Supporting information
Crystallographic Information File (CIF) https://doi.org/10.1107/S0108270103028671/bc1033sup1.cif | |
Structure factor file (CIF format) https://doi.org/10.1107/S0108270103028671/bc1033Isup2.hkl |
Because of the extraordinary affinity of europium towards oxygen, all chemical manipulations were performed in a glovebox under dry argon, with oxygen and moisture levels below 1 p.p.m. The accidental synthesis of Eu4OI6 resulted from a 1:1 mixture of EuI2 (Aldrich, 99.9%) and Li2(NCN) [synthesized according to Liu (2002)], which was placed in a tantalum ampoule that was sealed with an arc welder and jacketed with quartz, both under argon. The sample was heated to 1073 K for two days and then slowly cooled (6 K min−1) to room temperature. As a result of slight oxygen contamination (probably as LiOH) of the X-ray pure Li2(NCN), yellow prisms (about 3 ×0.5 ×0.5 mm in size) of Eu4OI6 were obtained. The phase seemingly acts as a getter for traces of oxygen, in agreement with independent observations (Meyer & Schleid, 1987). Compound (I) can also be synthesized through deliberately introducing oxygen-containing educts (e.g. Eu2O3), and crystals of Eu4OCl6 and Eu4OBr6 can be grown using identical conditions. The halide/cyanamide melts seemingly catalyze the growth of single crystals, which are difficult to obtain otherwise. Because of their sensitivity to oxygen and moisture, the single crystals were mounted in glass capillaries inside a glovebox for the X-ray measurements.
The empirical SADABS method was used for absorption correction. The refinement was started from the structure of the isotypic chloride phase, with anisotropic displacement parameters for Eu and I atoms and an isotropic displacement parameter for O atoms. The absolute structure was determined on the basis of 336 Friedel pairs [Flack parameter = 0.07 (4)].
Data collection: SMART (Bruker, 2001); cell refinement: SMART; data reduction: SAINT-Plus (Bruker, 1999); program(s) used to solve structure: SHELXTL (Sheldrick, 1998); program(s) used to refine structure: SHELXTL; molecular graphics: PLATON (Spek, 2003); software used to prepare material for publication: SHELXTL.
Eu4OI6 | Dx = 6.138 Mg m−3 |
Mr = 1385.24 | Mo Kα radiation, λ = 0.71073 Å |
Hexagonal, P63mc | Cell parameters from 9730 reflections |
Hall symbol: P 6c -2c | θ = 2.3–28.3° |
a = 10.404 (2) Å | µ = 28.82 mm−1 |
c = 7.996 (3) Å | T = 293 K |
V = 749.5 (3) Å3 | Prism, yellow |
Z = 2 | 0.15 × 0.10 × 0.09 mm |
F(000) = 1156 |
Bruker Apex CCD diffractometer | 727 independent reflections |
Radiation source: fine-focus sealed tube | 704 reflections with I > 2 σ(I) |
Graphite monochromator | Rint = 0.056 |
