
Supporting information
![]() | Crystallographic Information File (CIF) https://doi.org/10.1107/S0108270110014861/sq3237sup1.cif |
![]() | Structure factor file (CIF format) https://doi.org/10.1107/S0108270110014861/sq3237Isup2.hkl |
CCDC reference: 782523
Dark-blue plate crystals of the title compound with well developed {010} faces were grown by slow evaporation from an aqueous solution of oxalic acid dihydrate, caesium oxalate monohydrate and caesium dichromate (7:2:1).
The H atoms were all located in a difference map. They were initially refined with soft restraints on the bond lengths and angles to regularise their geometry (O—H = 0.82 Å) and Uiso(H) (in the range 1.2–1.5 times Ueq of the parent atom), after which the positions were refined with riding constraints.
Data collection: CrysAlis PRO (Oxford Diffraction, 2009); cell refinement: CrysAlis PRO (Oxford Diffraction, 2009); data reduction: CrysAlis PRO (Oxford Diffraction, 2009); program(s) used to solve structure: SIR92 (Altomare et al., 1994); program(s) used to refine structure: CRYSTALS (Betteridge et al., 2003); molecular graphics: CAMERON (Watkin et al., 1996); software used to prepare material for publication: CRYSTALS (Betteridge et al., 2003).
Cs3[Cr(C2O4)3]·2H2O | Z = 2 |
Mr = 750.80 | F(000) = 682 |
Triclinic, P1 | Dx = 3.081 Mg m−3 |
Hall symbol: -P 1 | Mo Kα radiation, λ = 0.71073 Å |
a = 8.2299 (5) Å | Cell parameters from 4324 reflections |
b = 10.2956 (6) Å | θ = 3.0–29.0° |
c = 10.9902 (5) Å | µ = 7.43 mm−1 |
α = 63.662 (5)° | T = 120 K |
β = 89.775 (4)° | Plate, blue |
γ = 77.221 (5)° | 0.22 × 0.15 × 0.13 mm |
V = 809.14 (9) Å3 |
Xcalibur, Sapphire3 diffractometer | 3326 reflections with I > 2σ(I) |
Graphite monochromator | Rint = 0.018 |
ω/2θ scans | θmax = 29.1°, θmin = 3.0° |
Absorption correction: multi-scan [CrysAlis PRO (Oxford Diffraction, 2009). Empirical absorption correction using spherical harmonics, implemented in SCALE3 ABSPACK scaling algorithm] | h = −8→10 |
Tmin = 0.743, Tmax = 1.000 | k = −13→13 |
5562 measured reflections | l = −11→14 |
3631 independent reflections |
Refinement on F2 | Primary atom site location: structure-invariant direct methods |
Least-squares matrix: full | Hydrogen site location: inferred from neighbouring sites |
R[F2 > 2σ(F2)] = 0.025 | H-atom parameters constrained |
wR(F2) = 0.059 | w = 1/[σ2(F2) + ( 0.03P)2 + 4.43P], where P = (max(Fo2,0) + 2Fc2)/3 |
S = 0.98 | (Δ/σ)max = 0.002 |
3621 reflections | Δρmax = 0.91 e Å−3 |
217 parameters | Δρmin = −1.62 e Å−3 |
0 restraints |
Cs3[Cr(C2O4)3]·2H2O | γ = 77.221 (5)° |
Mr = 750.80 | V = 809.14 (9) Å3 |
