Downloaded from http://rsta.royalsocietypublishing.org/ on June 18, 2017 Structure and magnetism of the A site scandium perovskite (Sc0.94Mn0.06)Mn0.65Ni0.35O3 synthesized at high pressure rsta.royalsocietypublishing.org Chris I. Thomas, Matthew R. Suchomel, Giap V. Duong, Andrew M. Fogg, John B. Claridge Research Cite this article: Thomas CI, Suchomel MR, Duong GV, Fogg AM, Claridge JB, Rosseinsky MJ. 2014 Structure and magnetism of the A site scandium perovskite (Sc0.94 Mn0.06 )Mn0.65 Ni0.35 O3 synthesized at high pressure. Phil. Trans. R. Soc. A 372: 20130012. http://dx.doi.org/10.1098/rsta.2013.0012 One contribution of 8 to a Theo Murphy Meeting Issue ‘Theo Murphy International Scientific Meeting between the UK and China on the chemistry and physics of functional materials’. Subject Areas: inorganic chemistry Keywords: ceramics, high-pressure phase, magnetic properties and crystal structure Author for correspondence: Matthew J. Rosseinsky e-mail: [email protected] Electronic supplementary material is available at http://dx.doi.org/10.1098/rsta.2013.0012 or via http://rsta.royalsocietypublishing.org. and Matthew J. Rosseinsky Department of Chemistry, University of Liverpool, Crown Street, Liverpool L69 7ZD, UK Scandium perovskite (Sc0.94 Mn0.06 )Mn0.65 Ni0.35 O3 , synthesized at high pressure and high temperature, has a triclinic structure (space group P1̄) at room √ temperature and ambient pressure with a 2ap × √ 2ap × 2ap structure with α ≈ 90◦ , β ≈ 89◦ , γ ≈ 90◦ . Magnetic measurements show that the material displays Curie–Weiss behaviour above 50 K with C = 2.11 emu K mol−1 (μeff = 4.11 µB per formula unit) and θ = −95.27 K. Bond valence sum analysis of the crystal structure shows that manganese is present in three different oxidation states (+2, +3, +4), with the +2 oxidation state on the A site resulting in a highly tilted perovskite structure (average tilt 21.2◦ compared with 15.7◦ calculated for LaCaMnNbO6 ), 2+ 4+ 3+ giving the formula (Sc3+ 0.94 Mn0.06 )(Mn0.41 Mn0.09 ) 2+ (Mn3+ 0.15 Ni0.35 )O3 . 1. Introduction Multiferroic materials have been receiving an increased amount of attention recently owing to the possibility of creating higher-density memory through electrical write and magnetic read [1]. Some classes of magnetic order remove the centre of symmetry in the crystal structure and produce coupling between the magnetization and polarization, e.g. TbMnO3 [2] and DyMnO3 [3]. A second approach is to impose polarization chemically on a structure that displays a permanent magnetization. This second approach can involve combining a stereochemically active lone-pair element such as Bi3+ 2014 The Author(s) Published by the Royal Society. All rights reserved. Downloaded from http://rsta.royalsocietypublishing.org/ on June 18, 2017 (a) Synthesis Polycrystalline Sc2 MnNiO6 and (Sc0.94 Mn0.06 )Mn0.65 Ni0.35 O3 were synthesized under high pressure and temperature using a Rockland Research 600 tonne press with the Walker octahedral multianvil design [15,16]. Stoichiometric amounts of Sc2 O3 (Alfa Aesar, 99.998%), MnO2 (Alfa Aesar, 99.997%) and NiO (Alfa Aesar, 99.998%) were intimately mixed by hand in a pestle and mortar before being placed in a platinum-lined Al2 O3 crucible inside a cylindrical graphite resistance furnace. The graphite furnace is then loaded into the centre of a cast octahedron (Aremco Ceramacast 584-OS). The octahedron is then loaded into the centre of eight truncated tungsten carbide cubes, with the truncations pressing into the faces of the octahedron, forming a cube. This cube is then placed between the six anvils in the press and placed under a hydraulic pressure of 7000 kpsi, which corresponds to a pressure for the sample of 6–7 GPa. Power is then fed to the graphite furnace, giving a sample temperature of 1200◦ C, and held for 30 min. The system is then quenched to room temperature by turning the furnace power off. The use of lower temperatures was attempted, but this resulted in a greater amount of impurity phase being formed. Overall, it was found that reproducing synthesis runs required very tight control of both the temperature and the duration of the heating to limit the amount of secondary phases. The material comes out of the press as a fragile pellet that is made up of small (less than 0.5 mm) black shiny crystals that can be broken away from the main pellet. All samples contained a small amount of an Mn-doped Sc2 O3 phase (less than 0.01 wt%). ......................................................... 