Federico
Serrano-Sánchez
a,
José Luis
Martínez
a,
François
Fauth
b and
José Antonio
Alonso
*a
aInstituto de Ciencia de Materiales de Madrid (ICMM), Consejo Superior de Investigaciones Científicas (CSIC), Sor Juana Inés de la Cruz 3, E-28049, Madrid, Spain. E-mail: ja.alonso@icmm.csic.es
bCELLS–ALBA Synchrotron, Cerdanyola del Valles, Barcelona, E-08290, Spain
First published on 16th April 2021
Rare-earth nickelates RNiO3 (R = Y, La⋯Lu) are electron-correlated perovskite materials where the interplay between charge and spin order results in a rich phase diagram, evolving from antiferromagnetic insulators to paramagnetic metals. They are well-known to undergo metal–insulator (MI) transitions as a function of temperature and the size of the rare-earth ion. For intermediate-size Eu3+ and Gd3+ ions, the MI transitions are described to happen at TMI = 463 K and 511 K, respectively. We have investigated their structural evolution across TMI with the excellent angular resolution of synchrotron X-ray diffraction, using high-crystalline quality samples prepared at elevated hydrostatic pressures. Unlike YNiO3, synthesized and measured under the same conditions, exhibiting a characteristic monoclinic phase (space group P21/n) in the insulating regime (below TMI), the present EuNiO3 and GdNiO3 samples do not exhibit such a symmetry, but their crystal structures can be defined in an orthorhombic superstructure of perovskite (space group Pbnm) in all the temperature interval, between 100 and 623 K for Eu and 298 K and 650 K for Gd. Nevertheless, an abrupt evolution of the unit-cell parameters is observed upon metallization above TMI. A prior report of a charge disproportionation effect by Mössbauer spectroscopy on Fe-doped perovskite samples seems to suggest that the distribution of two distinct Ni sites must not exhibit the required long-range ordering to be effectively detected by diffraction methods. An abrupt contraction of the b parameter of EuNiO3 in the 175–200 K range, coincident with the onset of antiferromagnetic ordering, suggests a magnetoelastic coupling, not described so far in rare-earth nickelates. The magnetic susceptibility is dominated by the paramagnetic signal of the rare-earth ions; however, the AC susceptibility curves yield a Néel temperature corresponding to the antiferromagnetic ordering of the Ni moments of TN = 197 K for EuNiO3, corroborated by specific heat measurements. For GdNiO3, a χT vs. T plot presents a clear change in the slope at TN = 187 K, also consistent with specific heat data. Magnetization measurements at 2 K under large fields up to 14 T show a complete saturation of the magnetic moments with a rather high ordered moment of 7.5μB per f.u.
The high-temperature Pbnm orthorhombic structure of RNiO3 (R = Pr → Lu) perovskites undergoes a reversible metallic to insulator (MI) transition, the temperature of which (TMI) increases along the rare earth series from PrNiO3 (TMI = 130 K) to LuNiO3 (TMI = 600 K). The LaNiO3 system behaves differently, as it displays a rhombohedral R-3c structure and solely a metallic behavior. This behavior is driven by the overlap of the Ni (3d) and O (2p) orbitals depending on R3+ cationic radius, which determines the p–d Ni–O bond length and octahedral Ni–Ô–Ni tilting angle.5,9 The structural parameters define the tolerance factor of the perovskite as t = dR–O/√2dNi–O, which has shown to be a determining factor of the valence bandwidth, and thus, the MI transition and magnetic behavior.
