inorganic compounds
Scheelite-type NaEr(MoO4)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
Explorations of the A1+–RE3+–Mo6+–O2− (A1+ is an alkali metal cation, RE3+ is a rare-earth metal cation) quaternary systems prepared by the high-temperature solution growth method led to the title structure, sodium erbium bis(molybdate), NaEr(MoO4)2. It is isostructural to the scheelite structure (CaWO4) and is composed of [MoO4]2− tetrahedra with symmetry and [(Na/Er)O8]14− polyhedra. The [(Na/Er)O8]14− polyhedron is a distorted tetragonal antiprism, also with symmetry, with statistically mixed Na/Er atoms at its centre. There are two sets of Na/Er—O bond lengths [2.420 (4) and 2.435 (3) Å], but just one set of Mo—O bond lengths [1.774 (4) Å].
Related literature
For the structures, properties and applications of the alkali rare-earth tungstates and molybdates with the general formula A1+RE3+(M6+O4)2 (A1+ is an alkali metal cation, RE3+ is a rare-earth metal cation, M6+ is Mo6+ or W6+), see: Huang et al. (2006); Klevtsova (1975); Klevtsova et al. (1972); Kolitsch (2001); Kuzmicheva et al. (2005); Li et al. (2006); Morozov et al. (2006); Stevens et al. (1991); Zhao et al. (2010). For the scheelite (CaWO4) structure, see: Sillen & Nylander (1943).
Experimental
Crystal data
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Data collection: CrystalClear (Rigaku, 2004); cell CrystalClear; data reduction: CrystalClear; program(s) used to solve structure: SHELXS97 (Sheldrick, 2008) and PLATON (Spek, 2009); 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
https://doi.org/10.1107/S160053681001264X/fb2187sup1.cif
contains datablocks I, global. DOI:Structure factors: contains datablock I. DOI: https://doi.org/10.1107/S160053681001264X/fb2187Isup2.hkl
Single crystals of NaEr(MoO4)2 have been prepared by the high temperature solution growth (HTSG) method in air. A powder mixture of Na2CO3 (0.4418 g), Er2O3 (0.2657 g) and MoO3 (2.000 g) at the molar ratio of Na:Er:Mo = 6:1:10 was first ground in an agate mortar and then transferred to a platinum crucible. The sample was gradually heated in air at 1173 K for 24 h. In this stage, the reagents were completely melted. After that, the intermediate product was slowly cooled to 673 K at the rate of 2 Kh-1. It was kept at 673 for another 10 h and then quenched to room temperature. The obtained crystals were light-red and of the prismatical shape. The dimensions of the used sample were typical for the grown crystals in this batch.
The Na and Er atoms are in substitutional disorder in the
The tentative that included the corresponding occupancy factors for the disordered Na/Er yielded Na1 : Er1 = 0.501 (2) : 0.499 (2). (The atomic positional and anisotropic displacement parameters of Na1 and Er1 atoms were constrained to be identical by using EADP and EXYZ constraint instructions (SHELXL-97; Sheldrick, 2008).) Therefore the ratio of Na and Er was fixed to 1:1 in the final model with the constrained positional and the displacement parameters of na and Er as given above. The highest peak in the difference equals to 1.12 e/Å3 at the distance of 0.83 Å from Na1/Er1 site while the deepest hole equals to -1.15 e/Å3 at the distance of 1.39 Å from Na1/Er1 site, too.Alkali rare-earth bis(molybdates) with the general formula A1+RE3+(MO4)2 (AI is an alkali-metal cation, RE3+ is a rare-earth metal cation, M is Mo6+ or W6+) have been the subject of interest for many decades, mainly due to their applications as suitable host materials for fluorescence (Kuzmicheva et al., 2005; Morozov et al., 2006; Li et al., 2006). Some of these crystals are isostructural to scheelite (CaWO4, I41/a; Sillen & Nylander, 1943), such as NaLa(MoO4)2 (Stevens et al., 1991), LiNd(MoO4)2 (Kolitsch, 2001), LiNd(WO4)2 (Huang et al., 2006) and LiDy(WO4)2 (Zhao et al., 2010).
In difference to CaWO4 with one cation species only, the cations A1+ and RE3+ are statistically disordered. Within alkali rare-earth bis(molybdates), different structures from the scheelite type have also been reported, such as LiLa(MoO4)2 (Pbca; Klevtsova, 1975) and CsDy(MoO4)2 (Pccm; Klevtsova et al. 1972).
