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The molecular title compound was solvothermally synthesized at 373 K and crystallized in the triclinic system, with space group P\overline 1. The Ge(IV) atom lies on an inversion center and is coordinated by four fluoride anions and two pyridine mol­ecules. Owing to the non-bridging nature of the fluoride anions, this material forms a molecular solid with close packing.

Supporting information

cif

Crystallographic Information File (CIF) https://doi.org/10.1107/S1600536802020408/fl6007sup1.cif
Contains datablocks global, I

hkl

Structure factor file (CIF format) https://doi.org/10.1107/S1600536802020408/fl6007Isup2.hkl
Contains datablock I

CCDC reference: 202295

Key indicators

  • Single-crystal X-ray study
  • T = 298 K
  • Mean [sigma](C-C) = 0.006 Å
  • R factor = 0.039
  • wR factor = 0.052
  • Data-to-parameter ratio = 12.4

checkCIF results

No syntax errors found

ADDSYM reports no extra symmetry


Yellow Alert Alert Level C:
GOODF_01 Alert C The least squares goodness of fit parameter lies outside the range 0.80 <> 2.00 Goodness of fit given = 0.769 PLAT_710 Alert C Delete 1-2-3 or 2-3-4 (CIF) Linear Torsion Angle # 5 N1 -GE1 -N1 -C1 -80.00100.00 2.666 1.555 1.555 1.555 PLAT_710 Alert C Delete 1-2-3 or 2-3-4 (CIF) Linear Torsion Angle # 10 N1 -GE1 -N1 -C5 99.00100.00 2.666 1.555 1.555 1.555
0 Alert Level A = Potentially serious problem
0 Alert Level B = Potential problem
3 Alert Level C = Please check

Comment top

Our research is currently focused on the sovolthermal synthesis of new layered and open-framework materials based on lower group 14 elements. We have used both cationic and anionic structure-directing agents, for the formation of anionic and cationic germanium-, tin- (Salami et al., 2001a,b, 2002; Lansky et al., 2001) and lead-based compounds (Tran et al., 2002). Our interest in these materials stems from their potential to yield chemically and thermally stable microporous zeotype materials, with advantageous materials properties, such as ion-exchange, separations and catalysis. We have successfully synthesized a series of new materials. We are also interested in these materials for their possible semiconducting properties, as well as for low-dimensional solid-state precursors to extended frameworks.

Recently, we used a predominantly non-aqueous environment, where the only source of water was present in the hexafluorophosphoric acid reagent (HF6P 60 wt% solution in water), which was added to a pyridine solvent. Hexafluorophosphoric acid was selected as a potential anionic structure directing agent. Instead, it acted as source of fluoride. Pyridine and fluoride combined with germanium to form BING-10, an octahedral complex (Fig. 1). The key feature of BING-10 is the non-bridging terminal fluorides, which results in the formation of a neutral molecular solid (Fig. 2). In the case of lead as the building block, the fluorides bridge the metal centres, to give rise to an extended layered material (BING-5; Tran et al., 2002).

BING-10 was obtained as isolated octahedral units that form a neutral molecular solid. Note that pyridine solvent molecules ended up as a monodentate ligand. There is only one crystallographically unique germanium centre, which is bonded to four fluorides and the N atoms of two pyridine molecules. The Ge—F distances are 1.768 (2) and 1.770 (2) Å, while the Ge—N distance is 2.014 (3) Å. All trans ligands define a 180° bond angle, since the molecule resides on the inversion centre. The cis-F—Ge—F bond angles are 89.96 (9) and 90.04 (9)°, while those of F—Ge—N vary from 89.82 (10) to 90.18 (10)°.

We are working further towards obtaining cationic and anionic germanates, especially new layered or open-framework materials. It would appear that a significant concentration of fluoride source in our systems is not suitable for the formation of an extended germanium oxide material. We are currently studying other combinations of germanium sources, solvents and structure directing agents, to isolate inorganic materials with semiconducting or anion-exchange capabilities.

Experimental top

The reaction mixture consisted of pyridine, germanium tetraethoxide and HF6P in a molar ratio of 16:1:1. Sovolthermal synthesis was conducted in a 23 ml capacity Teflon-lined Parr autoclave at 373 K for 6 d. The BING-10 crystals were colourless needles, and one was manually selected for single-crystal X-ray diffraction analysis. The yield was ca 65.7%.

Computing details top

Data collection: SMART (Bruker, 1999); cell refinement: SAINT (Bruker, 1999); data reduction: SAINT; program(s) used to solve structure: SHELXS90 (Sheldrick, 1990); program(s) used to refine structure: SHELXL97 (Sheldrick, 1997); molecular graphics: ORTEP-3 (Farrugia, 1997) and ATOMS (Dowty,1999); software used to prepare material for publication: SHELXL97.

