Abstract
The title compound, octaaqua(hydrogenfluorido)dicopper(II) hexafluoridoferrate(III) dihydrate, was synthesized under hydrothermal conditions. The Cu atom is coordinated by one F and five O atoms within a highly distorted octahedron, forming dimeric [Cu2(H2O)8HF2]3+ units by edge sharing. These units are hydrogen bonded to [FeF6]3− anions and to an interstitial water molecule. The former feature Fe3+ on a special position (
). The dimeric copper units are linked to adjacent dimers by F—H⋯F hydrogen bonds. Additional O—H⋯O and O—H⋯F hydrogen bonds help to consolidate the crystal packing.
Related literature
For other hydrated copper-iron fluorides, see: Kummer & Babel (1987 ▶); Leblanc & Ferey (1990 ▶). For F⋯F distances, see: Frevel & Rinn (1962 ▶); Massa & Herdtweck (1983 ▶). For asymmetrical F—H⋯F hydrogen bonding, see: Roesky et al. (1990 ▶); Gerasimenko et al. (2007 ▶); Gerken et al. (2002 ▶). For Pb8MnFe2F24, see: Le Bail & Mercier (1992 ▶). For valence-bond analysis, see: Brown & Altermatt (1985 ▶); Brese & O’Keeffe (1991 ▶).
Experimental
Crystal data
[Cu2(HF2)(H2O)8][FeF6]·2H2O
M r = 516.12
Triclinic,
a = 6.659 (2) Å
b = 7.450 (3) Å
c = 8.377 (5) Å
α = 107.37 (4)°
β = 106.89 (5)°
γ = 94.26 (3)°
V = 373.6 (3) Å3
Z = 1
Mo Kα radiation
μ = 3.91 mm−1
T = 293 K
0.11 × 0.10 × 0.05 mm
Data collection
Siemens AED2 diffractometer
Absorption correction: gaussian (SHELX76; Sheldrick, 2008 ▶) T min = 0.698, T max = 0.845
3303 measured reflections
3303 independent reflections
2044 reflections with I > 2σ(I)
3 standard reflections frequency: 120 min intensity decay: 15%
Refinement
R[F 2 > 2σ(F 2)] = 0.040
wR(F 2) = 0.080
S = 1.00
3303 reflections
133 parameters
15 restraints
H atoms treated by a mixture of independent and constrained refinement
Δρmax = 0.62 e Å−3
Δρmin = −0.63 e Å−3
Data collection: STADI4 (Stoe & Cie, 1998 ▶); cell refinement: STADI4; data reduction: X-RED (Stoe & Cie, 1998 ▶); program(s) used to solve structure: SHELXS97 (Sheldrick, 2008 ▶); program(s) used to refine structure: SHELXL97 (Sheldrick, 2008 ▶); molecular graphics: DIAMOND (Brandenburg, 1999 ▶) and ORTEP-3 (Farrugia, 1997 ▶); software used to prepare material for publication: publCIF (Westrip, 2009 ▶).
Supplementary Material
Crystal structure: contains datablocks I, global. DOI: 10.1107/S1600536809006874/fi2069sup1.cif
Structure factors: contains datablocks I. DOI: 10.1107/S1600536809006874/fi2069Isup2.hkl
Additional supplementary materials: crystallographic information; 3D view; checkCIF report
Table 1. Selected bond lengths (Å).
| Cu—F4 | 1.9058 (19) |
| Cu—O1 | 1.939 (2) |
| Cu—O2 | 1.958 (2) |
| Cu—O3 | 1.977 (2) |
| Cu—O4 | 2.349 (3) |
| Fe—F1 | 1.9204 (16) |
| Fe—F2i | 1.930 (2) |
| Fe—F3 | 1.9402 (17) |
| Cu—O3ii | 2.715 (3) |
| Cu⋯Cuii | 3.575 (3) |
Symmetry codes: (i)
; (ii)
.