2. Experimental 2 rsta.royalsocietypublishing.org Phil. Trans. R. Soc. A 372: 20130012 or Pb2+ on the A site of a perovskite structure with magnetically ordering transition metals on the B site, e.g. Bi2 MnNiO6 [4]. Here, the polar rhombohedral derivatives of perovskite structures based on Bi3+ have been popular platforms for combining magnetism and polarity; in particular, BiFeO3 -based derivatives have been the source of much work [5]. Other multiferroic efforts have focused on exploiting large differences in cation size to remove the centre of symmetry. For example, the coexistence of ferromagnetism and ferroelectricity has been demonstrated in the high-pressure phase of FeTiO3 , isostructural with LiNbO3 . This same approach has generated multiferroic interest in ScFeO3 , which can be synthesized under high pressure, adopts a polar derivative of the corundum structure and has permanent magnetization above room temperature [6]. The small size of both Fe2+ and Sc3+ drives the distortion from the perovskite to the closepacked, oxide-based corundum and LiNbO3 structures. A site displacement due to mismatched cation sizes has been proposed as a mechanism for obtaining polar behaviour in ferromagnetic Ni−Mn double perovskites, such as (La,Lu)2 MnNiO6 [7], and in Y2 NiMnO6 [8], with Y3+ being used as the small A site ion that drives the polarization-producing distortion. Sc3+ is smaller than both Lu3+ and Y3+ , so may induce a greater distortion in the perovskite structure if this can be retained despite the competition with corundum. Park & Parise [9] also noted that the smaller the M ion, the greater the tilting of the octahedra in the series MCrO3 (M = La–Lu, In, Sc), reaching a maximum at In. Few A site scandium perovskites are known, with ScAlO3 [10], ScCrO3 [9] and ScRhO3 [11] all requiring high-pressure synthesis. Attempts by several groups to synthesize perovskite ScMnO3 at 5 GPa proved unsuccessful, producing instead hexagonal ScMnO3 [12]. However, recently Chen et al. [13] used 12.5 GPa to produce perovskite ScMnO3 . This paper reports the outcome of synthesis addressing the target composition Sc2 MnNiO6 , which was selected on the basis of Sc3+ providing the distortion for ferroelectricity, with B site order of Mn4+ and Ni2+ and the associated half-filled–empty orbital superexchange providing the ferromagnetism [14]. Attempts to synthesize Sc2 MnNiO6 were unsuccessful, leading to the perovskite-based material with the distinct composition described here. Downloaded from http://rsta.royalsocietypublishing.org/ on June 18, 2017 (b) Characterization Magnetic characterization was carried out using a Quantum Design MPMS magnetometer, which was controlled using the MPMS software. (d) Energy-dispersive X-ray analysis The energy-dispersive X-ray spectroscopy (EDS) was carried out using a JEOL 2000FX transmission electron microscope operated at 200 kV. 3. Results Initial ambient-pressure synthesis attempts at the Sc2 MnNiO6 target composition afforded hexagonal ScMnO3 , NiMn2 O4 and unreacted oxides. High-pressure synthesis of the target Sc2 MnNiO6 afforded a multiphase mixture of two Sc−Mn−Ni−O ternary oxides together with Mn2 O3 and Mn3 O4 related phases. EDS analysis showed that the compositions of the crystallites clustered into two groups. One of these groups has the Mn : Ni elemental ratio of 2/3 : 1/3, whereas the other group, with fewer crystallites observed, has the inverse ratio (see electronic supplementary material, figure S1). Both groups of crystallites appeared to be slightly scandium-deficient, with an Sc : (Mn/Ni) ratio of 0.88 : 1, leading to the ratio Sc : Mn : Ni of 0.88 : 0.66 : 0.33. An ABO3 perovskite with transition metals on the B site alone would have the composition Sc0.88 Mn0.66 Ni0.33 O3−d , i.e. there would be A site vacancies, whereas full occupancy of both A and B sublattices would correspond to Sc0.94 Mn0.71 Ni0.35 O3 , with 0.06 of manganese on the A site. Manganese is known to be present on the A site of the high-pressure perovskites MnMO3 , where M = Ge [17], Sn [18], Si [19], Ti [20] or V [21], and in the B site ordered (In1−y Mny )MnO3 [22], where the B site ordered structure is realized through ordering of Mn3+ and Mn4+ . The mixed valence Mn2+ A site perovskite polymorph of Mn2 O3 has recently been isolated by high-pressure synthesis [23]. It appears that a high-pressure synthesis route is desirable if Mn2+ is to go on the A site of ABX3 -type perovskites. High-pressure synthesis was subsequently carried out at the new Sc0.94 Mn0.71 Ni0.35 O3 target composition (reaction conditions specified in the Experimental section) and yielded a material that appeared single-phase in the electron microscope. The EDS average composition was Sc0.94 Mn0.68 Ni0.36 O3−d (figure 1). Laboratory X-ray powder diffraction was consistent with a single-phase material based on a perovskite superstructure unit cell consistent with the presence of two distinct B sites. The initial ......................................................... (c) Magnetic measurements rsta.royalsocietypublishing.org Phil. Trans. R. Soc. A 372: 20130012 The phase purity was checked by powder X-ray diffraction (XRD) data with a Panalytical X’pert Pro Multi-Purpose X-ray diffractometer (Co Kα1 radiation, λ = 1.78901 Å) collected at ambient temperature. A sample from a single high-pressure run was loaded in a 0.5 mm diameter amorphous fused silica capillary (Markröhrchen Quarzkapillaren) and measured by synchrotron powder diffraction (SPD) at station I11 of the Diamond Light Source, Harwell. Data were collected stepwise over 1.821–141.953◦ 2θ (λ = 0.949831 Å). Another sample from a separate single high-pressure run (≈30 mg) was loaded in a 1.5 