Triclinic, P1 | Z = 2 |
a = 8.2299 (5) Å | Mo Kα radiation |
b = 10.2956 (6) Å | µ = 7.43 mm−1 |
c = 10.9902 (5) Å | T = 120 K |
α = 63.662 (5)° | 0.22 × 0.15 × 0.13 mm |
β = 89.775 (4)° |
Xcalibur, Sapphire3 diffractometer | 3631 independent reflections |
Absorption correction: multi-scan [CrysAlis PRO (Oxford Diffraction, 2009). Empirical absorption correction using spherical harmonics, implemented in SCALE3 ABSPACK scaling algorithm] | 3326 reflections with I > 2σ(I) |
Tmin = 0.743, Tmax = 1.000 | Rint = 0.018 |
5562 measured reflections |
R[F2 > 2σ(F2)] = 0.025 | 0 restraints |
wR(F2) = 0.059 | H-atom parameters constrained |
S = 0.98 | Δρmax = 0.91 e Å−3 |
3621 reflections | Δρmin = −1.62 e Å−3 |
217 parameters |
Experimental. The crystal was placed in the cold stream of an Oxford Cryosystems open-flow nitrogen cryostat (Cosier & Glazer, 1986) with a nominal stability of 0.1 K. Cosier, J. & Glazer, A. M. (1986). J. Appl. Cryst. 19, 105–107. |
x | y | z | Uiso*/Ueq | ||
Cs1 | 0.24540 (3) | 1.40826 (3) | −0.37553 (3) | 0.0105 | |
Cs2 | 0.69122 (3) | 1.03653 (3) | 0.33926 (3) | 0.0124 | |
Cs3 | 0.17374 (3) | 1.72892 (3) | 0.10003 (3) | 0.0115 | |
Cr4 | 0.22095 (8) | 1.09160 (7) | 0.23561 (7) | 0.0072 | |
O5 | 0.0406 (4) | 1.2776 (3) | 0.1568 (3) | 0.0109 | |
C6 | 0.0508 (5) | 1.3697 (5) | 0.2030 (4) | 0.0095 | |
O7 | −0.0465 (4) | 1.4936 (3) | 0.1676 (3) | 0.0127 | |
C8 | 0.2044 (5) | 1.3157 (5) | 0.3112 (4) | 0.0101 | |
O9 | 0.2811 (4) | 1.1766 (3) | 0.3532 (3) | 0.0113 | |
O10 | 0.2451 (4) | 1.4022 (4) | 0.3465 (3) | 0.0159 | |
O11 | 0.1677 (4) | 1.0415 (3) | 0.0895 (3) | 0.0099 | |
C12 | 0.2503 (5) | 1.0898 (5) | −0.0156 (4) | 0.0108 | |
O13 | 0.2270 (4) | 1.0800 (4) | −0.1212 (3) | 0.0167 | |
C14 | 0.3837 (5) | 1.1697 (5) | −0.0008 (4) | 0.0112 | |
O15 | 0.3835 (4) | 1.1824 (3) | 0.1113 (3) | 0.0102 | |
O16 | 0.4730 (4) | 1.2176 (4) | −0.0911 (3) | 0.0184 | |
O17 | 0.0684 (4) | 0.9793 (3) | 0.3519 (3) | 0.0115 | |
C18 | 0.1220 (5) | 0.8372 (5) | 0.3934 (4) | 0.0114 | |
O19 | 0.0362 (4) | 0.7456 (4) | 0.4400 (4) | 0.0179 | |
C20 | 0.3115 (5) | 0.7886 (5) | 0.3772 (4) | 0.0098 | |
O21 | 0.3855 (4) | 0.8979 (3) | 0.3349 (3) | 0.0112 | |
O22 | 0.3753 (4) | 0.6587 (4) | 0.4026 (3) | 0.0164 | |
O23 | 0.3219 (4) | 1.5124 (4) | −0.0218 (4) | 0.0214 | |
O24 | 0.6059 (5) | 1.3623 (4) | 0.3025 (4) | 0.0243 | |
H232 | 0.3810 | 1.4263 | 0.0196 | 0.0321* | |
H242 | 0.5066 | 1.3760 | 0.3194 | 0.0365* | |
H231 | 0.2406 | 1.5125 | −0.0641 | 0.0321* | |
H241 | 0.6028 | 1.4155 | 0.2190 | 0.0365* |
U11 | U22 | U33 | U12 | U13 | U23 | |