Table 2. Hydrogen-bond geometry (Å, °).
| D—H⋯A | D—H | H⋯A | D⋯A | D—H⋯A |
|---|---|---|---|---|
| O1—H11⋯F1iii | 1.00 (4) | 1.59 (4) | 2.590 (3) | 173 (4) |
| O1—H12⋯F2 | 0.99 (4) | 1.71 (4) | 2.679 (3) | 167 (4) |
| O2—H21⋯F1ii | 1.02 (5) | 1.61 (5) | 2.595 (3) | 161 (4) |
| O2—H22⋯O5iv | 0.98 (4) | 1.82 (4) | 2.699 (3) | 147 (5) |
| O3—H31⋯F3ii | 1.07 (5) | 1.52 (5) | 2.577 (2) | 167 (5) |
| O3—H32⋯F3v | 1.04 (5) | 1.64 (5) | 2.668 (3) | 171 (5) |
| O4—H41⋯F2vi | 1.02 (4) | 2.07 (9) | 2.766 (3) | 123 (8) |
| O4—H42⋯O5v | 1.01 (9) | 1.81 (9) | 2.793 (3) | 164 (8) |
| O5—H51⋯F2vii | 1.01 (6) | 2.05 (7) | 2.888 (3) | 139 (5) |
| O5—H51⋯F3viii | 1.01 (6) | 2.23 (5) | 3.072 (4) | 140 (6) |
| O5—H52⋯F4 | 1.05 (7) | 1.63 (7) | 2.676 (3) | 175 (6) |
| F4—H6⋯F4vi | 0.91 | 1.82 | 2.597 (4) | 142 |
Symmetry codes: (ii)
; (iii)
; (iv)
; (v)
; (vi)
; (vii)
; (viii)
.
Table 3. Valence-bond analysis according to the empirical expression from Brown & Altermatt (1985 ▶), using parameters for solids from Brese & O’Keeffe (1991 ▶).
| O1 | O2 | O3 | O4 | F4 | F1 | F2 | F3 | O5 | Σ | Σexpected | |
|---|---|---|---|---|---|---|---|---|---|---|---|
| Cu | 0.49 | 0.47 | 0.45 | 0.16 | 0.44 | 2.01 | 2 | ||||
| Fe | 0.51 (× 2) | 0.49 (× 2) | 0.48 (× 2) | 2.96 | 3 | ||||||
| H11 | 0.80 | 0.20 | 1 | 1 | |||||||
| H12 | 0.80 | 0.20 | 1 | 1 | |||||||
| H21 | 0.80 | 0.20 | 1 | 1 | |||||||
| H22 | 0.80 | 0.20 | 1 | 1 | |||||||
| H31 | 0.80 | 0.20 | 1 | 1 | |||||||
| H41 | 0.80 | 0.20 | 1 | 1 | |||||||
| H42 | 0.80 | 0.20 | 1 | 1 | |||||||
| H51 | 0.10 | 0.10 | 0.80 | 1 | 1 | ||||||
| H52 | 0.20 | 0.80 | 1 | 1 | |||||||
| H6 | 0.80 (× 0.5) | 1 | 1 | ||||||||
| 0.20 (× 0.5) | |||||||||||
| Σ | 2.09 | 2.07 | 2.05 | 1.76 | 1.14 | 0.91 | 0.99 | 0.98 | 2.00 | ||
| Σexpected | 2 | 2 | 2 | 2 | 1 | 1 | 1 | 1 | 2 |
Acknowledgments
Thanks are due to M. Leblanc for the single-crystal data collection.
