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Lithium tetrachloridoaluminate, LiAlCl4: a new polymorph (oP12, Pmn21) with Li+ in tetrahedral interstices
aInstitut für Anorganische Chemie und Strukturchemie, Lehrstuhl II: Material- und Strukturforschung, Heinrich-Heine-Universität Düsseldorf, Universitätsstrasse 1, D-40225 Düsseldorf, Germany
*Correspondence e-mail: wfrank@hhu.de
Dissolving lithium chloride and aluminium chloride in boiling para- or meta-xylene and keeping the colourless solution at room temperature led to crystal growth of a new modification of lithium tetrachloridoaluminate, LiAlCl4, which represents a second modification (oP12, Pmn21) of the ternary salt besides the long known monoclinic form [LiAlCl4(mP24, P21/c); Mairesse et al. (1977). Cryst. Struct. Commun. 6, 15–18]. The crystal structures of both modifications can be described as slightly distorted hexagonal closest packings of chloride anions. While the lithium cations in LiAlCl4(mP24) are in octahedral coordination and the aluminium and lithium ions in the solid of orthorhombic LiAlCl4 occupy tetrahedral interstices with site symmetries m and 1, respectively, the lithium cation site being half-occupied (defect wurtz-stannite-type structure). From (DSC) measurements, no evidence for a of the orthorhombic modification is found until the material melts at 148 °C (Tpeak = 152 °C). The melting point is nearly identical to the literature data for LiAlCl4(mP24) [146 °C; Weppner & Huggins (1976). J. Electrochem. Soc. 124, 35–38]. From the melts of both polymorphs, the monoclinic modification recrystallizes.
CCDC reference: 1570829
1. Chemical context
The series of known crystal structures of alkali metal tetrachloridoaluminates MAlCl4, with M = Li (Mairesse et al., 1977), Na (Baenziger, 1951), K (Mairesse et al., 1978a), Rb (Mairesse et al., 1979) and Cs (Gearhart et al., 1975; Mairesse et al., 1979) was completed about 40 years ago and comparative structural studies were made (Mairesse et al., 1979; Meyer & Schwan, 1980). With respect to both solid lithium tetrachloridoaluminate [LiAlCl4(mP24, P21/c); Mairesse et al., 1977] and melts of the salt were investigated (Weppner & Huggins, 1976, 1977). Besides the importance of common commercial lithium–thionyl chloride battery systems (Winter & Brodd, 2004), recently published studies on the conductivity of LiAlCl4 in dimethyl carbonate or mixtures with ethylene carbonate (Scholz et al., 2015) indicate that the substance is of continous interest. In the course of our on-going studies on arene complexation of main group metals (Frank, 1990; Frank et al., 1987, 1996; Frank & Wittmer, 1997; Kugel, 2004; Bredenhagen, 2014), we isolated a new polymorph of LiAlCl4(oP12, Pmn21) from mixtures of lithium chloride and aluminium chloride in boiling para- or meta-xylene, determined its by single-crystal X-ray diffraction and unequivocally proved of this ternary compound.
2. Structural commentary
LiAlCl4(oP12, Pmn21) crystallizes in a defect wurtz-stannite-type structure, an orthorhombic of the wurtzite-type structure, known from quaternary compounds of the type Cu2MIIMIVM4VI (MII = Mn, Fe, Co, Zn, Cd, Hg; MIV = Si, Ge, Sn; MVI = S, Se; except of cobalt; Schäfer & Nitsche, 1977). The of the title compound contains four chloride anions and two aluminium cations, located in special positions (Wyckoff position 2a), as well as two lithium cations and another four chloride anions in general positions (4b), with the lithium site being half occupied, i.e. the of the is defined by half a tetrachloridoaluminate anion and one half-occupied lithium ion (Fig. 1a).