ω scan | θmax = 28.3°, θmin = 2.3° |
Absorption correction: empirical (using intensity measurements) SADABS, Sheldrick, 1996 | h = −13→13 |
Tmin = 0.479, Tmax = 1.0 | k = −13→13 |
9730 measured reflections | l = −10→10 |
Refinement on F2 | Primary atom site location: structure-invariant direct methods |
Least-squares matrix: full | Secondary atom site location: difference Fourier map |
R[F2 > 2σ(F2)] = 0.027 | w = 1/[σ2(Fo2) + (0.0325P)2 + 11.61P] where P = (Fo2 + 2Fc2)/3 |
wR(F2) = 0.067 | (Δ/σ)max < 0.001 |
S = 1.09 | Δρmax = 0.86 e Å−3 |
727 reflections | Δρmin = −1.73 e Å−3 |
24 parameters | Absolute structure: Flack H D (1983), Acta Cryst. A39, 876-881 |
1 restraint | Absolute structure parameter: 0.07 (4) |
Eu4OI6 | Z = 2 |
Mr = 1385.24 | Mo Kα radiation |
Hexagonal, P63mc | µ = 28.82 mm−1 |
a = 10.404 (2) Å | T = 293 K |
c = 7.996 (3) Å | 0.15 × 0.10 × 0.09 mm |
V = 749.5 (3) Å3 |
Bruker Apex CCD diffractometer | 727 independent reflections |
Absorption correction: empirical (using intensity measurements) SADABS, Sheldrick, 1996 | 704 reflections with I > 2 σ(I) |
Tmin = 0.479, Tmax = 1.0 | Rint = 0.056 |
9730 measured reflections |
R[F2 > 2σ(F2)] = 0.027 | w = 1/[σ2(Fo2) + (0.0325P)2 + 11.61P] where P = (Fo2 + 2Fc2)/3 |
wR(F2) = 0.067 | Δρmax = 0.86 e Å−3 |
S = 1.09 | Δρmin = −1.73 e Å−3 |
727 reflections | Absolute structure: Flack H D (1983), Acta Cryst. A39, 876-881 |
24 parameters | Absolute structure parameter: 0.07 (4) |
1 restraint |
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. PLAT731 Type_1 Test for consistency of Bond su's and Coordinate su's in CIF A large ratio of the reported and calculated bond s.u.'s is found. The use of a DFIX instruction might cause such a warning since calculated s.u.'s are based on reported variances only. Note_1: su's on the unitcell dimensions are taken into account in the calculation of expected su's. This may result in large differences between expected and reported su's when this contribution is not included in the reported su's, in particular for inaccurate unitcells. Note_2: Another source for the discrepancy between calculated and reported su's can be that the validation software has access only to the variances of the refined parameters as opposed to the full co-variance matrix used by e.g. SHELXL for the calculation of derived parameters with associated su's. Constrained/restrained refinement may cause largei co-variances. |
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 | ||
Eu1 | 0.3333 | 0.6667 | 0.40454 (18) | 0.0234 (3) | |
Eu2 | 0.20583 (3) | −0.20583 (3) | 0.01196 (10) | 0.01521 (16) | |
I1 | 0.13479 (5) | −0.13479 (5) | 0.39107 (13) | 0.0202 (2) | |
