research communications
Single crystals of SnTe3O8 in the millimetre range grown by chemical vapor transport reactions
aInstitute for Chemical Technologies and Analytics, Division of Structural Chemistry, TU Wien, Getreidemarkt 9/164-SC, A-1060 Vienna, Austria
*Correspondence e-mail: matthias.weil@tuwien.ac.at
Tin(IV) trioxidotellurate(IV), SnTe3O8, is a member of the isotypic MIVTeIV3O8 (M = Ti, Zr, Hf, Sn) series crystallizing with eight formula units per in Ia. In comparison with the previous model of SnTe3O8 based on powder X-ray diffraction data [Meunier & Galy (1971). Acta Cryst. B27, 602–608], the current model based on single-crystal X-ray data is improved in terms of precision and accuracy. Nearly regular [SnO6] octahedra (Sn ..) are situated in the voids of an oxidotellurate(IV) framework built up by corner-sharing [TeO4] bisphenoids (Te 2..). A quantitative structural comparison revealed a very high degree of similarity for the structures with M = Ti, Zr, Sn in the MIVTe3O8 series.
Keywords: crystal structure; oxidotellurates; isotypism; electron lone pair.
CCDC reference: 2120742
1. Chemical context
The crystal chemistry of oxidotellurates(IV) is dominated by the presence of the 5s2 electron lone pair that, in the majority of cases, is stereochemically active, thus enabling one-sided coordination spheres around the TeIV atom (Christy et al., 2016). This peculiar building block often results in compounds with non-centrosymmetric structures or structures with polar directions exhibiting interesting physical properties (Ra et al., 2003; Kim et al., 2014). In this context, the microwave dielectric properties of MIVTe3O8 (M = Sn, Zr) ceramics were investigated some time ago (Subodh & Sebastian, 2008).
The MIVTe3O8 was originally determined for M = Ti from a single crystal in Ia using photographic Weissenberg X-ray data, whereas for M = Sn, Zr and Hf, the crystal structures were refined from powder X-ray data (Meunier & Galy, 1971). In subsequent studies, crystal-structure refinements on the basis of single-crystal X-ray data were reported for the mineral winstanleyite with composition (Ti0.96Fe0.04)Te3O8 (Bindi & Cipriani, 2003), and for the synthetic compound ZrTe3O8 (Noguera et al., 2003; Lu et al., 2019). A powder X-ray study of the Sn0.59Ti0.41Te3O8 crystallizing in the MIVTe3O8 structure type has also been reported (Ben Aribia et al., 2008).
of the isotypic seriesSingle-crystal growth of oxidotellurates(IV) can be accomplished through various crystallization methods including, for example, experiments under hydrothermal conditions (Weil et al., 2018), cooling from the melt (Stöger et al., 2009), from salt melts as fluxing agents (Weil, 2019), or from chemical vapor transport reactions (Missen et al., 2020). The latter method (Binnewies et al., 2012) is particularly suitable for growing large crystals of high quality and was the method of choice for crystal growth of SnTe3O8 for which a more precise and accurate structure appeared to be desirable.
2. Structural commentary
The 3O8 comprises one SnIV atom, one TeIV atom, and two oxide anions, residing on sites 8a (site symmetry ..), 24d (2..), 48e (1) and 16c (.3.), respectively. The tin atom is in an almost regular octahedral coordination by oxygen, with six equal Sn1—O1 distances, all trans angles equal to 180°, and cis angles ranging from 86.09 (4) to 93.91 (4)°. The Te1 site is coordinated by four O atoms in pairs of shorter (O1) and longer distances (O2) (Table 1). The resulting [TeO4] is a distorted bisphenoid. Considering the 5s2 electron lone pair at the TeIV atom, the corresponding [ΨTeO4] polyhedron has a shape intermediate between a square pyramid and a trigonal bipyramid with the non-bonding electron pair occupying an equatorial position (Fig. 1). The geometry index τ5 of the [ΨTeO4] polyhedron is 0.471 (τ5 = 0 for an ideal square pyramid and τ5 = 1 for an ideal trigonal bipyramid; Addison et al., 1984). The position of the electron lone pair was calculated with the LPLoc software (Hamani et al., 2020), with resulting fractional coordinates of x = 0.28655, y = 0, z = 1/4. The radius of the electron lone pair was calculated to be 1.07 Å with a distance of 0.90 Å from the Te1 position. The coordination numbers of the oxide anions are two and three: O1 coordinates to Sn1 and Te1 at the shorter of the two Te1—O distances whereas O2 coordinates to three Te1 atoms at the longer of the two Te1—O distances.
