research communications
of tin(IV) chloride octahydrate
aTU Bergakademie Freiberg, Institute of Inorganic Chemistry, Leipziger Strasse 29, D-09596 Freiberg, Germany
*Correspondence e-mail: horst.schmidt@chemie.tu-freiberg.de
The title compound, [SnCl4(H2O)2]·6H2O, was crystallized according to the solid–liquid phase diagram at lower temperatures. It is built-up of SnCl4(H2O)2 octahedral units (point group symmetry 2) and lattice water molecules. An intricate three-dimensional network of O—H⋯O and O—H⋯Cl hydrogen bonds between the complex molecules and the lattice water molecules is formed in the crystal structure.
Keywords: crystals structure; low-temperature salt hydrates; tin(IV) salts.
CCDC reference: 1032661
1. Chemical context
The interest in the stability of tin(IV) salts, especially at lower temperatures, has increased with the recent new determination of the et al., 2009). The phase diagram of tin(IV) chloride is not well investigated. Only some points in dilute solutions have been determined by Loomis (1897). For the existing hydrates (R = 8, 5, 4, 3 and 2), Meyerhoffer (1891) described the melting points and the existence fields. The crystal structures of the dihydrate (Semenov et al., 2005), trihydrate (Genge et al., 2004; Semenov et al., 2005), tetrahydrate (Genge et al., 2004; Shihada et al., 2004) and pentahydrate (Barnes et al., 1980; Shihada et al., 2004) have been determined previously. For these salt hydrates, vibrational spectra are also available, classifying all hydrate spectra with D4h symmetry (Brune & Zeil, 1962).
in aqueous solutions, which is complicated by the presence of chlorido complexes (Gajda2. Structural commentary
The tin(IV) ion in tin(IV) chloride octahydrate is situated on a twofold rotation axis and is coordinated by four Cl atoms and two water molecules in a cis-octahedral geometry (Fig. 1), as was observed before for the tetra- and pentahydrate (Shihada et al., 2004). In addition, three water molecules (O1, O2 and O3) are located around the octahedra as non-coordinating water molecules. Every water molecule of the first coordination sphere is connected with two water molecules of the second shell by hydrogen bonds. The chlorine atoms form only one hydrogen bond towards `free' water molecules of the second shell (Fig. 2).
3. Supramolecular features
Having a larger view of the ), it becomes obvious that these non-coordinating water molecules form chains between the octahedrally coordinated tin(IV) ions. These water molecules (O1 and O2) are connected via hydrogen bonds (Table 1) and the chains are oriented along the b-axis direction. Considering all types of hydrogen bonding, a three-dimensional network between the complex molecules and the lattice water molecules results.
in direction [001] (Fig. 34. Database survey
For et al. (2004); Semenov et al. (2005); Genge et al. (2004); Barnes et al. (1980).
determination of other tin(IV) chloride hydrates, see: Shihada5. Synthesis and crystallization
Tin(IV) chloride octahydrate was crystallized from an aqueous solution of 53.39 wt% SnCl4 at 263 K after 2 d. For preparing this solution, tin(IV) chloride pentahydrate (Acros Organics, 98%) was used. The content of Cl− was analysed by titration with AgNO3. The crystals are stable in their over a period of at least four weeks.
The samples were stored in a freezer or a cryostat at low temperatures. The crystals were separated and embedded in perfluorinated ether for X-ray diffraction analysis
6. Refinement
Crystal data, data collection and structure . The H atoms were placed in the positions indicated by difference Fourier maps. Distance restraints were applied for the geometries of all water molecules, with O—H and H—H distance restraints of 0.84 (1) and 1.4 (1) Å, respectively.
