inorganic compounds
of hexaaquadichloridoytterbium(III) chloride
aDepartment of Chemistry & Biochemistry, Central Connecticut State University, New Britain, CT 06053, USA
*Correspondence e-mail: crundwellg@mail.ccsu.edu
The 2(H2O)6]Cl, was determined at 110 K. Samples were obtained from evaporated acetonitrile solutions containing the title compound, which consists of a [YbCl2(H2O)6]+ cation and a Cl− anion. The cations in the title compound sit on a twofold axis and form O—H⋯Cl hydrogen bonds with the nearby Cl− anion. The coordination geometry around the metal centre forms a distorted square antiprism. The ytterbium complex is isotypic with the europium complex [Tambrornino et al. (2014). Acta Cryst. E70, i27].
of the title compound, [YbClKeywords: crystal structure; ytterbium(III); chloride; hydrogen bonding.
CCDC reference: 1062504
1. Related literature
The ytterbium complex is isotypic with the europium complex, the redetermined structure of which was published recently (Tambrornino et al. 2014) which was in turn similar to studies of other lanthanoid chloride hydrates (Marezio et al., 1961).
2. Experimental
2.1. Crystal data
|
2.3. Refinement
|
Data collection: CrysAlis CCD (Oxford Diffraction, 2009); cell CrysAlis RED (Oxford Diffraction, 2009); data reduction: CrysAlis RED; program(s) used to solve structure: SHELXS2014 (Sheldrick, 2008); program(s) used to refine structure: SHELXL2014 (Sheldrick, 2015); molecular graphics: PLATON (Spek, 2009) and ORTEP-3 for Windows (Farrugia, 2012); software used to prepare material for publication: SHELXL2014.
Supporting information
CCDC reference: 1062504
10.1107/S2056989015008488/br2249sup1.cif
contains datablock I. DOI:Structure factors: contains datablock I. DOI: 10.1107/S2056989015008488/br2249Isup2.hkl
In 40.0 ml of acetonitrile, 0.1945 grams (0.5019 mmol) of ytterbium(III) chloride hexahydrate was added to 0.1000 grams (0.5020 mmol) of di-2-pyridyl ketone oxime (dpko) with the hopes of synthesizing a Yb-dpko complex. The mixture was heated to dissolve the solids. Upon cooling and subsequent evaporation, small colorless crystals of the title compound were isolated. The metal chloride was purchased from Strem chemicals (99.9% purity) whereas the dpko was purchased from Sigma-Aldrich (99.9%). Both were used without additional purification.
H atoms were included and were allowed to refine to ideal O—H distances based upon geometric considerations. Thermal parameters for all H atoms were included in the
in riding motion approximation with Uiso = 1.5Ueq of the carrier atom.Data collection: CrysAlis CCD (Oxford Diffraction, 2009); cell
