research communications
of lead(II) tartrate: a redetermination
aInstitute for Chemical Technologies and Analytics, Division of Structural Chemistry, Vienna University of Technology, Getreidemarkt 9/164-SC, A-1060 Vienna, Austria
*Correspondence e-mail: mweil@mail.zserv.tuwien.ac.at
Single crystals of poly[μ4-tartrato-κ6O1,O3:O1′:O2,O4:O4′-lead], [Pb(C4H4O6)]n, were grown in a gel medium. In comparison with the previous of this compound from laboratory powder X-ray diffraction data [De Ridder et al. (2002). Acta Cryst. C58, m596–m598], the redetermination on the basis of single-crystal data reveals the all atoms with anisotropic displacement parameters and a much higher accuracy in terms of bond lengths and angles. It could be shown that a different or incorporation of water as reported for similarly gel-grown lead tartrate crystals is incorrect. In the structure, each Pb2+ cation is bonded to eight O atoms of five tartrate anions, while each tartrate anion links four Pb2+ cations. The resulting three-dimensional framework is stabilized by O—H⋯O hydrogen bonds between the OH groups of one tartrate anion and the carboxylate O atoms of adjacent anions.
Keywords: crystal structure; lead tartrate; gel growth; redetermination; O—H⋯O hydrogen bonds.
CCDC reference: 1039408
1. Chemical context
Crystal growth in gels (Henisch, 1970) is a convenient method to obtain single crystals of high quality from compounds with rather low solubility products. Therefore gel growth was the method of choice for single-crystal growth of the low-soluble fluorophosphate BaPO3F. This compound is interesting insofar as the polycrystalline material (prepared by fast precipitation) has orthorhombic symmetry whereas single crystals grown slowly in a gel have monoclinic symmetry. Both the orthorhombic and monoclinic BaPO3F phases belong to the same order–disorder (OD) family and can be derived from the baryte (BaSO4) structure type by replacing the SO42− anions with isoelectronic PO3F2− anions in two orientations (Stöger et al., 2013). The same baryte-type structure has been reported for PbPO3F on the basis of similar lattice parameters and of reflections (Walford, 1967). However, structural details were not determined at that time. In analogy with the barium compound, it was intended to grow crystals of lead fluorophosphate in a gel medium. In order to take into account the somewhat lower solubility of PbPO3F in comparison with BaPO3F (Lange, 1929), crystal-growth experiments were performed with lead salts in ammoniacal tartrate solutions to produce a soluble, poorly dissociated lead tartrate complex which lowers the concentration of Pb2+ to such an extent that its direct precipitation is prevented. In fact, after some days colourless single crystals appeared in the gel medium that, on the basis of unit-cell determinations, turned out to be lead tartrate, [Pb(C4H4O6)]. The structure of this compound was originally solved and refined from laboratory X-ray powder diffraction data in P212121 (De Ridder et al., 2002). However, some years later it was reported that gel-grown lead tartrate crystallizes as a dihydrate (Lillybai & Rahimkutty, 2010) or in a different (Pna21; Labutina et al., 2011). Motivated by these disagreements, it was decided to re-investigate the of gel-grown lead tartrate on the basis of single-crystal diffraction data for an unambiguous determination of the and the composition, and to obtain more precise results compared to the powder refinement.
2. Structural commentary
The present study confirms in principle the results of the previous powder X-ray diffraction study and reveals the determination of the ) and all non-H atoms refined with anisotropic displacement parameters. In comparison with the powder study, the higher precision and accuracy of the present model is, for example, reflected by the notable differences in the Pb—O bond lengths determined in the two studies (Table 1). An important result of the present study is that neither a different nor a different content in terms of an incorporation of water into the structure could be found on the basis of the single-crystal data.
(Flack parameter 0.003 (7); Flack, 1983The Pb2+ cation has a of eight considering a cut-off value of 3 Å for the ligating oxygen atoms. The is considerably distorted (Fig. 1), with Pb—O distances in the range 2.472 (2)–3.004 (2) Å (Table 1). The resulting bond-valence sum (Brown, 2002) of 1.75 valence units, using the parameters of Krivovichev & Brown (2001) for the Pb—O bonds, is reasonably close to the expected value of 2.0 valence units. Bond lengths and angles within the tartrate anion are in normal ranges.