supplementary crystallographic information
Comment
[Cu(H2O)4H0.5F]2(FeF6)(H2O)2 is the third hydrated copper–iron fluoride, the two previous ones being Cu3Fe2F12(H2O)12 (Kummer & Babel, 1987) and CuFe2F8(H2O)2 (Leblanc & Ferey, 1990). In this new compound, an almost perfect (FeF6)3- octahedron, placed on an inversion center, is connected exclusively by hydrogen bonding to edge-sharing bi-octahedral [Cu2(H2O)8HF2]3+ units and to an interstitial water molecule. The copper atom can be considered to be five-coordinated by four water molecules and one F atom in the fashion of a square pyramid (Figure 1). The square is constituted by the F atom and three water molecules at distances in the 1.906–1.977 Å range (Table 1), whereas Ow(4), at the top of the pyramid is at 2.349 Å (Jahn-Teller distortion). However, if one considers the next neighbour Ow(3) at 2.715 Å as sixth ligand, thecoordination can be described as very distorted octahedral, yielding centrosymmetric, dimeric units with a Cu—Cu distance of 3.575 Å. The dimers are bonded to adjacent dimers through F(4) by a HF2- ion (figure 2), however the F—F distance (2.597 Å) is much larger (Table 2) than usually observed (2.27 Å in LiHF2 (Frevel & Rinn, 1962), 2.28 in BaHF3 (Massa & Herdtweck, 1983). Moreover, the hydrogen atom H(6) which would have been expected at the 1/2, 1/2, 1/2 special position, exactly at the middle of the F(4)—F(4) atoms, in order to form a linear (F—H—F)- ion, was seen on the Fourier difference map as occupying more probably half a general position. It is then more a F—H···F bridge than a F—H—F one. Such asymmetrical F—H···F hydrogen bonding was observed in many cases for F—F distances going up to 2.686 Å in [(η5-C5Me5)NbF4(HF)AsF3]2 (Roesky et al., 1990), 2.429 to 2.512 Å in [OsO3F](HF)2[AsF6] (Gerken et al., 2002), 2.326 to 2.402 Å in Rb2-xKxZrF6(HF)2 (Gerasimenko et al., 2007).
The charge of the cations is balanced by the centrosymmetric anion [FeF6]3–. There are 14 water molecules around the (FeF6)3- octahedron, the H(51) atom corresponds to a bifurcated hydrogen bond towards F(2) and F(3) (figure 3). This helps the bond valence calculations to provide relatively satisfying results (Table 3), the largest disagreements being on O(4) and F(4). The contribution from the long Cu—Ow(3) distance is negligible.
Comparing with the Cu3Fe2F12(H2O)12 crystal structure (Kummer & Babel, 1987), also triclinic, there are strong differences. The three copper atoms and two Fe atoms are all placed on inversion centers. One (FeF6)3- octahedron is isolated, and the other forms chiolite-like square meshes by sharing F corners with tetra-hydrated Cu(H2O)4F2 elongated octahedra (the long distances are the two Cu—F ones, close to 2.32 Å for the three independent copper sites). In CuFe2F8(H2O)2 (Leblanc & Ferey, 1990), the CuF4(H2O)2 octahedra show two long Cu—F distances (2.451 Å). So, in both cases, the long distances are Cu—F ones, which is not the case of the title compound.
A study of the magnetic properties is currently in progress.
Experimental
Hydrothermal growth at 493 K from (2PbF2/2CuF2/FeF3) in HF 5M or 1M solutions, produced large crystals which could be identified as corresponding to Cu3Fe2F12(H2O)12 (Kummer & Babel, 1987) (5M solution) or to the title compound (1M). Both compounds are occurring with the same intense blue color and could have been confused if no powder pattern had been recorded. At other starting compositions, mixtures of both compounds could be observed, and also together especially with Pb8CuFe2F24 (starting from 2PbF2/CuF2/2FeF3 for instance), isostructural with Pb8MnFe2F24 (Le Bail & Mercier, 1992).
Refinement
The hydrogen atoms were all located on the difference Fourier map. Those of the water molecules were restrained to have Ow—H and H—H distances respectively close to 1.0 and 1.59 Å, their Uiso values were refined by groups of two. The hydrogen atom of the HF group was let at its difference Fourier map position with a fixed Uiso.
Figures
Fig. 1.
ORTEP-3 view (Farrugia, 1997) of the FeF63- octahedron, the isolated water molecule and the Cu(H2O)4F+ square-based pyramid which is forming octahedra dimeric units when considering the very long Cu-O3 distance (2.715Å). Displacement ellipsoids are shown at the 50% probability level. Symmetry-equivalent F atoms in the FeF6 group are generated by (i) -x, -y, -z. Symmetry-equivalent atoms in the [Cu2(H2O)8HF2]3+ unit are generated by (iii) 1-x, 1-y, -z.
