research communications
of strontium thiosulfate monohydrate
aTechnische Universität München, Department of Chemistry, Lichtenbergstr. 4, 85747 Garching, Germany
*Correspondence e-mail: wilhelm.klein@tum.de
SrS2O3·H2O was obtained from an aqueous solution of Na2S2O3 and Sr(NO3)2 and crystallizes in P with all atoms at general positions. The Sr2+ ion exhibits an [8 + 1] coordination defined by two terminal S and six O atoms of thiosulfate ions, one of the latter at a longer distance, and by one O atom of a water molecule. Two thiosulfate anions act as bidentate, four as monodentate ligands. The structure consists of mainly ionically interacting layers lying parallel to the crystallographic ab plane. The layers are connected by O—H⋯S and O—H⋯O hydrogen bonds of moderate strength.
Keywords: crystal structure; thiosulfate; strontium; hydrate; hydrogen bonding.
CCDC reference: 1977322
1. Chemical context
Although thiosulfuric acid and its salts are common topics in textbooks of inorganic chemistry, the preparation of the pure acid was achieved just recently by a sophisticated synthesis via reaction of Na2S2O3 and anhydrous HF (Hopfinger et al., 2018). Its salts are much better explored, as they are naturally and geologically widely spread (Caufield & Raiswell, 1999), and Na2S2O3, as well as (NH4)2S2O3, is produced on a large industrial scale (Barberá et al., 2012). To date, thiosulfates of alkaline earth metals are solely known as hydrates. For example, MgS2O3·6H2O has been investigated by Elerman et al. (1983) to determine its deformation electron density, and the first example of an S—H hydrogen bond that was confirmed by a single crystal-structure determination was found in BaS2O3·H2O (Manojlović-Muir, 1969).
Next to SrS2O3·5H2O (Held & Bohatý, 2004), the title compound represents the second known of a hydrate of strontium thiosulfate. As one route of preparation, the pentahydrate has been crystallized from aqueous solutions of Na2S2O3 and Sr(NO3)2, whereby these solutions were reported to show a tendency to decompose, inhibiting the growth of larger single crystals (Held & Bohatý, 2004). A possible step within the decomposition process, and maybe a competing product in a later stage of crystallization, might be associated with the monohydrate, the of which is presented here.
2. Structural commentary
SrS2O3·H2O crystallizes in the P with one formula unit in the and all atoms on general positions. Many structural features resemble the closely related pentahydrate of SrS2O3. The thiosulfate anion adopts a slightly distorted tetrahedral shape with a mean bond angle of 109.47° where the average O—S—O angles (110.32°) are slightly larger than the S—S—O angles (108.62°). Similar to the S—S bond length found in the pentahydrate (1.995 Å), the S—S bond length of 2.0044 (7) Å in the monohydrate is between those of the Ca (2.008 Å) and the Ba (1.979 Å) salts. The S—O bond lengths are between 1.466 (2) Å and 1.478 (2) Å and are in the same range as those of other alkaline earth thiosulfate hydrates (Table 1).
The Sr2+ cation is coordinated by five O and two S atoms, belonging to six neighbouring S2O32– anions, and one additional O atom of an H2O molecule. One of the anions acts as a bidentate S/O ligand, while the remaining five coordinate only via one S or O atom, respectively. These six O ligands are found in narrow Sr—O distances ranging from 2.531 (2) to 2.623 (2) Å, whereas the S atoms exhibit Sr—S distances of 3.1618 (6) and 3.2379 (6) Å. A more remote O atom at a distance of 3.305 (2) Å might also be ascribed to the first coordination sphere, although exhibiting a larger distance than the neighbouring S atoms. This [8 + 1] coordination of the Sr2+ atom (Fig. 1) again resembles the ninefold coordination of the cation in SrS2O3·5H2O, with the difference being that in the pentahydrate no S atoms are found in the first coordination sphere of Sr2+, but four water molecules instead. As a consequence of the presence of the larger S atoms close to Sr2+, in the title structure one O atom is shifted into an outer region of the coordination shell and thus is found at a considerably longer distance.
