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. 2023 Nov 27;62(49):20042–20049. doi: 10.1021/acs.inorgchem.3c02835

Anisotropic Thermal Expansion and a Second-Order Charge Order Transition in the Ferrimagnetic Dy2CuZnMn4O12 Perovskite with Triple A-Site Cation Ordering

Alexei A Belik 1,*
PMCID: PMC10910486  PMID: 38012860

Abstract

graphic file with name ic3c02835_0008.jpg

Dy2CuZnMn4O12 perovskite, belonging to the A-site columnar-ordered quadruple perovskite family with the general composition of A2A′A″B4O12, was prepared by a high-pressure, high-temperature method at 6 GPa and 1500 K. Its crystal structure was studied by synchrotron powder X-ray diffraction between 100 and 800 K. The ideal cation distribution (without antisite disorder) was found to be realized within the sensitivity of the synchrotron X-ray diffraction method. Between 100 and 400 K, it crystallizes in space group Pmmn (no. 59) and has layered charge ordering of Mn3+ and Mn4+ at the B sites. Above 425 K, it crystallizes in space group P42/nmc (no. 137) with one crystallographic B site and an average Mn3.5+ oxidation state. The charge ordering transition (at TCO = 425 K) appears to be of the second order as no anomalies were found on differential scanning calorimetry curves and temperature dependence of the unit cell volume, and the orthorhombic a and b lattice parameters merge gradually. The compound demonstrates anisotropic thermal expansion with the c lattice parameter decreasing with increasing temperature above 280 K. A ferrimagnetic transition occurs at TC = 116 K with an additional, gradual rise of magnetic susceptibilities below 45 K, probably due to increases of the ordered moments of the Dy sublattices.

Short abstract

A new member of the A-site columnar-ordered quadruple perovskites was prepared at high pressure, Dy2CuZnMn4O12, with triple A-site ordering, ferrimagnetic properties, and a charge-order transition.

1. Introduction

A-site columnar-ordered quadruple perovskite oxides with the general composition of A2A′A″B4O12 are a new playground in the perovskite science to play with compositional variations and their effects on physical properties.1 In comparison with classical ABO3 perovskites with one type of A sites and A-site-ordered quadruple perovskites, AA′3B4O12, with intrinsically two types of A sites (A with a 12-fold coordination and A′ with a square-planar coordination), A2A′A″B4O12 perovskites have an additional degree of freedom in the presence of the A″ site with a tetrahedral coordination (as the first coordination sphere). Therefore, a principally different, new set of cations, which are not usually located at A sites of perovskites, can be used for the A′′ site, such as Ga3+ and Zn2+.25

The parent structure of the A2A′A″B4O12 perovskites has P42/nmc symmetry and is formed through large tilts of the a+a+c type.1 This symmetry is retained in the majority of examples of such perovskites.1,6 The next most commonly observed symmetry is P42/n, which is produced through full or partial rock-salt-type B-cation orderings, A2A′A″B2B′2O12.1,6 The less common symmetries are P42mc (which is formed through polar distortions in CaMnTi2O6,7 CaMnTi2–xVxO6,8 and NaYMnMnTi4O12)9 and Pmmn (which is formed through layered-type B-cation ordering in RMn3O6 (R = Gd to Tm)10,11 and R2CuMnMn4O12 (R = Dy and Y)12 due to partial or full charge ordering of Mn3+ and Mn4+, respectively). The presence of charge-ordered structures based on the same element could suggest the existence of temperature-driven charge-(dis)ordered transitions as observed in simple perovskites (e.g., half-doped R3+0.5A2+0.5MnO3)13 or quadruple perovskites (e.g., ACu3Fe4O12).14 However, such charge-order transitions have not been observed so far in A2A′A″B4O12 perovskites.1,10

In this work, we prepared a new member of the A-site columnar-ordered quadruple perovskite family with the composition of Dy2CuZnMn4O12. In this compound, a new combination of the A/A′/A″ cations was used (R3+/Cu2+/Zn2+) to achieve the triple A-site cation ordering. This combination also gives an average oxidation state of Mn as +3.5—an ideal value for the realization of possible charge ordering. We indeed found that Dy2CuZnMn4O12 crystallizes in space group Pmmn at room temperature with 1:1 charge order of Mn3+ and Mn4+ at the B sites. High-temperature structural studies showed the existence of a charge-disorder transition above 425 K, which is of the second order. We also observed anisotropic thermal expansion above 280 K and a ferrimagnetic transition below TC = 116 K.

2. Experimental Section

Dy2CuZnMn4O12 was prepared from a stoichiometric mixture of o-DyMnO3, ZnO (99.9%), CuO (99.9%), and MnO2 (Alfa Aesar, 99.9%) at about 6 GPa and about 1500 K for 2 h in Au capsules. After annealing at 1500 K, the samples were cooled down to room temperature by turning off the heating current, and the pressure was slowly released. We note that the oxygen content of a commercial well-crystallized single-phase MnO2 chemical was confirmed by thermal analysis. Single-phase o-DyMnO3 was prepared from a stoichiometric mixture of Dy2O3 (99.9%) and Mn2O3 (99.99%) by annealing in air at 1430 K for 60 h with several intermediate grindings. After the high-pressure synthesis, the sample was recovered as black powder (Figure S1). Therefore, some measurements (such as, specific heat, resistivity, and dielectric constant), which require dense pellets, could not be performed. We note that the melting point of Au at 6 GPa is above 1600 K;15 therefore, Au capsules could be safely used for the synthesis at 1500 K. We did not observe any reaction between Au and Dy2CuZnMn4O12 or any damage of Au capsules.