mm diameter amorphous fused silica capillary (Markröhrchen Quarzkapillaren) and measured by powder neutron diffraction (PND) on the Polaris station at ISIS, Harwell. Rietveld refinements were performed with the TOPAS program. In combined SPD and PND refinements, the lattice parameters were refined independently, whereas the site occupancies and fractional coordinates were constrained to have the same values. Bond length calculations were made using the PND values. The lattice parameters were refined separately, as the PND and XRD samples came from two separate synthesis runs and so will have differing residual strains from the high-pressure synthesis. A slight difference is also expected due to the differing ambient conditions present for the PND and XRD measurements. 3 Downloaded from http://rsta.royalsocietypublishing.org/ on June 18, 2017 0 1.00 O 0.50 0.75 nO 2 Ni M 0.50 0.25 1.00 0 0 0.25 0.50 0.75 1.00 ScO1.5 Figure 1. EDS for 30 crystallites of (Sc0.94 Mn0.06 )Mn0.65 Ni0.35 O3 . The filled light grey square shows the ideal point for (Sc0.94 Mn0.06 )Mn0.65 Ni0.35 O3 , whereas the dark grey square shows the average value (Sc0.94(3) Mn0.68(2) Ni0.36(2) O3 ) for the 30 crystallites. White crosses give the error of the average value. refinement of synchrotron and neutron data was carried out using structural parameters from LuNiO3 [24] in P21 /n (see electronic supplementary material, figure S2a), with initially complete Sc occupancy of the A site and a disordered B site composition 0.66Mn/0.33Ni. Refinement of the B site occupancy showed that Ni was ordered uniquely on one of the two possible sites, so a B site ordered model was used from there on. Reducing the symmetry to P1̄ further improved the fit (see electronic supplementary material, figure S2b). This can most clearly be seen by comparing the P21 /n and P1̄ refinements (see electronic supplementary material, figure S2a,b) over the 14.9◦ and 21.7–21.9◦ 2θ ranges. The weighted profile R-factor Rwp decreases from 6.29% to 5.17%. The symmetry lowering is associated with the creation of two distinct A sites and four B sites. Refinement shows that Mn is only present on one of the two A sites. The Sc distribution was then investigated by comparing an A site-deficient model with the Mn on the Sc/Mn mixed A site replaced with vacancies. In this case, two of the four B sites are solely occupied by Mn and the other two are mixed Mn/Ni at an overall composition (Sc0.88 Vac0.12 )Mn0.66 Ni0.33 O3 (see electronic supplementary material, figure S2c). This was then compared with the refinement for a fully occupied Mn-containing A site (Sc0.94 Mn0.06 )Mn0.65 Ni0.35 O3 model. The A site-deficient model would require an average oxidation state for the Mn of +4.09 or an Ni state of +2.18. However, the filled A site model only requires the average Mn oxidation state to be +3.49. This is achievable through putting Mn2+ on the A site and having close to 2 : 1 Mn4+ : Mn3+ on the B site (full 2 : 1 gives 3.52). The model with a full A site with a small amount of Mn gave a clearly better fit (Rwp = 5.17% (see electronic supplementary material, figure S2b) versus Rwp = 6.15% (see electronic supplementary material, figure S2c)). The preference for a completely occupied Mn-containing A site in the (Sc0.94 Mn0.06 )Mn0.65 Ni0.35 O3 model is consistent with the expectation that high-pressure synthesis would produce dense phases (table 1). Figure 2 shows the refined structure of (Sc0.94 Mn0.06 )Mn0.65 Ni0.35 O3 . The final joint SPD and PND refinements are shown in figure 3. The 30% Mn/70% Ni mixed sites and Mn-only B sites order in a rock-salt manner. The symmetry lowering to triclinic does not change the basic B site ordering pattern from the LuNiO3 starting model—although there are four crystallographically ......................................................... 0.75 rsta.royalsocietypublishing.org Phil. Trans. R. Soc. A 372: 20130012 0.25 4 Downloaded from http://rsta.royalsocietypublishing.org/ on June 18, 2017 (a) (b) 5 ......................................................... rsta.royalsocietypublishing.org Phil. Trans. R. Soc. A 372: 20130012 a b c a c b (c) (d) b c a c a b Figure 2. The structure of (Sc0.94 Mn0.06 )Mn0.65 Ni0.35 O3 (tilt system a+ b− c− ), showing the two types of A site: large lighter grey (green online) spheres are pure Sc sites, whereas black spheres are mixed Sc/Mn sites. Lighter grey (red online) octahedra represent pure Mn sites, whereas darker grey (blue online) octahedra show mixed Mn/Ni sites. The small light grey spheres show the oxygen positions. (a) The view down [001] (pseudocubic a-axis). (b) The view along [110] (pseudocubic b-axis). (c) The view down [11̄0] (pseudocubic c-axis). (d) The A site ions only shown in a projection close to the view down the a-axis. (Online version in colour.) Table 1. Comparison of refinement statistics for refinements described in the main text. refinement P21 /n (Sc0.94 Mn0.06 )Mn0.65 Ni0.35 O3 Rwp (%) 6.29 figure electronic supplementary material, figure S2a P1̄ (Sc0.94 Mn0.06 )Mn0.65 Ni0.35 O3 5.17 electronic supplementary material, figure