details are summarized in Table 2
|
Supporting information
CCDC reference: 1032661
10.1107/S1600536814024271/br2243sup1.cif
contains datablock I. DOI:Structure factors: contains datablock I. DOI: 10.1107/S1600536814024271/br2243Isup2.hkl
The interest in the stability of tin(IV) salts, especially at lower temperatures, has increased with the recent new determination of the
in aqueous solutions, which is complicated by the presence of chlorocomplexes (Gajda et al., 2009). The phase diagram of tin(IV) chloride is not well investigated. Only some points in dilute solutions have been determined by Loomis (1897). For the existing hydrates (R = 8, 5, 4, 3 and 2), Meyerhoffer (1891) described the melting points and the existence fields. The crystal structures of the dihydrate (Semenov et al., 2005), trihydrate (Genge et al., 2004; Semenov et al., 2005), tetrahydrate (Genge et al., 2004; Shihada et al., 2004) and pentahydrate (Shihada et al., 2004) have been determined previously. For these salt hydrates, vibrational spectra are also available, classifying all hydrate spectra with D4h symmetry (Brune & Zeil, 1962).The tin(IV) ion in tin(IV) chloride octahydrate is coordinated by four Cl atoms and two water molecules in a cis geometry (Fig. 1), as was observed before for the tetra- and pentahydrate (Shihada et al., 2004). In addition, three water molecules (O1, O2 and O3) are located around the octahedra as non-coordinating water molecules. Every water molecule of the first coordination sphere is connected with two water molecules of the second shell by hydrogen bonds. The chlorine atoms form only one hydrogen bond towards `free' water molecules of the second shell (Fig. 2).
Having a larger view of the
in direction [001] (Fig. 3), it becomes obvious that these non-coordinating water molecules form chains between the octahedrally coordinated tin(IV) ions. These water molecules (O1 and O2) are connected via hydrogen bonds (Table 1) and the chains are oriented along the b-axis direction.For
determination of other tin(IV)chloride hydrates, see: Shihada et al. (2004); Semenov et al. (2005); Genge et al. (2004); Barnes et al. (1980).Tin(IV) chloride octahydrate was crystallized from an aqueous solution of 53.39 wt% SnCl4 at 263 K after 2 d. For preparing this solution, tin(IV)chloride pentahydrate (Acros Organics, 98%) was used. The content of Cl- was analysed by titration with AgNO3. The crystals are stable in their
over a period of at least four weeks.The samples were stored in a freezer or a cryostat at low temperatures. The crystals were separated and embedded in perfluorinated ether for X-ray diffraction analysis
Data collection: X-AREA (Stoe & Cie, 2009); cell