After thorough experimental and theoretical investigations, the exact mechanisms underlying the MI transition are still under discussion.10 Initially, the electronic localization was explained by a charge disproportionation into two different Ni sites as Ni3+ → Ni(3−δ)+ + Ni(3+δ)+ through the transition to the insulating regime.4,11–15 In this regime, the perovskite structure displays large and small octahedra with different average Ni–O bond lengths, which is realized in a monoclinic crystal structure defined in the P21/n space group. This is described as a breathing-like distortion in which the charge disproportionation removes the Ni electronic state degeneracy, opening a band gap. More recently, another related description places positive charges in the oxygen p-orbitals, with the electronic configuration of Ni2+ 3d8L in the metallic state and 3d8L2 + 3d8 in the insulating phase, with L denoting a positive charge held by the oxygen ligands, leaving the Ni valence state virtually the same in both octahedra.13,16,17 This explanation is named bond disproportionation and is based on the strong covalent character of the Ni–O bonds and the major contribution of the oxygen p-orbitals to the valence band top. Both descriptions include the distortion of the NiO6 octahedra and a charge rearrangement within the structure. Bond disproportionation has proven to be a good physical description to capture the basic properties using theoretical approaches,18 while many studies have reported experimental proof of the differently charged octahedral environment in the whole RNiO3 series, using X-ray absorption spectroscopy (XAS),19 Resonant X-Ray scattering,20 and Raman21 and Mössbauer spectroscopy.14 Moreover, similar electronic and magnetic structures have been observed for the series by soft X-ray magnetic diffraction,22 indicating the analogous behavior of the insulating phase.
The antiferromagnetic ordering at low temperature is also dependent on the size of R3+ cations as the Néel temperature TN is simultaneous with the MI transition for large R cations (R = Pr–Nd), while for the rest of the series (R = Sm–Lu), TN is well below TMI. This indicates that the MI transition is not associated with the onset of AF ordering. On the other hand, the occurrence of noticeable 16O–18O isotope shifts of TMI in RNiO3 (R = Pr, Nd, Sm and Eu) establishes the significance of electron–lattice coupling in these oxides.23 Soft X-ray and magnetic neutron diffraction experiments have described a non-collinear stacking of alternate up–up–down–down Ni spins along the propagation vector k = (1/2, 0, 1/2).22,24 Furthermore, magnetic rare-earth elements may display long-range ordering, as in HoNiO3.25
In the small RNiO3 (R = Y, Dy → Lu) derivatives, a structural transition accompanying the MI transition has been described by neutron and high-angular resolution X-ray diffraction. As mentioned, the orthorhombic high-temperature structure distorts into a monoclinic P21n structure,4,11,12,15,26,27 yielding the two differentiated Ni octahedra with long-range periodic order described as a breathing distortion. The experimental observations of the charge disproportionation suggest that this distortion is present in the insulating phase of the whole rare earth series.22 However, for larger RNiO3 (R = Pr → Gd), the structural transition had not been identified.
The metastable character of EuNiO3 has made it difficult to investigate.3,6,28 It presents a clear gap between the MI (TMI = 463 K) and antiferromagnetic transition (TN = 220 K). Neither the low temperature phase structure nor the magnetic properties of this compound have been reported. GdNiO3 has been studied and prepared under high O2 pressure conditions, showing no signs of monoclinic distortion below TMI = 510 K, with TN = 185 K.7 Besides, a large absorption cross section of Eu and Gd makes difficult any neutron diffraction characterization.
Recently, we described the structural transition to the monoclinic phase of SmNiO3, owing to an excellent crystallinity of the samples prepared at 3.5 GPa under oxidizing conditions, combined with high-angular resolution diffraction experiments.29 These allowed us to identify a monoclinic insulating phase and the subtle changes in the crystal structure across the transition. In the present study, an identical high-pressure preparation (3.5 GPa) of pure EuNiO3 and GdNiO3 perovskites is reported, along with a detailed diffraction study of the crystalline structure above and below the TMI using high-angular resolution synchrotron X-ray diffraction. Even though the monoclinic structure is not observed, a sharp variation of the structural parameters occurs at TMI. This indicates that the charge disproportionation preliminary observed by Mössbauer spectroscopy31,32 is a local phenomenon and there is no long-range order of the NiO6 octahedra. This structural study is complemented with the examination under the same diffraction conditions of YNiO3, providing with a reference of a compound that indeed experiences an orthorhombic-to-monoclinic transition across TMI. Finally, the susceptibility and heat capacity measurements of GdNiO3 and EuNiO3 perovskites are reported, showing for the first time some anomalies at the thermal evolution of the structural parameters of the Eu compound across TN, suggesting a magneto-elastic behavior.