S2b P1̄ with A site vacancies (Sc0.88 Vac0.12 )Mn0.66 Ni0.33 O3 6.15 electronic supplementary material, figure S2c .......................................................................................................................................................................................................... .......................................................................................................................................................................................................... .......................................................................................................................................................................................................... distinct sites, they divided into two pairs of equivalent occupancies (table 2). The A site ordering corresponds to corrugated layers of the distinct Sc-only and 12% Mn/88% Sc A sites in the ac plane stacked along the b-axis (figure 2d). The reduction in symmetry from P21 /n to P1̄ increases the number of crystallographically distinct A sites from one to two, and the number of B sites from two to four. The final refined values (table 2) reveal that manganese is observed on only one of the two possible A sites and that nickel is present on only two of the four possible B sites. Bond lengths and angles and bond Downloaded from http://rsta.royalsocietypublishing.org/ on June 18, 2017 (a) (b) intensity (arb. units) 2000 1000 4000 2000 0 0 10 20 30 40 50 60 2000 4000 6000 2q 8000 10 000 12 000 14 000 16 000 18 000 time of flight Figure 3. Combined refinement of (a) XRD λ = 0.949831 Å and (b) neutron data (backscattering bank Polaris) Rwp = 5.25%. Tick marks are given for allowed reflections; in the XRD pattern the lower tick marks refer to 0.01 wt% of an Mn-doped Sc2 O3 impurity phase. Table 2. Crystallographic data for (Sc0.94 Mn0.06 )Mn0.65 Ni0.35 O3 at room temperature from the combined refinements shown in figure 3. atom Wyckoff position oxidation x y z Biso occupancy Sc1 2i +3 0.9734(5) 0.9230(6) 0.7473(4) 0.35(4) 1.00 Sc2 2i +3 0.5231(5) 0.4264(6) 0.7582(4) 0.91(5) 0.88(8) Mn2 2i +2 0.5231(5) 0.4264(6) 0.7582(4) 0.91(5) 0.12(8) Mn3 1f +4 0.5 0 0.5 0.49(6) 1 Mn4 1c +4 0 0.5 0 0.22(6) 1 Mn5 1g +3 0 0.5 0.5 0.27(6) 0.307(10) Mn6 1d +3 0.5 0 0 0.27(6) 0.293(10) Ni5 1g +2 0 0.5 0.5 0.27(6) 0.693(10) Ni6 1d +2 0.5 0 0 0.27(6) 0.707(10) O1 2i −2 0.6832(9) 0.6740(9) 0.9462(6) 0.35(4) 1 O2 2i −2 0.7990(9) 0.1886(10) 0.5715(6) 0.01(1) 1 O3 2i −2 0.3739(10) 0.0550(1) 0.7386(7) 0.05(5) 1 O4 2i −2 0.1454(10) 0.5657(1) 0.7560(7) 0.03(3) 1 O5 2i −2 0.8325(9) 0.1906(10) 0.9337(6) 1.39(28) 1 O6 2i −2 0.6888(10) 0.7085(10) 0.5830(6) 0.42(17) 1 .......................................................................................................................................................................................................... .......................................................................................................................................................................................................... .......................................................................................................................................................................................................... .......................................................................................................................................................................................................... .......................................................................................................................................................................................................... .......................................................................................................................................................................................................... .......................................................................................................................................................................................................... .......................................................................................................................................................................................................... .......................................................................................................................................................................................................... .......................................................................................................................................................................................................... .......................................................................................................................................................................................................... .......................................................................................................................................................................................................... .......................................................................................................................................................................................................... .......................................................................................................................................................................................................... .......................................................................................................................................................................................................... valence