Acta Cryst. (2008). E64, i16 [ doi:10.1107/S1600536808003267 ]
-Lead tellurite from single-crystal dataThe crystal structure of the title compound,
-PbTeO3 (PTO), has been reported previously by Mariolacos [Anz. Oesterr. Akad. Wiss. Math. Naturwiss. Kl. (1969), 106, 128-130], refined on powder data. The current determination at room temperature from data obtained from single crystals grown by the Czochralski method shows a significant improvement in the precision of the geometric parameters when all atoms have been refined anisotropically. The selection of a centrosymmetric (C2/c) structure model was confirmed by the second harmonic generation test. The asymmetric unit contains three formula units. The structure of PTO is built up of three types of distorted [PbOx] polyhedra (x = 7 and 9) which share their O atoms with TeO3 pyramidal units. These main anionic polyhedra are responsible for establishing the two types of tunnel required for the stereochemical activity of the lone pairs of the Pb2+ and Te4+ cations.
Single crystals of PTO were grown by the Czochralski technique as described earlier (Kosse, Politova, Bush et al., 1983; Kosse, Politova, Astafiev et al., 1983). The chemical composition of tested crystals was confirmed with energy-dispersive spectrometry analysis (LINK AN10000). Second harmonic generation (SHG) measurements showed no positive signals at room temperature which is in accordance with the given space group.
The structure of PTO was solved by the direct method in space group C2/c where the atomic coordinates of all Pb and Te cations were found. The oxygen atoms were localized by difference Fourier maps.
The very high absorption coefficient (µ=56.32 mm-1) and imperfect shape of crystal are the reason why the program DIFABS (Walker & Stuart, 1983) was used for absorption correction.
The highest residual electron density peak (2.31 e A-3) is located 1.00Å from atom Pb1 and the deepest hole
(-2.06 e A-3) is located 1.46Å from atom O4.
Data collection: CAD-4-PC (Enraf–Nonius, 1993); cell refinement: CAD-4-PC (Enraf–Nonius, 1993); data reduction: CAD-4-PC (Enraf–Nonius, 1993); program(s) used to solve structure: SHELXS97 (Sheldrick, 2008); program(s) used to refine structure: SHELXL97 (Sheldrick, 2008); molecular graphics: DIAMOND (Brandenburg, 2005); software used to prepare material for publication: CIFTAB97 (Sheldrick, 2008).
| PbTeO3 | F000 = 3792 |
| Mr = 382.79 | Dx = 7.282 Mg m−3 |
| Monoclinic, C2/c | Mo Kα radiation λ = 0.71073 Å |
| Hall symbol: -C 2yc | Cell parameters from 24 reflections |
| a = 26.555 (5) Å | θ = 12.1–14.5º |
| b = 4.593 (1) Å | µ = 56.32 mm−1 |
| c = 17.958 (4) Å | T = 295 (2) K |
| β = 106.97 (3)º | Needle, colourless |
| V = 2094.9 (7) Å3 | 0.14 × 0.04 × 0.02 mm |
| Z = 24 |
| Enraf–Nonius CAD-4 diffractometer | Rint = 0.054 |
| Radiation source: fine-focus sealed tube | θmax = 32.0º |
| Monochromator: β-filter | θmin = 1.6º |
| T = 293(2) K | h = −39→37 |