Figures top
[Figure 1] Fig. 1. View of the molecules of BING-10, shown with ellipsoids at the 50% probability level.
[Figure 2] Fig. 2. The crystallographic a projection of BING-10, highlighting the germanium tetrafluoride dipyridine complex (colour scheme: Ge blue, F red, N green, C dark grey and H light grey).
(I) top
Crystal data top
[GeF4(C5H5N)2]Z = 1
Mr = 306.79F(000) = 152
Triclinic, P1Dx = 1.865 Mg m3
a = 6.4729 (13) ÅMo Kα radiation, λ = 0.71073 Å
b = 7.0928 (14) ÅCell parameters from 758 reflections
c = 7.2643 (14) Åθ = 6.4–43.7°
α = 115.138 (4)°µ = 2.84 mm1
β = 94.921 (4)°T = 298 K
γ = 109.954 (4)°Needle, colorless
V = 273.16 (9) Å30.17 × 0.05 × 0.04 mm
Data collection top
Bruker SmartApex CCD area-detector
diffractometer
1007 independent reflections
Radiation source: fine-focus sealed tube778 reflections with I > 2σ(I)
Graphite monochromatorRint = 0.058
ω scansθmax = 25.4°, θmin = 3.2°
Absorption correction: multi-scan
(XPREP; Sheldrick, 1997)
h = 77
Tmin = 0.827, Tmax = 0.893k = 88
2925 measured reflectionsl = 88
Refinement top
Refinement on F2Primary atom site location: structure-invariant direct methods
Least-squares matrix: fullSecondary atom site location: difference Fourier map
R[F2 > 2σ(F2)] = 0.039Hydrogen site location: inferred from neighbouring sites
wR(F2) = 0.052H-atom parameters constrained
S = 0.77 w = 1/[σ2(Fo2) + (0.007P)2]
where P = (Fo2 + 2Fc2)/3
1007 reflections(Δ/σ)max < 0.001
81 parametersΔρmax = 0.41 e Å3
0 restraintsΔρmin = 0.38 e Å3
Crystal data top
[GeF4(C5H5N)2]γ = 109.954 (4)°
Mr = 306.79V = 273.16 (9) Å3
Triclinic, P1Z = 1
a = 6.4729 (13) ÅMo Kα radiation
b = 7.0928 (14) ŵ = 2.84 mm1
c = 7.2643 (14) ÅT = 298 K
α = 115.138 (4)°0.17 × 0.05 × 0.04 mm
β = 94.921 (4)°
Data collection top
Bruker SmartApex CCD area-detector
diffractometer
1007 independent reflections
Absorption correction: multi-scan
(XPREP; Sheldrick, 1997)
778 reflections with I > 2σ(I)
Tmin = 0.827, Tmax = 0.893Rint = 0.058
2925 measured reflections
Refinement top
R[F2 > 2σ(F2)] = 0.0390 restraints
wR(F2) = 0.052H-atom parameters constrained
S = 0.77Δρmax = 0.41 e Å3
1007 reflectionsΔρmin = 0.38 e Å3
81 parameters
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.

