inorganic papers
Acta Cryst.(2005). E61, i73–i75 doi:10.1107/S160053680501113X Bobev and Bauer Ce
5Au0.43Ge3.57
i73
Acta Crystallographica Section E
Structure Reports Online
ISSN 1600-5368
Ce
5Au
xGe
4x[
x
= 0.43 (2)] with the orthorhombic
Sm
5Ge
4structure type
Svilen Bobeva* and Eric D. Bauerb
a
Department of Chemistry and Biochemistry, 304A Drake Hall, University of Delaware, Newark, DE 19716, USA, andbMST-10 Mail Stop K764, Los Alamos National Laboratory, Los Alamos, NM 87545, USA
Correspondence e-mail: sbobev@chem.udel.edu
Key indicators
Single-crystal X-ray study
T= 120 K
Mean(Ce–Ce) = 0.003 A˚ Disorder in main residue
Rfactor = 0.028
wRfactor = 0.056
Data-to-parameter ratio = 20.8
For details of how these key indicators were automatically derived from the article, see http://journals.iucr.org/e.
#2005 International Union of Crystallography Printed in Great Britain – all rights reserved
Single crystals of the title compound, pentacerium gold tetragermanium, were synthesized from the corresponding elements using a eutectic Au/Ge mixture as solvent. Structure determination of a crystal from that reaction revealed the composition Ce5AuxGe4x(x= 0.43). The compound is a new
ternary derivative of the Sm5Ge4 structure type that
crystal-lizes in the space group Pnma of the orthorhombic system. There are six atoms in the asymmetric unit, one Ce in Wyckoff site 4c, two Ce in 8d, two Ge in 4cand one Ge in 8d. Two of the Ge sites are statistically occupied by Ge and Au atoms, with a lack of long-range ordering. The results are consistent with an earlier report on the structure of the fully stoichiometric analog Ce5Ge4.
Comment
Binary rare earth silicides and germanides are important materials, which have been extensively studied in the last two to three decades. Of specific interest to us was the mixed-valent Kondo material CeSi2(Kohgi et al., 1990) and its Ge
analog CeGe2. Both compounds crystallize in the
body-centered tetragonal-ThSi2structure type (Villars & Calvert,
1991). However, there are certain homogeneity regions in both systems, which present a significant challenge to
[image:1.610.206.459.472.690.2]Received 24 March 2005 Accepted 11 April 2005 Online 16 April 2005
Figure 1
A view of the Ce5AuxGe4x structure projected approximately along
obtaining the phases as pure products and with defined composition. Moreover, from the crystal structure, one might expect rather anisotropic physical properties, and the avail-ability of sizeable single crystals becomes very important for precise property measurements.
To circumvent these synthetic challenges, we employed the flux-growth technique (Canfield & Fisk, 1992) to obtain high-quality single crystals from CeSi2 and CeGe2. Various
low-melting metals have been tried with differing degrees of success. In all cases, the resulting compounds were found to be solid solutions, CeMxSi2x and CeMxGe2x (M = metal
employed in the flux), or ternary Ce–M–Si and Ce–M–Ge intermetallics with different structure types. Here, we report the synthesis and structure of a new ternary Ce–Au–Ge compound. Detailed studies of the physical properties of this new material will be reported in a forthcoming publication.
The structure of Ce5AuxGe4x(x= 0.43) is a new ternary
derivative of the Sm5Ge4 structure type (Villars & Calvert,
1991). The fully stoichiometric analog Ce5Ge4 (Smith et al.,
1967) exhibits slightly different lattice parameters,a= 7.86 A˚ , b= 15.21 A˚ , andc= 8.04 A˚ , from those of the title compound. Although the cell dimensions for the latter were determined at 120 K, whereas for the unsubstituted compound the measurements were carried out at room temperature, the systematic elongation of all crystal axes of Ce5AuxGe4x(x=
0.43) is clearly seen. This is due to the nearly 18% larger atomic size of Au compared with that of Ge. Therefore, all interatomic distances are slightly longer than those in the binary phase Ce5Ge4.
Ce5AuxGe4x (x = 0.43) and its parent Ce5Ge4x
compounds can be viewed as polar intermetallics, i.e. compounds formed by electropositive and electronegative metals and semi-metals, following the Zintl concept (Zintl, 1939). There are six atoms in the asymmetric unit: Ce1 in Wyckoff site 4c, Ce2 in 8d, Ce3 in 8d, Ge1 in 4c, Ge2 in 4cand Ge3 in 8d. The structure can be considered as made up of Ge2
dumbbells and isolated Ge atoms, as shown in Fig. 1. Ge—Ge contacts with the dumbbells of 2.665 (2) A˚ compare well with Ge—Ge contacts found in other alkaline earth and rare earth germanides. The isolated Ge anions are coordinated by Ce2 cations only, and the shortest Ce—Ge contact is 2.9588 (15) A˚ , which agrees with the description above.