The X-ray
has shown that the title compound NaEr(MoO4)2 is isostructural with the scheelite. In the title structure, Na and Er atoms are disordered over the same 4a site while Mo atoms reside on 4b site. The structure of NaEr(MoO4)2 may be regarded as composed of [MoO4]2- tetrahedra and of [(Na/Er)O8]14- polyhedra (each in the form of a distorted tetragonal antiprism) that share the oxygens (Fig. 2). Each oxygen of the [MoO4]2- tetrahedron is shared by the different Na/Er polyhedron and each oxygen of the [(Na/Er)O8]14- polyhedron is shared by the different [MoO4]2- tetrahedron.For the structures, properties and applications of the alkali rare-earth tungstates and molybdates with the general formula A1+RE3+(M6+O4)2 (A1+ is an alkali metal cation, RE3+ is a rare-earth metal cation, M6+ is Mo6+ or W6+), see: Huang et al. (2006); Klevtsova (1975); Klevtsova et al. (1972); Kolitsch (2001); Kuzmicheva et al. (2005); Li et al. (2006); Morozov et al. (2006); Stevens et al. (1991); Zhao et al. (2010). For the scheelite (CaWO4) structure, see: Sillen & Nylander (1943).
Data collection: CrystalClear (Rigaku, 2004); cell
CrystalClear (Rigaku, 2004); data reduction: CrystalClear (Rigaku, 2004); program(s) used to solve structure: SHELXS97 (Sheldrick, 2008) and PLATON (Spek, 2009); program(s) used to refine structure: SHELXL97 (Sheldrick, 2008); molecular graphics: DIAMOND (Brandenburg, 2004); software used to prepare material for publication: SHELXTL (Sheldrick, 2008).NaEr(MoO4)2 | Dx = 5.590 Mg m−3 |
Mr = 510.13 | Mo Kα radiation, λ = 0.71073 Å |
Tetragonal, I41/a | Cell parameters from 365 reflections |
Hall symbol: -I 4ad | θ = 4.3–27.3° |
a = 5.1816 (8) Å | µ = 17.87 mm−1 |
c = 11.288 (3) Å | T = 173 K |
V = 303.07 (11) Å3 | Prism, red |
Z = 2 | 0.08 × 0.04 × 0.04 mm |
F(000) = 454 |
Rigaku Saturn70 CCD diffractometer | 172 independent reflections |
Radiation source: fine-focus sealed tube | 106 reflections with I > 2σ(I) |
Confocal monochromator | Rint = 0.026 |
Detector resolution: 28.5714 pixels mm-1 | θmax = 27.5°, θmin = 4.3° |
ω scans | h = −2→6 |
Absorption correction: multi-scan (rescaled SADABS; Sheldrick, 1997) | k = −5→6 |
Tmin = 0.263, Tmax = 0.489 | l = −14→14 |
520 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)] = 0.032 | w = 1/[σ^2^(Fo^2^) + (0.0639P)^2^] where P = (Fo^2^ + 2Fc^2^)/3 |
wR(F2) = 0.089 | (Δ/σ)max < 0.001 |
S = 0.84 | Δρmax = 1.12 e Å−3 |
172 reflections | Δρmin = −1.15 e Å−3 |
15 parameters | Extinction correction: SHELXL97 (Sheldrick, 2008), Fc*=kFc[1+0.001xFc2λ3/sin(2θ)]-1/4 |
0 restraints | Extinction coefficient: 0.055 (5) |
9 constraints |
NaEr(MoO4)2 | Z = 2 |
Mr = 510.13 | Mo Kα radiation |
Tetragonal, I41/a | µ = 17.87 mm−1 |
a = 5.1816 (8) Å | T = 173 K |
c = 11.288 (3) Å | 0.08 × 0.04 × 0.04 mm |
V = 303.07 (11) Å3 |
Rigaku Saturn70 CCD diffractometer | 172 independent reflections |
Absorption correction: multi-scan (rescaled SADABS; Sheldrick, 1997) | 106 reflections with I > 2σ(I) |
