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Single crystals of dizinc tellurium dichloride trioxide, Zn2(TeO3)Cl2, were synthesized via a transport reaction in sealed evacuated glass tubes. The compound has a layered structure in which the building units are [ZnO4Cl] square pyramids, distorted [ZnO2Cl2] tetrahedra and [TeO3E] tetrahedra (E is the 5s2 lone pair of the TeIV atom), joined through shared edges and corners to form charge-neutral layers. Cl atoms and Te-atom lone pairs protrude from the surfaces of each layer towards adjacent layers, and the layers are held together by dispersion forces only. The compound is isostructural with the synthetic compound CuZn(TeO3)Cl2 and the mineral sophiite, Zn2(SeO3)Cl2.

Supporting information

cif

Crystallographic Information File (CIF) https://doi.org/10.1107/S0108270103009715/bc1017sup1.cif
Contains datablocks global, I

hkl

Structure factor file (CIF format) https://doi.org/10.1107/S0108270103009715/bc1017Isup2.hkl
Contains datablock I

Comment top

The synthesis and crystal structure determination of the new compound Zn2(TeO3)Cl2, (I), is a further result of an ongoing study investigating the chemistry of tellurium oxohalogenides. The Te atom in (I) has a typical one-sided threefold coordination because of the presence of its 5 s2 lone pair (designated E) and its coordination polyhedron is therefore a [TeO3E] tetrahedron.

Atom Zn1 is coordinated by two O atoms and two Cl atoms, thus forming a distorted [ZnO2Cl2] tetrahedron. Atom Zn2 is coordinated by four O atoms and one Cl atom, which complete a distorted square [ZnO4Cl] pyramid. A distorted [ZnO4Cl2] octahedron is also formed if atom Cl1 is taken into account. However, the Zn2—Cl1 distance is long [3.2904 (5) Å], and atom Zn2 is located on the Cl2-atom side of the O-atom plane. Furthermore, bond valence sum calculations (Brown & Altermatt, 1985) give a negligible contribution from atom Cl1, suggesting that it should not be considered to be bonded to atom Zn2.

The three different building units, viz. [Zn1O2Cl2], [Zn2O4Cl] and [TeO3E], are connected so that infinite layers extending in the ac plane are formed (Fig 1). Each [ZnO4Cl] polyhedron is linked to two others by corner sharing so that infinite chains of [ZnO4Cl] polyhedra develop along the [001] direction within the layers. The chains are separated by [ZnO2Cl2] and [TeO3E] groups. Each [ZnO4Cl] polyhedron shares two corners with two [ZnO2Cl2] groups, as well as one corner and one edge with [TeO3E] groups (Fig 2).

The stereochemically active Te lone pairs are located in the space between the layers of the structure, pointing towards the space between the similarly protruding Cl atoms of the opposite layer. The shortest cation–anion distances between adjacent layers (Te···Cl1, Zn1···Cl1, Zn2···Cl1 and Zn1···Cl2) are similar to, or larger than, the cation–cation separation within the layers (Te···Zn2, Zn1···Zn2, Te···Zn1, Zn2···Zn2, Zn1···Zn1 and Te···Te; Table 2).

The long interlayer distances imply that the layers are only held together by attractive dispersion forces. Each layer can thus be considered as an infinite two-dimensional molecule. Assuming a Te—E radius of 1.25 Å (Galy et al., 1975), the fractional coordinates for the lone pair E (x = −0.02015, y = 0.33335 and z = 0.15126) yield E···Cl1 and E···Cl2 contact distances of \sim2.61 and \sim3.00 Å, respectively.

Compound (I) is isostructural with CuZn(TeO3)Cl2 (Johnsson & Törnroos, 2003). The mineral sophiite, Zn2(SeO3)Cl2 (Semenova et al., 1992), can also be considered as isostructural with (I), although, in contrast to (I), the coordination around atom Zn2 in the mineral creates a distorted [ZnO4Cl2] octahedron (Zn2—Cl1 = 2.68 Å and Zn2—Cl2 = 2.75 Å) with Zn2 located in the equatorial O-atom square plane. In sophiite, the coordination of both atom Cl1 and atom Cl2 to atom Zn2 is supported by bond-valence sum calculations.