Experimental
All starting materials were used as received [Ce (Ames Laboratory, ingot, 99.99% metal basis), Au (Alfa, foil, 99.999%), and Ge (Alfa, pieces, 99.999%)]. A mixture of the elements in the ratio Ce:Au:Ge = 1:0.72:0.28 was loaded into an alumina crucible, which was subse-quently enclosed in an evacuated fused silica jacket by flame-sealing. The reaction was carried out at a temperature of 1373 K for 6 h, followed by slow cooling (3.5 K h1) down to 823 K. At this point, the molten flux was removed by centrifugation. The products of the reaction were small crystals with a silver metallic luster. These were later identified as Ce5AuxGe4x(x= 0.43). The crystals are stable in
air and moisture, but decompose quickly in solutions of mineral acids.
Crystal data
Ce5Au0.43Ge3.57
Mr= 1043.82
Orthorhombic,Pnma a= 7.868 (5) A˚
b= 15.258 (7) A˚
c= 8.052 (6) A˚
V= 966.6 (11) A˚3
Z= 4
Dx= 7.173 Mg m 3
MoKradiation Cell parameters from 3569
reflections
= 2.7–26.4
= 40.31 mm1
T= 120 (2) K
Irregular fragment, metallic silver 0.070.060.05 mm
Data collection
Bruker APEX SMART CCD area-detector diffractometer
!scans
Absorption correction: multi-scan (SADABS; Sheldrick, 2003)
Tmin= 0.083,Tmax= 0.139 3569 measured reflections
1021 independent reflections 953 reflections withI> 2(I)
Rint= 0.040
max= 26.4
h=9!9
k=19!0
l=10!10
Refinement
Refinement onF2
R[F2> 2(F2)] = 0.028
wR(F2) = 0.056
S= 1.10 1021 reflections 49 parameters
w= 1/[2(F
o2) + (0.0163P)2 + 12.3954P]
whereP= (Fo2+ 2Fc2)/3
(/)max< 0.001
max= 1.46 e A˚ 3
min=1.77 e A˚ 3
Extinction correction:SHELXTL
(Sheldrick, 2001)
Extinction coefficient: 0.00019 (4)
Table 1
Selected geometric parameters (A˚ ).
Ce1—Ge1/Au1i
3.064 (2) Ce1—Ge2ii
3.103 (3) Ce1—Ge3/Au3iii 3.1657 (16) Ce1—Ge3/Au3iv 3.1658 (16) Ce1—Ge2v 3.261 (2) Ce1—Ge1/Au1vi 3.299 (3) Ce1—Ce2vii 3.5409 (16) Ce1—Ce2v 3.5410 (16) Ce2—Ge3/Au3viii 2.9588 (15) Ce2—Ge3/Au3iii 2.9791 (19) Ce2—Ge3/Au3ix 3.0528 (18) Ce2—Ge1/Au1vi 3.1259 (15)
Ce2—Ge2 3.1592 (19) Ce2—Ge1/Au1i
3.2191 (15) Ce2—Ce1vi 3.5410 (16) Ce3—Ge3/Au3x 3.0884 (17) Ce3—Ge2xi 3.1738 (15) Ce3—Ge3/Au3xii 3.2898 (15) Ce3—Ge2xiii 3.3082 (17) Ce3—Ge1/Au1xiv 3.3133 (17) Ce3—Ge3/Au3xv 3.334 (2) Ce3—Ce2xvi 3.6211 (15) Ge1/Au1—Ge2v 2.665 (2)
Symmetry codes: (i) x1;y;z; (ii) x;y;z1; (iii) xþ1
2;yþ1;z 1 2; (iv)
xþ1 2;y
1 2;z
1 2; (v)xþ
1 2;y;zþ
1 2; (vi)x
1 2;y;zþ
1 2; (vii)xþ
1 2;yþ
1 2;zþ
1 2;
(viii)x;y1;z; (ix)x;yþ1;zþ1; (x)xþ3
2;yþ1;zþ 1
2; (xi)xþ1;y;z; (xii)
xþ1
2;y1;zþ 3 2; (xiii)xþ
1 2;y;zþ
3
2; (xiv)x;y;zþ1; (xv)xþ1;yþ1;zþ1;
(xvi)xþ1;y;zþ1.
The structure refinement, assuming a composition Ce5Ge4,
converged to poor residuals and two of the three crystallographically unique Ge sites (Ge1, Ge3) exhibited unusually large anisotropic displacement parameters. By freeing the site occupation factor for each individual atom, while the remaining parameters were kept fixed, it became evident that those two sites are statistically occupied by Ge and Au atoms. The third Ge site (Ge2), along with the three Ce sites, proved to be fully occupied, with corresponding deviations from full occupancy within 3. This is consistent with the slightly larger unit-cell parameters for Ce5AuxGe4x compared with those for
Ce5Ge4(Smith et al., 1967). The Ge1/Au1 site was found to be a
nearly 75:25 statistical mixture of Ce and Au, whereas the Ce3/Au3 site is close to 90:10, leading to anxvalue of 0.43 (2). The highest peak and the deepest hole in the final difference Fourier map are 0.91 and 1.40 A˚ , respectively, from the Ce1/Au1 site.
