/wm2287sup1.cif
contains datablocks I, global. DOI:Structure factors: contains datablock I. DOI: 10.1107/S1600536809052271/wm2287Isup2.hkl
Single crystal of NaDy(WO4)2 were prepared by a high temperature solution reaction, using analytical reagents of Dy2O3, Na2CO3 and WO3 in the molar ratio of Na: Dy: W = 8:1:10. The starting mixture was finely ground in an agate mortar to ensure the best
and reactivity, and then transferred to a platinum crucible to be heated at a temperature of 773 K for 8 h. The sintered product was reground and continuously heated at 1273 K for 20 h, cooled to 673 K at a rate of 4 K/h, and then quenched to room temperature. A few light yellow and prismatically shaped crystals of the title compound were obtained.The Na1 and Dy1 atoms are in a substitutional-type disorder in the structure. Therefore the atomic position and anisotropic displacement parameters of Na1 and Dy1 atoms were constrained to be identical. In the initial least-squares
the occupancy factors of Na1 and Dy1 atoms were set to be free. The results show that the occupancy factors were close to 1:1, viz Na1: Dy1 = 0.50273: 0.49727, and were eventually fixed in a 1:1 ratio. The highest peak in the final difference is 1.55 e/Å3 from the W1 site, and the deepest hole is -1.40 e/Å3 from the Na1/Dy1 site.Data collection: CrystalClear (Rigaku, 2000); cell
CrystalClear (Rigaku, 2000); data reduction: CrystalClear (Rigaku, 2000); program(s) used to solve structure: SHELXS97 (Sheldrick, 2008); program(s) used to refine structure: SHELXL97 (Sheldrick, 2008); molecular graphics: DIAMOND (Brandenburg, 2004); software used to prepare material for publication: SHELXTL (Sheldrick, 2008).NaDy(WO4)2 | Dx = 7.186 Mg m−3 |
Mr = 681.19 | Mo Kα radiation, λ = 0.71073 Å |
Tetragonal, I41/a | Cell parameters from 405 reflections |
Hall symbol: -I 4ad | θ = 3.6–27.5° |
a = 5.2545 (5) Å | µ = 48.27 mm−1 |
c = 11.4029 (15) Å | T = 298 K |
V = 314.83 (6) Å3 | Prism, light yellow |
Z = 2 | 0.10 × 0.10 × 0.08 mm |
F(000) = 578 |
Rigaku Mercury70 diffractometer | 181 independent reflections |
Radiation source: fine-focus sealed tube | 143 reflections with I > 2σ(I) |
Graphite monochromator | Rint = 0.053 |
Detector resolution: 14.6306 pixels mm-1 | θmax = 27.5°, θmin = 4.3° |
ω scans | h = −6→6 |
Absorption correction: multi-scan (SADABS; Bruker, 1997) | k = −6→6 |
Tmin = 0.263, Tmax = 1.000 | l = −14→13 |
1128 measured reflections |
Refinement on F2 | Primary atom site location: structure-invariant direct methods |
Least-squares matrix: full | Secondary atom site location: difference Fourier map |
R[F2 > 2σ(F2)] = 0.024 | w = 1/[σ2(Fo2) + (0.0045P)2] where P = (Fo2 + 2Fc2)/3 |
wR(F2) = 0.056 | (Δ/σ)max < 0.001 |
S = 0.87 | Δρmax = 1.55 e Å−3 |
181 reflections | Δρmin = −1.40 e Å−3 |
15 parameters | Extinction correction: SHELXL97 (Sheldrick, 2008), Fc*=kFc[1+0.001xFc2λ3/sin(2θ)]-1/4 |
0 restraints | Extinction coefficient: 0.0295 (17) |
NaDy(WO4)2 | Z = 2 |
Mr = 681.19 | Mo Kα radiation |
Tetragonal, I41/a | µ = 48.27 mm−1 |
a = 5.2545 (5) Å | T = 298 K |
c = 11.4029 (15) Å | 0.10 × 0.10 × 0.08 mm |
V = 314.83 (6) Å3 |
Rigaku Mercury70 diffractometer | 181 independent reflections |
Absorption correction: multi-scan (SADABS; Bruker, 1997) | 143 reflections with I > 2σ(I) |