The nature of the resulting powder was assessed by laboratory X-ray diffraction (XRD) using a Bruker-AXS D8 diffractometer (40 kV, 30 mA), with Cu Kα radiation (λ = 1.5418 Å). The Synchrotron X-ray diffraction (SXRD) experiments were carried out in the transmission mode on the BL04-MSPD beamline of the ALBA synchrotron (Barcelona, Spain) using the highest angular resolution mode as provided by the MAD setup.30 The RNiO3 oxides were sealed in 0.7 mm diameter quartz capillaries that were rotating during the acquisition time to increase powder averaging. The beam energy was 28 keV (λ = 0.4427 Å) for R = Gd and Y and 32 keV (λ = 0.38776 Å) for R = Eu, selected to minimize absorption. Room temperature (RT, 298 K) patterns were collected for the three samples; then sequential SXRD patterns were collected at 100, 150, 200, 250, 295, 350, 373, 423, 448, 473, 498, 523, 573 and 623 K for EuNiO3 and 298, 400, 450, 277, 550 and 650 K for GdNiO3.
The analysis of the SXRD data was performed by the Rietveld method, using the FullProf Suite. The diffraction peak shape was defined by a pseudo-Voight function; a linear interpolation between points devoid of reflections was considered as the background. The final refinement included the scale factor, zero-point shift, width and asymmetry parameters, unit-cell parameters, atomic positions and isotropic displacement factors. No regions were excluded from the refinements.
Magnetic susceptibility was measured using a SQUID Magnetometer from Quantum Design (QD, USA) model MPMS-XL in the range of 1.8 K to 400 K and magnetic fields up to 5 T. Complementary data on magnetization at high magnetic fields (14 T) and AC magnetic susceptibility were performed in using the VSM and AC options of the PPMS system from QD. Heat capacity measurements in the range 1.8 K to 300 K at different applied external magnetic fields (up to 9 T) were measured using the PPMS system with a heat pulse method.
For YNiO3, the RT SXRD pattern clearly enables the visualization of typical reflection splitting suggesting a monoclinic symmetry. Fig. 1a shows the characteristic (−224)/(224) splitting observed in YNiO3, where these two peaks are perfectly resolved, whereas for GdNiO3 a single peak is observed for this reflection. As a reference, the subtle splitting recently described for SmNiO329 is also included in the figure; these three samples were collected with the same wavelength (λ = 0.4427 Å).
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Fig. 1 (a) Characteristic splitting (−224)/(224) observed for YNiO3 at RT shown in a region of the SXRD patterns of YNiO3 and GdNiO3 as a function of 2θ, in comparison with that detected for SmNiO3 (from ref. 29), and the absence of splitting experienced by GdNiO3 for the same reflection. b) Selected region of the SXRD patterns of EuNiO3 and GdNiO3 represented as a function of Q (Å−1), highlighting the (224) reflection, illustrating a similar width and the absence of the splitting characteristic of the monoclinic symmetry. |
A second related figure (Fig. 1b) is necessary to include together the data of GdNiO3 and EuNiO3, since this last pattern was collected at a different energy and wavelength (λ = 0.38776 Å); in this figure a representation as a function of Q (Å−1) is utilized. Fig. 2 shows that the characteristic (224) reflection is not apparently split, and a comparable peak width manifesting a similar degree of crystallization is observed.