Cs1 | 0.01255 (13) | 0.01076 (13) | 0.00794 (13) | −0.00429 (10) | 0.00199 (9) | −0.00333 (10) |
Cs2 | 0.00942 (13) | 0.01633 (15) | 0.01053 (13) | −0.00297 (10) | 0.00038 (10) | −0.00530 (11) |
Cs3 | 0.01112 (13) | 0.00979 (13) | 0.01416 (14) | −0.00417 (10) | 0.00049 (10) | −0.00511 (11) |
Cr4 | 0.0078 (3) | 0.0070 (3) | 0.0063 (3) | −0.0028 (2) | 0.0008 (2) | −0.0022 (3) |
O5 | 0.0107 (15) | 0.0105 (15) | 0.0112 (15) | −0.0011 (12) | −0.0022 (12) | −0.0053 (13) |
C6 | 0.009 (2) | 0.013 (2) | 0.0077 (19) | −0.0058 (16) | 0.0031 (15) | −0.0041 (17) |
O7 | 0.0126 (15) | 0.0096 (15) | 0.0147 (16) | −0.0012 (12) | 0.0016 (12) | −0.0052 (13) |
C8 | 0.010 (2) | 0.014 (2) | 0.0053 (19) | −0.0037 (17) | 0.0005 (15) | −0.0032 (17) |
O9 | 0.0153 (15) | 0.0088 (15) | 0.0094 (15) | −0.0024 (12) | −0.0008 (12) | −0.0039 (13) |
O10 | 0.0225 (17) | 0.0161 (17) | 0.0140 (16) | −0.0095 (14) | 0.0023 (13) | −0.0090 (14) |
O11 | 0.0117 (15) | 0.0094 (15) | 0.0096 (14) | −0.0051 (12) | 0.0020 (12) | −0.0040 (12) |
C12 | 0.011 (2) | 0.008 (2) | 0.012 (2) | −0.0005 (16) | 0.0008 (16) | −0.0041 (17) |
O13 | 0.0221 (17) | 0.0193 (18) | 0.0133 (16) | −0.0094 (14) | 0.0022 (13) | −0.0095 (14) |
C14 | 0.010 (2) | 0.010 (2) | 0.010 (2) | −0.0014 (16) | −0.0005 (16) | −0.0021 (17) |
O15 | 0.0137 (15) | 0.0117 (15) | 0.0073 (14) | −0.0070 (12) | 0.0026 (12) | −0.0043 (12) |
O16 | 0.0151 (16) | 0.028 (2) | 0.0123 (16) | −0.0115 (14) | 0.0049 (13) | −0.0060 (15) |
O17 | 0.0101 (15) | 0.0109 (15) | 0.0115 (15) | −0.0033 (12) | 0.0039 (12) | −0.0030 (13) |
C18 | 0.012 (2) | 0.012 (2) | 0.010 (2) | −0.0039 (16) | 0.0007 (16) | −0.0039 (18) |
O19 | 0.0100 (15) | 0.0143 (17) | 0.0267 (19) | −0.0061 (13) | 0.0036 (13) | −0.0054 (15) |
C20 | 0.010 (2) | 0.012 (2) | 0.0057 (19) | −0.0025 (16) | −0.0012 (15) | −0.0022 (17) |
O21 | 0.0092 (14) | 0.0094 (15) | 0.0114 (15) | −0.0022 (12) | 0.0003 (12) | −0.0017 (13) |
O22 | 0.0173 (17) | 0.0094 (16) | 0.0198 (17) | −0.0038 (13) | 0.0049 (13) | −0.0041 (14) |
O23 | 0.0171 (17) | 0.0216 (19) | 0.0283 (19) | −0.0024 (14) | −0.0039 (14) | −0.0147 (16) |
O24 | 0.0249 (19) | 0.026 (2) | 0.0247 (19) | −0.0111 (16) | 0.0064 (15) | −0.0115 (17) |
Cr4—O5 | 1.975 (3) | C12—C14 | 1.558 (6) |
Cr4—O9 | 1.970 (3) | C14—O15 | 1.296 (5) |
Cr4—O11 | 1.969 (3) | C14—O16 | 1.219 (5) |
Cr4—O15 | 1.984 (3) | O17—C18 | 1.291 (5) |
Cr4—O17 | 1.966 (3) | C18—O19 | 1.230 (5) |
Cr4—O21 | 1.972 (3) | C18—C20 | 1.564 (6) |
O5—C6 | 1.275 (5) | C20—O21 | 1.300 (5) |
C6—O7 | 1.237 (5) | C20—O22 | 1.225 (5) |
C6—C8 | 1.560 (6) | O23—H232 | 0.826 |
C8—O9 | 1.295 (5) | O23—H231 | 0.816 |
C8—O10 | 1.223 (5) | O24—H242 | 0.833 |