3. Packing features
In the 2+ cations are arranged in hexagonally packed rows extending parallel to [100] (Fig. 2). Each Pb2+ cation is bonded to five tartrate anions (three chelating and two in a monodentate fashion, Fig. 1) while each tartrate anion links four Pb2+ cations, leading to a three-dimensional framework. O—H⋯O hydrogen bonds (Table 2) between the hydroxy groups of one tartrate anion and the carboxylate O atoms of adjacent tartrate anions stabilize this arrangement. Since no solvent-accessible voids were observed in the an incorporation of water molecules as reported by Lillibay & Rahimkutty (2010) is impossible.
the Pb4. Database survey
Tartaric acid and its salts or coordination compounds have been structurally examined in great detail. The current release of the CSD (Version 5.35 with all updates; Groom & Allen, 2014) revealed 644 entries, including the pure acid, co-crystals, compounds with the hydrogen tartrate anion and compounds with the tartrate anion.
5. Synthesis and crystallization
Commercially available gelatin was dissolved in hot water. The solution (50 ml) was cooled to about 300 K and 300 mg of (NH4)2(PO3F)(H2O), prepared according to Schülke & Kayser (1991), were dissolved in the still liquid solution that was filled in a large test tube. After initiation of gelling, a second neutral gel layer was put on top of the first gel layer. After the neutral gel had set, an aqueous solution consisting of Pb(NO3)2 (30 mg) and sodium potassium tartrate (250 mg) was poured over the second gel layer. After three weeks, colourless single crystals of lead(II) tartrate, mostly with a block-like form, could be isolated. PbPO3F in the form of polycrystalline material was also present in the reaction mixture as revealed by powder X-ray diffraction measurements.
6. Refinement
Crystal data, data collection and structure . Atom labelling and starting coordinates for the were taken from the previous powder diffraction study (De Ridder et al., 2002). H atoms bonded to C atoms were placed in calculated positions and refined as riding atoms, with C—H = 0.98 Å and with Uiso(H) = 1.2Ueq(C). Hydroxyl H atoms were found from difference Fourier maps and refined with an O—H distance restraint of 0.85 (1) Å and with Uiso(H) = 1.2Ueq(O). The highest and lowest remaining electron densities are found 0.59 and 0.49 Å, respectively, from the Pb atom and are caused by truncation effects. No other electron densities attributable to additional atoms could be found, ruling out an incorporation of water molecules. Refinements in Pna21 as suggested by Labutina et al. (2011) led to unreasonable models.
details are summarized in Table 3
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Supporting information
CCDC reference: 1039408
https://doi.org/10.1107/S2056989014027376/su5041sup1.cif
contains datablocks I, general. DOI:Structure factors: contains datablock I. DOI: https://doi.org/10.1107/S2056989014027376/su5041Isup2.hkl
Data collection: APEX2 (Bruker, 2013); cell
SAINT-Plus (Bruker, 2013); data reduction: SAINT-Plus (Bruker, 2013); program(s) used to solve structure: SHELXS97 (Sheldrick, 2008); program(s) used to refine structure: SHELXL97 (Sheldrick, 2008); molecular graphics: ATOMS (Dowty, 2006); software used to prepare material for publication: publCIF (Westrip, 2010).[Pb(C4H4O6)] | F(000) = 632 |