Data collection:SMART(Bruker, 2002); cell refinement:SAINT
(Bruker, 2002); data reduction:SAINT; program(s) used to solve structure: SHELXTL (Sheldrick, 2001); program(s) used to refine
inorganic papers
i74
Bobev and Bauer Cestructure: SHELXTL; molecular graphics:XP inSHELXTL; soft-ware used to prepare material for publication:SHELXTL.
This work was funded in part by a University of Delaware start-up grant. Work at LANL is carried out under the auspicies of the US Department of Energy.
References
Bruker (2002).SMARTandSAINT. Bruker AXS Inc., Madison, Wisconsin, USA.
Canfield, P. C. & Fisk, Z. (1992).Philos. Mag. B,65, 1117–1123.
Kohgi, M., Ito, M., Satoh, T. Asano, H., Ishigaki, T. & Izumi, F. (1990).J. Magn. Magn. Mater.90, 433–434.
Sheldrick, G. M. (2001).SHELXTL. Bruker AXS Inc., Madison, Wisconsin, USA.
Sheldrick, G. M. (2003).SADABS. University of Go¨ttingen, Germany. Smith, G. S., Tharp, A. G. & Johnson, Q. (1967).Acta Cryst.23, 940–943. Villars, P. & Calvert, L. D. (1991).Pearson’s Handbook of Crystallographic
Data for Intermetallic Compounds, 2nd ed. Ohio: American Society for Metals.
Zintl, E. (1939).Angew. Chem.52, 1–6.
inorganic papers
Acta Cryst.(2005). E61, i73–i75 Bobev and Bauer Ce
supporting information
sup-1
Acta Cryst. (2005). E61, i73–i75
supporting information
Acta Cryst. (2005). E61, i73–i75 [https://doi.org/10.1107/S160053680501113X]
Ce
5Au
xGe
4−x[
x
= 0.43
(2)] with the orthorhombic Sm
5Ge
4structure type
Svilen Bobev and Eric D. Bauer
Pentacerium gold tetragermanium
Crystal data
Ce5Au0.43Ge3.57
Mr = 1043.82 Orthorhombic, Pnma
Hall symbol: -P 2ac 2n
a = 7.868 (5) Å
b = 15.258 (7) Å
c = 8.052 (6) Å
V = 966.6 (11) Å3
Z = 4
F(000) = 1752
Dx = 7.173 Mg m−3
Mo Kα radiation, λ = 0.71073 Å Cell parameters from 3569 reflections
θ = 2.7–26.4°
µ = 40.31 mm−1
T = 120 K Irregular, grey
0.07 × 0.06 × 0.05 mm
Data collection
Bruker APEX SMART CCD area-detector diffractometer
Radiation source: fine-focus sealed tube Graphite monochromator
Detector resolution: 8.3 pixels mm-1
ω scans
Absorption correction: multi-scan (SADABS; Sheldrick, 2003)
Tmin = 0.083, Tmax = 0.139
3569 measured reflections 1021 independent reflections 953 reflections with I > 2σ(I)
Rint = 0.040
θmax = 26.4°, θmin = 2.7°
h = −9→9
k = −19→0
l = −10→10
Refinement
Refinement on F2
Least-squares matrix: full
R[F2 > 2σ(F2)] = 0.028
wR(F2) = 0.056
S = 1.10 1021 reflections 49 parameters 0 restraints
Primary atom site location: structure-invariant direct methods
Secondary atom site location: difference Fourier map
w = 1/[σ2(F
o2) + (0.0163P)2 + 12.3954P]
where P = (Fo2 + 2Fc2)/3
(Δ/σ)max < 0.001
Δρmax = 1.46 e Å−3
Δρmin = −1.77 e Å−3
Extinction correction: SHELXTL (Sheldrick, 2001), Fc*=kFc[1+0.001xFc2λ3/sin(2θ)]-1/4
supporting information
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Acta Cryst. (2005). E61, i73–i75
Special details
Experimental. Crystals were selected and cut in Exxon Paratone N oil bath to the desired dimensions. A suitable one was chosen and it was mounted on the top of glass fiber and quickly placed under the cold nitrogen stream (ca 120 K) in a Bruker SMART CCD-based diffractometer. The crystal, despite the small size, diffracted strongly and an exposure time of 5 second per frame was found sufficient. The structure was solved readily using direct methods and refined on F2 using
the SHELXL package (Sheldrick, 2001). Data collection was performed with four batch runs at φ = 0.00 ° (456 frames), at φ = 90.00 ° (456 frames), at φ = 180.00 ° (230 frames), and at φ = 270.00 (230 frames). Frame width = 0.40 \& in ω. Data were merged, corrected for decay, and treated with multi-scan absorption corrections.