CrysAlis RED (Oxford Diffraction, 2009); data reduction: CrysAlis RED (Oxford Diffraction, 2009); program(s) used to solve structure: SHELXS2014 (Sheldrick, 2008); program(s) used to refine structure: SHELXL2014 (Sheldrick, 2015); molecular graphics: PLATON (Spek, 2009) and ORTEP-3 for Windows (Farrugia, 2012) (Farrugia, 2012); software used to prepare material for publication: SHELXL2014 (Sheldrick, 2015).Fig. 1. A view of the title compound (Farrugia, 2012). Displacement ellipsoids are drawn at the 50% probability level. H atoms have been omitted for clarity. |
[YbCl2(H2O)6]Cl | Dx = 2.671 Mg m−3 |
Mr = 387.49 | Melting point: 350 K |
Monoclinic, P2/c | Mo Kα radiation, λ = 0.71073 Å |
a = 7.8158 (11) Å | Cell parameters from 7486 reflections |
b = 6.4651 (3) Å | θ = 4.9–33.8° |
c = 12.7250 (18) Å | µ = 10.52 mm−1 |
β = 131.45 (2)° | T = 110 K |
V = 481.92 (16) Å3 | Block, light pink |
Z = 2 | 0.24 × 0.18 × 0.17 mm |
F(000) = 362 |
Oxford Diffraction Xcalibur Sapphire3 diffractometer | 1806 independent reflections |
Radiation source: fine-focus sealed tube | 1762 reflections with I > 2σ(I) |
Graphite monochromator | Rint = 0.042 |
Detector resolution: 16.1790 pixels mm-1 | θmax = 33.7°, θmin = 4.3° |
ω scans | h = −11→12 |
Absorption correction: multi-scan (CrysAlis PRO; Oxford Diffraction, 2009) | k = −9→9 |
Tmin = 0.187, Tmax = 0.268 | l = −19→19 |
12358 measured reflections |
Refinement on F2 | Hydrogen site location: difference Fourier map |
Least-squares matrix: full | H-atom parameters constrained |
R[F2 > 2σ(F2)] = 0.018 | w = 1/[σ2(Fo2) + (0.0207P)2] where P = (Fo2 + 2Fc2)/3 |
wR(F2) = 0.041 | (Δ/σ)max = 0.001 |
S = 1.12 | Δρmax = 0.91 e Å−3 |
1806 reflections | Δρmin = −0.96 e Å−3 |
51 parameters | Extinction correction: SHELXL2014 (Sheldrick, 2015), Fc*=kFc[1+0.001xFc2λ3/sin(2θ)]-1/4 |
0 restraints | Extinction coefficient: 0.0602 (13) |
[YbCl2(H2O)6]Cl | V = 481.92 (16) Å3 |
Mr = 387.49 | Z = 2 |
Monoclinic, P2/c | Mo Kα radiation |
a = 7.8158 (11) Å | µ = 10.52 mm−1 |
b = 6.4651 (3) Å | T = 110 K |
c = 12.7250 (18) Å | 0.24 × 0.18 × 0.17 mm |
β = 131.45 (2)° |
Oxford Diffraction Xcalibur Sapphire3 diffractometer | 1806 independent reflections |
Absorption correction: multi-scan (CrysAlis PRO; Oxford Diffraction, 2009) | 1762 reflections with I > 2σ(I) |
Tmin = 0.187, Tmax = 0.268 | Rint = 0.042 |
12358 measured reflections |
R[F2 > 2σ(F2)] = 0.018 | 0 restraints |
wR(F2) = 0.041 | H-atom parameters constrained |
S = 1.12 | Δρmax = 0.91 e Å−3 |
1806 reflections | Δρmin = −0.96 e Å−3 |
51 parameters |