sums are quoted in table 3. Bond valence sums are consistent with the presence of Mn2+ on the A site. The Mn-only B site bond lengths correspond to an Mn oxidation state of +4, whereas the site shared with Ni corresponds to an Mn oxidation state of +3. As the mixed Mn/Ni sites and Mn-only sites order in a rock-salt manner (figure 2), the Mn3+ and Mn4+ oxidation states are thus also rock-salt-ordered. As a result of the synchrotron, X-ray and neutron refinement being combined, the Biso values for the oxygen sites vary significantly from what is expected. This is due to the synchrotron X-ray data having vastly more counts and so dominating the thermal parameter calculation. So, as the values are more XRD-based, the values for low-scattering atoms such as oxygen become less precise. ......................................................... 3000 6 6000 rsta.royalsocietypublishing.org Phil. Trans. R. Soc. A 372: 20130012 intensity (arb. units) 4000 Downloaded from http://rsta.royalsocietypublishing.org/ on June 18, 2017 Table 3. Bond lengths (Å), selected angles (deg) and bond valence sums (BVS) in (Sc0.94 Mn0.06 )Mn0.65 Ni0.35 O3 at room temperature. BVS 2.44(9) 2.22(1) Sc 2.83 bond (B1−O−B2) angle (deg) 3.08(2) 2.67(5) 2.12(6) 3.55(4) 3.54(1) 2.13(4) 2.10(5) 3.59(0) 2.64(9) 2.10(1) .......................................................................................................................................................................................................... average 2.68(4) Sc2/Mn2−O 2.02(5) 2.84(1) .......................................................................................................................................................................................................... Sc 2.90 Mn 2.4 3.59(6) 3.44(6) 2.14(4) 2.31(9) 3.20(6) 2.08(9) 2.39(0) 3.52(9) 2.46(8) 2.12(4) .......................................................................................................................................................................................................... average Mn3−O 2.67(6) .......................................................................................................................................................................................................... 4 × 1.88(9) Mn 4.02 ....................... 2 × Mn3−O3−Ni6/Mn6 139.2(3) .......................................................................................... 1.89 (8) 2 × Mn3−O2−Ni5/Mn5 2 × Mn3−O6−Ni5/Mn5 137.2(3) 2 × 1.92(5) 2 × Mn4−O1−Ni6/Mn6 140.3(3) 2 × 1.92(6) 139.8(3) .......................................................................................................................................................................................................... average Mn4−O .......................................................................................................................................................................................................... Mn 3.76 ....................... .......................................................................................... 2 × Mn4−O4−Ni5/Mn5 2 × 1.88(5) ....................... 132.4(2) .......................................................................................... 2 × Mn4−O5−Ni6/Mn6 2 × 1.97(2) 137.5(3) .......................................................................................................................................................................................................... average 1.92(4) .......................................................................................................................................................................................................... Ni5/Mn5−O 2 × 2.00(6) Ni 2.17 ....................... 2 × 2.07(5) ....................... 2 × 2.01(2) 2 × Ni5/Mn5−O2−Mn3 139.8(3) .......................................................................................... Mn 2.89 2 × Ni5/Mn5−O4−Mn4 132.4(2) .......................................................................................... 2 × Ni5/Mn5−O6−Mn3 137.2(3) .......................................................................................................................................................................................................... average 2.02(4) .......................................................................................................................................................................................................... (Continued.) ......................................................... lengths (Å) rsta.royalsocietypublishing.org Phil. Trans. R. Soc. A 372: 20130012 bond (X−O) Sc1−O 7 Downloaded from http://rsta.royalsocietypublishing.org/ on June 18, 2017 Table 3. (Continued.) 