X-ray powder diffraction (XRPD) data were collected at room temperature on a RIGAKU MiniFlex600 diffractometer using Cu Kα radiation (2θ range of 8–100°, a step width of 0.02°, and scan speed of 2°/min). Synchrotron XRPD data were collected from 100 to 800 K on beamline BL02B2 of SPring-8 (the intensity data were taken between 2.08° and 78.22° at 0.006° intervals in 2θ using a wavelength of λ = 0.619283 Å).16 High statistics data with a measurement time of 100 s were collected at 100, 295, and 600 K; at all other temperatures, the measurement time was 10 s. The sample was placed into an open Lindemann glass capillary tube (inner diameter: 0.2 mm), which was rotated during measurements. The Rietveld analysis of all XRPD data was performed using the RIETAN-2000 program.17

Magnetic measurements were performed on a SQUID magnetometer (Quantum Design, MPMS3) between 2 and 400 K in applied fields of 100 Oe and 10 kOe under both zero-field-cooled (ZFC) and field-cooled on cooling (FCC) conditions. High-temperature data were taken at 70 kOe from 300 to 470 K. Isothermal magnetization measurements were performed between −70 and 70 kOe at different temperatures. A small sample weight of 11.09 mg was used for the dc magnetic measurements because of a large magnetic moment (1.82 emu at 5 K and 70 kOe). Frequency dependent alternating current (ac) susceptibility measurements were performed using a Quantum Design MPMS3 instrument at a zero static dc field and at different frequencies (f) and different applied oscillating magnetic fields (Hac) from 140 to 2 K using a 24.7 mg sample.

Differential scanning calorimetry (DSC) curves of a powder sample were recorded on a Mettler Toledo DSC1 STARe system under a N2 flow between 125 and 670 K in an open Al capsule with a heating/cooling rate of 10 K/min. Two DSC runs were performed to check the reproducibility. No DSC anomalies were found between 125 and 670 K.

3. Results and Discussion

Dy2CuZnMn4O12 was found to be single-phase within the sensitivity of the laboratory XRPD data. All its reflections could be indexed in orthorhombic symmetry with a = 7.2599 Å, b = 7.2709 Å, and c = 7.7736 Å. Therefore, the Pmmn structural model and the structural parameters of DyMn3O6 (as the initial ones)10 were used in the Rietveld analysis of Dy2CuZnMn4O12. Cu2+ (27 electrons) and Zn2+ (28 electrons) cations cannot be distinguished by (nonresonant) synchrotron XRPD. Therefore, we assumed the distribution of Cu2+ and Zn2+ based on their coordination preferences: Zn2+ cations have a strong preference for tetrahedral sites (among tetrahedral and square-planar ones) while Cu2+ cations have a strong preference for square-planar sites.18 We note that CaZnV2O619 and CaCuFeReO620 were recently prepared, where Zn2+ and Cu2+ cations are located in both square-planar (A′) and tetrahedral (A″) sites. However, these compounds were stabilized at much higher pressures of 12 and 15.5 GPa, respectively, and they were not stable at 6 GPa. Therefore, we can assume that usual tendencies in the site preferences for Cu2+ and Zn2+ cations are realized in Dy2CuZnMn4O12 prepared at 6 GPa.

Small antisite disorders are often realized in A2A′A″B4O12 perovskites with A = rare earths, A′ = Mn, and A″ = Mn. Such antisite disorders could be observed with synchrotron XRPD data as small (but detectable) deviations of occupation factors from unity (for ideal cation distribution models).35,11 However, during the structural analysis of Dy2CuZnMn4O12, all cation occupation factors converged to values close to unity. We report here the occupation factors at 600 K as the symmetry at 600 K is higher (see below) and the number of refined structural parameters is smaller. The following values were obtained (when all other structural and nonstructural parameters were refined simultaneously including atomic displacement parameters): g(Dy) = 0.985(2), g(Cu) = 0.482(3) (for a disordered model with the ideal g = 0.5), and g(Zn) = 0.995(6) with fixed g(Mn) = 1 and g(Cu) = 0.487(3), g(Zn) = 1.014(6), and g(Mn) = 1.018(2) with fixed g(Dy) = 1. We also note that when Mn was located at the tetrahedral A″ site (or the square-planar A′ site), its occupation factor was refined to be 1.265(7) (or 0.600(3) for the A′ site), that is, significantly larger than unity (or 0.5). Therefore, we concluded that the ideal cation distributions are realized in Dy2CuZnMn4O12 within the sensitivity of synchrotron XRPD data.

