Acta Cryst. (2008). E64, i77 [ doi:10.1107/S1600536808034168 ]
Neodymium strontium manganese oxide with ideal composition Nd0.5Sr0.5MnO3 was reported to have two different structure models. In one model, the x coordinate of an O atom is at x > 1/2, while in the other model the x-coordinate of this atom is at x < 1/2. Difference-density maps around this O atom obtained from the current redetermination clearly show that the structure with the O atom at x < 1/2 result in a more satisfactory model than that with x > 1/2. The title compound with a refined composition of Nd0.53 (5)Sr0.47 (5)MnO3 is a distorted perovskite-type structure with site symmetries 2mm for the statistically occupied (Nd, Sr) site and for the above-mentioned O atom, .2/m. for the Mn atom and ..2 for a second O-atom site. In contrast to previous studies, the displacement factors for all atoms were refined anisotropically.
A large single crystal was grown using a floating zone method (Nakamura et al., 1999). The bulk sample was put on a piece of filter paper and was etched by diluted nitric acid under a microscope. Finally, the sample was shaped into a 0.040 mm × 0.053 mm × 0.065 mm block. Nd0.45Sr0.55MnO3 exhibits a first order phase transition at TN = 225K. The present diffraction study was carried out at 241 (1) K close to the phase transition temperature.
The structure of Nd1 -xSrxMnO3 changes with the hole-concentration x. In the region x > 0.55 the structure has tetragonal symmetry. However, at x = 0.60 a phase with monoclinic symmetry was reported at low temperature (Kajimoto et al. , 1999). Below x = 0.55 it changes to orthorhombic symmetry. Since crystals with monoclinic, orthorhombic and tetragonal symmetries were found in preliminary experiments for crystal with approximate compositions of Nd0.45Sr0.55MnO3 (which is expected from the composition of the starting materials), the hole-concentration x (i.e. site occupation factors) were also refined besides the atomic coordinates and the temperature factors. The previous studies (Woodward et al. (1998); Caignaert et al. (1998); Angappane et al. (2004)) have used the standard setting of space group No. 74 in Imma. We decided to refine the structure with the setting in Ibmm, because in the orthorhombic phase the crystal axis is taken along the same direction as that of the tetragonal phase which is also adopted by many other physicists to make clear the relationships between the two phases. Furthermore, Nd0.45Sr0.55MnO3 is well known as having dx2-y2- type orbital-ordering of Mn and the physical and chemical properties are discussed based on the Ibmm setting.
When the coordinates by Caignaert et al. (1998) were used as starting parameters for refinement, the x-coordinate of O1 converged to 0.518 (1) with a R-factor of 0.0381. Fig. 2 (a) shows the difference density map onto (010) after this refinement in the range 0< z < 1/2 and 0 < x < 1 with the vertical and horizontal lengths of 3.80 Å × 5.48 Å. The cores of Nd/Sr, Mn and O1 are at (0, 1/4), (1/2, 1/2) and (0.52, 1/4). Since there are two high peaks at x = 0.45 and 0.55 in Fig 2 (a), O1 was split into O1(1) at x=0.45 and O1(2) at x=0.55. The site occupation factors of O1(1) and O1(2) became 0.96 (6) and 0.04 (6) after the refinement. Hence O1 was concluded to be located only at x=0.45. After the subsequent refinement the R-factor converged at 0.0289 and the difference density map became likewise more satisfactory (Fig. 2(b)).
Although the temperature factor U33 of O1 is 0.001 (1) Å2 and almost insignificant, it becomes 0.0015 (2) Å2 after the refinement of anharmonic vibration parameters (Dawson et al., 1967; Tanaka & Marumo, 1983) as well as the harmonic ones. Finally, refinement of the site occupation factors revealed a hole-concentration x of 0.47 (5) thus leading to a composition of Nd0.53Sr0.47MnO3.
Data collection: MXCSYS (MAC Science, 1995) and IUANGLE (Tanaka et al., 1994).; cell refinement: RSLC-3 UNICS system (Sakurai & Kobayashi, 1979); data reduction: RDEDIT (Tanaka, 2008); program(s) used to solve structure: QNTAO (Tanaka & Onuki, 2002; Tanaka et al., 2008); program(s) used to refine structure: QNTAO (Tanaka & Onuki, 2002; Tanaka et al., 2008); molecular graphics: ATOMS for Windows (Dowty, 2000); software used to prepare material for publication: RDEDIT (Tanaka, 2008).