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)
Ce1 0.29830 (10) 0.2500 0.00310 (9) 0.0104 (2) Ce2 0.12843 (7) 0.11570 (4) 0.34014 (6) 0.00863 (16) Ce3 0.98567 (6) 0.09877 (4) 0.81688 (6) 0.00863 (16)
Ge1 0.92333 (12) 0.2500 0.10583 (12) 0.0077 (4) 0.751 (4) Au1 0.92333 (12) 0.2500 0.10583 (12) 0.0077 (4) 0.249 (4) Ge2 0.18878 (17) 0.2500 0.63289 (17) 0.0071 (3)
Ge3 0.20994 (11) 0.95676 (6) 0.53502 (11) 0.0103 (3) 0.910 (3) Au3 0.20994 (11) 0.95676 (6) 0.53502 (11) 0.0103 (3) 0.090 (3)
Atomic displacement parameters (Å2)
U11 U22 U33 U12 U13 U23
Ce1 0.0144 (4) 0.0078 (4) 0.0091 (4) 0.000 −0.0003 (3) 0.000 Ce2 0.0104 (3) 0.0071 (3) 0.0084 (3) 0.0002 (2) 0.0006 (2) −0.0013 (2) Ce3 0.0089 (3) 0.0084 (3) 0.0085 (3) −0.0001 (2) −0.0005 (2) 0.0013 (2) Ge1 0.0093 (5) 0.0067 (6) 0.0070 (6) 0.000 −0.0005 (4) 0.000 Au1 0.0093 (5) 0.0067 (6) 0.0070 (6) 0.000 −0.0005 (4) 0.000 Ge2 0.0090 (7) 0.0053 (7) 0.0072 (7) 0.000 −0.0004 (5) 0.000 Ge3 0.0157 (5) 0.0081 (5) 0.0072 (5) −0.0026 (3) 0.0008 (4) 0.0005 (3) Au3 0.0157 (5) 0.0081 (5) 0.0072 (5) −0.0026 (3) 0.0008 (4) 0.0005 (3)
Geometric parameters (Å, º)
Ce1—Au1i 3.064 (2) Ce3—Ge1xiv 3.3133 (17)
Ce1—Ge1i 3.064 (2) Ce3—Au3xv 3.334 (2)
Ce1—Ge2ii 3.103 (3) Ce3—Ge3xv 3.334 (2)
Ce1—Au3iii 3.1657 (16) Ce3—Au3xvi 3.5999 (17)
Ce1—Ge3iii 3.1657 (16) Ce3—Ce2xvii 3.6211 (15)
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Acta Cryst. (2005). E61, i73–i75
Ce1—Ge3iv 3.1658 (16) Ge1—Ce1xi 3.064 (2)
Ce1—Ge2v 3.261 (2) Ge1—Ce2vii 3.1259 (15)
Ce1—Au1vi 3.299 (3) Ge1—Ce2v 3.1259 (15)
Ce1—Ge1vi 3.299 (3) Ge1—Ce2xviii 3.2191 (15)
Ce1—Ce2vii 3.5409 (16) Ge1—Ce2xi 3.2191 (15)
Ce1—Ce2v 3.5410 (16) Ge1—Ce1v 3.299 (3)
Ce2—Au3viii 2.9588 (15) Ge1—Ce3xix 3.3132 (17)
Ce2—Ge3viii 2.9588 (15) Ge1—Ce3ii 3.3132 (17)
Ce2—Au3iii 2.9791 (19) Ge2—Au1vi 2.665 (2)
Ce2—Ge3iii 2.9791 (19) Ge2—Ge1vi 2.665 (2)
Ce2—Au3ix 3.0528 (18) Ge2—Ce1xiv 3.103 (3)
Ce2—Ge3ix 3.0528 (18) Ge2—Ce2xx 3.1592 (19)
Ce2—Au1vi 3.1259 (15) Ge2—Ce3xxi 3.1737 (15)
Ce2—Ge1vi 3.1259 (15) Ge2—Ce3i 3.1738 (15)
Ce2—Ge2 3.1592 (19) Ge2—Ce1vi 3.261 (2)
Ce2—Ge1i 3.2191 (15) Ge2—Ce3xxii 3.3081 (17)