I2 | 0.46500 (5) | −0.46500 (5) | 0.70720 (13) | 0.0192 (2) | |
O | 0.3333 | 0.6667 | 0.1055 (19) | 0.007 (3)* |
U11 | U22 | U33 | U12 | U13 | U23 | |
Eu1 | 0.0251 (4) | 0.0251 (4) | 0.0200 (6) | 0.0125 (2) | 0.000 | 0.000 |
Eu2 | 0.0117 (2) | 0.0117 (2) | 0.0232 (3) | 0.0067 (2) | −0.00086 (16) | 0.00086 (16) |
I1 | 0.0136 (3) | 0.0136 (3) | 0.0288 (5) | 0.0032 (3) | 0.00165 (19) | −0.00165 (19) |
I2 | 0.0165 (3) | 0.0165 (3) | 0.0248 (5) | 0.0083 (4) | 0.00049 (19) | −0.00049 (19) |
Eu1—O | 2.391 (15) | Eu2—I2ix | 3.5458 (11) |
Eu1—I2i | 3.3891 (16) | Eu2—I2x | 3.5458 (11) |
Eu1—I2ii | 3.3891 (16) | Eu2—Eu1iv | 3.8900 (16) |
Eu1—I2iii | 3.3891 (16) | Eu2—Eu2xi | 3.9796 (14) |
Eu1—I1iii | 3.5794 (12) | Eu2—Eu2xii | 3.9796 (14) |
Eu1—I1ii | 3.5794 (12) | I1—Eu2xiii | 3.4032 (9) |
Eu1—I1i | 3.5794 (12) | I1—Eu2xiv | 3.4032 (9) |
Eu1—Eu2iii | 3.8900 (16) | I1—Eu1iv | 3.5794 (12) |
Eu1—Eu2i | 3.8900 (16) | I2—Eu2xv | 3.3757 (12) |
Eu1—Eu2ii | 3.8900 (16) | I2—Eu2xvi | 3.3757 (12) |
Eu2—Oiv | 2.416 (5) | I2—Eu1iv | 3.3891 (16) |
Eu2—I1 | 3.2905 (15) | I2—Eu2xvii | 3.5458 (11) |
Eu2—I2v | 3.3757 (12) | I2—Eu2xviii | 3.5458 (11) |
Eu2—I2vi | 3.3757 (12) | O—Eu2iii | 2.416 (5) |
Eu2—I1vii | 3.4032 (9) | O—Eu2i | 2.416 (5) |
Eu2—I1viii | 3.4032 (9) | O—Eu2ii | 2.416 (5) |
O—Eu1—I2i | 135.57 (3) | I1—Eu2—I2ix | 69.34 (2) |
O—Eu1—I2ii | 135.57 (3) | I2v—Eu2—I2ix | 144.44 (3) |
I2i—Eu1—I2ii | 74.64 (4) | I2vi—Eu2—I2ix | 74.51 (2) |
O—Eu1—I2iii | 135.57 (3) | I1vii—Eu2—I2ix | 140.62 (2) |
I2i—Eu1—I2iii | 74.64 (4) | I1viii—Eu2—I2ix | 71.08 (2) |
I2ii—Eu1—I2iii | 74.64 (4) | Oiv—Eu2—I2x | 74.63 (13) |
O—Eu1—I1iii | 88.28 (3) | I1—Eu2—I2x | 69.34 (2) |
I2i—Eu1—I1iii | 70.829 (18) | I2v—Eu2—I2x | 74.51 (2) |
I2ii—Eu1—I1iii | 70.829 (18) | I2vi—Eu2—I2x | 144.44 (3) |
I2iii—Eu1—I1iii | 136.16 (5) | I1vii—Eu2—I2x | 71.08 (2) |
O—Eu1—I1ii | 88.28 (3) | I1viii—Eu2—I2x | 140.62 (2) |
I2i—Eu1—I1ii | 70.829 (18) | I2ix—Eu2—I2x | 125.14 (4) |
I2ii—Eu1—I1ii | 136.16 (5) | Oiv—Eu2—Eu1iv | 35.8 (3) |
I2iii—Eu1—I1ii | 70.829 (18) | I1—Eu2—Eu1iv | 59.10 (3) |
I1iii—Eu1—I1ii | 119.910 (3) | I2v—Eu2—Eu1iv | 112.83 (3) |
O—Eu1—I1i | 88.28 (3) | I2vi—Eu2—Eu1iv | 112.83 (3) |
I2i—Eu1—I1i | 136.16 (5) | I1vii—Eu2—Eu1iv | 131.46 (2) |
I2ii—Eu1—I1i | 70.829 (18) | I1viii—Eu2—Eu1iv | 131.46 (2) |
I2iii—Eu1—I1i | 70.829 (18) | I2ix—Eu2—Eu1iv | 64.19 (2) |
I1iii—Eu1—I1i | 119.910 (3) | I2x—Eu2—Eu1iv | 64.19 (2) |
I1ii—Eu1—I1i | 119.910 (3) | Oiv—Eu2—Eu2xi | 34.56 (16) |
O—Eu1—Eu2iii | 36.203 (19) | I1—Eu2—Eu2xi | 109.689 (18) |
I2i—Eu1—Eu2iii | 111.68 (2) | I2v—Eu2—Eu2xi | 91.102 (16) |
I2ii—Eu1—Eu2iii | 111.68 (2) | I2vi—Eu2—Eu2xi | 53.882 (17) |