Tmin = 0.263, Tmax = 1.000 | Rint = 0.053 |
1128 measured reflections |
R[F2 > 2σ(F2)] = 0.024 | 15 parameters |
wR(F2) = 0.056 | 0 restraints |
S = 0.87 | Δρmax = 1.55 e Å−3 |
181 reflections | Δρmin = −1.40 e Å−3 |
Geometry. All e.s.d.'s (except the e.s.d. in the dihedral angle between two l.s. planes) are estimated using the full covariance matrix. The cell e.s.d.'s are taken into account individually in the estimation of e.s.d.'s in distances, angles and torsion angles; correlations between e.s.d.'s in cell parameters are only used when they are defined by crystal symmetry. An approximate (isotropic) treatment of cell e.s.d.'s is used for estimating e.s.d.'s involving l.s. planes. |
Refinement. Refinement of F2 against ALL reflections. The weighted R-factor wR and goodness of fit S are based on F2, conventional R-factors R are based on F, with F set to zero for negative F2. The threshold expression of F2 > σ(F2) is used only for calculating R-factors(gt) etc. and is not relevant to the choice of reflections for refinement. R-factors based on F2 are statistically about twice as large as those based on F, and R- factors based on ALL data will be even larger. |
x | y | z | Uiso*/Ueq | Occ. (<1) | |
Na1 | 0.5000 | −0.2500 | 0.1250 | 0.0068 (4) | 0.50 |
Dy1 | 0.5000 | −0.2500 | 0.1250 | 0.0068 (4) | 0.50 |
W1 | 0.0000 | 0.2500 | 0.1250 | 0.0091 (4) | |
O1 | 0.2419 (14) | 0.0977 (13) | 0.0404 (6) | 0.0187 (16) |
U11 | U22 | U33 | U12 | U13 | U23 | |
Na1 | 0.0090 (6) | 0.0090 (6) | 0.0024 (8) | 0.000 | 0.000 | 0.000 |
Dy1 | 0.0090 (6) | 0.0090 (6) | 0.0024 (8) | 0.000 | 0.000 | 0.000 |
W1 | 0.0098 (4) | 0.0098 (4) | 0.0076 (6) | 0.000 | 0.000 | 0.000 |
O1 | 0.024 (5) | 0.017 (4) | 0.015 (3) | 0.001 (3) | 0.003 (3) | 0.001 (3) |
(Na/Dy)1—O1i | 2.457 (7) | (Na/Dy)1—O1vii | 2.471 (7) |
(Na/Dy)1—O1ii | 2.457 (7) | (Na/Dy)1—O1 | 2.471 (7) |
(Na/Dy)1—O1iii | 2.457 (7) | W1—O1viii | 1.785 (7) |
(Na/Dy)1—O1iv | 2.457 (7) | W1—O1ix | 1.785 (7) |
(Na/Dy)1—O1v | 2.471 (7) | W1—O1 | 1.785 (7) |
(Na/Dy)1—O1vi | 2.471 (7) | W1—O1x | 1.785 (7) |
O1i—(Na/Dy)1—O1ii | 79.7 (3) | O1vi—(Na/Dy)1—O1vii | 98.76 (12) |
O1i—(Na/Dy)1—O1iii | 126.1 (2) | O1i—(Na/Dy)1—O1 | 68.80 (16) |
O1ii—(Na/Dy)1—O1iii | 126.1 (2) | O1ii—(Na/Dy)1—O1 | 76.3 (3) |
O1i—(Na/Dy)1—O1iv | 126.1 (2) | O1iii—(Na/Dy)1—O1 | 73.31 (14) |
O1ii—(Na/Dy)1—O1iv | 126.1 (2) | O1iv—(Na/Dy)1—O1 | 152.4 (3) |
O1iii—(Na/Dy)1—O1iv | 79.7 (3) | O1v—(Na/Dy)1—O1 | 98.76 (12) |
O1i—(Na/Dy)1—O1v | 152.4 (3) | O1vi—(Na/Dy)1—O1 | 98.76 (12) |
O1ii—(Na/Dy)1—O1v | 73.31 (14) | O1vii—(Na/Dy)1—O1 | 134.1 (3) |
O1iii—(Na/Dy)1—O1v | 68.80 (16) | O1viii—W1—O1ix | 107.0 (2) |
O1iv—(Na/Dy)1—O1v | 76.3 (3) | O1viii—W1—O1 | 114.6 (4) |
O1i—(Na/Dy)1—O1vi | 73.31 (14) | O1ix—W1—O1 | 107.0 (2) |
O1ii—(Na/Dy)1—O1vi | 152.4 (3) | O1viii—W1—O1x | 107.0 (2) |
O1iii—(Na/Dy)1—O1vi | 76.3 (3) | O1ix—W1—O1x | 114.6 (4) |
O1iv—(Na/Dy)1—O1vi | 68.80 (16) | O1—W1—O1x | 107.0 (2) |
O1v—(Na/Dy)1—O1vi | 134.1 (3) | W1—O1—Dy1ii | 131.4 (3) |
O1i—(Na/Dy)1—O1vii | 76.3 (3) | W1—O1—(Na/Dy)1ii | 131.4 (3) |
O1ii—(Na/Dy)1—O1vii | 68.80 (16) | W1—O1—(Na/Dy)1 | 120.8 (3) |
O1iii—(Na/Dy)1—O1vii | 152.4 (3) | Dy1ii—O1—(Na/Dy)1 | 103.7 (3) |
O1iv—(Na/Dy)1—O1vii | 73.31 (14) | (Na/Dy)1ii—O1—(Na/Dy)1 | 103.7 (3) |
O1v—(Na/Dy)1—O1vii | 98.76 (12) |