![[Figure 1]](./wm2198fig1thm.gif)
| Fig. 1. The structure of the distorted perovskite Nd0.53Sr0.47MnO3 with displacement ellipsoids drawn at the 90% probability level. |
![[Figure 2]](./wm2198fig2thm.gif)
| Fig. 2. The difference density map projected onto (010) plane with a range 0 < x < 1 and 0< z < 1/2. (a): The x-coordinate of O1 is > 1/2. (b): The x-coordinate of O1 is < 1/2. Contours are given at intervals of 0.5 e Å-3. Zero contours are drawn as thick lines, positive contours are drawn as thin lines, and negative contours are drawn as broken line. |
| Nd0.53Sr0.47MnO3 | F(000) = 394.64 |
| Mr = 218.81 | Dx = 6.479 Mg m−3 |
| Orthorhombic, Ibmm | Mo Kα radiation, λ = 0.71073 Å |
| Hall symbol: -I 2c 2c | Cell parameters from 30 reflections |
| a = 5.4785 (3) Å | θ = 35.6–37.8° |
| b = 5.4310 (3) Å | µ = 28.37 mm−1 |
| c = 7.6006 (5) Å | T = 241 K |
| V = 226.14 (2) Å3 | Block, black |
| Z = 4 | 0.07 × 0.05 × 0.04 mm |
| MAC Science M06XHF22 four-circle diffractometer | 966 independent reflections |
| Radiation source: fine-focus rotating anode | 679 reflections with F > 3σ(F) |
| graphite | Rint = 0.022 |
| Detector resolution: 1.25x1.25° pixels mm-1 | θmax = 74.7°, θmin = 5.3° |
| integrated intensities data fom ω/2θ scans | h = −12→14 |
| Absorption correction: numerical (CCDABS; Zhurov & Tanaka, 2003) | k = −12→14 |
| Tmin = 0.358, Tmax = 0.521 | l = −18→18 |
| 1255 measured reflections |
| Refinement on F | 14 restraints |
| Least-squares matrix: full | Weighting scheme based on measured s.u.'s |
| R[F2 > 2σ(F2)] = 0.028 | (Δ/σ)max = 0.0002 |
| wR(F2) = 0.066 | Δρmax = 2.17 e Å−3 |
| S = 1.19 | Δρmin = −3.38 e Å−3 |
| 927 reflections | Extinction correction: B–C type 1 Gaussian anisotropic (Becker & Coppens, 1975) |
| 65 parameters | Extinction coefficient: 0.029E04 (1) |
| Nd0.53Sr0.47MnO3 | V = 226.14 (2) Å3 |
| Mr = 218.81 | Z = 4 |
| Orthorhombic, Ibmm | Mo Kα radiation |
| a = 5.4785 (3) Å | µ = 28.37 mm−1 |
| b = 5.4310 (3) Å | T = 241 K |
| c = 7.6006 (5) Å | 0.07 × 0.05 × 0.04 mm |
| MAC Science M06XHF22 four-circle diffractometer | 966 independent reflections |
| Absorption correction: numerical (CCDABS; Zhurov & Tanaka, 2003) | 679 reflections with F > 3σ(F) |
| Tmin = 0.358, Tmax = 0.521 | Rint = 0.022 |
| 1255 measured reflections | θmax = 74.7° |
| R[F2 > 2σ(F2)] = 0.028 | Δρmax = 2.17 e Å−3 |
| wR(F2) = 0.066 | Δρmin = −3.38 e Å−3 |
| S = 1.19 | Absolute structure: ? |
| 927 reflections | Flack parameter: ? |
| 65 parameters | Rogers parameter: ? |
| 14 restraints |
Experimental. Multiple diffraction was avoided by ψ-scan. Intensities was measured at equi-temperature region of combinaion of angles ω and χ of four-circle diffractometer |