Refined structural parameters, primary bond lengths, and bond valence sums (BVS)21 of Dy2CuZnMn4O12 at 100 and 295 K are summarized in Tables 1 and 2 and Table S1. Experimental, calculated, and difference synchrotron XRPD patterns of Dy2CuZnMn4O12 at 295 K are shown in Figure 1. The crystal structure of Dy2CuZnMn4O12 at 295 K is presented in Figure 2a.

Table 1. Structure Parameters of Dy2CuZnMn4O12 at 100 K (the First Line for Each Site) and 295 K (the Second Line for Each Site) from Synchrotron XRPD Dataa.

site WP x y z Biso2)
Dy1 2a 0.25 0.25 0.7785(2) 0.08(2)
    0.25 0.25 0.7784(2) 0.27(3)
Dy2 2a 0.25 0.25 0.2786(2) 0.15(3)
    0.25 0.25 0.2786(2) 0.40(3)
Cu 2b 0.75 0.25 0.7349(4) 0.41(5)
    0.75 0.25 0.7374(5) 0.61(6)
Zn 2b 0.75 0.25 0.2486(4) 0.03(3)
    0.75 0.25 0.2488(5) 0.30(5)
Mn1 4c 0.5 0 0 0.03(5)
    0.5 0 0 0.11(8)
Mn2 4d 0 0.5 0.5 0.10(5)
    0 0.5 0.5 0.26(8)
O1 8g 0.4402(7) –0.0599(7) 0.2624(10) 0.61(8)
    0.4389(8) –0.0589(8) 0.2610(11) 1.02(9)
O2 4f 0.0634(10) 0.25 0.0336(13) 0.19(12)
    0.0623(10) 0.25 0.0344(13) 0.08(11)
O3 4e 0.25 0.5396(11) 0.9105(11) 0.18(13)
    0.25 0.5380(11) 0.9083(12) 0.30(14)
O4 4f 0.5391(12) 0.25 0.4231(13) 0.61(16)
    0.5389(11) 0.25 0.4238(13) 0.71(16)
O5 4e 0.25 0.4330(10) 0.5386(13) 0.06(11)
    0.25 0.4353(10) 0.5405(13) 0.25(13)
a

Source: Synchrotron powder X-ray diffraction (λ = 0.61928 Å); used d-space range: from 0.4916 to 7.1 Å. Crystal system: orthorhombic; space group Pmmn (no. 59, origin choice 2); Z = 2. Molecular weight: 865.6708 g/mol. The occupation factors (g) of all the sites are unity (g = 1). WP: Wyckoff position. No detectable impurities. 100 K: a = 7.25134(2) Å, b = 7.25958(2) Å, c = 7.76916(1) Å, and V = 408.9820(14) Å3; Rwp = 7.02%, Rp = 5.15%, RB = 2.86%, and RF = 1.41%; ρcal = 7.030 g/cm3. 295 K: a = 7.25988(2) Å, b = 7.27087(2) Å, c = 7.77362(2) Å, and V = 410.3355(19) Å3; Rwp = 7.26%, Rp = 5.33%, RB = 3.22%, and RF = 1.66%; ρcal = 7.006 g/cm3.

Table 2. Selected Bond Lengths (l (Å) < 2.8 Å), Bond Angles (deg), Bond Valence Sums, BVS, and Distortion Parameters of MnO6, Δ, in Dy2CuZnMn4O12 at 295 Ka.

Dy1–O5 × 2 2.288(9) Dy2–O2 × 2 2.337(9)
Dy1–O3 × 2 2.325(8) Dy2–O4 × 2 2.382(9)
Dy1–O2 × 2 2.412(9) Dy2–O5 × 2 2.441(9)
Dy1–O1 × 4 2.669(7) Dy2–O1 × 4 2.635(7)
BVS(Dy13+) +3.38 BVS(Dy23+) +3.13
Cu–O1 × 4 1.952(4) Zn–O3 × 2 1.967(9)
BVS(Cu2+) +1.91 Zn–O4 × 2 2.050(9)
    BVS(Zn2+) +1.77
Mn1–O2 × 2 1.892(2) Mn2–O5 × 2 1.901(2)
Mn1–O3 × 2 1.969(3) Mn2–O4 × 2 1.932(3)
Mn1–O1 × 2 2.120(8) Mn2–O1 × 2 1.958(8)
BVS(Mn13+) +3.29 BVS(Mn24+) +3.72
Δ(Mn1–O) 22.6 × 10–4 Δ(Mn2–O) 1.4 × 10–4
Mn1–O1–Mn2 × 2 144.73(9) Mn2–O4–Mn2 140.32(9)
Mn1–O2–Mn1 147.75(9) Mn2–O5–Mn2 145.35(9)
Mn1–O3–Mn1 134.33(9)    
a

BVS = ∑Ni=1νi, νi = exp[(R0li)/B], N is the coordination number, B = 0.37, R0(Dy3+) = 2.036, R0(Cu2+) = 1.679, R0(Zn2+) = 1.704, R0(Mn4+) = 1.753, and R0(Mn3+) = 1.76.