of SnTeIn the 3O8, the [SnO6] octahedra are isolated from each other and arranged in rows running parallel to [100]. Each of the [TeO4] bisphenoids shares corners (O2) with other [TeO4] bisphenoids to form a three-dimensional oxidotellurate(IV) framework. The [SnO6] octahedra are situated in the voids of this framework, thereby sharing each of the six corners with an individual [TeO4] bisphenoid. The of SnTe3O8 is depicted in Fig. 2.
of SnTeThe unit-cell parameter a from the previous powder X-ray study, 11.144 (3) Å, as well as interatomic distances of Sn1—O1 = 2.032 Å (6×), Te1—O1 = 1.850 Å (2×), Te1—O2 = 2.124 Å (2×), and angles O1—Te1—O1′ = 102.9°, and O2—Te1—O2′ = 156.8° (Meunier & Galy, 1971) agree with the present single-crystal study (Table 1), but with lower precision and accuracy. In comparison with the previous model based on powder X-ray data, the values of the bond-valence sums (Brown, 2002) using the parameters of Brese & O'Keeffe (1991) are much closer to the expected values of 4 for Sn and Te and 2 for O on basis of the current model [previous model: Sn1 4.28 valence units (v.u.), Te1 4.10 v.u., O1 2.09 v.u., O2 2.08 v.u.; current model: Sn1: 4.14 v.u., Te1 3.93 v.u., O1 1.99 v.u., O2 2.00 v.u.].
The relation of the isotypic crystal structures of MIVTe3O8 compounds with that of the fluorite structure has been discussed previously for TiTe3O8 (Meunier & Galy, 1971; Wells, 1975). The unit-cell parameter a of cubic TiTe3O8 is ∼2a of cubic CaF2, whereby the ordered distribution of the cationic sites leads to a doubling of the and also to a considerable distortion of the respective coordination environments. The original cubic coordination around the CaII cation in the fluorite structure is changed to an octahedral coordination of SnIV and a fourfold coordination of TeIV in the of the MIVTe3O8 compounds. Note that there are two additional O atoms at a distance of 3.2446 (19) Å around the MIV site and two pairs of additional O atoms at a distance of 2.9076 (12) and 3.3957 (13) Å around the Te1 site in SnTe3O8, completing an eightfold coordination in each case. Correspondingly, each of the two O sites has a fourfold coordination in case the much longer distances are counted.
A quantitative structural comparison of the MIVTe3O8 structures where single crystal data are available (M = Ti, Zr, Sn) was undertaken with the program compstru (de la Flor et al., 2016) available at the Bilbao Crystallographic Server (Aroyo et al., 2006). Table 2 lists the degree of (S), the maximum distance between the atomic positions of paired atoms (|u|), the arithmetic mean of all distances, and the measure of similarity (Δ) relative to SnTe3O8 as the reference structure. All these values show a very high similarity between the crystal structures in the isotypic MIVTe3O8 series.
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3. Synthesis and crystallization
Reagent-grade chemicals were used without further purification. SnO2 (71 mg, 0.47 mmol) and TeO2 (225 mg, 1.40 mmol) were thoroughly mixed in the molar ratio 1:3 and placed in a silica tube to which 50 mg of TeCl4 were added as the transport agent. The silica ampoule was then evacuated and torch-sealed, placed in a two-zone furnace using a temperature gradient 973 K (source) → 873 K (sink) for three days. Cubic, canary-yellow crystals had formed in the millimetre size range in the colder sink region as the only product (Fig. 3). Powder X-ray diffraction of the remaining material in the source region revealed SnTe3O8 as the main phase and SnO2 as a side phase. For the single-crystal diffraction study, a fragment was broken from a larger crystal.