The crystal structures of the title compound, as well as of the monoclinic modification of lithium tetrachloridoaluminate, can be described as slightly distorted hexagonal closest packings of chloride anions. While the lithium cations in LiAlCl4(mP24) are in octahedral coordination (Mairesse et al., 1977), the aluminium and lithium ions in the solid of orthorhombic LiAlCl4 occupy tetrahedral interstices with site symmetries m and 1, respectively, the lithium cation site being half-occupied (Figs. 1b and 1c). Hence, the solid state of the title compound represents a three-dimensional network of corner-sharing tetrahedra, while in LiAlCl4(mP24), the octahedral and tetrahedral polyhedra are connected via corners as well as edges. LiAlCl4(oP12) exhibits, as expected, shorter Li—Cl bonds (coordination number 4) as compared to corresponding bonds in monoclinic LiAlCl4 (coordination number 6). Using the Brown formalism (Brown & Altermatt, 1985), in both cases, bond orders which differ significantly from the expected value in view of the monovalent cation are computed (Table 1). In the case of orthorhombic LiAlCl4, the strong deviation is based on the statistical disorder mentioned above and corresponding averaged geometric parameters obtained for occupied and non-occupied tetrahedral interstices, leading to higher Li—Cl bond orders in view of the exponential relationship between bond length and bond order.
3. Raman spectra
Raman bands in the vibrational spectrum of the title compound (Fig. 2) can be assigned to the four normal modes of vibration of a five atomic tetrahedral moiety of composition AX4 (Nakamoto, 1986) νs(A1: 350 cm−1), δd(E: 136 and 126 cm−1), νd(F2: 523, 502, 487 and 478 cm−1) and δd(F2: 180 and 170 cm−1). As in the Raman spectra of other alkali metal tetrachloridoaluminates (Rytter & Øye, 1973; Rubbens et al., 1978) or NH4AlCl4 (Mairesse et al., 1978b), splitting of the bands is observed corresponding to the site effect and perturbation of the ideal tetrahedral symmetry of free AlCl4− anions caused by cation interactions.
4. and X-ray powder diffraction
From DSC measurements of the title compound (Fig. 3), no evidence for a is found until the material melts at 148 °C (Tpeak = 152 °C). The melting point is nearly identical to literature data for LiAlCl4(mP24) (146 °C; Weppner & Huggins, 1976), which seems to be the only modification that recrystallizes from the melts of both modifications. This is demonstrated by high-quality X-ray powder diffraction patterns of the title compound, crystallized from para-xylene solution, and of the crystalline solid obtained by recrystallization from the melt (Fig. 4). In view of the current data, we suppose LiAlCl4(oP12) to represent a metastable phase of lithium tetrachloridoaluminate whose melting point probably is nearly identical to that of monoclinic LiAlCl4 because it is very unlikely that a would not have been observed with the chosen DSC methods. The lower density of orthorhombic LiAlCl4 (1.89 g cm−3) compared to monoclinic LiAlCl4 (1.98 g cm−3; Mairesse et al., 1979) supports the assumption of its metastability.
5. Synthesis and crystallization
All sample preparations and manipulations were carried out in an atmosphere of dry argon (argon 5.0) using either Schlenk techniques or an MBraun LABstar glove-box. LiCl (beads, 99.9+%, anhydrous) and AlCl3 (powder, 99.99%) were purchased from Sigma–Aldrich and while LiCl was used as received, AlCl3 was first overlayed with elemental aluminium (grit, ≥97%, Sigma–Aldrich) and sublimed in a sealed ampoule in vacuo at 190 °C. p-Xylene (99%, Sigma–Aldrich) and m-xylene (99%, TCI) were refluxed with aluminium chloride, washed with 0.2 M NaOH, as well as distilled water, and distilled on molecular sieve 4 Å afterwards. In a typical reaction, 0.112 g (2.64 mmol) lithium chloride and 0.268 g (2.01 mmol) aluminium chloride were treated with 5 ml p-xylene and the mixture was refluxed for 30 min. Seperation of the warm colourless solution from residual LiCl and removal of 4 ml of the solvent under reduced pressure at room temperature led to the formation of colourless crystals of the title compound. LiAlCl4(oP12, Pmn21) was isolated in 60% yield after washing the crystalline material with p-xylene and drying the solid in vacuo at room temperature.
The FT–Raman spectrum was recorded using a Bruker MultiRam spectrometer (OPUS; Bruker, 2006) equipped with an RT-InGaAs-detector and an Nd:YAG-Laser at 1064 nm (Stokes: 3500–70 cm−1; resolution: 2 cm−1): νd(F2, AlCl4−): 523 (w), 502 (w), 487 (m), 478 (w); νs(A1, AlCl4−): 350 (vs); δd(F2, AlCl4−): 180 (s), 170 (s); δd(E, AlCl4−): 136 (m), 126 (s), 104 (m).