X-AREA (Stoe & Cie, 2009); data reduction: X-RED (Stoe & Cie, 2009); program(s) used to solve structure: SHELXS97 (Sheldrick, 2008); program(s) used to refine structure: SHELXL2012 (Sheldrick, 2008); molecular graphics: DIAMOND (Brandenburg, 2006); software used to prepare material for publication: publCIF (Westrip, 2010).The molecular unit in tin(IV) chloride octahydrate [symmetry code: (i) -x, y, -z+1/2]. The coordination in the second coordination shell in tin(IV) chloride octahydrate [symmetry code: (i) -x, y, -z+1/2]. Formation of chains by water molecules O1 and O2 (bold). Dashed lines indicate hydrogen bonds. |
[SnCl4(H2O)2]·6H2O | F(000) = 792 |
Mr = 404.62 | Dx = 1.941 Mg m−3 |
Monoclinic, C2/c | Mo Kα radiation, λ = 0.71073 Å |
a = 16.0224 (15) Å | Cell parameters from 13366 reflections |
b = 7.8530 (8) Å | θ = 1.8–29.6° |
c = 12.6766 (12) Å | µ = 2.63 mm−1 |
β = 119.739 (7)° | T = 200 K |
V = 1384.9 (2) Å3 | Plate, colourless |
Z = 4 | 0.34 × 0.23 × 0.12 mm |
Stoe IPDS 2T diffractometer | 1600 independent reflections |
Radiation source: fine-focus sealed tube | 1451 reflections with I > 2σ(I) |
Detector resolution: 6.67 pixels mm-1 | Rint = 0.030 |
rotation method scans | θmax = 27.5°, θmin = 2.9° |
Absorption correction: integration (Coppens, 1970) | h = −22→21 |
Tmin = 0.492, Tmax = 0.731 | k = −10→10 |
13041 measured reflections | l = −17→17 |
Refinement on F2 | 12 restraints |
Least-squares matrix: full | Hydrogen site location: difference Fourier map |
R[F2 > 2σ(F2)] = 0.021 | All H-atom parameters refined |
wR(F2) = 0.049 | w = 1/[σ2(Fo2) + (0.0133P)2 + 4.9358P] where P = (Fo2 + 2Fc2)/3 |
S = 1.11 | (Δ/σ)max = 0.001 |
1600 reflections | Δρmax = 1.01 e Å−3 |
92 parameters | Δρmin = −0.71 e Å−3 |
[SnCl4(H2O)2]·6H2O | V = 1384.9 (2) Å3 |
Mr = 404.62 | Z = 4 |
Monoclinic, C2/c | Mo Kα radiation |
a = 16.0224 (15) Å | µ = 2.63 mm−1 |
b = 7.8530 (8) Å | T = 200 K |
c = 12.6766 (12) Å | 0.34 × 0.23 × 0.12 mm |
β = 119.739 (7)° |
Stoe IPDS 2T diffractometer | 1600 independent reflections |
Absorption correction: integration (Coppens, 1970) | 1451 reflections with I > 2σ(I) |
Tmin = 0.492, Tmax = 0.731 | Rint = 0.030 |
13041 measured reflections |
R[F2 > 2σ(F2)] = 0.021 | 12 restraints |
wR(F2) = 0.049 | All H-atom parameters refined |
S = 1.11 | Δρmax = 1.01 e Å−3 |
1600 reflections | Δρmin = −0.71 e Å−3 |
92 parameters |
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 | 0.0000 | 0.86619 (3) | 0.2500 | 0.02527 (8) | |
Cl3 | 0.17022 (5) | 0.89264 (10) | 0.37662 (6) | 0.04076 (17) | |
O4 | −0.00709 (13) | 1.0623 (3) | 0.35862 (18) | 0.0342 (4) | |
Cl1 | 0.01591 (7) | 0.66227 (10) | 0.12053 (8) | 0.0504 (2) | |
O1 | 0.83339 (14) | 0.1224 (3) | 0.35849 (18) | 0.0341 (4) | |
O2 | 0.24917 (15) | 0.3119 (3) | 0.34936 (19) | 0.0377 (4) | |
O3 | 0.11311 (15) | 0.3211 (3) | 0.4228 (2) | 0.0380 (4) | |
H4A | 0.030 (2) | 1.146 (3) | 0.376 (3) | 0.057 (11)* | |
H4B | −0.0574 (14) | 1.086 (4) | 0.359 (3) | 0.044 (9)* | |
H3B | 0.085 (3) | 0.414 (3) | 0.414 (4) | 0.070 (13)* | |