Refinement. B—C anisotropic type1 extinction parameters (× 10 4s) are as follows 4087 (526) 6631 (1159) 3088 (391) -790 (416) -1835 (361) 3716 (625) Dawson et al. (1967) proposed the treatment of temperature factors including anharmonic thermal vibration (AHV) effect for high-symmetry crystals by means of series expansion of an one-particle-potential. Tanaka and Marumo (1983) generalized the treatment and anharmonic third and fourth order parameters were refined in the least-square program. AHV parameters were restricted by the site symmetry of Nd/Sr(2 mm), Mn(.2/m.), O1(2 mm) and O2(..2). The anharmonic potentials (V) are represented by the following equation: VNd,Sr,O1=c111u13+c123u1u22+c133u1u32+q1111u14 +q1122u12u22+q1133u12u32+q2222u24 +q2233u22u32+q3333u34 ···(1) VMn=q1111u14+q1122u12u22+q1133u12u32 +q2222u24+q2233u22u32+q3333u34+q1131u13u3 +q2231u22u1u3+q3331u33u1 ···(2) VO2=c211u12u2+c222u23+c233u32u2+c123u1u2u3 +q1111u14+q1122u12u22+q1133u12u32 +q2222u24+q2233u22u32+q3333u34+q1131u13u3 +q2231u22u1u3+q3331u33u1 ···(3) where (u1,u2,u3) is a displacement vector from equilibrium position of each atom. The displacement vector of Nd, Sr, O1 was defined on the coordinate system with axes parallel to the crystal axes, a, b and c. That of Mn and O2 was defined by equation (4) and (5) in terms of the lattice vectors a, b and c in the present study. u1= -0.18253a, u2= 0.18413b, u3= -0.13157c ···(4) u1= -0.11080a-0.14633b, u2= 0.13157c, u3= -0.14506a + 0.11177b ···(5) Since there is strong correlation between harmonic temperature factors and AHV parameters, the AHV parameters and the harmonic temperature factors were refined alternately. The significant AHV parameters cijk (× 10-19JÅ-3) and qiijk (× 10-19JÅ-3) are as follows: Nd and Sr; c111= -5.9 (49), c122= -3.8 (14), Mn; q2231= -1832 (1560), O1: q2222= -9.5 (39), q2233= 569.9 (2279), O2: c211= 3.7 (33), c233= 0.8 (7), c123= -5.5 (23), q2233= 9.1 (79), |
| x | y | z | Uiso*/Ueq | Occ. (<1) | |
| Nd | −0.00656 (9) | 0 | 0.25 | 0.00637 (4) | 0.53 (5) |
| Sr | −0.00656 (9) | 0 | 0.25 | 0.00637 (4) | 0.47 (5) |
| Mn | 0.5 | 0 | 0 | 0.00305 (7) | |
| O1 | 0.4499 (8) | 0 | 0.25 | 0.0112 (6) | |
| O2 | 0.75 | 0.25 | 0.0276 (4) | 0.0139 (5) |
| U11 | U22 | U33 | U12 | U13 | U23 | |
| Nd | 0.00653 (6) | 0.00685 (7) | 0.00574 (8) | 0 | 0 | 0 |
| Sr | 0.00663 (6) | 0.00685 (7) | 0.00574 (8) | 0 | 0 | 0 |
| Mn | 0.0035 (1) | 0.0030 (1) | 0.0027 (1) | 0 | 0 | 0 |
| O1 | 0.015 (1) | 0.017 (1) | 0.0015 (2) | 0 | 0 | 0 |
| O2 | 0.0148 (7) | 0.0116 (7) | 0.015 (1) | −0.0058 (6) | 0 | 0 |
| Mn—O1 | 1.9199 (6) | Ndii—O2 | 2.545 (2) |
| Mn—O2 | 1.9400 (4) | O1—O2 | 2.721 (3) |
| Ndi—Ndii | 3.8064 (5) | Ndi—Mn | 3.3043 (4) |
| Ndii—O1ii | 2.501 (4) | O1iii—O2ii | 2.738 (3) |
| Ndi—O2 | 2.545 (2) | O1—O1ii | 3.489 (4) |