As a characteristic feature of the 2O3·H2O is made up from layers extending parallel to the crystallographic ab plane (Fig. 2). Within the layers, the condensed coordination polyhedra are packed alternately to form double sheets in such a way that the terminal S2 atoms and water molecules are directed towards the layer boundaries (Fig. 3). The layers are linked by hydrogen bonds of medium strength between the water molecules (O4⋯O4ii) and the water molecules and thiosulfate anions via S2 atoms (Table 2). This involves also a bifurcated hydrogen bond O4—H1⋯(O4ii/S2iii). The O4—H2⋯S2i bond as well as the D⋯A distances are in the same range as in SrS2O3·5H2O (Held & Bohatý, 2004). For the H1 atom, a disorder model similar to that proposed for BaS2O3·H2O (Manojlović-Muir, 1975) was considered, which would result in shorter and more linear O4—H1⋯O4ii and O4—H1⋯S2iii bonds. However, a reasonable of these disordered H atoms was not possible.
SrS
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A striking analogy to the packing of the pentahydrate structure (Fig. 4a) is apparent. With the presence of five water molecules instead of one, the main packing of ions in SrS2O3·5H2O is only slightly changed as a result of the coordination of additional water molecules to the Sr2+ cation and widened by two non-coordinating and hydrogen-bonded water molecules situated between the layers. The S—S bond is nearly orthogonal to the layer plane; however, the layer boundaries are also formed by S atoms and water molecules, both forming hydrogen bonds. The very close relationship between the two crystal structures suggests a topotactical degradation of the pentahydrate. Because both hydrates were crystallized at room temperature, a temperature dependence of the crystallization does not seem to be the only possible driving force. An ageing process triggered by concentration or thermodynamic stability must be taken into account as well. The degradation process, possibly running via another so far unknown trihydrate after removal of the free water molecules, was not investigated up to now, and in addition a of the title compound could not been carried out because of the presence of large amounts of indistinguishable crystalline by-products, viz. NaNO3 and Sr(NO3)2.
The orthorhombic structure of BaS2O3·H2O is likewise found to form layers, which are separated by water molecules (Fig. 4b; Nardelli & Fava, 1962; Manojlović-Muir, 1975). Similar to the Sr homologue, two terminal S atoms are part of the first coordination sphere of the Ba2+ cation which has, caused by the larger ion radius, a different environment, namely by five thiosulfate anions as bidentate ligands and one additional water molecule. Interestingly, while the number of atoms forming the first coordination sphere is higher in the Ba compound, the number of directly coordinating anions is smaller.
3. Database survey
Besides SrS2O3, determinations for three further alkaline-earth thiosulfates have been reported, all of them as hydrates: BaS2O3·H2O (Nardelli & Fava, 1962; Manojlović-Muir, 1975), CaS2O3·6H2O (Held & Bohatý, 2004), and MgS2O3·6H2O (Nardelli et al., 1962; Baggio et al., 1969; Elerman et al., 1982,1983). Together with the known Sr compounds, SrS2O3·5H2O (Held & Bohatý, 2004) and the new monohydrate, the trend of incorporating smaller amounts of water into stable crystal structures with increasing cation radius is obvious for alkaline-earth metal thiosulfates. With the exception of two of the five water molecules in SrS2O3·5H2O, all water molecules in these compounds coordinate to the divalent cations. This trend is confirmed by divalent transition-metal thiosulfates, as there are those of Ni as the hexahydrate (Elerman et al., 1978; isostructural with the Mg salt) and of Cd as the dihydrate (Baggio et al., 1997). The only of a hydrate-free thiosulfate of a divalent cation is reported for Pb (Christensen et al., 1991). Table 1 collates S—S and averaged S—O bond lengths in the corresponding structures of these thiosulfates.
4. Synthesis and crystallization
Crystals of SrS2O3·H2O were grown from an aqueous solution of Na2S2O3·5H2O and Sr(NO3)2. The solution was stored at room temperature and the solvent was evaporated very slowly over several months. Single crystals were isolated from highly concentrated solutions where only a little of the mother liquor remained. Besides the title compound, crystals of NaNO3 and surplus Sr(NO3)2 were also found, and all of these compounds were identified in the X-ray powder pattern of the reaction mixture after drying at room temperature. From all these experiments, no hints of the presence of the pentahydrate were found.