| ω/2θ scans | k = −6→0 |
| Absorption correction: part of the refinement model (ΔF) (Walker & Stuart, 1983) | l = 0→26 |
| Tmin = 0.234, Tmax = 0.695 | 3 standard reflections |
| 3717 measured reflections | every 60 min |
| 3608 independent reflections | intensity decay: none |
| 1676 reflections with I > 2σ(I) |
| Refinement on F2 | Secondary atom site location: difference Fourier map |
| Least-squares matrix: full | w = 1/[σ2(Fo2) + (0.0301P)2] where P = (Fo2 + 2Fc2)/3 |
| R[F2 > 2σ(F2)] = 0.026 | (Δ/σ)max = 0.001 |
| wR(F2) = 0.063 | Δρmax = 2.31 e Å−3 |
| S = 0.77 | Δρmin = −2.06 e Å−3 |
| 3608 reflections | Extinction correction: SHELXL97 (Sheldrick, 2008), Fc*=kFc[1+0.001xFc2λ3/sin(2θ)]-1/4 |
| 137 parameters | Extinction coefficient: 0.000052 (5) |
| Primary atom site location: structure-invariant direct methods |
| PbTeO3 | V = 2094.9 (7) Å3 |
| Mr = 382.79 | Z = 24 |
| Monoclinic, C2/c | Mo Kα |
| a = 26.555 (5) Å | µ = 56.32 mm−1 |
| b = 4.593 (1) Å | T = 295 (2) K |
| c = 17.958 (4) Å | 0.14 × 0.04 × 0.02 mm |
| β = 106.97 (3)º |
| Enraf–Nonius CAD-4 diffractometer | 1676 reflections with I > 2σ(I) |
| Absorption correction: part of the refinement model (ΔF) (Walker & Stuart, 1983) | Rint = 0.054 |
| Tmin = 0.234, Tmax = 0.695 | 3 standard reflections |
| 3717 measured reflections | every 60 min |
| 3608 independent reflections | intensity decay: none |
| R[F2 > 2σ(F2)] = 0.026 | 137 parameters |
| wR(F2) = 0.063 | Δρmax = 2.31 e Å−3 |
| S = 0.77 | Δρmin = −2.06 e Å−3 |
| 3608 reflections |
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 | ||
| Pb1 | 0.183652 (15) | 0.21366 (10) | 0.73592 (2) | 0.01749 (9) | |
| Pb2 | 0.066493 (14) | 0.22395 (12) | 0.54345 (2) | 0.01847 (9) | |
| Pb3 | 0.162024 (14) | −0.24695 (10) | 0.913902 (19) | 0.01916 (9) | |
| Te1 | 0.04734 (2) | −0.23056 (15) | 0.36782 (3) | 0.01331 (11) | |
| Te2 | 0.06941 (2) | −0.25178 (16) | 0.70793 (3) | 0.01367 (11) | |
| Te3 | 0.20758 (3) | −0.30201 (15) | 0.59262 (4) | 0.01439 (13) | |
| O1 | 0.0204 (3) | −0.179 (2) | 0.4532 (4) | 0.0240 (17) | |
| O2 | 0.1172 (3) | −0.156 (2) | 0.4259 (5) | 0.0285 (19) | |
| O3 | 0.0559 (4) | −0.6348 (18) | 0.3703 (6) | 0.034 (2) | |
| O4 | 0.1359 (3) | −0.221 (2) | 0.7823 (4) | 0.0201 (15) | |
| O5 | 0.0952 (4) | −0.1694 (19) | 0.6233 (4) | 0.028 (2) | |
| O6 | 0.0659 (4) | −0.6528 (17) | 0.6935 (6) | 0.035 (2) | |
| O7 | 0.2214 (3) | −0.2120 (18) | 0.6999 (4) | 0.0180 (14) | |
| O8 | 0.1858 (4) | −0.683 (2) | 0.6000 (5) | 0.033 (2) | |
| O9 | 0.2781 (3) | −0.355 (2) | 0.6016 (6) | 0.034 (2) |
| U11 | U22 | U33 | U12 | U13 | U23 | |
| Pb1 | 0.01503 (16) | 0.0168 (2) | 0.02066 (16) | 0.00061 (16) | 0.00526 (13) | −0.00209 (16) |
| Pb2 | 0.01480 (15) | 0.0215 (2) | 0.01935 (15) | 0.00049 (18) | 0.00528 (12) | 0.00186 (17) |
| Pb3 | 0.02372 (17) | 0.02011 (19) | 0.01346 (14) | 0.00414 (19) | 0.00511 (12) | 0.00129 (16) |
| Te1 | 0.0161 (2) | 0.0109 (3) | 0.0145 (2) | 0.0019 (3) | 0.00698 (19) | −0.0003 (2) |