Fractional atomic coordinates and isotropic or equivalent isotropic displacement parameters (Å2) top
xyzUiso*/Ueq
Ge10.50000.50000.50000.0361 (2)
F10.3876 (3)0.6030 (3)0.3512 (3)0.0521 (6)
F20.3697 (3)0.6146 (3)0.6981 (3)0.0507 (6)
N10.2178 (5)0.2019 (4)0.3534 (4)0.0360 (8)
C10.0135 (5)0.1950 (4)0.2899 (4)0.0411 (10)
H10.00230.33060.31500.058 (12)*
C50.2334 (5)0.0057 (4)0.3173 (4)0.0450 (10)
H50.37460.00860.35980.044 (10)*
C20.1812 (7)0.0091 (6)0.1879 (6)0.0487 (11)
H20.32130.01090.14360.040 (11)*
C40.0430 (7)0.2008 (6)0.2186 (6)0.0488 (11)
H40.05660.33450.19680.069 (13)*
C30.1649 (7)0.2090 (7)0.1528 (6)0.0526 (11)
H30.29380.34780.08520.057 (12)*
Atomic displacement parameters (Å2) top
U11U22U33U12U13U23
Ge10.0308 (4)0.0350 (3)0.0416 (4)0.0131 (3)0.0050 (3)0.0193 (3)
F10.0456 (14)0.0450 (13)0.0606 (15)0.0128 (11)0.0061 (12)0.0298 (12)
F20.0449 (14)0.0438 (12)0.0537 (15)0.0189 (11)0.0205 (13)0.0140 (11)
N10.0298 (19)0.0360 (18)0.040 (2)0.0125 (15)0.0049 (16)0.0189 (16)
C10.042 (3)0.043 (2)0.041 (3)0.021 (2)0.011 (2)0.020 (2)
C50.045 (3)0.043 (2)0.050 (3)0.022 (2)0.006 (2)0.024 (2)
C20.030 (3)0.060 (3)0.047 (3)0.014 (2)0.006 (2)0.024 (2)
C40.056 (3)0.033 (2)0.045 (3)0.012 (2)0.003 (2)0.017 (2)
C30.047 (3)0.042 (3)0.049 (3)0.004 (2)0.006 (2)0.018 (2)
Geometric parameters (Å, º) top
Ge1—F21.7678 (19)C1—H10.9300
Ge1—F2i1.7678 (19)C5—C41.379 (4)
Ge1—F1i1.7696 (18)C5—H50.9300
Ge1—F11.7696 (18)C2—C31.373 (5)
Ge1—N1i2.014 (3)C2—H20.9300
Ge1—N12.014 (3)C4—C31.362 (5)
N1—C11.340 (3)C4—H40.9300
N1—C51.344 (3)C3—H30.9300
C1—C21.384 (4)
F2—Ge1—F2i180.00 (11)C5—N1—Ge1119.83 (19)
F2—Ge1—F1i90.04 (9)N1—C1—C2121.6 (3)
F2i—Ge1—F1i89.96 (9)N1—C1—H1119.2
F2—Ge1—F189.96 (9)C2—C1—H1119.2
F2i—Ge1—F190.04 (9)N1—C5—C4121.2 (3)
F1i—Ge1—F1180.0N1—C5—H5119.7
F2—Ge1—N1i89.94 (10)C4—C5—H5119.2
F2i—Ge1—N1i90.06 (10)C3—C2—C1119.2 (4)
F1i—Ge1—N1i90.18 (10)C3—C2—H2120.4
F1—Ge1—N1i89.82 (10)C1—C2—H2120.4
F2—Ge1—N190.06 (10)C3—C4—C5120.1 (4)
F2i—Ge1—N189.94 (10)C3—C4—H4120.0
F1i—Ge1—N189.82 (10)C5—C4—H4120.0
F1—Ge1—N190.18 (10)C4—C3—C2119.0 (4)
N1i—Ge1—N1180.0C4—C3—H3120.5
C1—N1—C5119.0 (3)C2—C3—H3120.5
C1—N1—Ge1121.14 (18)
F2—Ge1—N1—C157.7 (2)N1i—Ge1—N1—C599 (100)
F2i—Ge1—N1—C1122.3 (2)C5—N1—C1—C20.1 (5)
F1i—Ge1—N1—C1147.7 (2)Ge1—N1—C1—C2179.6 (2)
F1—Ge1—N1—C132.3 (2)C1—N1—C5—C40.7 (5)
N1i—Ge1—N1—C180 (100)Ge1—N1—C5—C4179.6 (2)
F2—Ge1—N1—C5122.6 (2)N1—C1—C2—C30.7 (5)
F2i—Ge1—N1—C557.4 (2)N1—C5—C4—C31.0 (5)
F1i—Ge1—N1—C532.6 (2)C5—C4—C3—C20.5 (6)
F1—Ge1—N1—C5147.4 (2)C1—C2—C3—C40.4 (6)
Symmetry code: (i) x+1, y+1, z+1.

Experimental details

Crystal data
Chemical formula[GeF4(C5H5N)2]
Mr306.79
Crystal system, space groupTriclinic, P1
Temperature (K)298
a, b, c (Å)6.4729 (13), 7.0928 (14), 7.2643 (14)
α, β, γ (°)115.138 (4), 94.921 (4), 109.954 (4)
V3)273.16 (9)
Z1
Radiation typeMo Kα
µ (mm1)2.84
Crystal size (mm)0.17 × 0.05 × 0.04
Data collection
DiffractometerBruker SmartApex CCD area-detector
diffractometer
Absorption correctionMulti-scan
(XPREP; Sheldrick, 1997)
Tmin, Tmax0.827, 0.893
No. of measured, independent and
observed [I > 2σ(I)] reflections
2925, 1007, 778
Rint0.058
(sin θ/λ)max1)0.602
Refinement
R[F2 > 2σ(F2)], wR(F2), S 0.039, 0.052, 0.77
No. of reflections1007
No. of parameters81
H-atom treatmentH-atom parameters constrained
Δρmax, Δρmin (e Å3)0.41, 0.38

Computer programs: SMART (Bruker, 1999), SAINT (Bruker, 1999), SAINT, SHELXS90 (Sheldrick, 1990), SHELXL97 (Sheldrick, 1997), ORTEP-3 (Farrugia, 1997) and ATOMS (Dowty,1999), SHELXL97.

Selected geometric parameters (Å, º) top
Ge1—F21.7678 (19)Ge1—N1i2.014 (3)
Ge1—F1i1.7696 (18)
F2—Ge1—F2i180.00 (11)F2i—Ge1—N1i90.06 (10)
F2—Ge1—F1i90.04 (9)F1i—Ge1—N1i90.18 (10)
F2i—Ge1—F1i89.96 (9)F1—Ge1—N1i89.82 (10)
F2—Ge1—N1i89.94 (10)N1i—Ge1—N1180.0
F2—Ge1—N1—C157.7 (2)F1i—Ge1—N1—C1147.7 (2)
F2i—Ge1—N1—C1122.3 (2)F1—Ge1—N1—C132.3 (2)
Symmetry code: (i) x+1, y+1, z+1.
 

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