Figure 1.

Figure 1

Experimental (black crosses), calculated (red line), and difference (blue line at the bottom) synchrotron powder X-ray diffraction patterns of Dy2CuZnMn4O12 at T = 295 K between 6 and 60°. The tick marks show possible Bragg reflection positions. The inset shows similar curves at T = 600 K between 6 and 26°.

Figure 2.

Figure 2

Crystal structures of Dy2CuZnMn4O12 at (a) T = 295 K in the charge-ordered state and (b) T = 600 K in the charge-disordered state.

The Pmmn structural model was used to obtain the lattice parameters between 100 and 450 K (Figure 3). At 425 and 450 K, the orthorhombic aO and bO lattice parameters already merged, suggesting a phase transition to a tetragonal structure. The orthorhombic splitting of reflections also disappeared (Figure 4). Therefore, at 450 K and above, we used the P42/nmc model3 to obtain temperature dependence of the lattice parameters. The refined structural parameters and bond lengths at 600 K are summarized in Tables 3 and 4, and the fitting patterns are shown in the inset of Figure 1. The crystal structure of Dy2CuZnMn4O12 at 600 K is given in Figure 2b. We note that the Cu site could be split from the 2a site (with g = 1) to the 4c site (with g = 0.5) in the P42/nmc model.

Figure 3.

Figure 3

(a) Temperature dependence of the aO, bO, and aT lattice parameters of Dy2CuZnMn4O12 between 100 and 800 K. (b) Temperature dependence of the cO and cT lattice parameters (the left-hand axis) and the unit-cell volume (the right-hand axis) of Dy2CuZnMn4O12. Errors are smaller than the symbol sizes. αV is the volumetric coefficient of thermal expansion calculated between T = 450 K and T = 775 K. O, orthorhombic; T, tetragonal.

Figure 4.

Figure 4

Temperature dependence of the synchrotron X-ray powder diffraction patterns of Dy2CuZnMn4O12 from 100 to 450 K (between 6 and 30°). The inset shows details near the 040O, 400O, and 400T reflections to emphasize the disappearance of the orthorhombic (O) distortion. T, tetragonal.

Table 3. Structure Parameters of Dy2CuZnMn4O12 at 600 K from Synchrotron X-ray Powder Diffraction Dataa.

atom WP g x y z Biso2)
Dy 4d 1 0.25 0.25 0.22151(5) 0.788(8)
Cu 4c 0.5 0.75 0.25 0.7642(8) 1.04(7)
Zn 2b 1 0.75 0.25 0.25 0.83(5)
Mn 8e 1 0 0 0 0.500(10)
O1 8g 1 0.25 0.0629(5) –0.0362(5) 0.68(7)
O2 8g 1 0.25 0.5393(5) 0.5849(5) 1.08(9)
O3 8f 1 0.4395(4) x 0.25 1.51(9)
a

g is the occupation factor. Source: Synchrotron powder X-ray diffraction (λ = 0.61928 Å); used d-space range: from 0.4916 to 7.1 Å. Crystal system: tetragonal; space group: P42/nmc (no. 137, origin choice 2); Z = 2. Molecular weight: 865.6708 g/mol. a = 7.30342(1) Å, c = 7.75007(2) Å, and V = 413.3886(12) Å3; Rwp = 7.26%, Rp = 5.40%, RB = 4.78%, and RF = 3.97%; ρcal = 6.955 g/cm3.

Table 4. Bond Lengths (in Å; Below 2.8 Å), Bond Angles (in deg), Bond-Valence Sum (BVS), and Distortion Parameters of MnO6 (Δ) in Dy2CuZnMn4O12 at 600 Ka.

Dy–O1 × 2 2.323(4) Mn–O1 × 2 1.904(1)
Dy–O2 × 2 2.363(4) Mn–O2 × 2 1.962(2)
Dy–O1 × 2 2.420(4) Mn–O3 × 2 2.036(1)
Dy–O3 × 4 2.666(1) Δ(MnO6) 7.6 × 10–4
BVS(Dy3+) +3.19 BVS(Mn3+) +3.47
Cu–O3 × 4 1.960(4) Mn–O1–Mn × 2 147.15(6)
BVS(Cu2+) +1.87 Mn–O2–Mn × 2 137.08(6)
Zn–O2 × 4 2.002(4) Mn–O3–Mn × 2 144.25(6)
BVS(Zn2+) +1.79    