| Te2 | 0.0136 (2) | 0.0106 (3) | 0.0157 (2) | −0.0002 (3) | 0.00254 (19) | −0.0021 (3) |
| Te3 | 0.0163 (3) | 0.0122 (3) | 0.0137 (2) | 0.0009 (2) | 0.0029 (2) | 0.0001 (2) |
| O1 | 0.022 (4) | 0.035 (5) | 0.016 (3) | −0.007 (4) | 0.008 (3) | −0.003 (3) |
| O2 | 0.013 (3) | 0.032 (5) | 0.037 (4) | 0.005 (3) | 0.002 (3) | 0.007 (4) |
| O3 | 0.056 (7) | 0.007 (4) | 0.040 (5) | 0.010 (4) | 0.014 (5) | −0.002 (3) |
| O4 | 0.017 (3) | 0.030 (4) | 0.014 (3) | −0.013 (4) | 0.006 (2) | −0.004 (3) |
| O5 | 0.050 (6) | 0.022 (4) | 0.014 (3) | 0.015 (4) | 0.012 (4) | 0.010 (3) |
| O6 | 0.044 (6) | 0.005 (3) | 0.057 (6) | −0.004 (4) | 0.019 (5) | −0.012 (4) |
| O7 | 0.020 (3) | 0.014 (3) | 0.020 (3) | 0.006 (3) | 0.007 (3) | 0.006 (3) |
| O8 | 0.053 (6) | 0.021 (4) | 0.024 (4) | −0.016 (4) | 0.013 (4) | 0.000 (3) |
| O9 | 0.013 (3) | 0.052 (6) | 0.039 (5) | 0.014 (4) | 0.010 (3) | 0.000 (4) |
| Pb1—O7 | 2.371 (8) | Pb3—O3v | 2.750 (11) |
| Pb1—O7i | 2.471 (7) | Te1—O3 | 1.870 (8) |
| Pb1—O8ii | 2.504 (8) | Te1—O2 | 1.876 (9) |
| Pb1—O4 | 2.628 (8) | Te1—O1 | 1.888 (7) |
| Pb2—O5 | 2.294 (8) | Te2—O6 | 1.859 (8) |
| Pb2—O1iii | 2.334 (8) | Te2—O5 | 1.878 (8) |
| Pb2—O1 | 2.528 (9) | Te2—O4 | 1.883 (7) |
| Pb2—O6ii | 2.758 (10) | Te3—O9 | 1.848 (8) |
| Pb3—O2iv | 2.246 (9) | Te3—O8 | 1.858 (9) |
| Pb3—O4 | 2.263 (6) | Te3—O7 | 1.899 (7) |
| Pb3—O9i | 2.471 (9) | ||
| O7—Pb1—O7i | 77.64 (19) | O6—Te2—O5 | 95.9 (4) |
| O7—Pb1—O8ii | 76.1 (3) | O6—Te2—O4 | 99.8 (5) |
| O7i—Pb1—O8ii | 96.7 (3) | O5—Te2—O4 | 94.1 (4) |
| O7—Pb1—O4 | 75.0 (2) | O9—Te3—O8 | 101.4 (5) |
| O7i—Pb1—O4 | 118.6 (2) | O9—Te3—O7 | 92.8 (4) |
| O8ii—Pb1—O4 | 127.2 (3) | O8—Te3—O7 | 96.0 (4) |
| O5—Pb2—O1iii | 93.7 (3) | Te1—O1—Pb2iii | 128.4 (4) |
| O5—Pb2—O1 | 80.5 (3) | Te1—O1—Pb2 | 112.6 (4) |
| O1iii—Pb2—O1 | 69.8 (3) | Pb2iii—O1—Pb2 | 110.2 (3) |
| O5—Pb2—O6ii | 69.3 (3) | Te1—O2—Pb3vi | 124.2 (4) |
| O1iii—Pb2—O6ii | 72.9 (3) | Te1—O3—Pb3vii | 108.1 (5) |
| O1—Pb2—O6ii | 129.5 (3) | Te2—O4—Pb3 | 132.5 (3) |
| O2iv—Pb3—O4 | 92.7 (3) | Te2—O4—Pb1 | 105.7 (3) |
| O2iv—Pb3—O9i | 77.7 (3) | Pb3—O4—Pb1 | 110.0 (3) |
| O4—Pb3—O9i | 81.7 (3) | Te2—O5—Pb2 | 122.1 (4) |
| O2iv—Pb3—O3v | 70.3 (3) | Te2—O6—Pb2viii | 109.0 (4) |
| O4—Pb3—O3v | 74.8 (3) | Te3—O7—Pb1 | 119.0 (3) |
| O9i—Pb3—O3v | 138.7 (3) | Te3—O7—Pb1ix | 108.2 (3) |
| O3—Te1—O2 | 94.2 (4) | Pb1—O7—Pb1ix | 116.2 (3) |
| O3—Te1—O1 | 100.2 (4) | Te3—O8—Pb1viii | 110.2 (4) |
| O2—Te1—O1 | 94.2 (4) | Te3—O9—Pb3ix | 139.0 (6) |
| Symmetry codes: (i) −x+1/2, y+1/2, −z+3/2; (ii) x, y+1, z; (iii) −x, −y, −z+1; (iv) x, −y, z+1/2; (v) x, −y−1, z+1/2; (vi) x, −y, z−1/2; (vii) x, −y−1, z−1/2; (viii) x, y−1, z; (ix) −x+1/2, y−1/2, −z+3/2. |
The authors thank Dr E. D. Politova for the single-crystal preparation and Dr S. Yu. Stefanovich for the SHG measurements. This research was supported by the Russian Foundation for Basic Research (grant No. 06–03–32449).