I2iii—Eu1—Eu2iii | 171.77 (3) | I1vii—Eu2—Eu2xi | 160.71 (2) |
I1iii—Eu1—Eu2iii | 52.07 (2) | I1viii—Eu2—Eu2xi | 109.012 (16) |
I1ii—Eu1—Eu2iii | 105.72 (3) | I2ix—Eu2—Eu2xi | 55.864 (13) |
I1i—Eu1—Eu2iii | 105.72 (3) | I2x—Eu2—Eu2xi | 109.051 (14) |
O—Eu1—Eu2i | 36.203 (19) | Eu1iv—Eu2—Eu2xi | 59.235 (15) |
I2i—Eu1—Eu2i | 171.77 (3) | Oiv—Eu2—Eu2xii | 34.56 (16) |
I2ii—Eu1—Eu2i | 111.68 (2) | I1—Eu2—Eu2xii | 109.689 (18) |
I2iii—Eu1—Eu2i | 111.68 (2) | I2v—Eu2—Eu2xii | 53.882 (17) |
I1iii—Eu1—Eu2i | 105.72 (3) | I2vi—Eu2—Eu2xii | 91.102 (16) |
I1ii—Eu1—Eu2i | 105.72 (3) | I1vii—Eu2—Eu2xii | 109.012 (16) |
I1i—Eu1—Eu2i | 52.07 (2) | I1viii—Eu2—Eu2xii | 160.71 (2) |
Eu2iii—Eu1—Eu2i | 61.53 (3) | I2ix—Eu2—Eu2xii | 109.051 (14) |
O—Eu1—Eu2ii | 36.203 (19) | I2x—Eu2—Eu2xii | 55.864 (13) |
I2i—Eu1—Eu2ii | 111.68 (2) | Eu1iv—Eu2—Eu2xii | 59.235 (15) |
I2ii—Eu1—Eu2ii | 171.77 (3) | Eu2xi—Eu2—Eu2xii | 60.0 |
I2iii—Eu1—Eu2ii | 111.68 (2) | Eu2—I1—Eu2xiii | 109.11 (2) |
I1iii—Eu1—Eu2ii | 105.72 (3) | Eu2—I1—Eu2xiv | 109.11 (2) |
I1ii—Eu1—Eu2ii | 52.07 (2) | Eu2xiii—I1—Eu2xiv | 141.41 (4) |
I1i—Eu1—Eu2ii | 105.72 (3) | Eu2—I1—Eu1iv | 68.83 (3) |
Eu2iii—Eu1—Eu2ii | 61.53 (3) | Eu2xiii—I1—Eu1iv | 99.216 (19) |
Eu2i—Eu1—Eu2ii | 61.53 (3) | Eu2xiv—I1—Eu1iv | 99.216 (19) |
Oiv—Eu2—I1 | 94.9 (3) | Eu2xv—I2—Eu2xvi | 72.24 (3) |
Oiv—Eu2—I2v | 84.9 (3) | Eu2xv—I2—Eu1iv | 105.17 (3) |
I1—Eu2—I2v | 142.48 (2) | Eu2xvi—I2—Eu1iv | 105.17 (3) |
Oiv—Eu2—I2vi | 84.9 (3) | Eu2xv—I2—Eu2xvii | 154.51 (3) |
I1—Eu2—I2vi | 142.48 (2) | Eu2xvi—I2—Eu2xvii | 103.95 (2) |
I2v—Eu2—I2vi | 74.99 (4) | Eu1iv—I2—Eu2xvii | 100.15 (3) |
Oiv—Eu2—I1vii | 141.71 (3) | Eu2xv—I2—Eu2xviii | 103.95 (2) |
I1—Eu2—I1vii | 88.65 (3) | Eu2xvi—I2—Eu2xviii | 154.51 (3) |
I2v—Eu2—I1vii | 70.13 (2) | Eu1iv—I2—Eu2xviii | 100.15 (3) |
I2vi—Eu2—I1vii | 114.36 (3) | Eu2xvii—I2—Eu2xviii | 68.27 (3) |
Oiv—Eu2—I1viii | 141.71 (3) | Eu1—O—Eu2iii | 108.0 (3) |
I1—Eu2—I1viii | 88.65 (3) | Eu1—O—Eu2i | 108.0 (3) |
I2v—Eu2—I1viii | 114.36 (3) | Eu2iii—O—Eu2i | 110.9 (3) |
I2vi—Eu2—I1viii | 70.13 (2) | Eu1—O—Eu2ii | 108.0 (3) |
I1vii—Eu2—I1viii | 76.35 (3) | Eu2iii—O—Eu2ii | 110.9 (3) |
Oiv—Eu2—I2ix | 74.63 (13) | Eu2i—O—Eu2ii | 110.9 (3) |
Symmetry codes: (i) −y, x−y, z; (ii) −x+y+1, −x+1, z; (iii) x, y+1, z; (iv) x, y−1, z; (v) −x+y+1, −x, z−1; (vi) −y, x−y−1, z−1; (vii) y, −x+y, z−1/2; (viii) x−y, x, z−1/2; (ix) y+1, −x+y+1, z−1/2; (x) x−y−1, x−1, z−1/2; (xi) −x+y+1, −x, z; (xii) −y, x−y−1, z; (xiii) x−y, x, z+1/2; (xiv) y, −x+y, z+1/2; (xv) −x+y+1, −x, z+1; (xvi) −y, x−y−1, z+1; (xvii) x−y, x−1, z+1/2; (xviii) y+1, −x+y, z+1/2. |
Experimental details
Crystal data | |
Chemical formula | Eu4OI6 |