Mr = 355.26 | Dx = 4.004 Mg m−3 |
Orthorhombic, P212121 | Mo Kα radiation, λ = 0.71073 Å |
Hall symbol: P 2ac 2ab | Cell parameters from 9854 reflections |
a = 7.9890 (2) Å | θ = 3.4–40.9° |
b = 8.8411 (3) Å | µ = 28.61 mm−1 |
c = 8.3434 (2) Å | T = 296 K |
V = 589.31 (3) Å3 | Block, colourless |
Z = 4 | 0.15 × 0.15 × 0.09 mm |
Bruker APEXII CCD diffractometer | 4512 independent reflections |
Radiation source: fine-focus sealed tube | 3836 reflections with I > 2σ(I) |
Graphite monochromator | Rint = 0.046 |
ω– and φ–scans | θmax = 43.7°, θmin = 3.4° |
Absorption correction: multi-scan (SADABS; Bruker, 2013) | h = −15→15 |
Tmin = 0.099, Tmax = 0.183 | k = −17→17 |
81742 measured reflections | l = −16→16 |
Refinement on F2 | Secondary atom site location: difference Fourier map |
Least-squares matrix: full | Hydrogen site location: inferred from neighbouring sites |
R[F2 > 2σ(F2)] = 0.021 | H atoms treated by a mixture of independent and constrained refinement |
wR(F2) = 0.042 | w = 1/[σ2(Fo2) + (0.0155P)2 + 1.1508P] where P = (Fo2 + 2Fc2)/3 |
S = 1.06 | (Δ/σ)max = 0.007 |
4512 reflections | Δρmax = 3.20 e Å−3 |
108 parameters | Δρmin = −2.26 e Å−3 |
2 restraints | Absolute structure: Flack (1983), 1959 Friedel pairs |
Primary atom site location: structure-invariant direct methods | Absolute structure parameter: −0.003 (7) |
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 | −0.342448 (9) | 0.001349 (17) | −0.054104 (9) | 0.01396 (2) | |
O1 | −0.0806 (2) | 0.1027 (2) | 0.1809 (3) | 0.0159 (3) | |
O2 | 0.1001 (3) | 0.1758 (3) | −0.0066 (2) | 0.0180 (4) | |
O3 | 0.1564 (2) | −0.0126 (3) | 0.3659 (2) | 0.0147 (3) | |
O4 | 0.2220 (2) | 0.3195 (2) | 0.3069 (2) | 0.0123 (3) | |
O5 | 0.5788 (3) | 0.0785 (3) | 0.3132 (3) | 0.0215 (4) | |
O6 | 0.4746 (3) | 0.2388 (3) | 0.4968 (3) | 0.0244 (5) | |
C1 | 0.0635 (3) | 0.1138 (3) | 0.1249 (3) | 0.0103 (3) | |
C2 | 0.2130 (3) | 0.0566 (3) | 0.2235 (3) | 0.0100 (3) | |
H2 | 0.2764 | −0.0171 | 0.1601 | 0.012* | |
C3 | 0.3222 (3) | 0.1966 (3) | 0.2538 (3) | 0.0101 (3) | |
H3 | 0.3686 | 0.2263 | 0.1497 | 0.012* | |
C4 | 0.4706 (3) | 0.1686 (3) | 0.3642 (3) | 0.0128 (4) | |
H3O | 0.224 (4) | −0.019 (6) | 0.443 (4) | 0.029 (12)* | |
H4O | 0.144 (4) | 0.288 (5) | 0.367 (4) | 0.015 (10)* |
U11 | U22 | U33 | U12 | U13 | U23 | |
Pb1 | 0.01063 (3) | 0.01446 (3) | 0.01679 (3) | 0.00067 (7) | −0.00006 (2) | 0.00120 (7) |
O1 | 0.0081 (6) | 0.0230 (9) | 0.0167 (8) | 0.0000 (6) | −0.0005 (6) | 0.0032 (7) |
O2 | 0.0155 (8) | 0.0274 (10) | 0.0111 (7) | 0.0026 (8) | −0.0009 (6) | 0.0057 (7) |
O3 | 0.0116 (5) | 0.0192 (9) | 0.0134 (6) | 0.0001 (8) | 0.0009 (5) | 0.0072 (7) |
O4 | 0.0092 (6) | 0.0113 (7) | 0.0165 (8) | 0.0011 (5) | 0.0001 (6) | 0.0004 (6) |
O5 | 0.0100 (7) | 0.0277 (11) | 0.0267 (11) | 0.0073 (7) | −0.0009 (7) | −0.0005 (8) |
O6 | 0.0252 (10) | 0.0242 (10) | 0.0237 (10) | 0.0083 (9) | −0.0156 (9) | −0.0090 (8) |
C1 | 0.0081 (8) | 0.0120 (8) | 0.0108 (8) | −0.0009 (6) | −0.0017 (6) | −0.0006 (6) |
C2 | 0.0081 (7) | 0.0121 (8) | 0.0098 (8) | 0.0003 (7) | 0.0004 (6) | 0.0011 (6) |