| Ndii—O1 | 2.7332 (5) | O2—O2iii | 3.8799 (5) |
| Ndi—O1 | 2.978 (4) | ||
| Ndii—Ndi—Mn | 55.020 (8) | Ndi—O1—Mn | 81.8 (1) |
| Mn—Ndi—O1 | 35.10 (8) | Ndii—O1—Mn | 89.07 (3) |
| Ndi—Ndii—Mn | 54.769 (6) | Mn—O1—O1ii | 95.15 (9) |
| Ndi—Ndii—O2 | 41.61 (5) | Ndii—O1ii—O1 | 51.11 (8) |
| Mn—Ndii—O1ii | 89.4 (1) | Ndi—O2—Ndii | 96.8 (1) |
| O1—Ndii—O1ii | 83.5 (1) | Ndi—O2—O2iii | 144.59 (7) |
| O1ii—Ndii—O2 | 121.6 (1) | Ndii—O2—O2iii | 47.83 (1) |
| Ndi—Mn—Ndii | 70.212 (7) | Ndii—Ndi—O2 | 41.61 (5) |
| Ndii—Mn—O1 | 55.54 (2) | O1—Ndi—O2 | 58.4 (1) |
| Ndi—O1—Ndii | 83.48 (9) | Ndi—Ndii—O1ii | 134.5 (1) |
| Ndi—O1—O2 | 52.83 (8) | Mn—Ndii—O1 | 35.39 (1) |
| Ndii—O1—O2 | 55.64 (6) | Mn—Ndii—O2iii | 87.76 (5) |
| O1ii—O1—O2 | 89.48 (6) | O1—Ndii—O2iii | 114.44 (5) |
| O1—O1ii—O2iii | 97.8 (1) | O2—Ndii—O2iii | 91.19 (7) |
| Ndi—O2—O1 | 68.77 (9) | Ndi—Mn—O2 | 50.22 (1) |
| Ndii—O2—O1 | 62.42 (8) | Ndi—O1—O1ii | 128.89 (6) |
| Ndii—Ndi—O1 | 45.51 (8) | Ndii—O1—O1ii | 45.41 (5) |
| Mn—Ndi—O2 | 35.85 (5) | Mn—O1—O2 | 45.48 (6) |
| Ndi—Ndii—O1 | 51.01 (1) | Ndii—O1ii—O2iii | 66.4 (1) |
| Ndi—Ndii—O2iii | 132.79 (5) | Ndi—O2—Mn | 93.92 (6) |
| Mn—Ndii—O2 | 35.71 (5) | Ndii—O2—Mn | 94.32 (6) |
| O1—Ndii—O2 | 61.94 (5) | Mn—O2—O2iii | 88.84 (2) |
| O1ii—Ndii—O2iii | 60.7 (1) | O1—O2—O2iii | 89.42 (6) |
| Ndi—Mn—O1 | 63.12 (2) | O1ii—O2iii—O2 | 81.49 (5) |
| Ndii—Mn—O2 | 49.98 (1) | Ndii—O2iii—O1ii | 52.84 (6) |
| Symmetry codes: (i) x+1, y, z; (ii) −x+1/2, y+1/2, z; (iii) x−1/2, y+1/2, −z. |
| Mn—O1 | 1.9199 (6) | Ndii—O2 | 2.545 (2) |
| Mn—O2 | 1.9400 (4) | Ndi—O1 | 2.7332 (5) |
| Ndi—O1i | 2.501 (4) | Ndii—O1 | 2.978 (4) |
| Symmetry codes: (i) −x+1/2, y+1/2, z; (ii) x+1, y, z. |
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Woodward et al. (1998) and Caignaert et al. (1998) determined the structure of Nd0.5Sr0.5MnO3 on the basis of powder X-ray diffraction data, whereas Kajimoto (1999) and Angappane et al. (2004) used single-crystal X-ray diffraction data for structure refinements. Except the model reported by Woodward et al. (1998), for all other structure models of Nd0.5Sr0.5MnO3 the x-coordinate of oxygen atom O1 was reported to be > 1/2. Since a new examination of the x-coordinate of O1 seemed desirable and anisotropic displacement factors were not reported in the previous studies, we decided to redetermine the structure of Nd0.45Sr0.55MnO3. The result of the structure analysis is presented in this communication.
The structure of the title compound derives from the perovskite-type (Fig. 1) and exhibits an orthorhombic distortion. The site symmetries are 2mm for the statistically occupied [(Nd,Sr)O12] polyhedron and for O1, .2/m. for the distorted [MnO6] octahedron and ..2 for O2.