8 bond (B1−O−B2) 2 × Ni6/Mn6−O1−Mn4 BVS Ni 2.20 ....................... 2 × 2.06(9) angle (deg) 140.3(3) ......................................................................................... 2 × Ni6/Mn6−O3−Mn3 Mn 2.93 ....................... 139.2(3) ......................................................................................... 2 × Ni6/Mn6-O5−Mn4 2 × 2.00(4) 137.5(3) .......................................................................................................................................................................................................... average 2.02(7) .......................................................................................................................................................................................................... (a) (b) c c b b Figure 4. A site environments for the Sc ions in the unit cell (a) Sc1 and (b) the mixed Sc2/Mn6 site. Light grey spheres are oxygen, black spheres are Sc, dark grey spheres are the calculated centres of the oxygen coordination spheres, and the joining black arrows are the displacement vectors from the centres of the oxygen positions. Both figures are viewed along the triclinic a-axis [1̄00]. The 1 : 3 A site ordered compounds AA3 Mn4 O12 (A = Mn3+ ) can also simultaneously show differing Mn oxidation states on the A and B sites, with the proportion of valence ordering on the B site being determined by the A cation. For example, in the case of A = Na [25], the Mn3+ and Mn4+ oxidation states order fully in distinct crystallographic sites. When A = Ca [26], the compound has 1 : 3 Ca : Mn3+ on the A site as well as 1 : 3 Mn4+ : Mn3+ order on the B site, with distinct crystallographic sites. However, when A = Bi [27], all Mn is present as Mn3+ . Thus, the high-pressure phases (In1−y Mny )MnO3 [22] and Mn2 O3 [23] and the new (Sc0.94 Mn0.06 )Mn0.65 Ni0.35 O3 composition reported here are rare in showing both A and B site Mn with differing oxidation states and the A site being Mn2+ . Within the Glazer–Woodward scheme, the P1̄ space group is described as a+ b− c− , where the rotations around the x-, y- and z-axes have differing magnitudes, with x-rotations being in phase and y- and z-rotations being in anti-phase. This relates to the monoclinic P21 /c tilting system a+ b− b− (when the P21 /n setting is used, the tilt system is described as b− b− c+ [28]). The tilting angle of the octahedra can be defined as φ = (180 − Φ)/2, where Φ is the Ni/Mn−O−Mn bond angle (Φ = 180◦ for a cubic perovskite, making φ = 0). Mean tilt angles of 22.1(2)◦ about 001 (figure 2a), 20.9(2)◦ about 110 (figure 2b) and 20.5(2)◦ about 11̄0 (figure 2c) are calculated. The average tilt of 21.2◦ compared to 15.7◦ calculated for LaCaMnNbO6 [29] demonstrates the high degree of tilting in (Sc0.94 Mn0.06 )Mn0.65 Ni0.35 O3 . As the b and c tilts are the same within error, there is no observed deviation from a+ b− b− (P21 /c), consistent with the tilting being controlled by the number of distinct B sites. The tilt angles signal a strong deviation from the cubic perovskite structure that is confirmed by four Sc−O bonds for each site being longer than 3 Å. Figure 4 shows the A site coordination ......................................................... lengths (Å) 2 × 2.00(8) rsta.royalsocietypublishing.org Phil. Trans. R. Soc. A 372: 20130012 bond (X−O) Ni6/Mn6−O Downloaded from http://rsta.royalsocietypublishing.org/ on June 18, 2017 c–1 (emu–1 mol) 0.05 120 80 40 0 0.04 0 0.03 9 400 100 200 temperature (K) 300 200 0 –200 0.02 –400 0.01 0 20 40 60 temperature (K) 80 100 –10 000 5000 0 field (Oe) 5000 10 000 Figure 5. (a) Zero field cooled (empty squares) and field cooled (filled squares) magnetization measurement with 100 Oe measuring field. Inset shows inverse susceptibility with Curie–Weiss behaviour, which was fitted between 170 and 280 K. (b) Magnetization versus field measured at 5 K. environments at the two sites, with the dark grey spheres showing the calculated centroids of the oxygen polyhedra. The Sc1 site is displaced by 0.540(2) Å, whereas the mixed Sc2/Mn6 site has the smaller displacement of 0.515(6) Å—in both cases, the displacements are antiferrodistortive. These distortions compare to ScCrO3 [9], where the displacement is 0.503(1) Å, and to ScAlO3 [10], where the displacement is 0.452(1) Å. Both ScCrO3 and ScAlO3 are Pbnm perovskites with the same b− b− c+ tilt system, close to that found in the present B site ordered material. Analysis of the displacement directions reveals that both the Sc1 and Sc2 sites move predominantly along the b-axis. Although the difference between the sites is relatively small (5% of the total displacement), the reduced displacement of the Sc2/Mn6 site coincides with the Mn occupancy of this site. Both Mn2+ and Sc3+ cations are too small to occupy a conventional perovskite A site, and