Ce2—Au1i 3.2191 (15) Ge2—Ce3xxiii 3.3081 (17)
Ce2—Ce1vi 3.5410 (16) Ge3—Ce2xxiv 2.9588 (15)
Ce3—Au3x 3.0884 (17) Ge3—Ce2xxv 2.9791 (19)
Ce3—Ge3x 3.0884 (17) Ge3—Ce2ix 3.0528 (18)
Ce3—Ge2xi 3.1738 (15) Ge3—Ce3xxvi 3.0884 (17)
Ce3—Au3xii 3.2898 (15) Ge3—Ce1xxv 3.1657 (16)
Ce3—Ge3xii 3.2898 (15) Ge3—Ce3xxvii 3.2898 (15)
Ce3—Ge2xiii 3.3082 (17) Ge3—Ce3xv 3.334 (2)
Ce3—Au1xiv 3.3133 (17)
Au1i—Ce1—Ge1i 0.00 (4) Au3xii—Ce3—Au1xiv 96.12 (4)
Au1i—Ce1—Ge2ii 89.54 (5) Ge3xii—Ce3—Au1xiv 96.12 (4)
Ge1i—Ce1—Ge2ii 89.54 (5) Ge2xiii—Ce3—Au1xiv 47.46 (3)
Au1i—Ce1—Au3iii 87.61 (2) Au3x—Ce3—Ge1xiv 84.63 (4)
Ge1i—Ce1—Au3iii 87.61 (2) Ge3x—Ce3—Ge1xiv 84.63 (4)
Ge2ii—Ce1—Au3iii 94.15 (2) Ge2xi—Ce3—Ge1xiv 84.03 (5)
Au1i—Ce1—Ge3iii 87.61 (2) Au3xii—Ce3—Ge1xiv 96.12 (4)
Ge1i—Ce1—Ge3iii 87.61 (2) Ge3xii—Ce3—Ge1xiv 96.12 (4)
Ge2ii—Ce1—Ge3iii 94.15 (2) Ge2xiii—Ce3—Ge1xiv 47.46 (3)
Au3iii—Ce1—Ge3iii 0.00 (4) Au1xiv—Ce3—Ge1xiv 0.00 (4)
Au1i—Ce1—Au3iv 87.61 (2) Au3x—Ce3—Au3xv 140.50 (4)
Ge1i—Ce1—Au3iv 87.61 (2) Ge3x—Ce3—Au3xv 140.50 (4)
Ge2ii—Ce1—Au3iv 94.15 (2) Ge2xi—Ce3—Au3xv 91.17 (5)
Au3iii—Ce1—Au3iv 170.40 (4) Au3xii—Ce3—Au3xv 80.58 (4)
Ge3iii—Ce1—Au3iv 170.40 (4) Ge3xii—Ce3—Au3xv 80.58 (4)
Au1i—Ce1—Ge3iv 87.61 (2) Ge2xiii—Ce3—Au3xv 87.43 (4)
Ge1i—Ce1—Ge3iv 87.61 (2) Au1xiv—Ce3—Au3xv 134.87 (4)
Ge2ii—Ce1—Ge3iv 94.15 (2) Ge1xiv—Ce3—Au3xv 134.87 (4)
Au3iii—Ce1—Ge3iv 170.40 (4) Au3x—Ce3—Ge3xv 140.50 (4)
Ge3iii—Ce1—Ge3iv 170.40 (4) Ge3x—Ce3—Ge3xv 140.50 (4)
Au3iv—Ce1—Ge3iv 0.00 (4) Ge2xi—Ce3—Ge3xv 91.17 (5)
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Acta Cryst. (2005). E61, i73–i75
Ge1i—Ce1—Ge2v 176.05 (4) Ge3xii—Ce3—Ge3xv 80.58 (4)
Ge2ii—Ce1—Ge2v 86.51 (4) Ge2xiii—Ce3—Ge3xv 87.43 (4)
Au3iii—Ce1—Ge2v 92.67 (2) Au1xiv—Ce3—Ge3xv 134.87 (4)
Ge3iii—Ce1—Ge2v 92.67 (2) Ge1xiv—Ce3—Ge3xv 134.87 (4)
Au3iv—Ce1—Ge2v 92.67 (2) Au3xv—Ce3—Ge3xv 0.00 (4)
Ge3iv—Ce1—Ge2v 92.67 (2) Au3x—Ce3—Au3xvi 79.24 (5)
Au1i—Ce1—Au1vi 91.69 (4) Ge3x—Ce3—Au3xvi 79.24 (5)
Ge1i—Ce1—Au1vi 91.69 (4) Ge2xi—Ce3—Au3xvi 84.06 (5)
Ge2ii—Ce1—Au1vi 178.77 (4) Au3xii—Ce3—Au3xvi 98.93 (4)
Au3iii—Ce1—Au1vi 85.91 (2) Ge3xii—Ce3—Au3xvi 98.93 (4)
