inorganic compounds
Filled skutterudite structure of europium ruthenium polyphosphide, EuRu4P12
aGraduate School of Materials Science and Engineering, Nagoya Institute of Technology, Gokiso-cho, Showa-ku, Nagoya, Japan
*Correspondence e-mail: kagomiya@nitech.ac.jp
The 4P12 is isotypic with filled skutterudite structures of rare earth transition metal polyphosphides: RFe4P12 (R = Ce, Pr, Nd, Sm and Eu), RRu4P12 (R = La, Ce, Pr and Nd) and ROs4P12 (R = La, Ce, Pr and Nd). The Ru cation is coordinated by six P anions in a distorted octahedral manner. The partially occupied Eu position (site occupancy 0.97) is enclosed by a cage formed by the corner-shared framework of the eight RuP6 octahedra.
of EuRuRelated literature
The title compound is isotypic with the Im form of LaFe4P12, see: Jeitschko & Braun (1977). For the single-crystal preparation and magnetic and electrical properties of EuRu4P12, see: Sekine et al. (2000). For hyperfine interaction in EuRu4P12, see: Grandjean et al. (1983); Indoh et al. (2002). For the method used to avoid multiple diffraction, see: Takenaka et al. (2008).
Experimental
Crystal data
|
Data collection
Refinement
|
Data collection: MXCSYS (MacScience, 1995) and IUANGLE (Tanaka et al., 1994); cell RSLC-3 UNICS system (Sakurai & Kobayashi, 1979); data reduction: RDEDIT (Tanaka, 2008); program(s) used to solve structure: QNTAO (Tanaka et al., 2008); program(s) used to refine structure: QNTAO; molecular graphics: ATOMS for Windows (Dowty, 2000); software used to prepare material for publication: RDEDIT.
Supporting information
https://doi.org/10.1107/S1600536810000589/br2130sup1.cif
contains datablocks global, I. DOI:Structure factors: contains datablock I. DOI: https://doi.org/10.1107/S1600536810000589/br2130Isup2.hkl
Multiple diffraction was avoided by using ψ-scans (Takenaka et al., 2008). Intensities were measured at the equi-temperature region of combination of angles ω and χ of a four-circle diffractometer. The intensities have not been included for the if the multiple diffraction cannot be avoided. In addition, the crystal was cooled to 100 K with an Oxford cryostream cooler installed on a four-circle diffractometer. Since the temperature of the sample depends on the ω and χ-angle and the X-ray diffraction measurement was carried out in the equi-temperature area, the ω and χ-angle had the limitation. Thus completeness of the independent reflection was less than 85%.
The title compound is isotypic with the Im3 form of LaFe4P12 (Jeitschko & Braun, 1977). For the single-crystal preparation and magnetic and electrical properties of LaRu4P12, see: Sekine et al. (2000). For hyperfine interaction in LaRu4P12, see: Grandjean et al. (1983); Indoh et al. (2002). For extinction correction method, see: Becker & Coppens (1975). For the method used to avoid multiple diffraction, see: Takenaka et al. (2008). [Please check added citations]
Data collection: MXCSYS (MacScience, 1995) and IUANGLE (Tanaka et al., 1994); cell
RSLC-3 UNICS system (Sakurai & Kobayashi, 1979); data reduction: RDEDIT (Tanaka, 2008); program(s) used to solve structure: QNTAO (Tanaka et al., 2008); program(s) used to refine structure: QNTAO (Tanaka et al., 2008); molecular graphics: ATOMS for Windows (Dowty, 2000); software used to prepare material for publication: RDEDIT (Tanaka, 2008).Eu0.97Ru4P12 | Dx = 5.925 Mg m−3 |
Mr = 923.37 | Mo Kα radiation, λ = 0.71073 Å |
Cubic, Im3 | Cell parameters from 37 reflections |
Hall symbol: -I 2 2 3 | θ = 36.0–37.7° |
a = 8.04163 (10) Å | µ = 13.37 mm−1 |
V = 520.04 (1) Å3 | T = 100 K |
Z = 2 | Sphere, black |
F(000) = 828.4 | 0.04 mm (radius) |
MacScience M06XHF22 four-circle diffractometer | 769 independent reflections |
Radiation source: fine-focus rotating anode | 625 reflections with F > 3σ(F) |
Graphite monochromator | Rint = 0.016 |