In the Pmmn model, there are two independent sites for the B cations, Mn1 (4c) and Mn2 (4d). The Mn1 and Mn2 sites have different BVS parameters of +3.29 and +3.72. More importantly, the Mn1 and Mn2 sites have very different octahedral distortion parameters of 22.6 × 10–4 and 1.4 × 10–4, respectively. These two facts give evidence that the Mn1 site should be occupied by Mn3+ cations resulting in a strong Jahn–Teller distortion of the Mn1O6 octahedron. The Mn2 site should be occupied by Mn4+ cations without strong Jahn–Teller distortions of the Mn2O6 octahedron. We note that BVS parameters for Mn3+ at B sites of perovskites (for example, in RMnO3 with strong Jahn–Teller distortions where Mn definitely has an oxidation state of +3)22,23 are often higher than expected (for example, +3.15 to +3.25). At 600 K in the P42/nmc model, there is one crystallographic site for the B cations. The BVS value of +3.47 was close to the expected average value of +3.5, and the octahedral distortion parameter had an intermediate value of 7.6 × 10–4, reflecting the statistical presence of 50% of Mn3+ cations. Therefore, we conclude that a charge-order (CO) structure is realized below TCO = 425 K. Figure 5 shows temperature dependence of the Mn–O, Cu–O, and Zn–O bond lengths. The Mn1–O1 bond shows a tendency for a gradual decrease with increasing temperature, and the Mn2–O1 and Mn–O1 bonds show a tendency for a gradual increase. Other bonds were nearly temperature independent within the sensitivity of the structural analysis based on synchrotron powder X-ray diffraction.

Figure 5.

Figure 5

Temperature dependence of (a) the Mn–O bond lengths and (b) the Cu–O and Zn–O bond lengths in Dy2CuZnMn4O12.

No DSC anomalies were detected near TCO = 425 K (Figure S2 of the Supporting Information). The temperature dependence of the unit cell volume (Figure 3b) shows no anomalies between 100 and 800 K. The orthorhombic aO and bO lattice parameters merge gradually when approaching TCO = 425 K. All of these observations suggest that the structural phase transition at TCO = 425 K is of the second order.

The orthorhombic aO and bO lattice parameters and tetragonal aT lattice parameter monotonically increase with temperature from 100 to 800 K (Figure 3). On the other hand, the orthorhombic cO lattice parameter slightly increases from 100 to 280 K and then decreases from 280 to 800 K (as cT above 425 K). Therefore, Dy2CuZnMn4O12 demonstrates anisotropic thermal expansion above 280 K. As shown in Figure 5, no detectable anomalies were observed on temperature dependence of the bond lengths. Therefore, the origin of the anisotropic thermal expansion is not clear at the moment. Neutron diffraction studies, which can locate oxygen atoms more accurately, will be needed to understand the structural evolution of Dy2CuZnMn4O12 with temperature more precisely.

Temperature-driven structural phase transitions in A2A′A″B4O12 perovskites have only been discovered so far in CaMnTi2O67 and CaMnTi2–xVxO68 during a ferroelectric-paraelectric phase transition (P42mcP42/nmc). The discovery of a charge-order transition in Dy2CuZnMn4O12 (PmmnP42/nmc) could suggest the existence of such temperature-driven transitions in other A2A′A″B4O12 perovskites that crystallize in space group Pmmn at room temperature (e.g., RMn3O610,11 and R2CuMnMn4O12).12 High-temperature DSC experiments were performed in the case of RMn3O6,10 but no anomalies were detected. Therefore, it was concluded that RMn3O6 does not show charge-order transitions up to 873 K. Our current results give evidence that such transitions could not be detected by DSC, and direct high-temperature structural studies are needed to discover such transitions.

FCC magnetic susceptibilities showed sharp rises below TC = 116 K in a small applied magnetic field of 100 Oe, suggesting the development of a strong ferromagnetic (FM) component (Figure 6) with additional, gradual rises below about 45 K. The additional anomalies could be more clearly seen on the ZFC curve and on the differential dχT/dT versus T curves (Figure S3). At H = 100 Oe, a difference between the ZFC and FCC χ versus T curves was observed below TC. At H = 10 kOe, almost no difference was detected between the ZFC and FCC χ versus T curves. The χ–1 versus T curves followed the Curie–Weiss law, and a fit by the law between 300 and 400 K gave a positive Curie–Weiss temperature, θ = +125 K, indicating predominantly FM interactions between magnetic ions. The calculated effective magnetic moment (μcalc) is 17.485μB (for the calculation we used 10.6μB for Dy3+, 4.899μB for Mn3+, 3.873μB for Mn4+, and 1.732μB for Cu2+ and an equation μcalc2 = 2 μDy2 + 2 μMn(III)2 + 2 μMn(IV)2 + μCu2). The experimental effective magnetic moment was about 9% smaller (μeff = 15.99μB). While the origin of this reduction is not clear at the moment, the same tendency was observed for all other members of the R2CuZnMn4O12 (for example, μcalc = 9.00μB versus μeff = 8.29μB for R = Lu) and R2CuGaMn4O12 series.3

Figure 6.

Figure 6

Left-hand axis presents ZFC (filled symbols) and FCC (empty symbols) dc magnetic susceptibility (χ = M/H) curves of Dy2CuZnMn4O12 measured at 100 Oe and 10 kOe (multiplied by 10). Right-hand axis shows the FCC χ–1 versus T curves at 10 kOe with the Curie–Weiss fit (black line). Parameters of the fit are shown on the figure.