5. Refinement
Crystal data, data collection and structure . Hydrogen atoms were refined with a restrained O—H distance of 0.85 (5) Å and Uiso(H) = 1.5Ueq(O). A free of H-atom positions resulted in a reliable shape for the water molecule and orientation with respect to possible hydrogen bonds, but included one short O—H distance of only 0.5 Å.
details are summarized in Table 3
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Supporting information
CCDC reference: 1977322
https://doi.org/10.1107/S2056989020000353/wm5535sup1.cif
contains datablocks global, I. DOI:Structure factors: contains datablock I. DOI: https://doi.org/10.1107/S2056989020000353/wm5535Isup2.hkl
Data collection: APEX3 (Bruker, 2015); cell
SAINT (Bruker, 2015); data reduction: SAINT (Bruker, 2015); program(s) used to solve structure: SHELXS97 (Sheldrick, 2008); program(s) used to refine structure: SHELXL2014 (Sheldrick, 2015); molecular graphics: DIAMOND (Brandenburg & Putz, 2012); software used to prepare material for publication: publCIF (Westrip, 2010).SrS2O3·H2O | Z = 2 |
Mr = 217.76 | F(000) = 208 |
Triclinic, P1 | Dx = 2.944 Mg m−3 |
a = 4.6858 (2) Å | Mo Kα radiation, λ = 0.71073 Å |
b = 5.9178 (3) Å | Cell parameters from 7034 reflections |
c = 9.0167 (4) Å | θ = 2.3–30.6° |
α = 84.889 (2)° | µ = 11.72 mm−1 |
β = 87.284 (2)° | T = 297 K |
γ = 80.785 (2)° | Block, colourless |
V = 245.68 (2) Å3 | 0.42 × 0.30 × 0.16 mm |
Bruker APEXII CCD diffractometer | 1504 independent reflections |
Radiation source: rotating anode FR591 | 1481 reflections with I > 2σ(I) |
MONTEL optic monochromator | Rint = 0.054 |
Detector resolution: 16 pixels mm-1 | θmax = 30.6°, θmin = 2.3° |
φ– and ω–rotation scans | h = −6→6 |
Absorption correction: numerical (SADABS; Krause et al., 2015) | k = −8→8 |
Tmin = 0.037, Tmax = 0.264 | l = −12→12 |
8011 measured reflections |
Refinement on F2 | Secondary atom site location: difference Fourier map |
Least-squares matrix: full | Hydrogen site location: difference Fourier map |
R[F2 > 2σ(F2)] = 0.024 | Only H-atom coordinates refined |
wR(F2) = 0.061 | w = 1/[σ2(Fo2) + (0.0324P)2 + 0.2036P] where P = (Fo2 + 2Fc2)/3 |
S = 1.10 | (Δ/σ)max = 0.001 |
1504 reflections | Δρmax = 0.97 e Å−3 |
71 parameters | Δρmin = −0.86 e Å−3 |
2 restraints | Extinction correction: SHELXL2014 (Sheldrick, 2015), Fc*=kFc[1+0.001xFc2λ3/sin(2θ)]-1/4 |
Primary atom site location: structure-invariant direct methods | Extinction coefficient: 0.085 (5) |
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 | ||
Sr | 0.01493 (4) | 0.73223 (3) | 0.16811 (2) | 0.01372 (10) | |
S1 | 0.47043 (11) | 0.20793 (8) | 0.16097 (5) | 0.01113 (12) | |