In consequence, while for YNiO3 the refinement of the crystal structure from the SXRD data at RT (in the insulating regime) was performed in the monoclinic space group P21/n, as previously reported from the neutron data,4,11 the preliminary trials in the mentioned symmetry for EuNiO3 and GdNiO3 were unsuccessful, yielding almost negligible monoclinic distortions (monoclinic β angles below 90.01°) and negative thermal factors for some Ni or oxygen atoms. Therefore, the orthorhombic space group Pbnm was considered at RT for EuNiO3 and GdNiO3. Fig. 2 shows the diffraction patterns after the Rietveld fit at room temperature for these two samples. As mentioned, for YNiO3 the excellent crystallinity together with the outstanding angular resolution of MSPD diffractometer yielded extremely narrow peaks (half-maximum width of typically FWHM = 0.01° at 12° 2θ), which were essential to discern the structural distortion associated with the charge disproportionation effect in this case. Therefore, only for YNiO3 at RT the superstructure of perovskite is defined in the monoclinic space group P21/n, with unit-cell parameters related to that of the aristotype a0 as a0 ≈ √2a0, b ≈ √2a0 and c ≈ 2a0. This model contains two different Ni atoms, Ni1 and Ni2, located at 2d and 2c sites, respectively, and three O atoms, O1, O2 and O3, located at the 4e general crystallographic positions. The structural parameters are detailed at the ESI in Table S1.† The Rietveld plot for YNiO3 at RT is also included in the ESI as Fig. S1.† The same attributes regarding the crystallinity and resolution (FWHM = 0.01° at 12° 2θ) also helped to demonstrate that EuNiO3 and GdNiO3 must be described as orthorhombic at RT.
In the orthorhombic model utilized to refine the structure for the Eu and Gd counterparts at RT, defined in the Pbnm space group, there is a unique Ni atom at 4b positions and two O1 and O2 atoms at 4c and 8b Wyckoff sites, respectively; Eu and Gd are also located at 4c sites. The structural parameters at RT are included in Table 1.
EuNiO3Pbnm | GdNiO3Pbnm | ||||
---|---|---|---|---|---|
Temperature (K) | 100 | 300 | 623 | 303 | 650 |
a (Å) | 5.28107(3) | 5.29060(3) | 5.31271(4) | 5.25967 | 5.28467(2) |
b (Å) | 5.46653(3) | 5.46506(3) | 5.46064(4) | 5.49015 | 5.49062(2) |
c (Å) | 7.52227(4) | 7.53586(5) | 7.55499(5) | 7.51213 | 7.53257(3) |
V (Å3) | 217.161(2) | 217.888(2) | 219.176(3) | 216.923(1) | 218.566(1) |
R 4c (x y ¼) | |||||
x | 0.9865(2) | 0.9870(2) | 0.9882(2) | 0.9852(1) | 0.9861(1) |
y | 0.0596(1) | 0.0584(2) | 0.0551(2) | 0.0631(1) | 0.0602(1) |
B iso (Å2) | 0.38 (2) | 0.60(2) | 0.99(2) | 0.26(1) | 0.73(1) |
O1 4c (x y ¼) | |||||
X | 0.083(2) | 0.082(3) | 0.078(2) | 0.087(2) | 0.086(2) |
Y | 0.478(2) | 0.480(2) | 0.478(2) | 0.475(1) | 0.476(2) |
B iso (Å2) | 0.61(2) | 1.1 (3) | 1.7(3) | 0.1(2) | 0.8(2) |
O2 8d (x y z) | |||||
x | 0.705(1) | 0.705(2) | 0.708(2) | 0.700(1) | 0.704(1) |
y | 0.295(1) | 0.297(2) | 0.301(2) | 0.297(1) | 0.299(1) |
z | 0.0468(9) | 0.046(1) | 0.045(1) | 0.0466(9) | 0.0445(8) |
B iso (Å2) | 0.02(20) | 0.1(1) | 0.1(2) | 0.5(1) | 0.5(1) |
Ni1 4b (½ 0 0) | |||||
B iso (Å2) | 0.37(4) | 0.52(4) | 0.64(4) | 0.25(3) | 0.52(3) |
Reliability factors | |||||
R I (%) | 6.11 | 5.97 | 5.97 | 3.82 | 3.67 |
R p (%) | 15.4 | 15.2 | 16.6 | 12.7 | 12.1 |
R wp (%) | 21.5 | 20.5 | 21.1 | 16.0 | 14.8 |
R exp (%) | 8.94 | 9.22 | 9.55 | 7.47 | 8.09 |
χ 2 | 5.79 | 4.95 | 4.87 | 4.59 | 3.36 |