4. Refinement
Crystal data, data collection and structure . Atomic coordinates and the labelling scheme were adapted from isotypic TiTe3O8 (Meunier & Galy, 1971).
details are summarized in Table 3
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Supporting information
CCDC reference: 2120742
https://doi.org/10.1107/S2056989021011828/hb7998sup1.cif
contains datablock I. DOI:Structure factors: contains datablock I. DOI: https://doi.org/10.1107/S2056989021011828/hb7998Isup2.hkl
Data collection: APEX3 (Bruker, 2018); cell
SAINT (Bruker, 2018); data reduction: SAINT (Bruker, 2018); program(s) used to solve structure: coordinates from previous program(s) used to refine structure: SHELXL (Sheldrick, 2015); molecular graphics: ATOMS (Dowty, 2006); software used to prepare material for publication: publCIF (Westrip, 2010).SnTe3O8 | Mo Kα radiation, λ = 0.71073 Å |
Mr = 629.49 | Cell parameters from 5266 reflections |
Cubic, Ia3 | θ = 3.7–38.9° |
a = 11.1574 (4) Å | µ = 16.04 mm−1 |
V = 1388.96 (15) Å3 | T = 296 K |
Z = 8 | Plate, light yellow |
F(000) = 2160 | 0.06 × 0.06 × 0.01 mm |
Dx = 6.021 Mg m−3 |
Bruker APEXII CCD diffractometer | 697 reflections with I > 2σ(I) |
ω– and φ–scans | Rint = 0.048 |
Absorption correction: multi-scan (SADABS; Krause et al., 2015) | θmax = 40.2°, θmin = 3.7° |
Tmin = 0.452, Tmax = 0.748 | h = −18→20 |
14087 measured reflections | k = −20→20 |
735 independent reflections | l = −19→20 |
Refinement on F2 | 0 restraints |
Least-squares matrix: full | w = 1/[σ2(Fo2) + (0.0127P)2 + 1.9293P] where P = (Fo2 + 2Fc2)/3 |
R[F2 > 2σ(F2)] = 0.014 | (Δ/σ)max = 0.001 |
wR(F2) = 0.030 | Δρmax = 1.27 e Å−3 |
S = 1.07 | Δρmin = −0.85 e Å−3 |
735 reflections | Extinction correction: SHELXL-2017/1 (Sheldrick 2015), Fc*=kFc[1+0.001xFc2λ3/sin(2θ)]-1/4 |
21 parameters | Extinction coefficient: 0.00046 (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. |
x | y | z | Uiso*/Ueq | ||
Sn1 | 0.000000 | 0.000000 | 0.000000 | 0.00501 (4) | |
Te1 | 0.20584 (2) | 0.000000 | 0.250000 | 0.00804 (4) | |
O1 | 0.43242 (10) | 0.13738 (10) | 0.39972 (11) | 0.0129 (2) | |
O2 | 0.16789 (10) | 0.16789 (10) | 0.16789 (10) | 0.0078 (3) |
U11 | U22 | U33 | U12 | U13 | U23 | |