Experimental. Sample was covered in mineral oil prior to mounting in cryo stream. Hydrogen atoms were included and were allowed to refine to ideal O—H distances based upon geometric considerations. Thermal parameters for all H atoms were included in the refinement in riding motion approximation with Uiso = 1.5Ueq of the carrier atom. CrysAlisPro, Oxford Diffraction Ltd., Version 1.171.33.52 (release 06-11-2009 CrysAlis171 .NET) Empirical absorption correction using spherical harmonics, implemented in SCALE3 ABSPACK scaling algorithm (Oxford Diffraction (2009). |
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 | ||
Yb1 | 0.5000 | 0.65776 (2) | 0.7500 | 0.01599 (6) | |
Cl1 | 0.32165 (12) | 0.34336 (8) | 0.56141 (7) | 0.02594 (12) | |
Cl2 | 0.0000 | −0.12652 (14) | 0.2500 | 0.02883 (16) | |
O1 | 0.1817 (3) | 0.5542 (3) | 0.71889 (19) | 0.0266 (3) | |
H1A | 0.1626 | 0.4279 | 0.7416 | 0.040* | |
H1B | 0.0569 | 0.6336 | 0.6823 | 0.040* | |
O2 | 0.7626 (3) | 0.9242 (3) | 0.85341 (19) | 0.0276 (3) | |
H2A | 0.7791 | 1.0181 | 0.9087 | 0.041* | |
H2B | 0.8611 | 0.9467 | 0.8434 | 0.041* | |
O3 | 0.5420 (3) | 0.8002 (3) | 0.93497 (19) | 0.0273 (3) | |
H3A | 0.6709 | 0.8455 | 1.0145 | 0.041* | |
H3B | 0.4315 | 0.8170 | 0.9361 | 0.041* |
U11 | U22 | U33 | U12 | U13 | U23 | |
Yb1 | 0.01594 (8) | 0.01718 (8) | 0.01703 (8) | 0.000 | 0.01184 (6) | 0.000 |
Cl1 | 0.0283 (3) | 0.0258 (3) | 0.0251 (3) | −0.00427 (18) | 0.0183 (2) | −0.00488 (18) |
Cl2 | 0.0271 (4) | 0.0336 (4) | 0.0299 (4) | 0.000 | 0.0206 (4) | 0.000 |
O1 | 0.0229 (8) | 0.0278 (8) | 0.0343 (9) | −0.0001 (6) | 0.0212 (8) | 0.0043 (7) |
O2 | 0.0293 (9) | 0.0262 (8) | 0.0359 (9) | −0.0096 (7) | 0.0253 (8) | −0.0098 (7) |
O3 | 0.0310 (9) | 0.0331 (8) | 0.0246 (8) | −0.0050 (7) | 0.0213 (8) | −0.0061 (7) |
Yb1—O2i | 2.3101 (17) | Yb1—O1i | 2.3433 (16) |
Yb1—O2 | 2.3101 (17) | Yb1—O1 | 2.3434 (17) |
Yb1—O3i | 2.3392 (17) | Yb1—Cl1i | 2.7211 (7) |
Yb1—O3 | 2.3392 (17) | Yb1—Cl1 | 2.7212 (7) |
O2i—Yb1—O2 | 83.56 (10) | O1i—Yb1—Cl1i | 76.75 (5) |
O2i—Yb1—O3i | 69.72 (6) | O1—Yb1—Cl1i | 78.60 (5) |
O2—Yb1—O3i | 76.09 (7) | O2i—Yb1—Cl1 | 108.14 (6) |
O2i—Yb1—O3 | 76.09 (7) | O2—Yb1—Cl1 | 143.38 (5) |
O2—Yb1—O3 | 69.72 (6) | O3i—Yb1—Cl1 | 75.99 (5) |
O3i—Yb1—O3 | 133.64 (9) | O3—Yb1—Cl1 | 146.11 (5) |
O2i—Yb1—O1i | 138.85 (6) | O1i—Yb1—Cl1 | 78.60 (5) |
O2—Yb1—O1i | 70.92 (6) | O1—Yb1—Cl1 | 76.75 (5) |
O3i—Yb1—O1i | 73.06 (7) | Cl1i—Yb1—Cl1 | 83.34 (3) |
O3—Yb1—O1i | 121.09 (7) | Yb1—O1—H1A | 125.5 |
O2i—Yb1—O1 | 70.92 (6) | Yb1—O1—H1B | 125.7 |
O2—Yb1—O1 | 138.85 (6) | H1A—O1—H1B | 108.8 |
O3i—Yb1—O1 | 121.09 (7) | Yb1—O2—H2A | 125.4 |
O3—Yb1—O1 | 73.06 (7) | Yb1—O2—H2B | 125.4 |
O1i—Yb1—O1 | 146.79 (9) | H2A—O2—H2B | 109.2 |
O2i—Yb1—Cl1i | 143.38 (5) | Yb1—O3—H3A | 125.4 |
O2—Yb1—Cl1i | 108.15 (6) | Yb1—O3—H3B | 125.4 |