S2 | 0.55500 (12) | 0.41404 (9) | 0.31260 (6) | 0.01678 (13) | |
O1 | 0.2582 (3) | 0.3477 (3) | 0.06042 (17) | 0.0163 (3) | |
O2 | 0.7385 (3) | 0.1265 (3) | 0.07573 (19) | 0.0178 (3) | |
O3 | 0.3580 (4) | 0.0090 (3) | 0.23659 (19) | 0.0221 (3) | |
O4 | −0.0933 (5) | 0.7998 (4) | 0.4397 (2) | 0.0309 (4) | |
H1 | 0.024 (9) | 0.827 (8) | 0.491 (5) | 0.046* | |
H2 | −0.223 (8) | 0.774 (7) | 0.487 (4) | 0.046* |
U11 | U22 | U33 | U12 | U13 | U23 | |
Sr | 0.01592 (13) | 0.01292 (12) | 0.01266 (13) | −0.00269 (7) | −0.00130 (7) | −0.00167 (7) |
S1 | 0.0116 (2) | 0.0105 (2) | 0.0117 (2) | −0.00225 (16) | −0.00057 (16) | −0.00182 (16) |
S2 | 0.0202 (3) | 0.0170 (2) | 0.0145 (2) | −0.00505 (19) | −0.00235 (19) | −0.00465 (18) |
O1 | 0.0159 (7) | 0.0160 (7) | 0.0168 (7) | 0.0000 (6) | −0.0053 (6) | −0.0030 (6) |
O2 | 0.0145 (7) | 0.0194 (7) | 0.0188 (7) | 0.0006 (6) | 0.0027 (6) | −0.0057 (6) |
O3 | 0.0316 (9) | 0.0187 (7) | 0.0191 (8) | −0.0146 (7) | −0.0033 (7) | 0.0023 (6) |
O4 | 0.0339 (11) | 0.0433 (11) | 0.0187 (9) | −0.0151 (9) | 0.0037 (8) | −0.0071 (8) |
Sr—O4 | 2.531 (2) | S1—O2 | 1.4768 (16) |
Sr—O2i | 2.5698 (16) | S1—O1 | 1.4776 (15) |
Sr—O2ii | 2.5708 (17) | S1—S2 | 2.0044 (7) |
Sr—O1iii | 2.5934 (15) | S1—Srvii | 3.4816 (5) |
Sr—O3iv | 2.6010 (17) | S2—Srviii | 3.2379 (6) |
Sr—O1 | 2.6226 (15) | O1—Sriii | 2.5934 (15) |
Sr—S2 | 3.1618 (6) | O2—Srvii | 2.5698 (16) |
Sr—S2v | 3.2379 (6) | O2—Srii | 2.5708 (16) |
Sr—O3i | 3.305 (2) | O3—Srix | 2.6010 (17) |
Sr—S1 | 3.4768 (5) | O3—Srvii | 3.305 (2) |
Sr—S1i | 3.4816 (5) | O4—H1 | 0.78 (4) |
Sr—Srvi | 4.1762 (4) | O4—H2 | 0.76 (3) |
S1—O3 | 1.4663 (16) | ||
O4—Sr—O2i | 93.29 (7) | O1iii—Sr—S1i | 80.94 (3) |
O4—Sr—O2ii | 145.14 (6) | O3iv—Sr—S1i | 86.26 (4) |
O2i—Sr—O2ii | 71.34 (6) | O1—Sr—S1i | 150.22 (3) |
O4—Sr—O1iii | 138.36 (6) | S2—Sr—S1i | 152.443 (14) |
O2i—Sr—O1iii | 75.45 (5) | S2v—Sr—S1i | 89.500 (14) |
O2ii—Sr—O1iii | 69.30 (5) | O3i—Sr—S1i | 24.78 (3) |
O4—Sr—O3iv | 73.47 (6) | S1—Sr—S1i | 170.625 (18) |
O2i—Sr—O3iv | 77.99 (6) | O4—Sr—Srvi | 122.71 (6) |
O2ii—Sr—O3iv | 72.79 (5) | O2i—Sr—Srvi | 35.68 (4) |
O1iii—Sr—O3iv | 138.90 (5) | O2ii—Sr—Srvi | 35.66 (4) |
O4—Sr—O1 | 126.88 (7) | O1iii—Sr—Srvi | 68.15 (3) |
O2i—Sr—O1 | 139.15 (5) | O3iv—Sr—Srvi | 71.93 (4) |
O2ii—Sr—O1 | 77.29 (5) | O1—Sr—Srvi | 109.27 (4) |
O1iii—Sr—O1 | 69.30 (5) | S2—Sr—Srvi | 129.735 (12) |
O3iv—Sr—O1 | 116.91 (6) | S2v—Sr—Srvi | 134.574 (12) |
O4—Sr—S2 | 80.16 (6) | O3i—Sr—Srvi | 80.32 (3) |
O2i—Sr—S2 | 152.24 (4) | S1—Sr—Srvi | 124.721 (11) |
O2ii—Sr—S2 | 98.85 (4) | S1i—Sr—Srvi | 58.002 (9) |
O1iii—Sr—S2 | 126.47 (3) | O3—S1—O2 | 108.96 (11) |
