Abstract
The title compound, Nd3Fe5O12 (NdIG), has an iron garnet structure. One of the Fe atoms is coordinated by six O atoms in a slightly distorted octahedral geometry and has
site symmetry. The other Fe atom is coordinated by four O atoms in a slightly distorted tetrahedral geometry and has
site symmetry. The FeO6 octahedron and FeO4 tetrahedron are linked together by corners. The Nd atom is coordinated by eight O atoms in a distorted dodecahedral geometry and has 222 site symmetry. The O atoms occupy general positions.
Related literature
The title compound is isotypic with the Ia
d form of Y3Fe5O12 (YIG), see: Bonnet et al. (1975 ▶). For crystal growth from low-temperature liquid-phase epitaxy, see: Fratello et al. (1986 ▶). X-ray intensities were measured avoiding multiple diffraction, see: Takenaka et al. (2008 ▶). For details of the full-matrix least-squares program QNTAO, see: Tanaka et al. (2008 ▶). For the anisotropic extinction refinement, see: Becker & Coppens (1975 ▶).
Experimental
Crystal data
Nd3Fe5O12
M r = 903.97
Cubic,
a = 12.6128 (2) Å
V = 2006.48 (6) Å3
Z = 8
Synchrotron radiation
λ = 0.67171 Å
μ = 18.30 mm−1
T = 298 K
0.025 mm (radius)
Data collection
Rigaku AFC four-circle diffractometer
Absorption correction: spherical [transmission coefficients for spheres tabulated in International Tables C (1992 ▶), Table 6.3.3.3, were interpolated with Lagrange’s method (four point interpolation; Yamauchi et al., 1965 ▶)] T min = 0.502, T max = 0.527
6653 measured reflections
1159 independent reflections
1159 reflections with F > 3σ(F)
R int = 0.017
Refinement
R[F 2 > 2σ(F 2)] = 0.016
wR(F 2) = 0.018
S = 1.42
6653 reflections
23 parameters
Δρmax = 1.61 e Å−3
Δρmin = −1.75 e Å−3
Data collection: AFC-5, specially designed for PF-BL14A (Rigaku Corporation, 1984 ▶) and IUANGLE (Tanaka et al., 1994 ▶).; cell refinement: RSLC-3 (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.
Supplementary Material
Crystal structure: contains datablocks global, I. DOI: 10.1107/S1600536809036794/br2118sup1.cif
Structure factors: contains datablocks I. DOI: 10.1107/S1600536809036794/br2118Isup2.hkl
Additional supplementary materials: crystallographic information; 3D view; checkCIF report
Table 1. Selected geometric parameters (Å, °).
| Nd1—O1 | 2.41820 (10) |
| Nd1—O1i | 2.52960 (10) |
| Fe1—O1 | 2.03300 (10) |
| Fe2—O1ii | 1.87550 (10) |
| O1—Fe1—O1i | 85.59 (1) |
| O1ii—Fe2—O1iii | 114.47 (1) |
| O1ii—Fe2—O1iv | 99.87 (1) |
Symmetry codes: (i)
; (ii)
; (iii)
; (iv)
.
Acknowledgments
The authors thank Dr V. J. Fratello for supplying the crystals.
supplementary crystallographic information
Comment
The title compound, Nd3Fe5O12 (NdIG), was difficult to be grown. It was grown by the low-temperature-liquid-phase epitaxy for the first time by Fratello et al. (1986). Though the crystal structure was assumed as iron-garnet-type structure by lattice constant and extinction rule, the complete structure was not determined. In this paper, we determine the O atom position and the complete structure by the full matrix least-squares program QNTAO. Since the R-factor is small and the residual density has no significant peaks where no atoms exists, the structure was finally determined to be iron-garnet structure. It is isotypic with the Ia3d form of Y3Fe5O12 (YIG). (Bonnet et al., 1975). The Nd atom is coordinated by eight oxygen atoms. It forms a distorted dodecahedron. There are two Fe site symmetries. One of the Fe atom is coordinated by six oxygen atoms with site symmetry 3. It forms a slightly distorted octahedron. The other Fe atom is coordinated by four oxygen atoms, site symmetry 4. It forms a slightly distorted tetrahedron. FeO6 octahedron and FeO4 tetrahedron are linked together by corners. The structure of NdIG is drawn in Fig.1. And displacement ellipsoids of NdO8 is drawn in Fig.2.