Ge3iii—Ce1—Au1vi 85.91 (2) Ge2xiii—Ce3—Au3xvi 147.46 (4)
Au3iv—Ce1—Au1vi 85.91 (2) Au1xiv—Ce3—Au3xvi 159.14 (3)
Ge3iv—Ce1—Au1vi 85.91 (2) Ge1xiv—Ce3—Au3xvi 159.14 (3)
Ge2v—Ce1—Au1vi 92.27 (5) Au3xv—Ce3—Au3xvi 62.45 (5)
Au1i—Ce1—Ge1vi 91.69 (4) Ge3xv—Ce3—Au3xvi 62.45 (5)
Ge1i—Ce1—Ge1vi 91.69 (4) Au3x—Ce3—Ce2xvii 98.22 (3)
Ge2ii—Ce1—Ge1vi 178.77 (4) Ge3x—Ce3—Ce2xvii 98.22 (3)
Au3iii—Ce1—Ge1vi 85.91 (2) Ge2xi—Ce3—Ce2xvii 128.23 (4)
Ge3iii—Ce1—Ge1vi 85.91 (2) Au3xii—Ce3—Ce2xvii 50.79 (3)
Au3iv—Ce1—Ge1vi 85.91 (2) Ge3xii—Ce3—Ce2xvii 50.79 (3)
Ge3iv—Ce1—Ge1vi 85.91 (2) Ge2xiii—Ce3—Ce2xvii 119.87 (4)
Ge2v—Ce1—Ge1vi 92.27 (5) Au1xiv—Ce3—Ce2xvii 146.91 (3)
Au1vi—Ce1—Ge1vi 0.00 (3) Ge1xiv—Ce3—Ce2xvii 146.91 (3)
Au1i—Ce1—Ce2vii 127.59 (4) Au3xv—Ce3—Ce2xvii 50.147 (19)
Ge1i—Ce1—Ce2vii 127.59 (4) Ge3xv—Ce3—Ce2xvii 50.147 (19)
Ge2ii—Ce1—Ce2vii 123.10 (3) Au3xvi—Ce3—Ce2xvii 50.02 (3)
Au3iii—Ce1—Ce2vii 124.25 (3) Ge2v—Ge1—Ce1xi 118.17 (6)
Ge3iii—Ce1—Ce2vii 124.25 (3) Ge2v—Ge1—Ce2vii 65.57 (4)
Au3iv—Ce1—Ce2vii 53.80 (3) Ce1xi—Ge1—Ce2vii 138.78 (3)
Ge3iv—Ce1—Ce2vii 53.80 (3) Ge2v—Ge1—Ce2v 65.57 (4)
Ge2v—Ce1—Ce2vii 55.16 (4) Ce1xi—Ge1—Ce2v 138.78 (3)
Au1vi—Ce1—Ce2vii 56.02 (2) Ce2vii—Ge1—Ce2v 81.92 (5)
Ge1vi—Ce1—Ce2vii 56.02 (2) Ge2v—Ge1—Ce2xviii 140.35 (2)
Au1i—Ce1—Ce2v 127.59 (4) Ce1xi—Ge1—Ce2xviii 71.07 (4)
Ge1i—Ce1—Ce2v 127.59 (4) Ce2vii—Ge1—Ce2xviii 82.72 (4)
Ge2ii—Ce1—Ce2v 123.10 (3) Ce2v—Ge1—Ce2xviii 135.06 (4)
Au3iii—Ce1—Ce2v 53.80 (3) Ge2v—Ge1—Ce2xi 140.35 (2)
Ge3iii—Ce1—Ce2v 53.80 (3) Ce1xi—Ge1—Ce2xi 71.07 (4)
Au3iv—Ce1—Ce2v 124.25 (3) Ce2vii—Ge1—Ce2xi 135.06 (4)
Ge3iv—Ce1—Ce2v 124.25 (3) Ce2v—Ge1—Ce2xi 82.72 (4)
Ge2v—Ce1—Ce2v 55.16 (4) Ce2xviii—Ge1—Ce2xi 79.07 (5)
Au1vi—Ce1—Ce2v 56.02 (2) Ge2v—Ge1—Ce1v 118.82 (6)
Ge1vi—Ce1—Ce2v 56.02 (2) Ce1xi—Ge1—Ce1v 123.01 (4)
Ce2vii—Ce1—Ce2v 70.72 (4) Ce2vii—Ge1—Ce1v 69.26 (2)
Au3viii—Ce2—Ge3viii 0.00 (5) Ce2v—Ge1—Ce1v 69.26 (2)
Au3viii—Ce2—Au3iii 92.33 (4) Ce2xviii—Ge1—Ce1v 65.80 (4)
Ge3viii—Ce2—Au3iii 92.33 (4) Ce2xi—Ge1—Ce1v 65.80 (4)
supporting information
sup-5
Acta Cryst. (2005). E61, i73–i75
Ge3viii—Ce2—Ge3iii 92.33 (4) Ce1xi—Ge1—Ce3xix 70.60 (2)
Au3iii—Ce2—Ge3iii 0.00 (5) Ce2vii—Ge1—Ce3xix 75.59 (3)