Thermal analysis (differential scanning calorimetry) was carried out with a Mettler Toledo DSC 1 calorimeter (STARe; Mettler-Toledo, 2008) equipped with an FRS 5 sensor using medium pressure steel crucibles without sealing rings. Measurements were carried out in an atmosphere of dry nitrogen at a heating/cooling rate of 5 °C min−1 between 0 and 170 °C. First measurement heating: Tonset = 148 °C (Tpeak = 152 °C), endothermic, melting; first measurement cooling: Tonset = 132 °C (Tpeak = 132 °C), exothermic, crystallization; second measurement heating: Tonset = 149 °C (Tpeak = 152 °C), endothermic, melting; second measurement cooling: Tonset = 139 °C (Tpeak = 138 °C), exothermic, crystallization; third measurement heating: Tonset = 148 °C (Tpeak = 152 °C), endothermic, melting; third measurement cooling: Tonset = 139 °C (Tpeak = 139 °C), exothermic, crystallization. An alternative melting-point determination was carried out with a Mettler Toledo MP 90 Melting Point System: Tmp = 149 °C.
X-ray powder diffraction patterns were measured using a Stoe & Cie STADI P (WinXPOW; Stoe & Cie, 2003) Debye–Scherrer diffractometer working in transmission mode with Cu Kα1 radiation [Ge(111) monochromator]. Simulations of powder patterns from single-crystal data were carried out using the computer program PowderCell (Kraus & Nolze, 2000).
6. Refinement
Crystal data, data collection and structure . The lithium cation site (general position, Wyckoff site 4b) is half occupied.
details are summarized in Table 2
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Supporting information
CCDC reference: 1570829
https://doi.org/10.1107/S205698901701235X/wm5410sup1.cif
contains datablock I. DOI:Structure factors: contains datablock I. DOI: https://doi.org/10.1107/S205698901701235X/wm5410Isup2.hkl
Data collection: X-AREA (Stoe & Cie, 2009); cell
X-AREA (Stoe & Cie, 2009); data reduction: X-AREA (Stoe & Cie, 2009); program(s) used to solve structure: SHELXT (Sheldrick, 2015a); program(s) used to refine structure: SHELXL2014 (Sheldrick, 2015b); molecular graphics: DIAMOND (Brandenburg, 2016); software used to prepare material for publication: publCIF (Westrip, 2010).LiAlCl4 | Dx = 1.887 Mg m−3 |
Mr = 175.72 | Mo Kα radiation, λ = 0.71073 Å |
Orthorhombic, Pmn21 | Cell parameters from 6814 reflections |
a = 7.8273 (10) Å | θ = 3.0–29.7° |
b = 6.4466 (10) Å | µ = 1.90 mm−1 |
c = 6.1304 (8) Å | T = 173 K |
V = 309.34 (7) Å3 | Needle-shaped, colorless |
Z = 2 | 0.65 × 0.10 × 0.03 mm |
F(000) = 168 |
Stoe IPDS 2T diffractometer | 870 reflections with I > 2σ(I) |
Radiation source: fine-focus sealed tube | Rint = 0.092 |
φ–scans | θmax = 29.1°, θmin = 3.2° |
Absorption correction: multi-scan (X-AREA; Stoe & Cie, 2009) | h = −10→10 |
Tmin = 0.431, Tmax = 0.583 | k = −8→8 |
3388 measured reflections | l = −8→8 |
880 independent reflections |
Refinement on F2 | 1 restraint |