O11—C12 | 1.294 (5) | O24—H241 | 0.831 |
C12—O13 | 1.229 (5) | ||
O5—Cr4—O9 | 82.68 (13) | O9—C8—O10 | 125.9 (4) |
O5—Cr4—O11 | 91.74 (13) | Cr4—O9—C8 | 113.4 (3) |
O9—Cr4—O11 | 169.10 (13) | Cr4—O11—C12 | 115.1 (3) |
O5—Cr4—O15 | 93.94 (13) | O11—C12—O13 | 125.2 (4) |
O9—Cr4—O15 | 88.75 (13) | O11—C12—C14 | 114.1 (4) |
O11—Cr4—O15 | 82.29 (12) | O13—C12—C14 | 120.7 (4) |
O5—Cr4—O17 | 91.23 (13) | C12—C14—O15 | 113.4 (4) |
O9—Cr4—O17 | 97.77 (13) | C12—C14—O16 | 120.9 (4) |
O11—Cr4—O17 | 91.68 (13) | O15—C14—O16 | 125.7 (4) |
O15—Cr4—O17 | 172.15 (13) | Cr4—O15—C14 | 115.1 (3) |
O5—Cr4—O21 | 172.73 (13) | Cr4—O17—C18 | 112.0 (3) |
O9—Cr4—O21 | 94.89 (13) | O17—C18—O19 | 125.2 (4) |
O11—Cr4—O21 | 91.73 (13) | O17—C18—C20 | 113.4 (4) |
O15—Cr4—O21 | 92.85 (13) | O19—C18—C20 | 121.4 (4) |
O17—Cr4—O21 | 82.29 (13) | C18—C20—O21 | 113.2 (4) |
Cr4—O5—C6 | 114.4 (3) | C18—C20—O22 | 120.2 (4) |
O5—C6—O7 | 125.8 (4) | O21—C20—O22 | 126.6 (4) |
O5—C6—C8 | 114.2 (4) | Cr4—O21—C20 | 110.6 (3) |
O7—C6—C8 | 120.0 (4) | H232—O23—H231 | 109.5 |
C6—C8—O9 | 113.4 (4) | H242—O24—H241 | 105.2 |
C6—C8—O10 | 120.7 (4) |
D—H···A | D—H | H···A | D···A | D—H···A |
O23—H232···O15 | 0.83 | 2.25 | 2.963 (7) | 145 |
O24—H242···O10 | 0.83 | 2.15 | 2.974 (7) | 173 |
O23—H231···C6i | 0.82 | 2.58 | 3.333 (7) | 154 |
O23—H231···O7i | 0.82 | 1.99 | 2.809 (7) | 178 |
O24—H241···O23ii | 0.83 | 2.10 | 2.886 (7) | 158 |
Symmetry codes: (i) −x, −y+3, −z; (ii) −x+1, −y+3, −z. |
Experimental details
Crystal data | |
Chemical formula | Cs3[Cr(C2O4)3]·2H2O |
Mr | 750.80 |
Crystal system, space group | Triclinic, P1 |
Temperature (K) | 120 |
a, b, c (Å) | 8.2299 (5), 10.2956 (6), 10.9902 (5) |
α, β, γ (°) | 63.662 (5), 89.775 (4), 77.221 (5) |
V (Å3) | 809.14 (9) |
Z | 2 |
Radiation type | Mo Kα |
µ (mm−1) | 7.43 |
Crystal size (mm) | 0.22 × 0.15 × 0.13 |
Data collection | |
Diffractometer | Xcalibur, Sapphire3 diffractometer |
Absorption correction | Multi-scan [CrysAlis PRO (Oxford Diffraction, 2009). Empirical absorption correction using spherical harmonics, implemented in SCALE3 ABSPACK scaling algorithm] |
Tmin, Tmax | 0.743, 1.000 |
No. of measured, independent and observed [I > 2σ(I)] reflections | 5562, 3631, 3326 |
Rint | 0.018 |
(sin θ/λ)max (Å−1) | 0.684 |
Refinement | |
R[F2 > 2σ(F2)], wR(F2), S | 0.025, 0.059, 0.98 |
No. of reflections | 3621 |
No. of parameters | 217 |
H-atom treatment | H-atom parameters constrained |
Δρmax, Δρmin (e Å−3) | 0.91, −1.62 |
Computer programs: CrysAlis PRO (Oxford Diffraction, 2009), SIR92 (Altomare et al., 1994), CRYSTALS (Betteridge et al., 2003), CAMERON (Watkin et al., 1996).