Experimental top

Compound (I) was synthesized by chemical transport reactions in sealed evacuated soda-glass tubes. ZnO (ABCR, +99%), ZnCl2 (Avocado Research Chemicals Ltd., +98%) and TeO2 (ABCR, +99%) were used as starting materials. Equimolar amounts of ZnCl2, ZnO and TeO2 were mixed in a mortar and put in a glass tube (length ~6 cm), which was then evacuated and heated for 140 h at 770 K in a muffle furnace. The product appeared as colourless transparent plate-like single crystals and powder. The crystals are hygroscopic. The synthesis product was characterized in a scanning electron microscope (SEM, Jeol 820) with an energy-dispersive spectrometer (EDS, LINK AN10000) on ten different single crystals, giving a composition of 41.2 ± 1.3 at % Zn, 20.4 ± 0.6 at % Te, and 38.3 ± 1.2 at % Cl. No Si originating from the glass tubes was detected.

Refinement top

The maximum residual peak (0.78) is located 0.76 Å from the Te atom and the largest hole (−0.85) 0.73 Å from the Te atom.

Computing details top

Data collection: SMART (Bruker, 1999); cell refinement: SAINT (Bruker, 2001); data reduction: SAINT; program(s) used to solve structure: SHELXS97 (Sheldrick, 1990); program(s) used to refine structure: SHELXL97 (Sheldrick, 2001b); molecular graphics: DIAMOND (Brandenburg, 2000); software used to prepare material for publication: SHELXTL/PC (Sheldrick, 2001a) and PLATON (Spek, 2003).

Figures top
[Figure 1] Fig. 1. The layer features in (I) along [001]. [TeO3E] polyhedra are pink, [ZnO4Cl] polyhedra are green and [ZnO2Cl2] polyhedra are blue. O atoms are red, Cl atoms are light blue and Te lone pairs (E) are yellow.
[Figure 2] Fig. 2. The arrangement of coordination polyhedra around a central [ZnO4Cl] square pyramid. Colors are as described in Fig. 1.
dizinc tellurium dichloride trioxide top
Crystal data top
Zn2(TeO3)Cl2F(000) = 1360
Mr = 377.24Dx = 4.048 Mg m3
Orthorhombic, PccnMo Kα radiation, λ = 0.71073 Å
Hall symbol: -P 2ab 2acCell parameters from 5733 reflections
a = 10.4467 (9) Åθ = 2.4–32.5°
b = 15.4969 (13) ŵ = 13.14 mm1
c = 7.6471 (6) ÅT = 123 K
V = 1238.00 (18) Å3Plate, colourless
Z = 80.33 × 0.31 × 0.03 mm
Data collection top
Bruker SMART 2K CCD
diffractometer
2248 independent reflections
Radiation source: normal-focus sealed tube2119 reflections with I > 2σ(I)
Graphite monochromatorRint = 0.036
ω scansθmax = 32.6°, θmin = 2.4°
Absorption correction: numerical
(SHELXTL/PC (Sheldrick, 2001a) and PLATON (Spek, 2003)
h = 1515
Tmin = 0.035, Tmax = 0.709k = 2323
20130 measured reflectionsl = 1111
Refinement top
Refinement on F20 restraints
Least-squares matrix: fullPrimary atom site location: structure-invariant direct methods
R[F2 > 2σ(F2)] = 0.016Secondary atom site location: difference Fourier map
wR(F2) = 0.039 w = 1/[σ2(Fo2) + (0.0156P)2]
where P = (Fo2 + 2Fc2)/3
S = 1.26(Δ/σ)max = 0.002
2248 reflectionsΔρmax = 0.78 e Å3
73 parametersΔρmin = 0.85 e Å3
Crystal data top
Zn2(TeO3)Cl2V = 1238.00 (18) Å3
Mr = 377.24Z = 8
Orthorhombic, PccnMo Kα radiation
a = 10.4467 (9) ŵ = 13.14 mm1
b = 15.4969 (13) ÅT = 123 K
c = 7.6471 (6) Å0.33 × 0.31 × 0.03 mm
Data collection top
Bruker SMART 2K CCD
diffractometer
2248 independent reflections
Absorption correction: numerical
(SHELXTL/PC (Sheldrick, 2001a) and PLATON (Spek, 2003)
2119 reflections with I > 2σ(I)
Tmin = 0.035, Tmax = 0.709Rint = 0.036
20130 measured reflections
Refinement top
R[F2 > 2σ(F2)] = 0.01673 parameters
wR(F2) = 0.0390 restraints
S = 1.26Δρmax = 0.78 e Å3
2248 reflectionsΔρmin = 0.85 e Å3
Special details top