thus drive extensive tilting to reduce their coordination number. The relatively small difference between the refined tilts along 1̄1̄0 and 110 indicates that the deviation from the monoclinic structure where the tilts would be equal is minor. The driving force behind this deviation is thus the preferential ordering of the manganese cations on one of the two A sites in the P1̄ structure, which is not possible in the single A site P21 /n structure. Although the number of B sites also increases, there are effectively only two distinct sites in the lower-symmetry structure, consistent with the creation of two distinct A sites as the reason for the observed triclinic symmetry. The Goldschmidt tolerance factor [30] for (Sc0.94 Mn0.06 )Mn0.65 Ni0.35 O3 is 0.81, which is below the suggested stability limit for perovskites of t ≈ 0.85 [29], consistent with the requirement for synthesis under high pressures [31]. Consistent with the absence of magnetic Bragg scattering in the room-temperature neutron diffraction data, (Sc0.94 Mn0.06 )Mn0.65 Ni0.35 O3 is a paramagnet to low temperatures. Curie–Weiss analysis of the susceptibility (figure 5a) between 170 and 280 K affords C = 2.11 emu K mol−1 (μeff = 4.11 µB per f.u. (formula unit)) and θ = −95.27 K. This compares well with the calculated C of 2.09 emu K mol−1 (µeff = 4.09 µB per f.u.) for the charge distribution 2+ 4+ 3+ 3+ 2+ of (Sc3+ 0.94 Mn0.06 )(Mn0.41 Mn0.09 ) (Mn0.15 Ni0.35 )O3 assigned on the basis of the refined crystal structure using bond valence sum considerations. The negative Weiss temperature is expected due to the presence of dominant antiferromagnetic interactions. Divergence of the zero field cooled and field cooled magnetizations below 18 K can be associated with the B site cation disorder and the presence of competing ferromagnetic Mn4+ –Ni2+ exchange interactions. Commensurate with the transition to a cooperative magnetic state, the hysteresis measurement at 5 K (figure 5b) shows a small coercive field (72 Oe) with remanent magnetization of 6 emu mol−1 (0.001 µB per f.u.) but the loop does not saturate in a 1 T field. ......................................................... 0.06 160 rsta.royalsocietypublishing.org Phil. Trans. R. Soc. A 372: 20130012 0.07 c (emu mol–1) (b) 200 0.08 M (emu mol–1) (a) Downloaded from http://rsta.royalsocietypublishing.org/ on June 18, 2017 4. Conclusion to Diamond, where we thank Dr C. Tang, Dr J. Parker and Dr S. Thompson for assistance on the I11 diffractometer, and access to ISIS, where we thank Dr R. Smith and Dr S. Hull for assistance on the Polaris instrument. References 1. Scott JF. 2007 Data storage: multiferroic memories. Nat. Mater. 6, 256–257. (doi:10.1038/ nmat1868) 2. Ribeiro JL. 2010 Symmetry, incommensurate magnetism and ferroelectricity: the case of the rare-earth manganites RMnO3 . J. Phys. Conf. Ser. 226, 012013. (doi:10.1088/17426596/226/1/012013) 3. Ribeiro JL. 2007 Symmetry and magnetically driven ferroelectricity in rare-earth manganites RMnO3 (R = Gd,Tb,Dy). Phys. Rev. B 76, 144417. (doi:10.1103/PhysRevB.76.144417) 4. Azuma M, Takata K, Saito T, Ishiwata S, Shimakawa Y, Takano M. 2005 Designed ferromagnetic, ferroelectric Bi2 NiMnO6 . J. Am. Chem. Soc. 127, 8889–8892. (doi:10.1021/ ja0512576) 5. Catalan G, Scott JF. 2009 Physics and applications of bismuth ferrite. Adv. Mater. 21, 2463–2485. (doi:10.1002/adma.200802849) 6. Li M-R et al. 2012 A polar corundum oxide displaying weak ferromagnetism at room temperature. J. Am. Chem. Soc. 134, 3737–3747. (doi:10.1021/ja208395z) 7. Singh DJ, Park CH. 2008 Polar behavior in a magnetic perovskite from A-site size disorder: a density functional study. Phys. Rev. Lett. 100, 087601. (doi:10.1103/PhysRevLett.100.087601) 8. Kumar S, Giovannetti G, van den brink J, Picozzi S. 2010 Theoretical prediction of multiferroicity in double perovskite Y2 NiMnO6 . Phys. Rev. B 82, 134429. (doi:10.1103/ PhysRevB.82.134429) 9. Park JH, Parise JB. 1997 High pressure synthesis of a new chromite, ScCrO3 Mater. Res. Bull. 32, 1617–1624. (doi:10.1016/S0025-5408(97)00151-7) 10. Ross NL. 1998 High pressure study of ScAlO3 perovskite. Phys. Chem. Miner. 25, 597–602. (doi:10.1007/s002690050153) 11. Belik AA, Matsushita Y, Tanaka M, Takayama-Muromachi E. 2013 High-pressure synthesis, crystal structures, and properties of ScRhO3 and InRhO3 perovskites. Inorg. Chem. 52, 12 005– 12 011. (doi:10.1021/ic401760m) 12. Uusi-Esko K, Malm J, Imamura N, Yamauchi H, Karppinen M. 2008 Characterization of RMnO3 (R = Sc, Y, Dy–Lu): high-pressure synthesized metastable perovskites and their hexagonal precursor phases. Mater. Chem. Phys. 112, 1029–1034. (doi:10.1016/j.matchemphys. 