O3iv—Sr—S2 | 74.28 (4) | O3—S1—O1 | 112.09 (10) |
O1—Sr—S2 | 57.20 (3) | O2—S1—O1 | 109.91 (9) |
O4—Sr—S2v | 69.28 (5) | O3—S1—S2 | 109.49 (7) |
O2i—Sr—S2v | 108.83 (4) | O2—S1—S2 | 109.77 (7) |
O2ii—Sr—S2v | 144.82 (4) | O1—S1—S2 | 106.59 (7) |
O1iii—Sr—S2v | 76.67 (4) | O3—S1—Sr | 115.97 (8) |
O3iv—Sr—S2v | 142.38 (4) | O2—S1—Sr | 134.05 (7) |
O1—Sr—S2v | 82.74 (4) | O1—S1—Sr | 43.98 (6) |
S2—Sr—S2v | 94.134 (15) | S2—S1—Sr | 64.00 (2) |
O4—Sr—O3i | 65.98 (6) | O3—S1—Srvii | 70.87 (8) |
O2i—Sr—O3i | 46.05 (5) | O2—S1—Srvii | 41.53 (7) |
O2ii—Sr—O3i | 114.88 (5) | O1—S1—Srvii | 141.36 (6) |
O1iii—Sr—O3i | 78.38 (4) | S2—S1—Srvii | 108.24 (2) |
O3iv—Sr—O3i | 104.37 (6) | Sr—S1—Srvii | 170.625 (18) |
O1—Sr—O3i | 138.65 (4) | S1—S2—Sr | 81.26 (2) |
S2—Sr—O3i | 144.49 (3) | S1—S2—Srviii | 109.00 (2) |
S2v—Sr—O3i | 64.83 (3) | Sr—S2—Srviii | 94.134 (15) |
O4—Sr—S1 | 106.66 (6) | S1—O1—Sriii | 134.66 (9) |
O2i—Sr—S1 | 159.58 (4) | S1—O1—Sr | 112.99 (8) |
O2ii—Sr—S1 | 89.34 (4) | Sriii—O1—Sr | 110.70 (5) |
O1iii—Sr—S1 | 91.84 (3) | S1—O2—Srvii | 116.07 (9) |
O3iv—Sr—S1 | 103.11 (4) | S1—O2—Srii | 134.93 (10) |
O1—Sr—S1 | 23.03 (3) | Srvii—O2—Srii | 108.66 (6) |
S2—Sr—S1 | 34.737 (12) | S1—O3—Srix | 135.58 (10) |
S2v—Sr—S1 | 82.985 (14) | S1—O3—Srvii | 84.35 (8) |
O3i—Sr—S1 | 147.67 (3) | Srix—O3—Srvii | 104.37 (6) |
O4—Sr—S1i | 75.63 (6) | Sr—O4—H1 | 122 (3) |
O2i—Sr—S1i | 22.40 (4) | Sr—O4—H2 | 128 (3) |
O2ii—Sr—S1i | 93.64 (4) | H1—O4—H2 | 109 (4) |
Symmetry codes: (i) x−1, y+1, z; (ii) −x+1, −y+1, −z; (iii) −x, −y+1, −z; (iv) x, y+1, z; (v) x−1, y, z; (vi) −x, −y+2, −z; (vii) x+1, y−1, z; (viii) x+1, y, z; (ix) x, y−1, z. |
D—H···A | D—H | H···A | D···A | D—H···A |
O4—H2···S2x | 0.76 (3) | 2.62 (4) | 3.344 (2) | 163 (4) |
O4—H1···O4xi | 0.78 (4) | 2.42 (4) | 2.962 (4) | 128 (4) |
O4—H1···S2xii | 0.78 (4) | 2.84 (4) | 3.458 (2) | 138 (4) |
Symmetry codes: (x) −x, −y+1, −z+1; (xi) −x, −y+2, −z+1; (xii) −x+1, −y+1, −z+1. |
Cation/solvent molecules | S—S | mean S—O |
Ba2+/1 H2Oa | 1.979 | 1.477 |
Sr2+/5 H2Ob | 1.995 | 1.472 |
Sr2+/1 H2Oc | 2.004 | 1.474 |
Ca2+/6 H2Ob | 2.008 | 1.468 |
Mg2+/6 H2Od | 2.019 | 1.471 |
Ni2+/6 H2Oe | 2.015 | 1.459 |
Cd2+/2 H2Of | 2.056 | 1.454 |
Pb2+/0 H2Og | 2.11 | 1.455 |
Notes: (a) Manojlović-Muir (1975); (b) Held & Bohatý (2004); (c) this work; (d) Elerman et al. (1983); (e) Elerman et al. (1978); (f) Baggio et al. (1997); (g) Christensen et al. (1991). |
Funding information
This work was supported by the Technische Universität München within the funding programme Open Access Publishing.
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