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. The maximum reidual peak (0.78 e A% −3) at 0.76 Å from Te and the largest hole (−0.85 e A% −3) at 0.73 Å from Te.

Fractional atomic coordinates and isotropic or equivalent isotropic displacement parameters (Å2) top
xyzUiso*/Ueq
Te0.027310 (10)0.402129 (7)0.206734 (14)0.00851 (4)
Zn10.00533 (2)0.611195 (14)0.34136 (3)0.01034 (5)
Zn20.262829 (19)0.472915 (13)0.39691 (3)0.01050 (5)
Cl10.08591 (5)0.71091 (3)0.16362 (6)0.01791 (9)
Cl20.20529 (4)0.62193 (3)0.42240 (5)0.01485 (8)
O10.08543 (12)0.41703 (8)0.43657 (15)0.0109 (2)
O20.18948 (11)0.44213 (8)0.14190 (15)0.0109 (2)
O30.05712 (12)0.51026 (8)0.19405 (15)0.0110 (2)
Atomic displacement parameters (Å2) top
U11U22U33U12U13U23
Te0.00795 (6)0.01028 (6)0.00730 (6)0.00006 (3)0.00070 (3)0.00087 (3)
Zn10.01156 (9)0.01211 (10)0.00736 (9)0.00078 (7)0.00012 (7)0.00044 (7)
Zn20.00824 (9)0.01573 (10)0.00752 (9)0.00144 (7)0.00034 (6)0.00048 (6)
Cl10.0275 (2)0.01342 (19)0.01281 (18)0.00274 (16)0.00504 (16)0.00109 (14)
Cl20.01096 (18)0.01445 (18)0.01915 (19)0.00067 (14)0.00075 (14)0.00190 (14)
O10.0107 (5)0.0144 (5)0.0076 (5)0.0024 (4)0.0005 (4)0.0002 (4)
O20.0087 (5)0.0165 (6)0.0076 (5)0.0004 (4)0.0000 (4)0.0002 (4)
O30.0088 (5)0.0126 (6)0.0117 (5)0.0010 (5)0.0019 (4)0.0005 (4)
Geometric parameters (Å, º) top
Te—O11.8738 (11)Zn1—Cl22.2919 (5)
Te—O21.8708 (12)Zn2—O12.0680 (13)
Te—O31.8962 (13)Zn2—O22.1488 (12)
Zn1—O1i1.9430 (12)Zn2—O2ii1.9965 (12)
Zn1—O32.0021 (12)Zn2—O3iii2.0223 (12)
Zn1—Cl12.2235 (5)Zn2—Cl22.3941 (5)
O2—Te—O185.08 (5)O2ii—Zn2—O189.19 (5)
O2—Te—O396.59 (5)O3iii—Zn2—O1159.71 (5)
O1—Te—O395.15 (5)O2ii—Zn2—O2152.57 (7)
O1i—Zn1—O3101.51 (5)O3iii—Zn2—O292.76 (5)
O1i—Zn1—Cl1121.85 (4)O1—Zn2—O273.77 (5)
O3—Zn1—Cl195.55 (4)O1—Zn2—Cl299.61 (4)
O1i—Zn1—Cl2101.15 (4)O2ii—Zn2—Cl2102.52 (4)
O3—Zn1—Cl2117.92 (4)O2—Zn2—Cl2101.45 (4)
Cl1—Zn1—Cl2118.575 (19)O3iii—Zn2—Cl297.88 (4)
O2ii—Zn2—O3iii96.98 (5)
Symmetry codes: (i) x, y+1, z+1; (ii) x+1/2, y, z+1/2; (iii) x+1/2, y+1, z+1/2.