H3A | 0.145 (3) | 0.326 (6) | 0.387 (4) | 0.082 (15)* | |
H1A | 0.837 (3) | 0.169 (5) | 0.420 (2) | 0.063 (12)* | |
H2A | 0.270 (4) | 0.405 (3) | 0.341 (5) | 0.100 (18)* | |
H2B | 0.291 (3) | 0.251 (5) | 0.404 (3) | 0.099 (18)* | |
H1B | 0.805 (4) | 0.190 (6) | 0.299 (4) | 0.14 (2)* |
U11 | U22 | U33 | U12 | U13 | U23 | |
Sn1 | 0.03433 (13) | 0.02255 (12) | 0.02383 (12) | 0.000 | 0.01815 (10) | 0.000 |
Cl3 | 0.0320 (3) | 0.0591 (4) | 0.0315 (3) | 0.0162 (3) | 0.0161 (3) | 0.0064 (3) |
O4 | 0.0290 (9) | 0.0348 (10) | 0.0440 (10) | −0.0046 (8) | 0.0220 (8) | −0.0141 (9) |
Cl1 | 0.0809 (6) | 0.0363 (4) | 0.0615 (5) | −0.0147 (4) | 0.0563 (5) | −0.0188 (3) |
O1 | 0.0356 (10) | 0.0410 (11) | 0.0311 (9) | 0.0046 (8) | 0.0206 (8) | −0.0013 (8) |
O2 | 0.0387 (11) | 0.0412 (11) | 0.0372 (10) | −0.0055 (9) | 0.0218 (9) | −0.0020 (9) |
O3 | 0.0369 (10) | 0.0334 (10) | 0.0508 (12) | −0.0016 (8) | 0.0273 (10) | −0.0054 (9) |
Sn1—O4 | 2.1064 (18) | Sn1—Cl3 | 2.3906 (7) |
Sn1—O4i | 2.1064 (18) | Sn1—Cl1 | 2.3954 (7) |
Sn1—Cl3i | 2.3906 (7) | Sn1—Cl1i | 2.3954 (7) |
O4—Sn1—O4i | 86.01 (12) | Cl3i—Sn1—Cl1 | 94.12 (3) |
O4—Sn1—Cl3i | 87.81 (6) | Cl3—Sn1—Cl1 | 92.55 (3) |
O4i—Sn1—Cl3i | 84.90 (5) | O4—Sn1—Cl1i | 88.99 (6) |
O4—Sn1—Cl3 | 84.90 (5) | O4i—Sn1—Cl1i | 174.47 (6) |
O4i—Sn1—Cl3 | 87.81 (6) | Cl3i—Sn1—Cl1i | 92.55 (3) |
Cl3i—Sn1—Cl3 | 170.03 (4) | Cl3—Sn1—Cl1i | 94.12 (3) |
O4—Sn1—Cl1 | 174.47 (6) | Cl1—Sn1—Cl1i | 96.09 (4) |
O4i—Sn1—Cl1 | 88.99 (6) |
Symmetry code: (i) −x, y, −z+1/2. |
D—H···A | D—H | H···A | D···A | D—H···A |
O1—H1B···O2ii | 0.84 (1) | 1.90 (2) | 2.729 (3) | 169 (6) |
O2—H2B···O3iii | 0.84 (1) | 2.04 (2) | 2.825 (3) | 157 (5) |
O2—H2A···O1iv | 0.84 (1) | 1.94 (2) | 2.762 (3) | 168 (5) |
O1—H1A···Cl3v | 0.84 (1) | 2.68 (3) | 3.389 (2) | 143 (4) |
O3—H3A···O2 | 0.84 (1) | 1.95 (2) | 2.763 (3) | 163 (4) |
O3—H3B···Cl1i | 0.83 (1) | 2.43 (1) | 3.260 (2) | 173 (4) |
O4—H4B···O1vi | 0.83 (1) | 1.77 (1) | 2.598 (3) | 176 (4) |
O4—H4A···O3vii | 0.84 (1) | 1.80 (1) | 2.635 (3) | 176 (4) |
Symmetry codes: (i) −x, y, −z+1/2; (ii) −x+1, y, −z+1/2; (iii) −x+1/2, −y+1/2, −z+1; (iv) x−1/2, y+1/2, z; (v) −x+1, −y+1, −z+1; (vi) x−1, y+1, z; (vii) x, y+1, z. |
D—H···A | D—H | H···A | D···A | D—H···A |
O1—H1B···O2i | 0.840 (10) | 1.900 (16) | 2.729 (3) | 169 (6) |
O2—H2B···O3ii | 0.835 (10) | 2.04 (2) | 2.825 (3) | 157 (5) |
O2—H2A···O1iii | 0.837 (10) | 1.938 (15) | 2.762 (3) | 168 (5) |
O1—H1A···Cl3iv | 0.836 (10) | 2.68 (3) | 3.389 (2) | 143 (4) |
O3—H3A···O2 | 0.837 (10) | 1.952 (17) | 2.763 (3) | 163 (4) |
O3—H3B···Cl1v | 0.834 (10) | 2.431 (11) | 3.260 (2) | 173 (4) |
O4—H4B···O1vi | 0.833 (10) | 1.767 (11) | 2.598 (3) | 176 (4) |
O4—H4A···O3vii | 0.837 (10) | 1.800 (11) | 2.635 (3) | 176 (4) |
Symmetry codes: (i) −x+1, y, −z+1/2; (ii) −x+1/2, −y+1/2, −z+1; (iii) x−1/2, y+1/2, z; (iv) −x+1, −y+1, −z+1; (v) −x, y, −z+1/2; (vi) x−1, y+1, z; (vii) x, y+1, z. |