D—H···A | D—H | H···A | D···A | D—H···A |
O23—H232···O15 | 0.83 | 2.25 | 2.963 (7) | 145 |
O24—H242···O10 | 0.83 | 2.15 | 2.974 (7) | 173 |
O23—H231···C6i | 0.82 | 2.58 | 3.333 (7) | 154 |
O23—H231···O7i | 0.82 | 1.99 | 2.809 (7) | 178 |
O24—H241···O23ii | 0.83 | 2.10 | 2.886 (7) | 158 |
Symmetry codes: (i) −x, −y+3, −z; (ii) −x+1, −y+3, −z. |
The title compound, Cs3[Cr(C2O4)3].2H2O, (I), represents a new salt of the tris(oxalato)chromate(III) anion, as this is the first study of the caesium analogue and the first report of any tris(oxalato)metallate with Cs+ cations. The first examples of [Cr(oxalate)3]3- were studied by Werner (1912). The [Cr(oxalate)3]3- anion has more recently been used as a component in molecular radical cation salts of BEDT-TTF [bis(ethylenedithio)tetrathiafulvalene] (Martin et al., 1997), which have been widely studied because of the opportunities they afford for making new combinations of physical properties through crystal engineering. The series of BEDT-TTF salts containing tris(oxalato)chromate anions can be paramagnetic superconductors, semiconductors or metallic proton conductors, depending on whether the counter-cation is NH4+, H3O+, Li+, Na+, K+, Rb+ or Cs+ (Martin et al., 2007). These materials can also be superconducting or semiconducting, depending on the spatial distribution of the D and L enantiomers of [Cr(oxalate)3]3- (Martin et al., 1999). It is the opportunities for crystal engineering afforded by [Cr(oxalate)3]3- that have led us to synthesise the caesium analogue, (I), which completes the series of alkali metal tris(oxalato)chromates.
In (I), the CrIII cation is coordinated by three bidentate oxalate groups in an approximate octahedral geometry (Fig. 1). The Cr—O distances fall in the range 1.967 (3)–1.984 (3) Å and the internal O—Cr—O angles of the chelate rings are 82.67 (13), 82.33 (13) and 82.29 (13)°, similar to those observed in the alkali metal tris(oxalato)chromate salts of lithium (Sekine et al., 1994), sodium (Bulc et al., 1982), rubidium (van Niekerk & Schoening, 1952) and potassium (Taylor, 1978). The Cs+ compound crystallises in the triclinic space group P1 and has two formula units in the asymmetric unit. The lithium analogue also crystallises in space group P1 with Z = 2, the sodium analogue in the monoclinic space group C2/c with Z = 8, and the potassium and rubidium analogues in the monoclinic space group P21/c, with Z = 4.