Sn1 | 0.00501 (4) | 0.00501 (4) | 0.00501 (4) | −0.00031 (3) | −0.00031 (3) | −0.00031 (3) |
Te1 | 0.00518 (5) | 0.01273 (6) | 0.00620 (5) | 0.000 | 0.000 | −0.00229 (4) |
O1 | 0.0095 (4) | 0.0117 (4) | 0.0174 (5) | 0.0019 (3) | 0.0018 (4) | 0.0094 (4) |
O2 | 0.0078 (3) | 0.0078 (3) | 0.0078 (3) | 0.0020 (3) | 0.0020 (3) | 0.0020 (3) |
Sn1—O1i | 2.0421 (11) | Sn1—O1vi | 2.0421 (11) |
Sn1—O1ii | 2.0421 (11) | Te1—O1v | 1.8800 (11) |
Sn1—O1iii | 2.0421 (11) | Te1—O1vii | 1.8800 (11) |
Sn1—O1iv | 2.0421 (11) | Te1—O2viii | 2.1278 (3) |
Sn1—O1v | 2.0421 (11) | Te1—O2 | 2.1278 (3) |
O1i—Sn1—O1ii | 86.09 (4) | O1iv—Sn1—O1vi | 93.91 (4) |
O1i—Sn1—O1iii | 93.91 (4) | O1v—Sn1—O1vi | 86.09 (4) |
O1ii—Sn1—O1iii | 180.00 (9) | O1v—Te1—O1vii | 102.42 (8) |
O1i—Sn1—O1iv | 86.09 (4) | O1v—Te1—O2viii | 79.05 (4) |
O1ii—Sn1—O1iv | 93.91 (4) | O1vii—Te1—O2viii | 86.60 (6) |
O1iii—Sn1—O1iv | 86.09 (4) | O1v—Te1—O2 | 86.60 (6) |
O1i—Sn1—O1v | 93.91 (4) | O1vii—Te1—O2 | 79.05 (4) |
O1ii—Sn1—O1v | 86.09 (4) | O2viii—Te1—O2 | 157.05 (6) |
O1iii—Sn1—O1v | 93.91 (4) | Te1ix—O1—Sn1x | 134.17 (6) |
O1iv—Sn1—O1v | 180.00 (9) | Te1—O2—Te1xi | 117.94 (2) |
O1i—Sn1—O1vi | 180.00 (9) | Te1—O2—Te1xii | 117.94 (2) |
O1ii—Sn1—O1vi | 93.91 (4) | Te1xi—O2—Te1xii | 117.94 (2) |
O1iii—Sn1—O1vi | 86.09 (4) |
Symmetry codes: (i) y, −z+1/2, x−1/2; (ii) −x+1/2, −y, z−1/2; (iii) x−1/2, y, −z+1/2; (iv) z−1/2, −x+1/2, −y; (v) −z+1/2, x−1/2, y; (vi) −y, z−1/2, −x+1/2; (vii) −z+1/2, −x+1/2, −y+1/2; (viii) x, −y, −z+1/2; (ix) −y+1/2, −z+1/2, −x+1/2; (x) −x+1/2, −y, z+1/2; (xi) z, x, y; (xii) y, z, x. |
TiTe3O8 a | (Ti0.96Fe0.04)Te3O8 b | ZrTe3O8c | ZrTe3O8 d | |
MIV1 | 0 | 0 | 0 | 0 |
Te1 | 0.0475 | 0.0360 | 0.0065 | 0.0059 |
O1 | 0.1061 | 0.0834 | 0.0713 | 0.0694 |
O2 | 0.1374 | 0.0968 | 0.0543 | 0.0446 |
S | 0.0107 | 0.0102 | 0.0076 | 0.0092 |
dav | 0.0878 | 0.0668 | 0.0453 | 0.0436 |
Δ | 0.011 | 0.008 | 0.006 | 0.006 |
Notes: (a) a = 10.956 (3) Å; Meunier & Galy (1971); (b) a = 10.965 (1) Å; Bindi & Cipriani (2003); (c) a = 11.308 (1) Å; Noguera et al. (2003); (d) a = 11.340 (4) Å; Lu et al. (2019). |
Acknowledgements
The X-ray centre of the Vienna University of Technology is acknowledged for financial support and for providing access to the single-crystal and powder X-ray diffractometers.