O3i—Yb1—Cl1i | 146.11 (5) | H3A—O3—H3B | 109.2 |
O3—Yb1—Cl1i | 75.99 (5) |
Symmetry code: (i) −x+1, y, −z+3/2. |
D—H···A | D—H | H···A | D···A | D—H···A |
O1—H1A···Cl2ii | 0.91 | 2.37 | 3.2499 (19) | 163 |
O1—H1B···Cl1iii | 0.91 | 2.50 | 3.171 (2) | 131 |
O2—H2A···Cl1iv | 0.87 | 2.36 | 3.1460 (18) | 150 |
O2—H2B···Cl2v | 0.87 | 2.38 | 3.1806 (18) | 154 |
O3—H3A···Cl2vi | 0.88 | 2.33 | 3.179 (2) | 163 |
O3—H3B···Cl1vii | 0.88 | 2.48 | 3.1758 (19) | 136 |
Symmetry codes: (ii) −x, −y, −z+1; (iii) −x, −y+1, −z+1; (iv) −x+1, y+1, −z+3/2; (v) −x+1, −y+1, −z+1; (vi) x+1, y+1, z+1; (vii) x, −y+1, z+1/2. |
D—H···A | D—H | H···A | D···A | D—H···A |
O1—H1A···Cl2i | 0.91 | 2.37 | 3.2499 (19) | 163.3 |
O1—H1B···Cl1ii | 0.91 | 2.50 | 3.171 (2) | 130.9 |
O2—H2A···Cl1iii | 0.87 | 2.36 | 3.1460 (18) | 149.6 |
O2—H2B···Cl2iv | 0.87 | 2.38 | 3.1806 (18) | 153.5 |
O3—H3A···Cl2v | 0.88 | 2.33 | 3.179 (2) | 162.5 |
O3—H3B···Cl1vi | 0.88 | 2.48 | 3.1758 (19) | 136.0 |
Symmetry codes: (i) −x, −y, −z+1; (ii) −x, −y+1, −z+1; (iii) −x+1, y+1, −z+3/2; (iv) −x+1, −y+1, −z+1; (v) x+1, y+1, z+1; (vi) x, −y+1, z+1/2. |
Acknowledgements
This research was also funded in part by a CCSU–AAUP research grant and CCSU Faculty–Student Research Grants.
References
Farrugia, L. J. (2012). J. Appl. Cryst. 45, 849–854. Web of Science CrossRef CAS IUCr Journals Google Scholar
Marezio, M., Plettinger, H. A. & Zachariasen, W. H. (1961). Acta Cryst. 14, 234–236. CrossRef CAS IUCr Journals Web of Science Google Scholar
Oxford Diffraction (2009). CrysAlis CCD,CrysAlis PRO and CrysAlis RED. Oxford Diffraction Ltd, Abington, England. Google Scholar
Sheldrick, G. M. (2008). Acta Cryst. A64, 112–122. Web of Science CrossRef CAS IUCr Journals Google Scholar
Sheldrick, G. M. (2015). Acta Cryst. C71, 3–8. Web of Science CrossRef IUCr Journals Google Scholar
Spek, A. L. (2009). Acta Cryst. D65, 148–155. Web of Science CrossRef CAS IUCr Journals Google Scholar
Tambornino, F., Bielec, P. & Hoch, C. (2014). Acta Cryst. E70, i27. CSD CrossRef 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.
Samples gathered from the mother liquor were coated with mineral oil prior to mounting to reduce sample decay. The ytterbium complex is isomorphous with a recently published redetermination of a europium complex (Tambrornino, et al. 2014) which was in turn similar to studies of other lanthanoid chloride hydrates (Marezio, et al. 1961).
Crystals of ytterbium(III) chloride hexahydrate consist of a [YbCl2(H2O)6]1+ cation and a chlorine anion. The covalent nature of the lanthanoid +3 cations are not surprising given their high charge density. An ORTEP of the title compound is shown in Fig. 1.