2008.07.009) 13. Chen H, Yu T, Gao P, Bai J, Tao J, Tyson TA, Wang L, Lalancette R. 2013 Synthesis and structure of perovskite ScMnO3 . Inorg. Chem. 52, 9692–9697. (doi:10.1021/ic4016838) 14. Dass RI, Yan JQ, Goodenough JB. 2003 Oxygen stoichiometry, ferromagnetism, and transport properties of La2−x NiMnO6+d . Phys. Rev. B 68, 064415. (doi:10.1103/PhysRevB.68.064415) 15. Walker D, Carpenter MA, Hitch CM. 1990 Some simplifications to multianvil devices for high pressure experiments. Am. Mineralogist 75, 1020–1028. See http://www.minsocam. org/ammin/AM75/AM75_1020.pdf. ......................................................... Acknowledgements. We thank EPSRC (EP/C511794/1 and EP/H000925) for support and the STFC for access rsta.royalsocietypublishing.org Phil. Trans. R. Soc. A 372: 20130012 (Sc0.94 Mn0.06 )Mn0.65 Ni0.35 O3 can be prepared only using a high-pressure, high-temperature route, consistent with the low perovskite tolerance factor. The presence of three distinct charge states on the B site (Mn4+ , Mn3+ , Ni2+ ) and Mn2+ on the A site is unusual and may be required to stabilize the highly distorted A site environment preferred by the Sc3+ cation. The stabilizing effect of the Mn2/3 Ni1/3 B site composition on the perovskite structure for small A site cations is consistent with the observation that BiMn2/3 Ni1/3 O3 [32] can be prepared at ambient pressure, whereas Bi2 NiMnO6 [4], BiNiO3 [33] and BiMnO3 [34] all require high-pressure synthesis. (Sc0.94 Mn0.06 )Mn0.65 Ni0.35 O3 crystallizes in P1̄, with the distortion away from the familiar P21 /n two B site, single A site structure of LuNiO3 being driven by the need to form two distinct A sites to accommodate Mn2+ . 10 Downloaded from http://rsta.royalsocietypublishing.org/ on June 18, 2017 11 ......................................................... rsta.royalsocietypublishing.org Phil. Trans. R. Soc. A 372: 20130012 16. Huppertz H. 2011 New synthetic discoveries via high-pressure solid-state chemistry. Chem. Commun. 47, 131–140. (doi:10.1039/c0cc02715d) 17. Ito E, Matsui Y. 1979 High-pressure transformations in silicates, germanates, and titanates with ABO3 stoichiometry. Phys. Chem. Miner. 4, 265–273. (doi:10.1007/BF00307950) 18. Leinenweber K, Utsumi W, Tsuchida Y, Yagi T, Kurita K. 1991 Unquenchable highpressure perovskite polymorphs of MnSnO3 and FeTiO3 . Phys. Chem. Miner. 18, 244–250. (doi:10.1007/BF00202576) 19. Fujino K, Suzuki K, Hamane D, Seto Y, Nagai T, Sata N. 2008 High-pressure phase relation of MnSiO3 up to 85 GPa: existence of MnSiO3 perovskite. Am. Mineralogist 93, 653–657. (doi:10.2138/am.2008.2645) 20. Ross NL, Ko J, Prewitt CT. 1989 A new phase transition in MnTiO3 : LiNbO3 -perovskite structure. Phys. Chem. Miner. 16, 621–629. (doi:10.1007/BF00223309) 21. Syono Y, Akimoto S-I, Endoh Y. 1971 High pressure synthesis of ilmenite and perovskite type MnVO3 and their magnetic properties. J. Phys. Chem. Solids 32, 243–249. (doi:10.1016/ S0022-3697(71)80026-4) 22. Belik AA, Matsushita Y, Tanaka M, Takayama-Muromachi E. 2010 (In1−y Mny )MnO3 (1/9 ≤ y ≤ 1/3): unusual perovskites with unusual properties. Angew. Chem. Int. Edn. 49, 7723–7727. (doi:10.1002/anie.201003080) 23. Ovsyannikov SV et al. 2013 Perovskite-like Mn2 O3 : a path to new manganites. Angew. Chem. Int. Edn. 52, 1494–1498. (doi:10.1002/anie.201208553) 24. Alonso JA, Martinez-Lope MJ, Casais MT, Garcia-Munoz JL, Fernandez-Diaz MT. 2000 Roomtemperature monoclinic distortion due to charge disproportionation in RNiO3 perovskites with small rare-earth cations (R = Ho, Y, Er, Tm, Yb, and Lu): a neutron diffraction study. Phys. Rev. B 61, 1756–1763. (doi:10.1103/PhysRevB.61.1756) 25. Prodi A, Gilioli E, Gauzzi A, Licci F, Marezio M, Bolzoni F, Huang Q, Santoro A, Lynn JW. 2004 Charge, orbital and spin ordering phenomena in the mixed valence manganite 3+ 4+ (NaMn3+ 3 )(Mn2 Mn2 )O12 . Nat. Mater. 3, 48–52. (doi:10.1038/nmat1038) 26. Przenioslo R, Sosnowska I, Suard E, Hewat A, Fitch A. 2004 Charge ordering and anisotropic thermal expansion of the manganese perovskite CaMn7 O12 . Physica B 344, 358–367. (doi:10.1016/j.physb.2003.10.013) 27. Okamoto H, Imamura N, Karppinen M, Yamauchi H, Fjellvåg H. 2010 Crystal structure of the monoclinic and cubic polymorphs of BiMn7 O12 . J. Solid State Chem. 183, 186–191. (doi:10.1016/j.jssc.2009.10.013) 28. Mitchell RH. 2002 Perovskites: modern and ancient. Thunder Bay Ontario, Canada: Almaz. 29. Bos J-WG, Attfield JP. 2004 Structural and magnetic properties of the double perovskite LaCaMnNbO6 . Z. Anorg. Allg. Chem. 630, 2248–2252. (doi:10.1002/zaac.200400159) 30. Goldschmidt VM. 1926 Laws of crystal chemistry. Naturwissenschaften 14, 477–485. (doi:10.1007/BF01507527) 31. Navrotsky A. 1998 Energetics and crystal chemical systematics among ilmenite, lithium niobate, and perovskite structures. Chem. Mater. 10, 2787–2793. (doi:10.1021/cm9801901) 32. Hughes H, Allix MMB, Bridges CA, Claridge JB, Kuang X, Niu H, Taylor S, Song W, Rosseinsky MJ. 2005 A polar oxide with a large magnetization synthesized at ambient pressure. J. Am. Chem. Soc. 127, 13 790–13 791. (doi:10.1021/ja054839w) 33. Ishiwata S, Azuma M, Takano M, Nishibori E, Takata M, Sakata M, Kato K. 2002 High pressure synthesis, crystal structure and physical properties of a new Ni(II) perovskite BiNiO3 . J. Mater. Chem. 12, 3733–3737. (doi:10.1039/b206022a) 34. Atou T, Chiba H, Ohoyama K, Yamaguchi Y, Syono Y. 1999 Structure determination of ferromagnetic perovskite BiMnO3 . J. Solid State Chem. 145, 639–642. (doi:10.1006/jssc. 1999.8267)
© Copyright 2026 Paperzz