Experimental details
Crystal data | |
Chemical formula | [SnCl4(H2O)2]·6H2O |
Mr | 404.62 |
Crystal system, space group | Monoclinic, C2/c |
Temperature (K) | 200 |
a, b, c (Å) | 16.0224 (15), 7.8530 (8), 12.6766 (12) |
β (°) | 119.739 (7) |
V (Å3) | 1384.9 (2) |
Z | 4 |
Radiation type | Mo Kα |
µ (mm−1) | 2.63 |
Crystal size (mm) | 0.34 × 0.23 × 0.12 |
Data collection | |
Diffractometer | Stoe IPDS 2T diffractometer |
Absorption correction | Integration (Coppens, 1970) |
Tmin, Tmax | 0.492, 0.731 |
No. of measured, independent and observed [I > 2σ(I)] reflections | 13041, 1600, 1451 |
Rint | 0.030 |
(sin θ/λ)max (Å−1) | 0.650 |
Refinement | |
R[F2 > 2σ(F2)], wR(F2), S | 0.021, 0.049, 1.11 |
No. of reflections | 1600 |
No. of parameters | 92 |
No. of restraints | 12 |
H-atom treatment | All H-atom parameters refined |
Δρmax, Δρmin (e Å−3) | 1.01, −0.71 |
Computer programs: X-AREA (Stoe & Cie, 2009), X-RED (Stoe & Cie, 2009), SHELXS97 (Sheldrick, 2008), SHELXL2012 (Sheldrick, 2008), DIAMOND (Brandenburg, 2006), publCIF (Westrip, 2010).
References
Barnes, J. C., Sampson, H. A. & Weakley, T. J. R. (1980). J. Chem. Soc. Dalton Trans. pp. 949–953. CSD CrossRef Web of Science Google Scholar
Brandenburg, K. (2006). DIAMOND. Crystal Impact GbR, Bonn, Germany. Google Scholar
Brune, H. A. & Zeil, W. (1962). Z. Phys. Chem. Neue Folge, 32, 384–400. CrossRef CAS Google Scholar
Coppens, P. (1970). In Crystallographic Computing, edited by F. R. Ahmed, S. R. Hall & C. P. Huber, pp. 255–270. Copenhagen: Munksgaard. Google Scholar
Gajda, T., Sipos, P. & Gamsjäger, H. (2009). Monatsh. Chem. 140, 1293–1303. Web of Science CrossRef CAS Google Scholar
Genge, A. R. J., Levason, W., Patel, R., Reid, G. & Webster, M. (2004). Acta Cryst. C60, i47–i49. Web of Science CrossRef CAS IUCr Journals Google Scholar
Loomis, E. H. (1897). Phys. Rev. (Series I), 4, 273–296. Google Scholar
Meyerhoffer, M. (1891). Bull. Soc. Chem. Paris, 3, 85–86. Google Scholar
Semenov, S. N., Maltsev, E. Y., Timokhin, I. G., Drozdov, A. A. & Troyanov, S. I. (2005). Mendeleev Commun. 15, 205–207. Web of Science CrossRef Google Scholar
Sheldrick, G. M. (2008). Acta Cryst. A64, 112–122. Web of Science CrossRef CAS IUCr Journals Google Scholar
Shihada, A.-F., Abushamleh, A. S. & Weller, F. (2004). Z. Anorg. Allg. Chem. 630, 841–847. Web of Science CSD CrossRef CAS Google Scholar
Stoe & Cie (2009). X-AREA and X-RED. Stoe & Cie, Darmstadt, Germany. Google Scholar
Westrip, S. P. (2010). J. Appl. Cryst. 43, 920–925. Web of Science CrossRef CAS IUCr Journals Google Scholar
This is an open-access article distributed under the terms of the Creative Commons Attribution (CC-BY) Licence, which permits unrestricted use, distribution, and reproduction in any medium, provided the original authors and source are cited.