Au3viii—Ce2—Au3ix 73.60 (4) Ce2v—Ge1—Ce3xix 131.62 (4)
Ge3viii—Ce2—Au3ix 73.60 (4) Ce2xviii—Ge1—Ce3xix 83.92 (5)
Au3iii—Ce2—Au3ix 120.62 (4) Ce2xi—Ge1—Ce3xix 141.32 (4)
Ge3iii—Ce2—Au3ix 120.62 (4) Ce1v—Ge1—Ce3xix 135.59 (3)
Au3viii—Ce2—Ge3ix 73.60 (4) Ge2v—Ge1—Ce3ii 66.17 (4)
Ge3viii—Ce2—Ge3ix 73.60 (4) Ce1xi—Ge1—Ce3ii 70.60 (2)
Au3iii—Ce2—Ge3ix 120.62 (4) Ce2vii—Ge1—Ce3ii 131.62 (4)
Ge3iii—Ce2—Ge3ix 120.62 (4) Ce2v—Ge1—Ce3ii 75.59 (3)
Au3ix—Ce2—Ge3ix 0.00 (5) Ce2xviii—Ge1—Ce3ii 141.32 (4)
Au3viii—Ce2—Au1vi 107.62 (4) Ce2xi—Ge1—Ce3ii 83.92 (5)
Ge3viii—Ce2—Au1vi 107.62 (4) Ce1v—Ge1—Ce3ii 135.59 (3)
Au3iii—Ce2—Au1vi 92.36 (4) Ce3xix—Ge1—Ce3ii 88.28 (6)
Ge3iii—Ce2—Au1vi 92.36 (4) Au1vi—Ge2—Ge1vi 0.00 (4)
Au3ix—Ce2—Au1vi 147.01 (4) Au1vi—Ge2—Ce1xiv 120.05 (7)
Ge3ix—Ce2—Au1vi 147.01 (4) Ge1vi—Ge2—Ce1xiv 120.05 (7)
Au3viii—Ce2—Ge1vi 107.62 (4) Au1vi—Ge2—Ce2xx 64.27 (5)
Ge3viii—Ce2—Ge1vi 107.62 (4) Ge1vi—Ge2—Ce2xx 64.27 (5)
Au3iii—Ce2—Ge1vi 92.36 (4) Ce1xiv—Ge2—Ce2xx 139.33 (3)
Ge3iii—Ce2—Ge1vi 92.36 (4) Au1vi—Ge2—Ce2 64.27 (5)
Au3ix—Ce2—Ge1vi 147.01 (4) Ge1vi—Ge2—Ce2 64.27 (5)
Ge3ix—Ce2—Ge1vi 147.01 (4) Ce1xiv—Ge2—Ce2 139.33 (3)
Au1vi—Ce2—Ge1vi 0.0 Ce2xx—Ge2—Ce2 80.88 (6)
Au3viii—Ce2—Ge2 95.93 (5) Au1vi—Ge2—Ce3xxi 133.27 (3)
Ge3viii—Ce2—Ge2 95.93 (5) Ge1vi—Ge2—Ce3xxi 133.27 (3)
Au3iii—Ce2—Ge2 142.36 (4) Ce1xiv—Ge2—Ce3xxi 72.02 (4)
Ge3iii—Ce2—Ge2 142.36 (4) Ce2xx—Ge2—Ce3xxi 78.53 (5)
Au3ix—Ce2—Ge2 96.91 (4) Ce2—Ge2—Ce3xxi 138.09 (5)
Ge3ix—Ce2—Ge2 96.91 (4) Au1vi—Ge2—Ce3i 133.27 (3)
Au1vi—Ce2—Ge2 50.16 (3) Ge1vi—Ge2—Ce3i 133.27 (3)
Ge1vi—Ce2—Ge2 50.16 (3) Ce1xiv—Ge2—Ce3i 72.02 (4)
Au3viii—Ce2—Ge1i 160.26 (3) Ce2xx—Ge2—Ce3i 138.09 (5)
Ge3viii—Ce2—Ge1i 160.26 (3) Ce2—Ge2—Ce3i 78.52 (5)
Au3iii—Ce2—Ge1i 88.10 (5) Ce3xxi—Ge2—Ce3i 93.28 (6)
Ge3iii—Ce2—Ge1i 88.10 (5) Au1vi—Ge2—Ce1vi 114.22 (7)
Au3ix—Ce2—Ge1i 89.22 (5) Ge1vi—Ge2—Ce1vi 114.22 (7)
Ge3ix—Ce2—Ge1i 89.22 (5) Ce1xiv—Ge2—Ce1vi 125.74 (5)
Au1vi—Ce2—Ge1i 92.08 (4) Ce2xx—Ge2—Ce1vi 66.92 (3)
Ge1vi—Ce2—Ge1i 92.08 (4) Ce2—Ge2—Ce1vi 66.92 (3)
Ge2—Ce2—Ge1i 95.72 (5) Ce3xxi—Ge2—Ce1vi 71.48 (4)
Au3viii—Ce2—Au1i 160.26 (3) Ce3i—Ge2—Ce1vi 71.49 (4)