Experimental
Single crystals of neodymium iron garnet were prepared by low temperature liquid phase epitaxy on Sm3(ScGa)5O12 seeds with lattice parameters near the projected values for NdIG.
Refinement
The Becker–Coppens type 1 Gaussian anisotropic extinction parameters were employed (× 10-4 seconds). z11 = 10.2 (5), z22 = 10 (2), z33 = 12 (2), z12 = 1(1), z13 = -0.5 (7), z23 = -1(1). X-ray intensities were measured avoiding multiple diffraction. (Takenaka et al., 2008).
Figures
Fig. 1.
The structure of Nd3Fe5O12. Small red and large green spheres represent O and Nd atoms, respectively. Purple octahedron and blue tetrahedron represent FeO6 and FeO4 units, respectively.
Fig. 2.
View of NdO8 with displacement ellipsoids at the 90% probability level. Green and red ellipsoids represent Nd and O atoms, in Fig.1.
Crystal data
| Nd3Fe5O12 | Dx = 5.985 Mg m−3 |
| Mr = 903.97 | Synchrotron radiation, λ = 0.67171 Å |
| Cubic, Ia3d | Cell parameters from 24 reflections |
| Hall symbol: -I 4bd 2c 3 | θ = 35.7–42.4° |
| a = 12.6128 (2) Å | µ = 18.30 mm−1 |
| V = 2006.48 (6) Å3 | T = 298 K |
| Z = 8 | Sphere, black |
| F(000) = 3248 | 0.03 mm (radius) |
Data collection
| Rigaku AFC four-circle diffractometer | 1159 independent reflections |
| Si 111 | 1159 reflections with F > 3σ(F) |
| Detector resolution: 1.25×1.25 degrees pixels mm-1 | Rint = 0.017 |
| ω/2θ scans | θmax = 53.9°, θmin = 3.7° |
| Absorption correction: for a sphere Transmission coefficients for spheres tabulated in International Tables C (1992\bbr00), Table 6.3.3.3, were interpolated with Lagrange's method (four point interpolation; Yamauchi et al., 1965). | h = −8→30 |
| Tmin = 0.502, Tmax = 0.527 | k = −8→30 |
| 6653 measured reflections | l = −8→30 |
Refinement
| Refinement on F | Primary atom site location: isomorphous structure methods |
| Least-squares matrix: full | Weighting scheme based on measured s.u.'s |
| R[F2 > 2σ(F2)] = 0.016 | (Δ/σ)max = 0.003 |
| wR(F2) = 0.018 | Δρmax = 1.61 e Å−3 |
| S = 1.42 | Δρmin = −1.75 e Å−3 |
| 6653 reflections | Extinction correction: (B-C type 1 Gaussian anisotropic; Becker & Coppens (1975) |
| 23 parameters | Extinction coefficient: 0.308 (5) |
Fractional atomic coordinates and isotropic or equivalent isotropic displacement parameters (Å2)
| x | y | z | Uiso*/Ueq | ||
| Nd1 | 0.125000 | 0.000000 | 0.250000 | 0.00557 (1) | |
| Fe1 | 0.000000 | 0.000000 | 0.000000 | 0.00501 (1) | |
| Fe2 | 0.375000 | 0.000000 | 0.250000 | 0.00564 (1) | |
| O1 | −0.029295 (2) | 0.053092 (2) | 0.149342 (2) | 0.00762 (5) |
Atomic displacement parameters (Å2)
| U11 | U22 | U33 | U12 | U13 | U23 | |
| Nd1 | 0.00421 (1) | 0.00525 (1) | 0.00525 (1) | 0 | 0 | 0.00121 (1) |
| Fe1 | 0.00501 (2) | 0.00501 (2) | 0.00501 (2) | −0.00024 (2) | −0.00024 (2) | −0.00024 (2) |