Temperature dependence of magnetic susceptibilities of Dy2CuZnMn4O12 was qualitatively similar to that of the parent Dy2MnMnMn4O12 (= DyMn3O6).10 But the absolute values of magnetic susceptibilities were about 10 times larger in Dy2CuZnMn4O12 at both H = 100 Oe and 10 kOe. This fact suggests that the ordered moments in Dy2CuZnMn4O12 were much larger than those of Dy2MnMnMn4O12. Recent neutron diffraction studies found that the ordered moments were significantly reduced (in comparison with the expected full moments) in an isostructural compound Y2MnMnMn4O12 due to competing exchange interactions, and there was a competition between antiferromagnetic and ferrimagnetic ground states.24 The magnetic frustration could be reduced through the introduction of nonmagnetic Zn2+ cations into the A″ site in Dy2CuZnMn4O12 and through the full charge ordering of Mn3+ and Mn4+, resulting in larger ordered magnetic moments. The gradual rise of magnetic susceptibilities below 45 K could be caused by the gradual increase of the ordered moments of the Dy3+ sublattices, but it was difficult (from the available data) to determine at what temperature the Dy3+ sublattices start to order.

On the other hand, temperature dependence of magnetic susceptibilities of Dy2CuZnMn4O12 was different from that of Dy2CuMnMn4O12 at small magnetic fields and at temperatures below about 40 K.12 In Dy2CuMnMn4O12, magnetic susceptibilities decreased at low temperatures. This fact suggests different magnetic structures for these two compounds. The magnetic susceptibility behavior of Dy2CuMnMn4O12 was consistent with the determined magnetic structure, where the Dy1 and Dy2 sublattices order antiferromagnetically relative to each other but with different magnitudes, and the resulting uncompensated moment on the Dy sublattices aligns antiferromagnetically relative to the FM Mn sublattices.12

Isothermal magnetization measurements (Figure 7) showed a behavior typical for soft ferrimagnets with a coercive field, HC, of about 200 Oe at T = 5 K and a large saturation magnetization, MS, of about 25.6μB (at T = 5 K and H = 70 kOe). The near saturation value was already observed from about H = 20 kOe. This saturation value is smaller than the full magnetization of 35μB expected for a full FM alignment (using the maximum value of 10 μB for Dy3+). On the other hand, Dy3+ cations have a noticeable single-ion anisotropy; therefore, the full moment of Dy3+ cannot be reached in powder samples. Magnetic structures of related compounds, Dy2CuMnMn4O12 and Y2CuGaMn4O12, were investigated by neutron diffraction. It was found that the B-site Mn sublattices are ordered ferromagnetically but with reduced magnetic moments (2.2μB per Mn in Y2CuGaMn4O12 and 2.5μB per Mn4+ and 3.3μB per Mn3+ in Dy2CuMnMn4O12). Considering uncertainties in ordered moments on the Dy and Mn sublattices, the maximum contribution of 1μB from the Cu sublattice of Dy2CuZnMn4O12 can be neglected in the discussion below.

Figure 7.

Figure 7

M versus H curves of Dy2CuZnMn4O12 at 5, 25, 60, and 100 K (f.u.: formula unit). The left-hand inset compares M versus H curves of Dy2CuZnMn4O12 and Lu2CuZnMn4O12 at 5 K. The right-hand inset compares M versus H curves of Dy2CuZnMn4O12 and Dy2MnMnMn4O1210 at 5 K. MS is the magnetization value at H = 70 kOe and T = 5 K.

MS was about 9.5μB (at T = 5 K) in a related compound without magnetic rare-earth cations, Lu2CuZnMn4O12 (the inset of Figure 7), given an average moment of 2.4μB per Mn, which is close to the experimentally determined values in the related compounds. Assuming a similar magnetic structure with similar ordered moments at the B sublattices in Dy2CuZnMn4O12 and Lu2CuZnMn4O12, the difference in the MS values could be attributed to the Dy3+ sublattices. The difference was about 16μB, which was significantly larger than the maximum Dy3+ ordered moment. This fact suggests that both Dy3+ sublattices (Dy1 and Dy2) give FM contributions to the magnetic structure with an average value of 8μB. Therefore, M versus H curves of Dy2CuZnMn4O12 (and comparison with the related compounds) suggest that the Mn1 and Mn2 sublattices are ordered ferromagnetically and the Dy1 and Dy2 sublattices are ordered ferromagnetically relative to each other and to the Mn sublattices.

4. Conclusions

In conclusion, we prepared a new member of the A-site columnar-ordered quadruple perovskites, Dy2CuZnMn4O12, which crystallizes in the charge-order structure at room temperature with Pmmn symmetry. Using direct high-temperature structural studies, we could detect a charge-disorder transition above 425 K, while other methods could not detect such a transition. Triple A-site cation ordering was realized through a new combination of the A/A′/A″ cations (Dy3+/Cu2+/Zn2+). Dy2CuZnMn4O12 exhibits a ferrimagnetic transition below 116 K with a large saturation magnetization and involvement of the Dy3+ sublattices at low temperatures.

Acknowledgments

The synchrotron radiation experiments were performed at SPring-8 with the approval of Japan Synchrotron Radiation Research Institute (proposal numbers: 2023A1496 and 2023A2361). We thank Dr. S. Kobayashi for his help at BL02B2 of SPring-8.