Ge3viii—Ce2—Au1i 160.26 (3) Au1vi—Ge2—Ce3xxii 66.37 (4)
Au3iii—Ce2—Au1i 88.10 (5) Ge1vi—Ge2—Ce3xxii 66.37 (4)
Ge3iii—Ce2—Au1i 88.10 (5) Ce1xiv—Ge2—Ce3xxii 71.73 (3)
Au3ix—Ce2—Au1i 89.22 (5) Ce2xx—Ge2—Ce3xxii 75.22 (3)
Ge3ix—Ce2—Au1i 89.22 (5) Ce2—Ge2—Ce3xxii 130.52 (5)
supporting information
sup-6
Acta Cryst. (2005). E61, i73–i75
Ge1vi—Ce2—Au1i 92.08 (4) Ce3i—Ge2—Ce3xxii 143.66 (5)
Ge2—Ce2—Au1i 95.72 (5) Ce1vi—Ge2—Ce3xxii 134.92 (3)
Ge1i—Ce2—Au1i 0.00 (3) Au1vi—Ge2—Ce3xxiii 66.37 (4)
Au3viii—Ce2—Ce1vi 116.38 (4) Ge1vi—Ge2—Ce3xxiii 66.37 (4)
Ge3viii—Ce2—Ce1vi 116.38 (4) Ce1xiv—Ge2—Ce3xxiii 71.73 (3)
Au3iii—Ce2—Ce1vi 145.26 (3) Ce2xx—Ge2—Ce3xxiii 130.52 (5)
Ge3iii—Ce2—Ce1vi 145.26 (3) Ce2—Ge2—Ce3xxiii 75.22 (3)
Au3ix—Ce2—Ce1vi 56.81 (4) Ce3xxi—Ge2—Ce3xxiii 143.66 (5)
Ge3ix—Ce2—Ce1vi 56.81 (4) Ce3i—Ge2—Ce3xxiii 77.96 (4)
Au1vi—Ce2—Ce1vi 96.63 (5) Ce1vi—Ge2—Ce3xxiii 134.92 (3)
Ge1vi—Ce2—Ce1vi 96.63 (5) Ce3xxii—Ge2—Ce3xxiii 88.45 (6)
Ge2—Ce2—Ce1vi 57.92 (4) Ce2xxiv—Ge3—Ce2xxv 146.51 (3)
Ge1i—Ce2—Ce1vi 58.18 (4) Ce2xxiv—Ge3—Ce2ix 106.40 (4)
Au1i—Ce2—Ce1vi 58.18 (4) Ce2xxv—Ge3—Ce2ix 88.07 (4)
Au3x—Ce3—Ge3x 0.00 (4) Ce2xxiv—Ge3—Ce3xxvi 95.24 (4)
Au3x—Ce3—Ge2xi 94.27 (5) Ce2xxv—Ge3—Ce3xxvi 92.08 (6)
Ge3x—Ce3—Ge2xi 94.27 (5) Ce2ix—Ge3—Ce3xxvi 139.83 (4)
Au3x—Ce3—Au3xii 97.15 (5) Ce2xxiv—Ge3—Ce1xxv 140.29 (4)
Ge3x—Ce3—Au3xii 97.15 (5) Ce2xxv—Ge3—Ce1xxv 72.90 (3)
Ge2xi—Ce3—Au3xii 168.54 (3) Ce2ix—Ge3—Ce1xxv 69.39 (3)
Au3x—Ce3—Ge3xii 97.15 (5) Ce3xxvi—Ge3—Ce1xxv 72.32 (3)
Ge3x—Ce3—Ge3xii 97.15 (5) Ce2xxiv—Ge3—Ce3xxvii 78.19 (4)
Ge2xi—Ce3—Ge3xii 168.54 (3) Ce2xxv—Ge3—Ce3xxvii 70.37 (4)
Au3xii—Ce3—Ge3xii 0.00 (4) Ce2ix—Ge3—Ce3xxvii 133.96 (4)
Au3x—Ce3—Ge2xiii 132.02 (4) Ce3xxvi—Ge3—Ce3xxvii 82.85 (5)
Ge3x—Ce3—Ge2xiii 132.02 (4) Ce1xxv—Ge3—Ce3xxvii 134.37 (4)
Ge2xi—Ce3—Ge2xiii 84.58 (4) Ce2xxiv—Ge3—Ce3xv 69.97 (4)
Au3xii—Ce3—Ge2xiii 87.11 (5) Ce2xxv—Ge3—Ce3xv 143.48 (4)
Ge3xii—Ce3—Ge2xiii 87.11 (5) Ce2ix—Ge3—Ce3xv 77.60 (5)
Au3x—Ce3—Au1xiv 84.63 (4) Ce3xxvi—Ge3—Ce3xv 78.75 (5)
Ge3x—Ce3—Au1xiv 84.63 (4) Ce1xxv—Ge3—Ce3xv 70.63 (3)
Ge2xi—Ce3—Au1xiv 84.03 (5) Ce3xxvii—Ge3—Ce3xv 141.24 (3)