Fig. 2.
Crystal packing with view along [010]. Hydrogen bonding is shown as dashed lines. Copper coordination shown as distorted octahedra (adding O(3) at 2.715 Å from Cu) sharing an edge.
Fig. 3.
The 14 water molecules, from the Cu coordination sphere or isolated, involved in hydrogen bonding with the FeF63- octahedron.
Crystal data
| [Cu2(H2F)(H2O)8][FeF6]·2H2O | Z = 1 |
| Mr = 516.12 | F(000) = 257 |
| Triclinic, P1 | Dx = 2.294 Mg m−3 |
| Hall symbol: -P 1 | Mo Kα radiation, λ = 0.71069 Å |
| a = 6.659 (2) Å | Cell parameters from 28 reflections |
| b = 7.450 (3) Å | θ = 2.7–35° |
| c = 8.377 (5) Å | µ = 3.91 mm−1 |
| α = 107.37 (4)° | T = 293 K |
| β = 106.89 (5)° | Platelet, blue |
| γ = 94.26 (3)° | 0.11 × 0.10 × 0.05 mm |
| V = 373.6 (3) Å3 |
Data collection
| Siemens AED2 diffractometer | 2044 reflections with I > 2σ(I) |
| Radiation source: fine-focus sealed tube | Rint = 0.0000 |
| graphite | θmax = 35.0°, θmin = 2.7° |
| 2θ/ω scans | h = −10→10 |
| Absorption correction: gaussian (SHELX76; Sheldrick, 2008) | k = −12→11 |
| Tmin = 0.698, Tmax = 0.845 | l = 0→13 |
| 3303 measured reflections | 3 standard reflections every 120 min |
| 3303 independent reflections | intensity decay: 15% |
Refinement
| Refinement on F2 | Secondary atom site location: difference Fourier map |
| Least-squares matrix: full | Hydrogen site location: difference Fourier map |
| R[F2 > 2σ(F2)] = 0.040 | H atoms treated by a mixture of independent and constrained refinement |
| wR(F2) = 0.080 | w = 1/[σ2(Fo2) + (0.03P)2] where P = (Fo2 + 2Fc2)/3 |
| S = 1.00 | (Δ/σ)max = 0.004 |
| 3303 reflections | Δρmax = 0.62 e Å−3 |
| 133 parameters | Δρmin = −0.63 e Å−3 |
| 15 restraints | Extinction correction: SHELXL97 (Sheldrick, 2008), Fc*=kFc[1+0.001xFc2λ3/sin(2θ)]-1/4 |
| Primary atom site location: structure-invariant direct methods | Extinction coefficient: 0.0072 (17) |
Special details
| 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. |
Fractional atomic coordinates and isotropic or equivalent isotropic displacement parameters (Å2)
| x | y | z | Uiso*/Ueq | Occ. (<1) | |
| Cu | 0.60473 (5) | 0.55727 (4) | 0.23479 (4) | 0.01662 (8) | |
| Fe | 0.0000 | 0.0000 | 0.0000 | 0.01433 (10) | |
| F1 | 0.2310 (3) | −0.0246 (2) | −0.0944 (2) | 0.0270 (3) | |
| F2 | 0.2029 (3) | 0.1318 (2) | 0.2331 (2) | 0.0275 (3) | |