Supporting Information Available

The Supporting Information is available free of charge at https://pubs.acs.org/doi/10.1021/acs.inorgchem.3c02835.

  • Bond distances of Dy2CuZnMn4O12 at 100 K, DSC curves, details of M vs H curves, M vs T curves, and differential magnetic susceptibility curves, ac magnetic susceptibility curves, and a photograph of the as-synthesized powder (PDF)

The author declares no competing financial interest.

Supplementary Material

ic3c02835_si_001.pdf (423.1KB, pdf)

References

  1. Belik A. A. Rise of A-site Columnar-Ordered A2A′A″B4O12 Quadruple Perovskites with Intrinsic Triple Order. Dalton Trans. 2018, 47, 3209–3217. 10.1039/C7DT04490A. [DOI] [PubMed] [Google Scholar]
  2. Liu R.; Khalyavin D. D.; Tsunoda N.; Kumagai Y.; Oba F.; Katsuya Y.; Tanaka M.; Yamaura K.; Belik A. A. Spin-Glass Magnetic Properties of A-Site Columnar-Ordered Quadruple Perovskites Y2MnGa(Mn4–xGax)O12 with 0 ≤ x ≤ 3. Inorg. Chem. 2019, 58, 14830–14841. 10.1021/acs.inorgchem.9b02542. [DOI] [PubMed] [Google Scholar]
  3. Belik A. A.; Khalyavin D. D.; Matsushita Y.; Yamaura K. Triple A-site Cation Ordering in the Ferrimagnetic Y2CuGaMn4O12 Perovskite. Inorg. Chem. 2022, 61, 14428–14435. 10.1021/acs.inorgchem.2c02343. [DOI] [PMC free article] [PubMed] [Google Scholar]
  4. Belik A. A.; Liu R.; Yamaura K. Spin-glass to Long-range Order to Spin-glass Evolution of Magnetic Properties with the Composition in Sm2MnZnMn4–xTixO12 (x = 1, 2, and 3) Perovskites. J. Alloys Compd. 2023, 932, 167727 10.1016/j.jallcom.2022.167727. [DOI] [Google Scholar]
  5. Belik A. A.; Liu R.; Yamaura K. Realization of Triple A-site Cation Ordering through the Dy/Mn/Zn Combination in the Ferrimagnetic Dy2MnZnMn4–xTixO12 Perovskites. Ceram. Int. 2023, 49, 14327–14334. 10.1016/j.ceramint.2023.01.019. [DOI] [Google Scholar]
  6. Azuma M.; Yamada I.; Yamaura K.; Belik A. A.; Yamamoto T.; Fukuda M.. 4.20 - High Pressure Studies of Transition Metal Oxides. In Comprehensive Inorganic Chemistry III, 3rd ed.; Reedijk J., Poeppelmeier K. R., Eds.; Elsevier: Oxford, 2023; pp 681–718. 10.1016/B978-0-12-823144-9.00141-2. [DOI] [Google Scholar]
  7. Aimi A.; Mori D.; Hiraki K.; Takahashi T.; Shan Y. J.; Shirako Y.; Zhou J. S.; Inaguma Y. High-Pressure Synthesis of A-site Ordered Double Perovskite CaMnTi2O6 and Ferroelectricity Driven by Coupling of A-site Ordering and the Second-order Jahn–Teller Effect. Chem. Mater. 2014, 26, 2601–2608. 10.1021/cm500016z. [DOI] [Google Scholar]
  8. Fukuda M.; Nishikubo T.; Pan Z.; Sakai Y.; Zhang M.-H.; Kawaguchi S.; Yu H.; Okimoto Y.; Koshihara S.-Y.; Itoh M.; Rödel J.; Azuma M. Enhanced Spontaneous Polarization by V4+ Substitution in a Lead-Free Perovskite CaMnTi2O6. Inorg. Chem. 2020, 59, 11749–11756. 10.1021/acs.inorgchem.0c01697. [DOI] [PubMed] [Google Scholar]
  9. Scatena R.; Liu R.; Shvartsman V. V.; Khalyavin D. D.; Inaguma Y.; Yamaura K.; Belik A. A.; Johnson R. D. Hybrid Improper Ferroelectricity in Columnar (NaY)MnMnTi4O12. Angew. Chem., Int. Ed. 2023, 62, e202305994 10.1002/anie.202305994. [DOI] [PubMed] [Google Scholar]
  10. Zhang L.; Matsushita Y.; Yamaura K.; Belik A. A. Five-fold Ordering in High-pressure Provskites RMn3O6 (R = Gd-Tm and Y). Inorg. Chem. 2017, 56, 5210–5218. 10.1021/acs.inorgchem.7b00347. [DOI] [PubMed] [Google Scholar]
  11. Belik A. A.; Zhang L.; Matsushita Y.; Katsuya Y.; Tanaka M.; Yamaura K. Crystal Structures of Cation Non-stoichiometric RMn3O6 (R = Gd, Er, and Tm) Manganites Belonging to A-site Columnar-ordered Quadruple Perovskite Family. J. Solid State Chem. 2019, 275, 43–48. 10.1016/j.jssc.2019.04.004. [DOI] [Google Scholar]