| Fe2 | 0.00442 (3) | 0.00625 (2) | 0.00625 (2) | 0 | 0 | 0 |
| O1 | 0.00791 (8) | 0.00880 (9) | 0.00614 (7) | −0.00027 (7) | 0.00102 (6) | 0.00041 (7) |
Geometric parameters (Å, °)
| Nd1—O1 | 2.41820 (10) | Fe1—O1i | 2.03300 (10) |
| Nd1—O1i | 2.52960 (10) | Fe1—O1viii | 2.03300 (10) |
| Nd1—O1ii | 2.41820 (10) | Fe1—O1ix | 2.03300 (10) |
| Nd1—O1iii | 2.52960 (10) | Fe1—O1x | 2.03300 (10) |
| Nd1—O1iv | 2.41820 (10) | Fe1—O1xi | 2.03300 (10) |
| Nd1—O1v | 2.52960 (10) | Fe2—O1xii | 1.87550 (10) |
| Nd1—O1vi | 2.41820 (10) | Fe2—O1iv | 1.87550 (10) |
| Nd1—O1vii | 2.52960 (10) | Fe2—O1xiii | 1.87550 (10) |
| Fe1—O1 | 2.03300 (10) | Fe2—O1vi | 1.87550 (10) |
| O1—Nd1—O1i | 67.83 (1) | O1—Fe1—O1viii | 85.59 (1) |
| O1—Nd1—O1ii | 72.82 (1) | O1—Fe1—O1ix | 180.00 |
| O1—Nd1—O1iii | 124.94 (1) | O1—Fe1—O1x | 94.41 (1) |
| O1—Nd1—O1iv | 110.91 (1) | O1—Fe1—O1xi | 94.41 (1) |
| O1—Nd1—O1v | 72.97 (1) | O1xii—Fe2—O1vi | 114.47 (1) |
| O1—Nd1—O1vi | 159.79 (1) | O1xii—Fe2—O1iv | 114.47 (1) |
| O1—Nd1—O1vii | 95.60 (1) | O1xii—Fe2—O1xiii | 99.87 (1) |
| O1—Fe1—O1i | 85.59 (1) |
Symmetry codes: (i) z, x, y; (ii) x, −y, −z+1/2; (iii) z, −x, −y+1/2; (iv) −x+1/4, −z+1/4, −y+1/4; (v) −z+1/4, −y+1/4, −x+1/4; (vi) −x+1/4, z−1/4, y+1/4; (vii) −z+1/4, y−1/4, x+1/4; (viii) y, z, x; (ix) −x, −y, −z; (x) −z, −x, −y; (xi) −y, −z, −x; (xii) x+1/2, y, −z+1/2; (xiii) x+1/2, −y, z.
Footnotes
Supplementary data and figures for this paper are available from the IUCr electronic archives (Reference: BR2118).
References
- Becker, P. J. & Coppens, P. (1975). Acta Cryst. A31, 417–425.
- Bonnet, M., Delapalme, A., Fuess, H. & Thomas, M. (1975). Acta Cryst. B31, 2233–2240.
- Dowty, E. (2000). ATOMS for Windows Shape Software, Kingsport, Tennessee, USA.
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- International Tables for X-ray Crystallography, Vol. C (1992). Birmingham: Kynoch Press.
- Rigaku Corporation (1984). AFC-5 Rigaku Corporation, Tokyo, Japan.
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- Tanaka, K., Kumazawa, S., Tsubokawa, M., Maruno, S. & Shirotani, I. (1994). Acta Cryst. A50, 246–252.
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- Yamauchi, J., Moriguchi, S. & Ichimatsu, S. (1965). Numerical calculation methods for computers Tokyo: Baifūkan.
Associated Data
This section collects any data citations, data availability statements, or supplementary materials included in this article.
Supplementary Materials
Crystal structure: contains datablocks global, I. DOI: 10.1107/S1600536809036794/br2118sup1.cif
Structure factors: contains datablocks I. DOI: 10.1107/S1600536809036794/br2118Isup2.hkl
Additional supplementary materials: crystallographic information; 3D view; checkCIF report