Mr | 1385.24 |
Crystal system, space group | Hexagonal, P63mc |
Temperature (K) | 293 |
a, c (Å) | 10.404 (2), 7.996 (3) |
V (Å3) | 749.5 (3) |
Z | 2 |
Radiation type | Mo Kα |
µ (mm−1) | 28.82 |
Crystal size (mm) | 0.15 × 0.10 × 0.09 |
Data collection | |
Diffractometer | Bruker Apex CCD diffractometer |
Absorption correction | Empirical (using intensity measurements) SADABS, Sheldrick, 1996 |
Tmin, Tmax | 0.479, 1.0 |
No. of measured, independent and observed [I > 2 σ(I)] reflections | 9730, 727, 704 |
Rint | 0.056 |
(sin θ/λ)max (Å−1) | 0.667 |
Refinement | |
R[F2 > 2σ(F2)], wR(F2), S | 0.027, 0.067, 1.09 |
No. of reflections | 727 |
No. of parameters | 24 |
No. of restraints | 1 |
w = 1/[σ2(Fo2) + (0.0325P)2 + 11.61P] where P = (Fo2 + 2Fc2)/3 | |
Δρmax, Δρmin (e Å−3) | 0.86, −1.73 |
Absolute structure | Flack H D (1983), Acta Cryst. A39, 876-881 |
Absolute structure parameter | 0.07 (4) |
Computer programs: SMART (Bruker, 2001), SMART, SAINT-Plus (Bruker, 1999), SHELXTL (Sheldrick, 1998), SHELXTL, PLATON (Spek, 2003).
Eu1—O | 2.391 (15) | Eu2—I2iv | 3.3757 (12) |
Eu1—I2i | 3.3891 (16) | Eu2—I1v | 3.4032 (9) |
Eu1—I1ii | 3.5794 (12) | Eu2—I2vi | 3.5458 (11) |
Eu1—Eu2ii | 3.8900 (16) | Eu2—Eu1iii | 3.8900 (16) |
Eu2—Oiii | 2.416 (5) | Eu2—Eu2vii | 3.9796 (14) |
Eu2—I1 | 3.2905 (15) | ||
Eu2ii—Eu1—Eu2i | 61.53 (3) | Eu1—O—Eu2ii | 108.0 (3) |
Eu2ii—Eu1—Eu2viii | 61.53 (3) | Eu1—O—Eu2i | 108.0 (3) |
Eu2i—Eu1—Eu2viii | 61.53 (3) | Eu2ii—O—Eu2i | 110.9 (3) |
Eu1iii—Eu2—Eu2ix | 59.235 (15) | Eu1—O—Eu2viii | 108.0 (3) |
Eu1iii—Eu2—Eu2vii | 59.235 (15) | Eu2ii—O—Eu2viii | 110.9 (3) |
Eu2ix—Eu2—Eu2vii | 60.0 | Eu2i—O—Eu2viii | 110.9 (3) |
Symmetry codes: (i) −y, x−y, z; (ii) x, y+1, z; (iii) x, y−1, z; (iv) −y, x−y−1, z−1; (v) y, −x+y, z−1/2; (vi) y+1, −x+y+1, z−1/2; (vii) −y, x−y−1, z; (viii) −x+y+1, −x+1, z; (ix) −x+y+1, −x, z. |
Europium oxyhalides of general formula Eu4OX6 (X = Cl and Br) was first referred to by Tanguy et al. (1970), who indexed their X-ray patterns on the basis of the pattern of Ba4OCl6. The formation of single crystals has been observed as a by-product from oxygen-containing melts (Meyer & Schleid, 1987), and a systematic route based on reaction mixtures incorporating EuX3 (X = Cl and Br), Eu2O3 and lithium metal succeeded in growing pale-yellow single crystals of good quality (Schleid & Meyer, 1987a). The synthesis and structure determination of the iodide phase Eu4OI6, however, have not yet been studied. The present contribution is part of a project targeted at synthesizing rare-earth cyanamides/carbodiimides, during which, by accident, we found a simple way to grow single crystals of Eu4OX6 (X = Cl, Br and I).