Tmin = 0.263, Tmax = 0.489 | Rint = 0.026 |
520 measured reflections |
R[F2 > 2σ(F2)] = 0.032 | 15 parameters |
wR(F2) = 0.089 | 0 restraints |
S = 0.84 | Δρmax = 1.12 e Å−3 |
172 reflections | Δρmin = −1.15 e Å−3 |
Geometry. All esds (except the esd in the dihedral angle between two l.s. planes) are estimated using the full covariance matrix. The cell esds are taken into account individually in the estimation of esds in distances, angles and torsion angles; correlations between esds in cell parameters are only used when they are defined by crystal symmetry. An approximate (isotropic) treatment of cell esds is used for estimating esds 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) | |
Er1 | 0.0000 | 0.2500 | 0.1250 | 0.0081 (5) | 0.50 |
Na1 | 0.0000 | 0.2500 | 0.1250 | 0.0081 (5) | 0.50 |
Mo1 | 0.5000 | 0.7500 | 0.1250 | 0.0086 (5) | |
O1 | 0.2568 (6) | 0.5968 (6) | 0.0397 (3) | 0.0204 (12) |
U11 | U22 | U33 | U12 | U13 | U23 | |
Er1 | 0.0070 (6) | 0.0070 (6) | 0.0102 (8) | 0.000 | 0.000 | 0.000 |
Na1 | 0.0070 (6) | 0.0070 (6) | 0.0102 (8) | 0.000 | 0.000 | 0.000 |
Mo1 | 0.0067 (6) | 0.0067 (6) | 0.0124 (8) | 0.000 | 0.000 | 0.000 |
O1 | 0.025 (2) | 0.017 (2) | 0.019 (2) | 0.0012 (15) | −0.0045 (14) | −0.0007 (17) |
Er1—O1i | 2.420 (4) | Er1—O1vii | 2.435 (3) |
Er1—O1ii | 2.420 (4) | Mo1—O1viii | 1.774 (4) |
Er1—O1iii | 2.420 (4) | Mo1—O1ix | 1.774 (4) |
Er1—O1iv | 2.420 (4) | Mo1—O1 | 1.774 (4) |
Er1—O1v | 2.435 (3) | Mo1—O1x | 1.774 (4) |
Er1—O1vi | 2.435 (3) | O1—Na1iii | 2.420 (4) |
Er1—O1 | 2.435 (3) | O1—Er1iii | 2.420 (4) |
O1i—Er1—O1ii | 79.63 (16) | O1v—Er1—O1vii | 99.01 (7) |
O1i—Er1—O1iii | 126.16 (10) | O1vi—Er1—O1vii | 99.01 (7) |
O1ii—Er1—O1iii | 126.16 (10) | O1—Er1—O1vii | 133.38 (18) |
O1i—Er1—O1iv | 126.16 (10) | O1i—Er1—Er1xi | 38.03 (7) |
O1ii—Er1—O1iv | 126.16 (10) | O1ii—Er1—Er1xi | 69.88 (9) |
O1iii—Er1—O1iv | 79.62 (16) | O1iii—Er1—Er1xi | 159.67 (8) |
O1i—Er1—O1v | 75.78 (12) | O1iv—Er1—Er1xi | 101.19 (8) |
O1ii—Er1—O1v | 68.76 (7) | O1v—Er1—Er1xi | 37.75 (8) |
O1iii—Er1—O1v | 152.76 (16) | O1vi—Er1—Er1xi | 101.99 (9) |
O1iv—Er1—O1v | 73.67 (7) | O1—Er1—Er1xi | 85.52 (9) |
O1i—Er1—O1vi | 68.76 (7) | O1vii—Er1—Er1xi | 131.38 (8) |
O1ii—Er1—O1vi | 75.78 (12) | O1i—Er1—Na1xi | 38.03 (7) |
O1iii—Er1—O1vi | 73.67 (7) | O1ii—Er1—Na1xi | 69.88 (9) |
O1iv—Er1—O1vi | 152.76 (16) | O1iii—Er1—Na1xi | 159.67 (8) |
O1v—Er1—O1vi | 133.38 (18) | O1iv—Er1—Na1xi | 101.19 (8) |
O1i—Er1—O1 | 73.67 (7) | O1v—Er1—Na1xi | 37.75 (8) |
O1ii—Er1—O1 | 152.76 (16) | O1vi—Er1—Na1xi | 101.99 (9) |
O1iii—Er1—O1 | 75.78 (12) | O1—Er1—Na1xi | 85.52 (9) |
O1iv—Er1—O1 | 68.76 (7) | O1vii—Er1—Na1xi | 131.38 (8) |
O1v—Er1—O1 | 99.01 (7) | O1viii—Mo1—O1ix | 114.2 (2) |
O1vi—Er1—O1 | 99.01 (7) | O1viii—Mo1—O1 | 107.15 (11) |
O1i—Er1—O1vii | 152.76 (16) | O1ix—Mo1—O1 | 107.15 (11) |
O1ii—Er1—O1vii | 73.67 (7) | O1viii—Mo1—O1x | 107.15 (11) |