| F3 | −0.0278 (3) | 0.2400 (2) | −0.0437 (2) | 0.0272 (4) | |
| F4 | 0.4365 (3) | 0.5885 (3) | 0.3872 (2) | 0.0338 (4) | |
| O1 | 0.5648 (3) | 0.2890 (3) | 0.2113 (3) | 0.0283 (4) | |
| O2 | 0.5992 (3) | 0.8217 (3) | 0.2411 (3) | 0.0244 (4) | |
| O3 | 0.7470 (3) | 0.5094 (3) | 0.0530 (3) | 0.0219 (4) | |
| O4 | 0.9139 (3) | 0.6601 (3) | 0.4849 (3) | 0.0262 (4) | |
| O5 | 0.2376 (4) | 0.8884 (3) | 0.4476 (3) | 0.0291 (4) | |
| H11 | 0.641 (6) | 0.188 (5) | 0.158 (6) | 0.064 (10)* | |
| H12 | 0.424 (5) | 0.226 (6) | 0.201 (6) | 0.064 (10)* | |
| H21 | 0.667 (7) | 0.876 (7) | 0.167 (5) | 0.084 (12)* | |
| H22 | 0.604 (8) | 0.935 (5) | 0.341 (5) | 0.084 (12)* | |
| H31 | 0.866 (7) | 0.623 (6) | 0.067 (8) | 0.117 (16)* | |
| H32 | 0.829 (8) | 0.398 (6) | 0.022 (8) | 0.117 (16)* | |
| H41 | 0.937 (15) | 0.679 (15) | 0.615 (5) | 0.24 (3)* | |
| H42 | 1.049 (10) | 0.734 (13) | 0.487 (12) | 0.24 (3)* | |
| H51 | 0.211 (11) | 0.909 (10) | 0.330 (6) | 0.16 (2)* | |
| H52 | 0.315 (12) | 0.770 (8) | 0.430 (10) | 0.16 (2)* | |
| H6 | 0.4219 | 0.4979 | 0.4375 | 0.080* | 0.50 |
Atomic displacement parameters (Å2)
| U11 | U22 | U33 | U12 | U13 | U23 | |
| Cu | 0.02080 (15) | 0.01342 (14) | 0.01901 (15) | 0.00339 (11) | 0.01121 (12) | 0.00561 (11) |
| Fe | 0.0157 (2) | 0.0129 (2) | 0.0174 (2) | 0.00267 (17) | 0.00901 (19) | 0.00591 (18) |
| F1 | 0.0276 (8) | 0.0268 (8) | 0.0391 (9) | 0.0100 (6) | 0.0248 (7) | 0.0139 (7) |
| F2 | 0.0255 (8) | 0.0296 (8) | 0.0217 (8) | −0.0025 (6) | 0.0064 (6) | 0.0038 (6) |
| F3 | 0.0295 (8) | 0.0181 (7) | 0.0442 (10) | 0.0077 (6) | 0.0185 (8) | 0.0176 (7) |
| F4 | 0.0475 (11) | 0.0338 (9) | 0.0375 (10) | 0.0184 (8) | 0.0290 (9) | 0.0192 (8) |
| O1 | 0.0285 (10) | 0.0151 (8) | 0.0470 (13) | 0.0038 (7) | 0.0227 (9) | 0.0086 (8) |
| O2 | 0.0386 (11) | 0.0138 (8) | 0.0261 (10) | 0.0040 (7) | 0.0177 (8) | 0.0074 (7) |
| O3 | 0.0270 (9) | 0.0179 (8) | 0.0281 (10) | 0.0056 (7) | 0.0191 (8) | 0.0079 (7) |
| O4 | 0.0243 (9) | 0.0267 (10) | 0.0261 (10) | 0.0042 (8) | 0.0076 (8) | 0.0074 (8) |
| O5 | 0.0359 (11) | 0.0279 (10) | 0.0264 (10) | 0.0109 (9) | 0.0128 (9) | 0.0093 (8) |
Geometric parameters (Å, °)
| Cu—F4 | 1.9058 (19) | F2—O5v | 2.888 (3) |
| Cu—O1 | 1.939 (2) | F3—O3iii | 2.577 (2) |
| Cu—O2 | 1.958 (2) | F3—O3vi | 2.668 (3) |
| Cu—O3 | 1.977 (2) | F3—O5vii | 3.072 (4) |