Eu4OI6 crystallizes in a hexagonal system in P63mc and is isotypic with Eu4OCl6 and Eu4OBr6. The most important structural feature of Eu4OI6 is the tetrahedral [Eu4O]6+ unit (Fig. 1) containing divalent europium. The O atom resides in the center of the tetrahedron, the Eu—O distances being similar to one another [Eu1—O = 2.39 Å and Eu2—O = 2.42 Å]. The Eu—Eu distances are 3.89 (Eu1—Eu2) and 3.98 Å (Eu2—Eu2), and the tetrahedral angles are very close to their ideal values, namely 108.0 (3)° for Eu1—O—Eu2 and 110.9 (3)° for Eu2—O—Eu2. The average Eu—O (2.41 Å) and Eu—Eu (3.94 Å) distances in Eu4OI6 are only slightly larger than those in Eu4OCl6 (2.36 and 3.86 Å, respectively) and Eu4OBr6 (2.39 and 3.90 Å, respectively).
The Eu coordination is augmented by neighboring iodide anions, with interatomic distances ranging from 3.39 to 3.58 Å (Eu1, six bonds) and from 3.29 to 3.55 Å (Eu2, seven bonds). On the basis of the tabulated bond-valence parameter for the EuII—O [r0 = 2.147 Å (Brese & O'Keeffe, 1991)] and EuII—I bonds [r0 = 2.869 Å (generated from the crystal structure of EuI2; Sanchez et al., 1985)], the empirical valences of atoms Eu1 and Eu2 sum to 1.69 and 2.11, respectively. Even including the three very long Eu1—O distances [3.96 Å] in the calculation, the Eu1 valence sum does not fully match the divalent state. We note that a similar effect is missing in Ba4OCl6, thereby indicating the possibility of weak metal–metal bonding in the rare-earth tetrahedron through residual electron density. In fact, the EuII—EuII distances in Eu4OI6 are almost identical with those in elemental Eu (3.99 Å; Sutton, 1965), and similar effects of metal–metal bonding in less than fully oxidized rare-earth metal compounds have been described in corresponding quantum-chemical investigations of extended solids (Landrum et al., 1999).
When projected along [001] (Fig. 2), the crystal structure of Eu4OI6 exhibits one-dimensional hexagonal channels of approximate diameter 4.86 Å (atom-to-atom distance), which can be compared with the corresponding channel diameters in Eu4OBr6 (4.70 Å) and in Eu4OCl6 (4.62 Å). Analogous channels are also observed in related rare-earth oxyhalides, such as Sm4OCl6 [4.61 Å; calculated with the data given by Schleid & Meyer (1987b)] and Yb4OCl6 (4.37 Å; Schleid & Meyer, 1987c). It is not yet known whether these channels can provide enough empty space for the inclusion of other chemical species. To the best of our knowledge, hexagonal channels filled with only halide anions are exclusively found in the rare-earth oxyhalides. For related oxoselenate or phosphate compounds, similar hexagonal channels have been described in combination with electron `lone-pairs' on the Se and P atoms (Wontcheu & Schleid, 2003; Morris et al., 1994). In Tb3O2Cl[SeO3]2 (Wontcheu & Schleid, 2002), two chloride anions in diametrically opposed positions around the hexagon are involved in the channel formation.