Detector resolution: 1.25 x 1.25° pixels mm-1 | θmax = 74.2°, θmin = 3.6° |
ω/2θ scans | h = −18→20 |
Absorption correction: for a sphere [transmission coefficients for spheres tabulated in International Tables Vol. C (1992), Table 6.3.3.3, were interpolated with Lagrange's method (four-point interpolation; Yamauchi et al., 1965)] | k = −21→21 |
Tmin = 0.486, Tmax = 0.526 | l = −18→20 |
1564 measured reflections |
Refinement on F | Weighting scheme based on measured s.u.'s |
Least-squares matrix: full | (Δ/σ)max = 0.018 |
R[F2 > 2σ(F2)] = 0.020 | Δρmax = 2.08 e Å−3 |
wR(F2) = 0.024 | Δρmin = −1.14 e Å−3 |
S = 1.54 | Extinction correction: B–C type 1 Gaussian isotropic (Becker & Coppens, 1975) |
1304 reflections | Extinction coefficient: 0.068 (6) |
30 parameters |
Eu0.97Ru4P12 | Z = 2 |
Mr = 923.37 | Mo Kα radiation |
Cubic, Im3 | µ = 13.37 mm−1 |
a = 8.04163 (10) Å | T = 100 K |
V = 520.04 (1) Å3 | 0.04 mm (radius) |
MacScience M06XHF22 four-circle diffractometer | 769 independent reflections |
Absorption correction: for a sphere [transmission coefficients for spheres tabulated in International Tables Vol. C (1992), Table 6.3.3.3, were interpolated with Lagrange's method (four-point interpolation; Yamauchi et al., 1965)] | 625 reflections with F > 3σ(F) |
Tmin = 0.486, Tmax = 0.526 | Rint = 0.016 |
1564 measured reflections |
R[F2 > 2σ(F2)] = 0.020 | 30 parameters |
wR(F2) = 0.024 | Δρmax = 2.08 e Å−3 |
S = 1.54 | Δρmin = −1.14 e Å−3 |
1304 reflections |
x | y | z | Uiso*/Ueq | Occ. (<1) | |
Eu1 | 0.000000 | 0.000000 | 0.000000 | 0.00270 (2) | 0.970 (4) |
Ru1 | 0.250000 | 0.250000 | 0.250000 | 0.001840 (15) | |
P1 | 0.000000 | 0.359329 | 0.143386 | 0.00283 (4) |
U11 | U22 | U33 | U12 | U13 | U23 | |
Eu1 | 0.00271 (3) | 0.00271 (3) | 0.00271 (3) | 0 | 0 | 0 |
Ru1 | 0.00185 (3) | 0.00185 (3) | 0.00185 (3) | 0.000108 (17) | 0.000108 (17) | 0.000108 (17) |
P1 | 0.00268 (10) | 0.00301 (10) | 0.00285 (10) | 0 | 0 | −0.00009 (7) |
Eu1—P1 | 3.1112 (3) | Ru1—P1i | 2.3558 (1) |
Eu1—Ru1 | 3.4821 (1) | P1—P1ii | 2.3061 (1) |
Ru1—P1 | 2.3558 (1) | P1—P1i | 3.0829 (1) |
Eu1—P1—Ru1 | 77.78 | Ru1—P1—P1i | 49.13 |
Eu1—P1—P1ii | 68.25 | P1—Ru1—P1i | 81.74 |
Eu1—P1—P1i | 109.77 | P1ii—P1—P1i | 89.59 |
Ru1—P1—P1ii | 111.34 |
Symmetry codes: (i) −z+1/2, x+1/2, −y+1/2; (ii) −x, y, −z. |
Experimental details
Crystal data | |
Chemical formula | Eu0.97Ru4P12 |
Mr | 923.37 |
Crystal system, space group | Cubic, Im3 |
Temperature (K) | 100 |
a (Å) | 8.04163 (10) |
V (Å3) | 520.04 (1) |
Z | 2 |
Radiation type | Mo Kα |
µ (mm−1) | 13.37 |
Crystal size (mm) | 0.04 (radius) |
Data collection | |
Diffractometer | MacScience M06XHF22 four-circle |
Absorption correction | For a sphere [transmission coefficients for spheres tabulated in International Tables Vol. C (1992), Table 6.3.3.3, were interpolated with Lagrange's method (four-point interpolation; Yamauchi et al., 1965)] |
Tmin, Tmax | 0.486, 0.526 |
No. of measured, independent and observed [F > 3σ(F)] reflections | 1564, 769, 625 |
Rint | 0.016 |
(sin θ/λ)max (Å−1) | 1.354 |
Refinement | |
R[F2 > 2σ(F2)], wR(F2), S | 0.020, 0.024, 1.54 |
No. of reflections | 1304 |
No. of parameters | 30 |
No. of restraints | ? |
Δρmax, Δρmin (e Å−3) | 2.08, −1.14 |
Computer programs: MXCSYS (MacScience, 1995) and IUANGLE (Tanaka et al., 1994), RSLC-3 UNICS system (Sakurai & Kobayashi, 1979), RDEDIT (Tanaka, 2008), QNTAO (Tanaka et al., 2008), ATOMS for Windows (Dowty, 2000).
Eu1—P1 | 3.1112 (3) | P1—P1i | 2.3061 (1) |
Eu1—Ru1 | 3.4821 (1) | P1—P1ii | 3.0829 (1) |
Ru1—P1 | 2.3558 (1) |
Symmetry codes: (i) −x, y, −z; (ii) −z+1/2, x+1/2, −y+1/2. |
Acknowledgements
Part of this study was supported by the International Training Programme (ITP) from the Japan Society for the Promotion of Science (JSPS).
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