| Cu—O4 | 2.349 (3) | F4—F4iv | 2.597 (4) |
| Fe—F1 | 1.9204 (16) | F4—O1 | 2.632 (3) |
| Fe—F2i | 1.930 (2) | F4—O5 | 2.676 (3) |
| Fe—F3 | 1.9402 (17) | F4—O2 | 2.730 (3) |
| F1—O1ii | 2.590 (3) | F4—O4 | 3.006 (3) |
| F1—O2iii | 2.595 (3) | O1—O3 | 2.804 (3) |
| F1—F2 | 2.709 (3) | O2—O5viii | 2.699 (3) |
| F1—F3i | 2.728 (2) | O2—O3 | 2.814 (3) |
| F1—F3 | 2.732 (2) | O2—O4 | 3.061 (3) |
| F1—F2i | 2.736 (3) | O2—O3iii | 3.113 (4) |
| F1—O1 | 3.051 (4) | O3—O3iii | 3.128 (4) |
| F2—O1 | 2.679 (3) | O4—O4ix | 2.768 (4) |
| F2—F3i | 2.714 (3) | O4—O5x | 2.793 (3) |
| F2—F3 | 2.759 (3) | Cu—O3iii | 2.715 (3) |
| F2—O4iv | 2.766 (3) | Cu—Cuiii | 3.575 (3) |
| F4—Cu—O1 | 86.42 (9) | F1i—Fe—F2i | 89.43 (9) |
| F4—Cu—O2 | 89.89 (8) | F1—Fe—F3 | 90.08 (7) |
| O1—Cu—O2 | 171.49 (9) | F1i—Fe—F3 | 89.92 (7) |
| F4—Cu—O3 | 173.09 (9) | F2i—Fe—F3 | 89.06 (9) |
| O1—Cu—O3 | 91.47 (9) | F2—Fe—F3 | 90.94 (9) |
| O2—Cu—O3 | 91.30 (8) | H11—O1—H12 | 109 (3) |
| F4—Cu—O4 | 89.27 (9) | H21—O2—H22 | 104 (3) |
| O1—Cu—O4 | 97.50 (10) | H31—O3—H32 | 98 (3) |
| O2—Cu—O4 | 90.11 (9) | H41—O4—H42 | 103 (4) |
| O3—Cu—O4 | 97.53 (9) | H51—O5—H52 | 102 (3) |
| F1—Fe—F2i | 90.57 (9) |
Symmetry codes: (i) −x, −y, −z; (ii) −x+1, −y, −z; (iii) −x+1, −y+1, −z; (iv) −x+1, −y+1, −z+1; (v) x, y−1, z; (vi) x−1, y, z; (vii) −x, −y+1, −z; (viii) −x+1, −y+2, −z+1; (ix) −x+2, −y+1, −z+1; (x) x+1, y, z.
Hydrogen-bond geometry (Å, °)
| D—H···A | D—H | H···A | D···A | D—H···A |
| O1—H11···F1ii | 1.00 (4) | 1.59 (4) | 2.590 (3) | 173 (4) |
| O1—H12···F2 | 0.99 (4) | 1.71 (4) | 2.679 (3) | 167 (4) |
| O2—H21···F1iii | 1.02 (5) | 1.61 (5) | 2.595 (3) | 161 (4) |
| O2—H22···O5viii | 0.98 (4) | 1.82 (4) | 2.699 (3) | 147 (5) |
| O3—H31···F3iii | 1.07 (5) | 1.52 (5) | 2.577 (2) | 167 (5) |
| O3—H32···F3x | 1.04 (5) | 1.64 (5) | 2.668 (3) | 171 (5) |
| O4—H41···F2iv | 1.02 (4) | 2.07 (9) | 2.766 (3) | 123 (8) |
| O4—H42···O5x | 1.01 (9) | 1.81 (9) | 2.793 (3) | 164 (8) |
| O5—H51···F2xi | 1.01 (6) | 2.05 (7) | 2.888 (3) | 139 (5) |
| O5—H51···F3vii | 1.01 (6) | 2.23 (5) | 3.072 (4) | 140 (6) |
| O5—H52···F4 | 1.05 (7) | 1.63 (7) | 2.676 (3) | 175 (6) |
| F4—H6···F4iv | 0.91 | 1.82 | 2.597 (4) | 142 |
Symmetry codes: (ii) −x+1, −y, −z; (iii) −x+1, −y+1, −z; (viii) −x+1, −y+2, −z+1; (x) x+1, y, z; (iv) −x+1, −y+1, −z+1; (xi) x, y+1, z; (vii) −x, −y+1, −z.