Brandenburg, K. (2005). DIAMOND. Crystal Impact GbR, Bonn, Germany.
Brown, I. D. (1974). J. Solid State Chem. 11, 214–233.
Enraf–Nonius (1993). CAD-4-PC. Enraf–Nonius, Delft, The Netherlands.
Gaitan, M., Jerez, A., Noguerlas, J., Pico, C. & Veiga, M. L. (1987). Synth. React. Inorg. Chem. 17, 479–483.
Galy, J., Meunier, G., Anderson, S. & Astrom, A. (1975). J. Solid State Chem. 13, 142–159.
Gillespie, R. J. (1972). Molecular Geometry. London: Van Nostrand Reihold.
Kosse, L. I., Politova, E. D., Astafiev, A. V., Guriev, A. V., Turok, I. I. & Venevtsev, Yu. N. (1983). Sov. Phys. Solid State, 25, 1170–1172.
Kosse, L. I., Politova, E. D., Bush, A. A., Astafiev, A. V., Stefanovich, S. Yu., Myzgin, E. A. & Venevtsev, Yu. N. (1983). Sov. Phys. Crystallogr. 28, 300–301.
Mariolacos, K. (1969). Anz. Oesterr. Akad. Wiss. Math. Naturwiss. Kl. 106, 128–130.
Robertson, D. S., Shaw, N. & Young, I. M. (1976). J. Phys. D Appl. Phys. 9, 1257–1262.
Sciau, P., Lapasset, J. & Moret, J. (1986). Acta Cryst. C42, 1688–1690.
Sheldrick, G. M. (2008). Acta Cryst. A64, 112–122.
Spiridonov, E. & Tananaeva, L. (1982). Dokl. Acad. Sci. USSR Earth. Sci. Sect. 262, 177–179.
Tananaeva, O. I., Latypova, Z. Kh. & Novoselova, A. V. (1977). Inorg. Mater. 13, 324–325.
Tananaeva, O. I. & Novoselova, A. V. (1977). Inorg. Mater. 13, 910–912.
Walker, N. & Stuart, D. (1983). Acta Cryst. A39, 158–166.
Williams, S. (1979). Miner. Mag. 43, 453–459.
Young, I. M. (1979). J. Mater. Sci. 14, 1579–, 1585.
Crystals with the Pb2+ and Te4+ cations having stereochemically active lone-pairs are very attractive materials for ferroelectric and non-linear optical applications. The knowledge of the crystal structures of these compounds should provide important information about the unusual mechanism of formation of their polar properties. The investigation of the PbO-TeO2 system (Robertson et al., 1976; Young, 1979) has provided evidence of a large number of different phases. The polymorphism, crystal structure and thermodynamic status of PbTeO3 (PTO) are not fully established and literature reports give conflicting statements (Tananaeva et al.,1977; Robertson et al.,1976; Young, 1979). Several different polymorphs have previously been described: monoclinic (Mariolacos, 1969), triclinic (Williams, 1979), tetragonal (Sciau et al., 1986) and cubic (Gaitan et al.,1987). It should be mentioned that Spiridonov & Tananaeva (1982) described α-PbTeO3 as orthorhombic. The tetragonal phase was shown to be ferroelectric. The phase change from the tetragonal to the monoclinic form at 783 K has been shown to be irreversible (Young, 1979). The present paper deals with the crystal structure determination of α-PTO. This structure can be described in terms of complex irregular Pb2+ polyhedra with 7 and 9 apices and separate Te4+O3 groups (Fig. 1,2). Three kinds of Pb—O distances can be distinguished: three short contacts (2.25–2.53 Å), three longer distances (2.63–2.96 Å) and three abnormally long distances (3.02–3.26 Å). The different Pb polyhedra are connected by face, edge and corner sharing through the Pb—O bonds forming the network with the honeycomb-like chains parallel to c axis. The Te4+ cations coordinate to three O atoms in a one-sided pyramidal coordination TeO3E (E are lone-pair electrons). The Te—O distances are in the range 1.85–1.90 Å. The O—Te—O angles are close to 100°. The next-nearest anions are located at distances greater than 2.7 Å. In accordance with Brown (1974) these additional weak contacts are important for the determination of the correct coordination geometry of the Te cations. Depending on the type of Te4+O3 E units, two types of tunnels are formed running along [010], which represent the required space for the electron lone pairs within the structure. According to Gillespie (1972), Galy et al. (1975) the electronic lone pair E is sitting inside these non-bonding regions.