C3 | 0.0067 (8) | 0.0129 (8) | 0.0107 (8) | 0.0005 (6) | −0.0001 (6) | 0.0011 (6) |
C4 | 0.0075 (7) | 0.0137 (9) | 0.0172 (10) | −0.0003 (7) | −0.0017 (7) | 0.0003 (7) |
Pb1—O1i | 2.472 (2) | O3—H3O | 0.843 (10) |
Pb1—O5ii | 2.482 (2) | O4—C3 | 1.420 (3) |
Pb1—O6iii | 2.594 (2) | O4—H4O | 0.845 (10) |
Pb1—O3i | 2.5972 (17) | O5—C4 | 1.250 (3) |
Pb1—O4iv | 2.6878 (19) | O6—C4 | 1.270 (3) |
Pb1—O4iii | 2.7866 (19) | C1—C2 | 1.536 (3) |
Pb1—O2iv | 2.935 (2) | C2—C3 | 1.535 (3) |
Pb1—O1 | 3.004 (2) | C2—H2 | 0.9800 |
O1—C1 | 1.246 (3) | C3—C4 | 1.522 (3) |
O2—C1 | 1.261 (3) | C3—H3 | 0.9800 |
O3—C2 | 1.411 (3) | ||
O1i—Pb1—O5ii | 72.93 (7) | C1—O1—Pb1v | 126.48 (16) |
O1i—Pb1—O6iii | 74.36 (7) | C2—O3—Pb1v | 120.65 (14) |
O5ii—Pb1—O6iii | 99.96 (9) | C2—O3—H3O | 118 (3) |
O1i—Pb1—O3i | 62.88 (6) | Pb1v—O3—H3O | 115 (3) |
O5ii—Pb1—O3i | 135.70 (7) | C3—O4—Pb1vi | 108.28 (13) |
O6iii—Pb1—O3i | 71.85 (8) | C3—O4—H4O | 111 (3) |
O1i—Pb1—O4iv | 64.23 (6) | Pb1vi—O4—H4O | 121 (3) |
O5ii—Pb1—O4iv | 69.82 (7) | C4—O5—Pb1vii | 128.07 (19) |
O6iii—Pb1—O4iv | 138.58 (7) | C4—O6—Pb1viii | 125.98 (18) |
O3i—Pb1—O4iv | 87.75 (6) | O1—C1—O2 | 125.1 (2) |
O1i—Pb1—O4iii | 122.21 (6) | O1—C1—C2 | 119.4 (2) |
O5ii—Pb1—O4iii | 82.70 (7) | O2—C1—C2 | 115.4 (2) |
O6iii—Pb1—O4iii | 59.20 (6) | O3—C2—C3 | 113.16 (19) |
O3i—Pb1—O4iii | 123.07 (6) | O3—C2—C1 | 110.14 (19) |
O4iv—Pb1—O4iii | 148.738 (15) | C3—C2—C1 | 105.30 (18) |
O1i—Pb1—O2iv | 118.51 (7) | O3—C2—H2 | 109.4 |
O5ii—Pb1—O2iv | 119.10 (7) | C3—C2—H2 | 109.4 |
O6iii—Pb1—O2iv | 140.78 (8) | C1—C2—H2 | 109.4 |
O3i—Pb1—O2iv | 81.74 (7) | O4—C3—C4 | 111.99 (19) |
O4iv—Pb1—O2iv | 65.93 (6) | O4—C3—C2 | 110.38 (18) |
O4iii—Pb1—O2iv | 119.18 (6) | C4—C3—C2 | 114.25 (19) |
O1i—Pb1—O1 | 150.22 (4) | O4—C3—H3 | 106.6 |
O5ii—Pb1—O1 | 77.58 (7) | C4—C3—H3 | 106.6 |
O6iii—Pb1—O1 | 115.47 (6) | C2—C3—H3 | 106.6 |
O3i—Pb1—O1 | 145.98 (6) | O5—C4—O6 | 126.2 (3) |
O4iv—Pb1—O1 | 101.71 (6) | O5—C4—C3 | 115.9 (2) |
O4iii—Pb1—O1 | 56.54 (5) | O6—C4—C3 | 117.9 (2) |
O2iv—Pb1—O1 | 72.91 (6) |
Symmetry codes: (i) −x−1/2, −y, z−1/2; (ii) −x+1/2, −y, z−1/2; (iii) −x, y−1/2, −z+1/2; (iv) x−1/2, −y+1/2, −z; (v) −x−1/2, −y, z+1/2; (vi) x+1/2, −y+1/2, −z; (vii) −x+1/2, −y, z+1/2; (viii) −x, y+1/2, −z+1/2. |
D—H···A | D—H | H···A | D···A | D—H···A |
O3—H3O···O2vii | 0.84 (1) | 2.02 (4) | 2.646 (3) | 131 (5) |
O4—H4O···O6ix | 0.85 (1) | 1.79 (1) | 2.618 (3) | 169 (4) |
Symmetry codes: (vii) −x+1/2, −y, z+1/2; (ix) x−1/2, −y+1/2, −z+1. |
For the previous refinement: a = 7.99482 (3), b = 8.84525 (4), c = 8.35318 (4) Å. |
Bond | current refinement | previous refinement |
Pb—O1i | 2.472 (2) | 2.859 (12) |
Pb—O5ii | 2.482 (2) | 2.398 (11) |
Pb—O6iii | 2.594 (2) | 2.575 (12) |
Pb—O3i | 2.5972 (17) | 2.637 (9) |
Pb—O4iv | 2.6878 (19) | 2.649 (11) |
Pb—O4iii | 2.7866 (19) | 2.847 (12) |
Pb—O2iv | 2.935 (2) | 2.975 (13) |
Pb—O1 | 3.004 (2) | 2.754 (12) |
Symmetry codes: (i) -x - 1/2, -y, z - 1/2; (ii) -x + 1/2, -y, z - 1/2; (iii) -x, y - 1/2, -z + 1/2; (iv) x - 1/2, -y + 1/2, -z. |
Acknowledgements
The X-ray centre of the Vienna University of Technology is acknowledged for providing access to the single-crystal and powder X-ray diffractometers.
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