All three of the Cs+ cations form close contacts with both the oxalate and the water O atoms. The numerous Cs—O close contacts to oxalate O atoms are in the range 3.02 (1)–3.51 (1) Å, with each of the three Cs+ cations forming seven such Cs—O contacts, including a single short contact to a water O atom [3.11 (1), 3.11 (1) and 3.27 (1) Å]. There is hydrogen bonding between the oxalate O atoms and three of the H atoms on the two water molecules, while the fourth H atom forms a hydrogen bond with the O atom of a neighbouring water molecule (Table 1). By comparison, the lithium [Cr(oxalate)3]3- analogue has six water molecules, four of which are coordinated to Li+ cations and two tetrahedrally hydrogen-bonded to other water molecules or oxalate ligands. The three Li+ cations have octahedral, square-pyramidal and tetrahedral coordination geometries. The sodium salt contains five water molecules. Four of these form a separate layer containing polymeric chains of H2O molecules and Na+ cations between the [Cr(oxalate)3]3- layers, whilst a fifth resides in cavities between these layers. The four water molecules in the layers with Na+ cations form two interlayer hydrogen bonds, while the fifth H2O molecule forms hydrogen bonds with both the H2O/Na+ layer and the [Cr(oxalate)3]3- layer. The Na+ cations in the H2O/Na+ layers form close contacts with water O atoms within the layer and also with oxalate O atoms in the [Cr(oxalate)3]3- layer, whilst the other Na+ cations form only close contacts with oxalate O atoms in the anion layer. The potassium salt contains 2.7 water molecules, all of which form hydrogen bonds to two K+ cations and two oxalate O atoms. Two K+ cations are coordinated to six oxalate O atoms and two H2O molecules, whilst the third K+ cation is coordinated to four oxalate O atoms and two H2O molecules. The rubidium salt contains three water molecules which are hydrogen bonded to a single oxalate O atom each. Two H2O are also hydrogen-bonded to each other, whilst the third is coordinated to two Rb+ cations. Two Rb+ cations are coordinated to six oxalate O atoms and two H2O molecules, whilst the third is coordinated to five oxalate O atoms and two H2O molecules.
The structure of Cs3Cr(C2O4)3.2H2O is built up of layers of [Cr(oxalate)3]3- anions in the bc plane that stack in the a direction, with each layer consisting exclusively of only a single enantiomer (Fig. 2) of either D- or L-[Cr(oxalate)3]3- anions and adjacent layers consisting exclusively of the opposing enantiomer. Na3Cr(oxalate)3.5H2O is also built up of layers of opposing D- or L-[Cr(oxalate)3]3- anions in the c direction, with adjacent layers having opposing enantiomers (Fig. 3). These [Cr(oxalate)3]3- layers are segregated by layers built up of polymeric chains of H2O and Na+ cations. The anion packing in Li3Cr(oxalate)3.6H2O does not consist of layers of a single enantiomer. Instead, pairs of D- and L-[Cr(oxalate)3]3- anions form columns in the a direction segregated by the H2O/Li+ layers. The packing of [Cr(oxalate)3]3- anions in the potassium and rubidium salts is similar, with pairs of opposing enantiomers in the bc plane rather than enantiomers occupying discrete layers.
In summary, the [Cr(oxalate)3]3- anion has now been studied with a series of counter-cations including five alkali metal cations. It has been postulated that the structures of the NH4+ and K+ salts differ due to the ability of the ammonium cation to form tetrahedral hydrogen bonds, and no conclusions could be drawn on the effects of changing the size of the cation (van Niekerk & Schoening, 1952). Whilst the alkali metal atomic radii increase in size in the order Li–Na–K–Rb–Cs, we have observed no direct correlation between cation size and packing of the [Cr(oxalate)3]3- layer. As expected, the smaller members of the family contain more coordinated water than the larger members. There is also no relationship between cation size and the chirality of the layers, with the Na+ and Cs+ salts having segregated layers of each enantiomer whilst the Li+, K+ and Rb+ salt layers contain mixtures of both enantiomers. The structures of the segregated layers of enantiomers in the Na+ and Cs+ salts differ greatly, as can be seen by the packing of [Cr(oxalate)3]3- anions in the Na+ salt in Fig. 3 compared with the Cs+ salt in Fig. 2.
The [Cr(oxalate)3]3- anion has been used as a component in molecular radical cation salts of BEDT-TTF to study the effects of small structural changes upon the bulk physical properties. The Li+, K+ and Rb+ salts all give a hexagonal packing arrangement of [Cr(oxalate)3]3- anions and cations, with a guest solvent molecule able to fit into the hexagonal cavity which differs in size depending on which cation is present. This can lead to metallic, semiconducting or superconducting behaviour. Interestingly, it is the Na+ and Cs+ salts which have given non-hexagonal packing arrangements in semiconducting BEDT-TTF salts (Martin et al., 2007 and 2008), both salts having no layer segration by enantiomer. The Na+ salt contains separate layers of BEDT-TTF, [Cr(oxalate)3]3- anions or Na+/H2O, whilst the salt grown from Cs3[Cr(oxalate)3].2H2O contains only layers of BEDT-TTF or H2O/[Cr(oxalate)3]3-, with no Cs+ being included in the structure.