  12. Vibhakar A. M.; Khalyavin D. D.; Manuel P.; Liu J.; Belik A. A.; Johnson R. D. Spontaneous Rotation of Ferrimagnetism Driven by Antiferromagnetic Spin Canting. Phys. Rev. Lett. 2020, 124, 127201 10.1103/PhysRevLett.124.127201. [DOI] [PubMed] [Google Scholar]
  13. Salamon M. B.; Jaime M. The Physics of Magnanites: Structure and Transport. Rev. Mod. Phys. 2001, 73, 583–628. 10.1103/RevModPhys.73.583. [DOI] [Google Scholar]
  14. Yamada I. High-pressure Synthesis, Electronic States, and Structure-property Relationships of Perovskite Oxides, ACu3Fe4O12 (A: Divalent Alkaline Earth or Trivalent Rare-earth Ion). J. Ceram. Soc. Jpn. 2014, 122, 846–851. 10.2109/jcersj2.122.846. [DOI] [Google Scholar]
  15. Decker D. L.; Vanfleet H. B. Melting and High-temperature Electrical Resistance of Gold under Pressure. Phys. Rev. 1965, 138, A129–A133. 10.1103/PhysRev.138.A129. [DOI] [Google Scholar]
  16. Kawaguchi S.; Takemoto M.; Osaka K.; Nishibori E.; Moriyoshi C.; Kubota Y.; Kuroiwa Y.; Sugimoto K. High-throughput Powder Diffraction Measurement System Consisting of Multiple MYTHEN Detectors at Beamline BL02B2 of SPring-8. Rev. Sci. Instrum. 2017, 88, 085111 10.1063/1.4999454. [DOI] [PubMed] [Google Scholar]
  17. Izumi F.; Ikeda T. A Rietveld-analysis Program RIETAN-98 and its Applications to Zeolites. Mater. Sci. Forum 2000, 321–324, 198–205. 10.4028/www.scientific.net/MSF.321-324.198. [DOI] [Google Scholar]
  18. Waroquiers D.; Gonze X.; Rignanese G.-M; Welker-Nieuwoudt C.; Rosowski F.; Göbel M.; Schenk S.; Degelmann P.; André R.; Glaum R.; Hautier G. Statistical Analysis of Coordination Environments in Oxides. Chem. Mater. 2017, 29, 8346–8360. 10.1021/acs.chemmater.7b02766. [DOI] [Google Scholar]
  19. Fukuda M.; Nishikubo T.; Yu H. W.; Okimoto Y.; Koshihara S.-Y.; Yamaura K.; Azuma M. A-Site Columnar-Ordered Perovskite CaZnV2O6 as a Pauli-Paramagnetic Metal. Inorg. Chem. 2023, 62, 8372–8378. 10.1021/acs.inorgchem.3c00940. [DOI] [PubMed] [Google Scholar]
  20. Solana-Madruga E.; Kearins P. S.; Ritter C.; Arévalo-López Á. M.; Attfield J. P. 1:1 Ca2+:Cu2+ A-site Order in a Ferrimagnetic Double Double Perovskite. Angew. Chem., Int. Ed. 2022, 61, e202209497 10.1002/anie.202209497. [DOI] [PMC free article] [PubMed] [Google Scholar]
  21. Brese N. E.; O’Keeffe M. Bond-valence Parameters for Solids. Acta Crystallogr., Sect. B: Struct. Sci. 1991, 47, 192–197. 10.1107/S0108768190011041. [DOI] [Google Scholar]
  22. Alonso J. A.; Martinez-Lope M. J.; Casais M. T.; Fernandez-Diaz M. T. Evolution of the Jahn-Teller Distortion of MnO6 Octahedra in RMnO3 Perovskites (R = Pr, Nd, Dy, Tb, Ho, Er, Y): A Neutron Diffraction Study. Inorg. Chem. 2000, 39, 917–923. 10.1021/ic990921e. [DOI] [PubMed] [Google Scholar]
  23. Tachibana M.; Shimoyama T.; Kawaji H.; Atake T.; Takayama-Muromachi E. Jahn-Teller Distortion and Magnetic Transitions in Perovskite RMnO3 (R = Ho, Er, Tm, Yb, and Lu). Phys. Rev. B: Condens. Matter Mater. Phys. 2007, 75, 144425 10.1103/PhysRevB.75.144425. [DOI] [Google Scholar]
  24. Vibhakar A. M.; Khalyavin D. D.; Manuel P.; Steinke N. J.; Zhang L.; Yamaura K.; Belik A. A.; Johnson R. D. Magnetic Inhomogeneities in the Quadruple Perovskite Manganite [Y2–xMnx]Mn6O12. Phys. Rev. B: Condens. Matter Mater. Phys. 2023, 108, 054403 10.1103/PhysRevB.108.054403. [DOI] [Google Scholar]

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Supplementary Materials

ic3c02835_si_001.pdf (423.1KB, pdf)

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