Table 3 Valence-bond analysis according to the empirical expression from Brown & Altermatt (1985), using parameters for solids from Brese & O'Keeffe (1991)
| O1 | O2 | O3 | O4 | F4 | F1 | F2 | F3 | O5 | Σ | Σ expected | |
| Cu | 0.49 | 0.47 | 0.45 | 0.16 | 0.44 | 2.01 | 2 | ||||
| Fe | 0.51 (x2) | 0.49 (x2) | 0.48 (x2) | 2.96 | 3 | ||||||
| H11 | 0.80 | 0.20 | 1 | 1 | |||||||
| H12 | 0.80 | 0.20 | 1 | 1 | |||||||
| H21 | 0.80 | 0.20 | 1 | 1 | |||||||
| H22 | 0.80 | 0.20 | 1 | 1 | |||||||
| H31 | 0.80 | 0.20 | 1 | 1 | |||||||
| H41 | 0.80 | 0.20 | 1 | 1 | |||||||
| H42 | 0.80 | 0.20 | 1 | 1 | |||||||
| H51 | 0.10 | 0.10 | 0.80 | 1 | 1 | ||||||
| H52 | 0.20 | 0.80 | 1 | 1 | |||||||
| H6 | 0.80 (x0.5) | 1 | 1 | ||||||||
| 0.20 (x0.5) | |||||||||||
| Σ | 2.09 | 2.07 | 2.05 | 1.76 | 1.14 | 0.91 | 0.99 | 0.98 | 2.00 | ||
| Σexpected | 2 | 2 | 2 | 2 | 1 | 1 | 1 | 1 | 2 |
Footnotes
Supplementary data and figures for this paper are available from the IUCr electronic archives (Reference: FI2069).
References
- Brandenburg, K. (1999). DIAMOND Crystal Impact GbR, Bonn, Germany.
- Brese, N. E. & O’Keeffe, M. (1991). Acta Cryst. B47, 192–197.
- Brown, I. D. & Altermatt, D. (1985). Acta Cryst. B41, 244–247.
- Farrugia, L. J. (1997). J. Appl. Cryst.30, 565.
- Frevel, L. K. & Rinn, H. W. (1962). Acta Cryst.15, 286.
- Gerasimenko, A. V., Didenko, N. A. & Kavun, V. Y. (2007). Acta Cryst. E63, i198.
- Gerken, M., Dixon, D. A. & Schrobilgen, G. J. (2002). Inorg. Chem.41, 259–277. [DOI] [PubMed]
- Kummer, S. & Babel, D. (1987). Z. Naturforsch. Teil B, 42, 1403–1410.
- Le Bail, A. & Mercier, A.-M. (1992). Eur. J. Solid State Inorg. Chem.29, 183–190.
- Leblanc, M. & Ferey, G. (1990). Acta Cryst. C46, 13–15.
- Massa, W. & Herdtweck, E. (1983). Acta Cryst. C39, 509–512.
- Roesky, H. W., Sotoodeh, M., Xu, Y. M., Schrumpf, F. & Noltemeyer, M. (1990). Z. Anorg. Allg. Chem.580, 131–138.
- Sheldrick, G. M. (2008). Acta Cryst. A64, 112–122. [DOI] [PubMed]
- Stoe & Cie (1998). STADI4 and X-RED Stoe & Cie, Darmstadt, Germany.
- Westrip, S. P. (2009). publCIF In preparation.
Associated Data
This section collects any data citations, data availability statements, or supplementary materials included in this article.
Supplementary Materials
Crystal structure: contains datablocks I, global. DOI: 10.1107/S1600536809006874/fi2069sup1.cif
Structure factors: contains datablocks I. DOI: 10.1107/S1600536809006874/fi2069Isup2.hkl
Additional supplementary materials: crystallographic information; 3D view; checkCIF report