Experimental details

Crystal data
Chemical formulaZn2(TeO3)Cl2
Mr377.24
Crystal system, space groupOrthorhombic, Pccn
Temperature (K)123
a, b, c (Å)10.4467 (9), 15.4969 (13), 7.6471 (6)
V3)1238.00 (18)
Z8
Radiation typeMo Kα
µ (mm1)13.14
Crystal size (mm)0.33 × 0.31 × 0.03
Data collection
DiffractometerBruker SMART 2K CCD
diffractometer
Absorption correctionNumerical
(SHELXTL/PC (Sheldrick, 2001a) and PLATON (Spek, 2003)
Tmin, Tmax0.035, 0.709
No. of measured, independent and
observed [I > 2σ(I)] reflections
20130, 2248, 2119
Rint0.036
(sin θ/λ)max1)0.759
Refinement
R[F2 > 2σ(F2)], wR(F2), S 0.016, 0.039, 1.26
No. of reflections2248
No. of parameters73
Δρmax, Δρmin (e Å3)0.78, 0.85

Computer programs: SMART (Bruker, 1999), SAINT (Bruker, 2001), SAINT, SHELXS97 (Sheldrick, 1990), SHELXL97 (Sheldrick, 2001b), DIAMOND (Brandenburg, 2000), SHELXTL/PC (Sheldrick, 2001a) and PLATON (Spek, 2003).

Selected geometric parameters (Å, º) top
Te—O11.8738 (11)Zn1—Cl22.2919 (5)
Te—O21.8708 (12)Zn2—O12.0680 (13)
Te—O31.8962 (13)Zn2—O22.1488 (12)
Zn1—O1i1.9430 (12)Zn2—O2ii1.9965 (12)
Zn1—O32.0021 (12)Zn2—O3iii2.0223 (12)
Zn1—Cl12.2235 (5)Zn2—Cl22.3941 (5)
O2—Te—O185.08 (5)O2ii—Zn2—O189.19 (5)
O2—Te—O396.59 (5)O3iii—Zn2—O1159.71 (5)
O1—Te—O395.15 (5)O2ii—Zn2—O2152.57 (7)
O1i—Zn1—O3101.51 (5)O3iii—Zn2—O292.76 (5)
O1i—Zn1—Cl1121.85 (4)O1—Zn2—O273.77 (5)
O3—Zn1—Cl195.55 (4)O1—Zn2—Cl299.61 (4)
O1i—Zn1—Cl2101.15 (4)O2ii—Zn2—Cl2102.52 (4)
O3—Zn1—Cl2117.92 (4)O2—Zn2—Cl2101.45 (4)
Cl1—Zn1—Cl2118.575 (19)O3iii—Zn2—Cl297.88 (4)
O2ii—Zn2—O3iii96.98 (5)
Symmetry codes: (i) x, y+1, z+1; (ii) x+1/2, y, z+1/2; (iii) x+1/2, y+1, z+1/2.
Inter- and intra-layer distances (Å) top
Te···Cl1i3.1841 (5)
Zn1···Cl1ii3.7923 (5)
Zn2···Cl1i4.4850 (6)
Zn1···Cl2iii5.2262 (6)
Te···Zn23.0613 (3)
Zn1···Zn2iv3.2992 (3)
Te···Zn13.4166 (4)
Zn2···Zn2v3.8329 (3)
Zn1···Zn1vi4.2162 (5)
Te···Tevii4.4186 (3)
Symmetry codes: (i) −x,y − 1/2,1/2 − z; (ii) x,3/2 − y,1/2 + z; (iii) 1/2 − x,3/2 − y,z; (iv) x − 1/2,1 − y,1/2 − z; (v) 1/2 − x,y,z − 1/2; (vi) −x,1 − y,1 − z; (vii) −x,1 − y,-z
 

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