The thermal evolution of the structural parameters of EuNiO3 and GdNiO3 has been studied across the metal-to-insulator transition (Fig. 3 and 4). In the case of Eu, the SXRD data could also be collected below RT, across the antiferromagnetic-ordering transition, occurring at TN = 220 K.28 The crystal structure for both compounds was refined in the orthorhombic crystallographic model in all the temperature interval. Fig. 3 illustrates the goodness of the fit for the high-temperature patterns, e.g. 623 K for EuNiO3 and 650 K for GdNiO3. Fig. 3a shows that, for EuNiO3, the a unit-cell parameter steadily increases for the whole temperature range 100–600 K, while b experiences a non-monotonic evolution with two anomalies: the former at about 175–200 K, coincident with the magnetic ordering temperature, and the second anomaly includes an abrupt contraction and, then, an expansion, concomitant with the MI transition, happening at TMI = 463 K.6Fig. 3c displays a similar contraction and then expansion of the c axis at the same characteristic temperature, across the phase transition upon entering the metallic regime. As a result of that evolution, the volume also exhibits a characteristic contraction; the calculated superimposed volume contraction is ΔV/V = 0.12%, which is of the same order of magnitude as those observed for other rare-earth nickelates upon metallization. For GdNiO3, a less detailed temperature-dependent data collection could be performed, but basically the same overall evolution of the unit-cell parameters across the MI transition (TMI = 511 K (ref. 7)) is observed, as illustrated in Fig. 4; the continuous expansion of the a parameter is accompanied by a non-monotonic contraction and then expansion in b and c parameters, as well as the unit-cell volume.
Therefore, we have verified by high-angular resolution diffraction tools that EuNiO3 and GdNiO3, prepared under the same high-pressure conditions as those of YNiO3 and SmNiO329 and exhibiting a comparable degree of crystallinity (as evaluated by the similar width of the diffraction peaks), do not offer evidence of a monoclinic distortion below TMI, in the insulating region, unlike those previously observed for SmNiO3,29 YNiO34,11,12 and other small rare-earth nickelates.4,12,27 This is in contrast with the previous results of Mössbauer spectroscopy of 57Fe-doped samples of EuNiO3 and GdNiO3, yielding evidence of the existence of two different environments for Fe, from what it was concluded that a charge disproportionation effect at the Ni sites was active in the insulation phases of these perovskites.31,32 This result is, of course, an indirect evidence for the existence of two types of nickel positions in the insulating state of nickelate RNiO3 lattices.32 The present results, clearly indicating that an orthorhombic symmetry must be considered in all the temperature range, seem to suggest that the distribution of two distinct Ni sites must not exhibit the required long-range ordering to be effectively detected by diffraction methods. In these Fe-doped samples, it is conceivable that the two Fe sites, and therefore the Ni sites to which they replace, could be distributed at random within the crystallographic lattice, not providing with the essential coherence to unveil the characteristic features (either at the unit-cell parameters, and namely the monoclinic beta angle, as well as the internal symmetry necessary to define two distinct environments for Ni atoms) of an ordered charge-disproportionated state. The reason why EuNiO3 and GdNiO3 exhibit the proposed disordered charge disproportionation, while the neighboring SmNiO3 perovskite is ordered, is uncertain, although it could be related to the nature of the rare-earth ion.