O1iii—Er1—O1vii | 68.76 (7) | O1ix—Mo1—O1x | 107.15 (11) |
O1iv—Er1—O1vii | 75.78 (12) | O1—Mo1—O1x | 114.2 (2) |
Symmetry codes: (i) −y+3/4, x+1/4, z+1/4; (ii) y−3/4, −x+1/4, z+1/4; (iii) −x, −y+1, −z; (iv) x, y−1/2, −z; (v) y−1/4, −x+1/4, −z+1/4; (vi) −y+1/4, x+1/4, −z+1/4; (vii) −x, −y+1/2, z; (viii) y−1/4, −x+5/4, −z+1/4; (ix) −y+5/4, x+1/4, −z+1/4; (x) −x+1, −y+3/2, z; (xi) −x+1/2, −y+1/2, −z+1/2. |
Experimental details
Crystal data | |
Chemical formula | NaEr(MoO4)2 |
Mr | 510.13 |
Crystal system, space group | Tetragonal, I41/a |
Temperature (K) | 173 |
a, c (Å) | 5.1816 (8), 11.288 (3) |
V (Å3) | 303.07 (11) |
Z | 2 |
Radiation type | Mo Kα |
µ (mm−1) | 17.87 |
Crystal size (mm) | 0.08 × 0.04 × 0.04 |
Data collection | |
Diffractometer | Rigaku Saturn70 CCD diffractometer |
Absorption correction | Multi-scan (rescaled SADABS; Sheldrick, 1997) |
Tmin, Tmax | 0.263, 0.489 |
No. of measured, independent and observed [I > 2σ(I)] reflections | 520, 172, 106 |
Rint | 0.026 |
(sin θ/λ)max (Å−1) | 0.649 |
Refinement | |
R[F2 > 2σ(F2)], wR(F2), S | 0.032, 0.089, 0.84 |
No. of reflections | 172 |
No. of parameters | 15 |
Δρmax, Δρmin (e Å−3) | 1.12, −1.15 |
Computer programs: CrystalClear (Rigaku, 2004), SHELXS97 (Sheldrick, 2008) and PLATON (Spek, 2009), SHELXL97 (Sheldrick, 2008), DIAMOND (Brandenburg, 2004), SHELXTL (Sheldrick, 2008).
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Alkali rare-earth bis(molybdates) with the general formula A1+RE3+(MO4)2 (AI is an alkali-metal cation, RE3+ is a rare-earth metal cation, M is Mo6+ or W6+) have been the subject of interest for many decades, mainly due to their applications as suitable host materials for fluorescence (Kuzmicheva et al., 2005; Morozov et al., 2006; Li et al., 2006). Some of these crystals are isostructural to scheelite (CaWO4, I41/a; Sillen & Nylander, 1943), such as NaLa(MoO4)2 (Stevens et al., 1991), LiNd(MoO4)2 (Kolitsch, 2001), LiNd(WO4)2 (Huang et al., 2006) and LiDy(WO4)2 (Zhao et al., 2010).
In difference to CaWO4 with one cation species only, the cations A1+ and RE3+ are statistically disordered. Within alkali rare-earth bis(molybdates), different structures from the scheelite type have also been reported, such as LiLa(MoO4)2 (Pbca; Klevtsova, 1975) and CsDy(MoO4)2 (Pccm; Klevtsova et al. 1972).
The X-ray diffraction analysis has shown that the title compound NaEr(MoO4)2 is isostructural with the scheelite. In the title structure, Na and Er atoms are disordered over the same 4a site while Mo atoms reside on 4b site. The structure of NaEr(MoO4)2 may be regarded as composed of [MoO4]2- tetrahedra and of [(Na/Er)O8]14- polyhedra (each in the form of a distorted tetragonal antiprism) that share the oxygens (Fig. 2). Each oxygen of the [MoO4]2- tetrahedron is shared by the different Na/Er polyhedron and each oxygen of the [(Na/Er)O8]14- polyhedron is shared by the different [MoO4]2- tetrahedron.