Symmetry codes: (i) x, y−1/2, −z; (ii) −x+1, −y, −z; (iii) y+1/4, −x+1/4, z+1/4; (iv) −y+3/4, x−3/4, z+1/4; (v) y+3/4, −x+1/4, −z+1/4; (vi) −y+1/4, x−3/4, −z+1/4; (vii) −x+1, −y−1/2, z; (viii) −x, −y+1/2, z; (ix) −y+1/4, x+1/4, −z+1/4; (x) y−1/4, −x+1/4, −z+1/4. |
Experimental details
Crystal data | |
Chemical formula | NaDy(WO4)2 |
Mr | 681.19 |
Crystal system, space group | Tetragonal, I41/a |
Temperature (K) | 298 |
a, c (Å) | 5.2545 (5), 11.4029 (15) |
V (Å3) | 314.83 (6) |
Z | 2 |
Radiation type | Mo Kα |
µ (mm−1) | 48.27 |
Crystal size (mm) | 0.10 × 0.10 × 0.08 |
Data collection | |
Diffractometer | Rigaku Mercury70 diffractometer |
Absorption correction | Multi-scan (SADABS; Bruker, 1997) |
Tmin, Tmax | 0.263, 1.000 |
No. of measured, independent and observed [I > 2σ(I)] reflections | 1128, 181, 143 |
Rint | 0.053 |
(sin θ/λ)max (Å−1) | 0.649 |
Refinement | |
R[F2 > 2σ(F2)], wR(F2), S | 0.024, 0.056, 0.87 |
No. of reflections | 181 |
No. of parameters | 15 |
Δρmax, Δρmin (e Å−3) | 1.55, −1.40 |
Computer programs: CrystalClear (Rigaku, 2000), SHELXS97 (Sheldrick, 2008), SHELXL97 (Sheldrick, 2008), DIAMOND (Brandenburg, 2004), SHELXTL (Sheldrick, 2008).
(Na/Dy)1—O1i | 2.457 (7) | W1—O1 | 1.785 (7) |
(Na/Dy)1—O1 | 2.471 (7) |
Symmetry code: (i) y+1/4, −x+1/4, z+1/4. |
References
Brandenburg, K. (2004). DIAMOND. Crystal Impact GbR, Bonn, Germany. Google Scholar
Han, X. M., Lin, Z. B., Hu, Z. S. & Wang, G. F. (2002). Mater. Res. Innov. 6, 118–121. Web of Science CrossRef CAS Google Scholar
Huang, X. Y., Lin, Z. B., Zhang, L. Z., Chen, J. T. & Wang, G. F. (2006). Cryst. Growth Des. 6, 2271–2274. Web of Science CrossRef CAS Google Scholar
Li, H., Hong, G. & Yue, S. (1990). Zhongguo Xitu Xuebao, 8, 37–41. CAS Google Scholar
Perets, S., Tseitlin, M., Shneck, R. Z., Mogilyanski, D., Kimmel, G. & Burshtein, Z. J. (2007). J. Cryst. Growth, 305, 257–264. Web of Science CrossRef CAS Google Scholar
Rigaku. (2000). CrystalClear. Rigaku Corporation, Tokyo, Japan. Google Scholar
Sheldrick, G. M. (1997). SADABS, University of Göttingen, Germany. Google Scholar
Sheldrick, G. M. (2008). Acta Cryst. A64, 112–122. Web of Science CrossRef CAS IUCr Journals Google Scholar
Sillen, L. G. & Nylander, A. L. (1943). Arkiv Kemi Mineral. Geol. 17, 1–27. Google Scholar
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In the past years an increasing interest in the synthesis and characterization of rare-earth double tungstate(VI) crystals with general formula ARE(WO4)2 (A = alkali metal, RE = rare-earth metal) has been observed due to their interesting magnetic, electric and optical properties (Perets et al., 2007; Huang et al., 2006; Li et al., 1990; Han et al., 2002). These compounds are attractive solid-state laser host materials because of their large rare-earth ion admittance. Most of these crystals have tetragonal symmetry and crystallize with the scheelite structure (CaWO4) in space group I41/a (Sillen & Nylander, 1943). In the title structure, the Ca2+ position of the original CaWO4 structure is statistically occupied by Na+ and Dy3+ ions in an 1:1 ratio. The crystal structure of NaDy(WO4)2 is composed of a two-direction packing of isolated WO4 tetrahedra interconnected by distorted [(Na/Dy)O8] dodecahedra, as shown in Fig. 2.