It is certainly remarkable that both GdNiO3 and EuNiO3, placed at the middle of the rare-earth series, exhibit a distinct behavior concerning the absence of long-range ordering detectable by diffraction methods. For Gd3+, the 4f orbitals are half-filled (4f7 configuration), hence particularly stable. As such, f–f transitions are not possible (this is the reason why this ion does not absorb any wavelength, and hence it is colourless). At the same time, Gd3+ is strongly paramagnetic, and the anisotropic nature of the Gd–Gd interactions may account for a homogeneous molecular field on the Ni sites. It is undeniable that the local molecular field of the rare-earth ions on neighboring Ni atoms may be of importance in the establishment or absence of long-range ordering between NiO6 octahedra. Regarding Eu3+, it is also well-known that Eu2+ is more stable than Eu3+ because of the magic configuration 4f.7 Therefore, we cannot exclude some admixture with Eu2+, isoelectronic with Gd3+, and hence, the same considerations regarding the isotropic molecular field on neighbouring Ni ions and the absence of long-range ordering of the Ni3+δ and Ni3−δ octahedra could also apply here.
Among the rare earth ions, most of them stabilize the R3+ valence state, with the corresponding paramagnetic moment. The case of Eu is usually special, because the most stable valence state is Eu2+, with J = S = 7/2 and the magnetic moment is close to 7μB. Formally, the Eu3+ (J = 0) ion in principle does not carry any magnetic moment. In the practice, however, the paramagnetic moment of Eu3+ is reported to be close to 3.4μB. In our case, we estimate that the valence state is Eu3+; however, probably due to the local electrical and magnetic fields coming from the Ni sublattice, the J levels possibly undergo a complex admixture, yielding a slightly higher effective moment. The obtained effective moment for EuNiO3 is 5.5μB, for the 220–320 K temperature range, which will imply a local magnetic moment of the Eu site around 4.7μB (assuming 1.73μB for low-spin Ni3+), which could be considered as not unreasonable. Also, the broad bump in the magnetic susceptibility in the temperature range between 50 K and 180 K, could be related to a different population (temperature and local-field dependent) of the J levels.
In order to detect the TN of this compound, we also performed measurements of AC susceptibility around the expected ordering temperature at different excitation frequencies. Only the data at 5 kHz showed a weak peak in the real part of the magnetic susceptibility around 197 K, which we identify as TN (upper inset of Fig. 5).
Moreover, the magnetic field dependence of the magnetization up to 5 T shows a linear behavior below TN, indicating the antiferromagnetic character of the magnetic ordering, as shown in Fig. 6. Only the low temperature (1.8 K) hysteresis loop shows a rather weak curvature, probably related to a weak magnetic polarization on the Eu3+ ions.
In order to ascertain more clearly the antiferromagnetic ordering temperature (TN) in EuNiO3, we prepared a compressed pellet (1 Ton) from the powder sample to be able to measure the specific heat in a wide range of temperatures and applied magnetic fields. Fig. 7 displays the specific heat at 0 and 9 T of the externally applied field.
The specific heat of EuNiO3 shows a clear peak close to 200 K, indicating the magnetic phase transition temperature, TN. However, in this temperature range, we have an important contribution to the specific heat coming from the lattice vibrations. A simple approach of this lattice component can be estimated by the approximation of three harmonic oscillators, sited at different frequencies. The calculation of three harmonic oscillators at frequencies equivalent to 160 K, 250 K and 580 K, is shown in Fig. 7 as blue squares. This calculation is able to reproduce well a temperature range between 100 K up to 250 K, where the contribution to the specific heat is considered to come only from the lattice vibration and magnetic ordering. For low temperatures, this simple model is not valid, due to additional components to the specific heat (electronic and crystal field levels). By a direct subtraction of the experimental data from this calculation, we indeed obtain a rather good approximation of the magnetic-only specific heat of this compound (EuNiO3) for the temperature range between 120 K to 230 K. The magnetic component of specific heat is presented in the inset of Fig. 7, showing a clear delta-like transition around the ordering temperature (TN = 197 K). Moreover, upon repeating the same measurement under a strong applied magnetic field of 9 T, with the same calculation of the lattice contribution (the same three harmonic oscillators at the same frequencies), the obtained results are similar, indicating that the magnetic transition is not dependent on the applied magnetic field, thus confirming a pure antiferromagnetic character.