References
Addison, A. W., Rao, T. N., Reedijk, J., van Rijn, J. & Verschoor, G. C. (1984). J. Chem. Soc. Dalton Trans. pp. 1349–1356. CSD CrossRef Web of Science Google Scholar
Aroyo, M. I., Perez-Mato, J. M., Capillas, C., Kroumova, E., Ivantchev, S., Madariaga, G., Kirov, A. & Wondratschek, H. (2006). Z. Kristallogr. 221, 15–27. Web of Science CrossRef CAS Google Scholar
Ben Aribia, W., Loukil, M., Kabadou, A. & Ben Salah, A. (2008). Powder Diffr. 23, 228–231. CAS Google Scholar
Bindi, L. & Cipriani, C. (2003). Can. Mineral. 41, 1469–1473. Web of Science CrossRef ICSD CAS Google Scholar
Binnewies, M., Glaum, R., Schmidt, M. & Schmidt, P. (2012). Chemical Vapor Transport Reactions. Berlin, Boston: De Gruyter,. Google Scholar
Brese, N. E. & O'Keeffe, M. (1991). Acta Cryst. B47, 192–197. CrossRef CAS Web of Science IUCr Journals Google Scholar
Brown, I. D. (2002). The Chemical Bond in Inorganic Chemistry: The Bond Valence Model. Oxford University Press. Google Scholar
Bruker (2018). APEX3 and SAINT. Bruker-AXS Inc. Madison, Wisconsin, USA. Google Scholar
Christy, A. G., Mills, S. J. & Kampf, A. R. (2016). Miner. Mag. 80, 415–545. Web of Science CrossRef CAS Google Scholar
Dowty, E. (2006). ATOMS. Shape Software, Kingsport, Tennessee, USA. Google Scholar
Flor, G. de la, Orobengoa, D., Tasci, E., Perez-Mato, J. M. & Aroyo, M. I. (2016). J. Appl. Cryst. 49, 653–664. Web of Science CrossRef IUCr Journals Google Scholar
Hamani, D., Masson, O. & Thomas, P. (2020). J. Appl. Cryst. 53, 1243–1251. Web of Science CrossRef CAS IUCr Journals Google Scholar
Kim, Y. H., Lee, D. W. & Ok, K. M. (2014). Inorg. Chem. 53, 5240–5245. Web of Science CrossRef ICSD CAS PubMed Google Scholar
Krause, L., Herbst-Irmer, R., Sheldrick, G. M. & Stalke, D. (2015). J. Appl. Cryst. 48, 3–10. Web of Science CSD CrossRef ICSD CAS IUCr Journals Google Scholar
Lu, W., Gao, Z., Du, X., Tian, X., Wu, Q., Li, C., Sun, Y., Liu, Y. & Tao, X. (2019). Inorg. Chem. 58, 7794–7802. Web of Science CrossRef ICSD PubMed Google Scholar
Meunier, G. & Galy, J. (1971). Acta Cryst. B27, 602–608. CrossRef ICSD IUCr Journals Web of Science Google Scholar
Missen, O. P., Weil, M., Mills, S. J. & Libowitzky, E. (2020). Acta Cryst. B76, 1–6. Web of Science CrossRef ICSD IUCr Journals Google Scholar
Noguera, O., Thomas, P., Masson, O. & Champarnaud-Mesjard, J. C. (2003). Z. Kristallogr. New Cryst. Struct. 218, 293–294. CrossRef ICSD CAS Google Scholar
Ra, H.-S., Ok, K. M. & Halasyamani, P. S. (2003). J. Am. Chem. Soc. 125, 7764–7765. Web of Science CrossRef ICSD PubMed CAS Google Scholar
Sheldrick, G. M. (2015). Acta Cryst. C71, 3–8. Web of Science CrossRef IUCr Journals Google Scholar
Stöger, B., Weil, M., Zobetz, E. & Giester, G. (2009). Acta Cryst. B65, 167–181. Web of Science CrossRef ICSD IUCr Journals Google Scholar
Subodh, G. & Sebastian, M. T. (2008). Jpn. J. Appl. Phys. 47, 7943–7946. Web of Science CrossRef CAS Google Scholar
Weil, M. (2019). Acta Cryst. E75, 26–29. Web of Science CrossRef ICSD IUCr Journals Google Scholar
Weil, M., Shirkhanlou, M., Füglein, E. & Libowitzky, E. (2018). Crystals, 8, 51. Web of Science CrossRef ICSD Google Scholar
Wells, A. F. (1975). Structural Inorganic Chemistry, 4th ed, pp. 207–208. Oxford: Clarendon Press. Google Scholar
Westrip, S. P. (2010). J. Appl. Cryst. 43, 920–925. Web of Science CrossRef CAS IUCr Journals Google Scholar
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