Least-squares matrix: full | w = 1/[σ2(Fo2) + (0.022P)2 + 0.166P] where P = (Fo2 + 2Fc2)/3 |
R[F2 > 2σ(F2)] = 0.028 | (Δ/σ)max < 0.001 |
wR(F2) = 0.075 | Δρmax = 0.48 e Å−3 |
S = 1.21 | Δρmin = −0.46 e Å−3 |
880 reflections | Absolute structure: Flack x determined using 386 quotients [(I+)-(I-)]/[(I+)+(I-)] (Parsons et al., 2013) |
37 parameters | Absolute structure parameter: 0.1 (2) |
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 | Occ. (<1) | |
Li1 | 0.246 (2) | 0.1671 (19) | 0.493 (3) | 0.035 (3) | 0.5 |
Cl1 | 0.0000 | 0.31452 (19) | 0.34835 (19) | 0.0305 (3) | |
Cl2 | 0.22483 (12) | 0.18042 (11) | 0.88033 (12) | 0.0317 (2) | |
Cl3 | 0.5000 | 0.35454 (16) | 0.3896 (3) | 0.0295 (3) | |
Al1 | 0.0000 | 0.3312 (2) | −0.0004 (3) | 0.0229 (3) |
U11 | U22 | U33 | U12 | U13 | U23 | |
Li1 | 0.043 (8) | 0.033 (6) | 0.029 (8) | 0.001 (6) | 0.002 (6) | 0.000 (4) |
Cl1 | 0.0300 (5) | 0.0405 (6) | 0.0208 (7) | 0.000 | 0.000 | 0.0010 (4) |
Cl2 | 0.0313 (4) | 0.0314 (4) | 0.0324 (5) | 0.0078 (3) | 0.0067 (5) | 0.0017 (5) |
Cl3 | 0.0300 (5) | 0.0226 (4) | 0.0360 (6) | 0.000 | 0.000 | −0.0055 (6) |
Al1 | 0.0244 (8) | 0.0212 (6) | 0.0233 (8) | 0.000 | 0.000 | 0.0008 (5) |
Li1—Cl1 | 2.322 (17) | Cl2—Li1iv | 2.356 (14) |
Li1—Cl2i | 2.356 (14) | Cl3—Al1v | 2.1354 (18) |
Li1—Cl2 | 2.38 (2) | Cl3—Li1vi | 2.413 (17) |
Li1—Cl3 | 2.413 (17) | Al1—Cl3vii | 2.1354 (18) |
Cl1—Al1 | 2.1404 (19) | Al1—Cl2viii | 2.1392 (11) |
Cl1—Li1ii | 2.322 (17) | Al1—Cl2ix | 2.1392 (11) |
Cl2—Al1iii | 2.1392 (11) | ||
Cl1—Li1—Cl2i | 111.0 (7) | Li1iv—Cl2—Li1 | 104.6 (5) |
Cl1—Li1—Cl2 | 108.0 (7) | Al1v—Cl3—Li1vi | 113.1 (4) |
Cl2i—Li1—Cl2 | 109.5 (6) | Al1v—Cl3—Li1 | 113.1 (4) |
Cl1—Li1—Cl3 | 112.2 (6) | Li1vi—Cl3—Li1 | 111.1 (7) |
Cl2i—Li1—Cl3 | 108.6 (7) | Cl3vii—Al1—Cl2viii | 108.85 (6) |
Cl2—Li1—Cl3 | 107.5 (7) | Cl3vii—Al1—Cl2ix | 108.85 (6) |
Al1—Cl1—Li1ii | 113.7 (5) | Cl2viii—Al1—Cl2ix | 110.70 (8) |
Al1—Cl1—Li1 | 113.7 (5) | Cl3vii—Al1—Cl1 | 111.28 (9) |
Li1ii—Cl1—Li1 | 111.9 (9) | Cl2viii—Al1—Cl1 | 108.58 (6) |
Al1iii—Cl2—Li1iv | 114.3 (4) | Cl2ix—Al1—Cl1 | 108.58 (6) |
Al1iii—Cl2—Li1 | 114.4 (4) |
Symmetry codes: (i) −x+1/2, −y, z−1/2; (ii) −x, y, z; (iii) x, y, z+1; (iv) −x+1/2, −y, z+1/2; (v) −x+1/2, −y+1, z+1/2; (vi) −x+1, y, z; (vii) −x+1/2, −y+1, z−1/2; (viii) −x, y, z−1; (ix) x, y, z−1. |
Li1—Cl1 | 2.322 (17) | Li—Cl1 | 2.475 (7) |
Li1—Cl2 | 2.381 (21) | Li1—Cl2x | 2.729 (7) |
Li1—Cl2i | 2.356 (14) | Li1—Cl2xi | 2.841 (7) |
Li1—Cl3 | 2.413 (17) | Li1—Cl3 | 2.594 (7) |
Li1—Cl3xii | 2.769 (7) | ||
Li1—Cl4xiii | 2.493 (7) | ||
Σs(Li—Cl) | 1.17 | Σs(Li—Cl) | 0.87 |
Symmetry codes: (i) -x+1/2, -y, z-1/2; (x) -x, y-1/2, -z+1/2; (xi) x, -y+1/2, z+1/2; (xii) -x, y-1/2, -z+1/2; (xiii) 1-x, y-1/2, -z+1/2. |
Acknowledgements
We thank E. Hammes and P. Roloff for technical support.
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