The joint analysis of the magnetization and specific heat data indicates that the EuNiO3 system undergoes antiferromagnetic ordering at TN = 197 K, and at low temperatures there is a very weak polarization by the applied magnetic field on the Eu ions. Moreover, the abrupt contraction of the b parameter of this perovskite in the 175–200 K range, coincident with the onset of the antiferromagnetic ordering, suggests a magnetoelastic coupling, not described so far in rare-earth nickelates.
The magnetic susceptibility of GdNiO3 is displayed in Fig. 8. In principle, the magnetic susceptibility shows a simple behavior with a rather high value of ∼1 emu mol−1 at low temperatures, without any clear anomaly at any temperature, as probably the susceptibility is dominated by the high magnetic moment of the Gd3+ ions. The magnetic ordering temperature of this compound is reported as TN = 185 K.7 The linear behavior (see the lower inset of Fig. 8) of the inverse of the magnetic susceptibility in the paramagnetic regime (T > 200 K) implies a paramagnetic moment of almost 9μB per f.u. (including Gd and Ni ions) and a Weiss temperature of θ = −5.5 K, indicating the presence of rather weak antiferromagnetic interactions in the paramagnetic phase.
In order to explore the ordering temperature for the Ni sublattice, the plot of χT vs. T is enlightening; this curve presents a clear change in the slope at TN = 187 K. This behavior is totally consistent with that reported from the specific heat data, showing that the antiferromagnetic ordering of GdNiO3 occurs at TN = 185 K.7
Moreover, the magnetic field dependence of the magnetization is presented in Fig. 9. The initial measurements up to 5 T and low temperature (2 K) of the hysteresis loops seem to indicate an initial process of saturation of the magnetization, but rather incomplete. We performed a second measurement up to higher magnetic fields (14 T), where a complete saturation is observed with a rather high ordered moment of 7.5μB per f.u., for magnetic fields higher than 7 T. However, for temperatures below and above the TN = 187 K, a linear behavior, similar to that expected for an antiferromagnetic system, is clearly observed.
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Fig. 9 Hysteresis loops for GdNiO3 at different temperatures with applied magnetic fields up to 14 T. |
We could conclude that some type of ferromagnetic-like saturation at high magnetic fields is observed in GdNiO3 at very low temperatures (T < 10 K), mostly related to the Gd3+ ions. In order to clarify this point, we performed detailed measurements of the magnetic susceptibility at low temperatures, for different applied fields, as represented in Fig. 10.
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Fig. 10 Low-temperature dependence of the magnetic susceptibility of GdNiO3, measured at different applied fields from 100 Oe up to 25 kOe. |
Clearly, the low-temperature magnetic susceptibility shows a maximum close to 2.7 K for small applied magnetic fields (100 Oe). When the magnetic field increases, this maximum is displaced and it finally disappears for higher magnetic fields (B > 5 kOe). The data of the hysteresis loops and the magnetic susceptibility at low temperatures and at different applied fields seem to indicate that the Gd sublattice, with an important magnetic moment per ion (around 8μB), is polarized by the external magnetic field, but an actual long-range ordering of the Gd sublattice is not achieved above 1.75 K.
Footnote |
† Electronic supplementary information (ESI) available. See DOI: 10.1039/d1dt00646k |
This journal is © The Royal Society of Chemistry 2021 |