P.
Mandal
a,
Shridevi S.
Bhat
a,
Y.
Sundarayya
a,
A.
Sundaresan
*a,
C. N. R.
Rao
a,
V.
Caignaert
b,
B.
Raveau
b and
E.
Suard
c
aChemistry and Physics of Materials Unit and International Centre for Materials Science, Jawaharlal Nehru Centre for Advanced Scientific Research, Jakkur P.O., Bangalore 560 064, India
bCRISMAT, UMR 6508, CNRS-ENSICAEN, Universite de Caen, 14050, Caen Cedex, France
cInstitut Laue Langevin, 6, Rue Jules Horowitz, 38042, Grenoble Cedex 9, France
First published on 4th November 2011
(Bi0.5Sr0.5)(Fe0.5Mn0.5)O3 crystallizes in a rhombohedral structure, with space group Rc, where the cations Bi3+/Sr2+ and Fe3+/Mn4+ occupy 6a and 6b sites respectively. Neutron diffraction, Mössbauer and magnetization measurements confirm long range antiferromagnetic ordering of the Fe3+ and Mn4+ moments at TN (226 K). Below TN, this oxide exhibits a cluster glass behavior and at low temperatures (∼30 K) a spin glass state is observed. The complex magnetic behavior is attributed to cation disorder in the system. Magnetic properties of this oxide are compared with those of the isostructural Bi0.5La0.5Fe0.5Mn0.5O3 where both Fe and Mn ions exist in trivalent state.
Another interesting aspect is that stoichiometric LaMnO3 is an antiferromagnetic insulator (TN∼143 K) with an orthorhombic structure,2,9 while BiMnO3 is ferromagnetic (TC∼105 K),10 despite La3+ and Bi3+ ions have similar ionic radii (0.645 Å). The stereochemical activity of 6s2 lone pair electrons of Bi3+ ions influences the structure and hence the physical properties.11 For example, BiFeO3 is antiferromagnetic (TN = 643 K) and ferroelectric (TC = 1103 K) at room temperature.12 It may be mentioned here, except BiFeO3, most of the other Bi based compounds are stabilized in the perovskite structure under high pressure and high temperature. The compound, BiFe0.5Mn0.5O3, synthesized at high pressure and temperature, has an orthorhombic structure and exhibits a temperature-induced magnetization reversal below TN = 240 K.13 However, it is possible to stabilize this compound at ambient pressure by partial substitution at the A or B sites.14,15 For example, La or Sr substitutions at the Bi–site of the high pressure BiFe0.5Mn0.5O3 phase stabilize it in the perovskite structure at ambient pressure. In La0.5Bi0.5Fe0.5Mn0.5O3, Fe3+ and Mn3+ orders antiferromagnetically at 240 K and this compound is a multiferroic and exhibits a spin-glass state at low temperature.16 It is worthwhile to investigate and compare the physical properties of two close systems with 50% of La and Sr substituted at the Bi-site of BiFe0.5Mn0.5O3, having d5–d4 (La doped) and d5–d3 (Sr doped) spin configuration respectively. Interestingly, both compounds have an identical crystal structure (Rc) but they differ in their magnetic properties. Bi0.5La0.5Fe0.5Mn0.5O3 (BLFMO) shows an antiferromagnetic ordering with spin canting below TN∼220 K whereas Bi0.5Sr0.5Fe0.5Mn0.5O3 (BSFMO) exhibits a complex magnetic behavior. Below TN (226 K), Bi0.5Sr0.5Fe0.5Mn0.5O3 exhibits a cluster glass state and at further low temperature 30 K a spin-glass state is observed.
The absence of super-lattice reflection in X-ray and neutron diffraction patterns suggests no A-site ordering between Bi and Sr cations or B-site ordering between Fe and Mn ions. A weak broad peak around 2θ∼20°, where there is no nuclear Bragg reflection, could be seen in neutron data at 300 K for both compounds which develops into a clear reflection with increased intensity at low temperatures as shown in Fig. 1 and 2. The presence of a broad peak at 300 K might be due to short range magnetic interactions of Fe3+/Mn4+ and Fe3+/Mn3+ ions in Sr and La substituted compounds, respectively. Our attempt to refine site occupancies of Bi3+ and Sr2+ ions gave unrealistic values with large errors which may be due to their close neutron scattering lengths. Further, Rietveld refinement on room temperature X-ray data showed site occupancies of Bi and Sr to be close to 1:
1 ratio and therefore site occupancies of Bi and Sr (La) were fixed whereas the occupancies of Fe and Mn sites were refined and found to be stoichiometric. These facts are in accordance with energy-dispersive X-ray spectroscopy (EDX) data collected at various spots. Also, the refinement of oxygen occupancy does not deviate significantly from the stoichiometric value and therefore was kept fixed. Fig. 1b and 2b shows the Rietveld refinements on the neutron data for BSFMO and BLFMO collected at 90 K and 4 K, respectively. In Fig. 1b, the magnetic reflection near 2θ∼20° has been zoomed in for clarity. This reflection is rather weak which may be due to the fact that the data was collected at relatively higher temperature (90 K). The magnetic reflections in the low temperature neutron diffraction patterns (shown by arrows) were modelled by G-type antiferromagnetic coupling of disordered Fe/Mn moments aligned along the c-axis of the hexagonal lattice. Though the magnitudes of the magnetic moments associated with Fe3+ (S = 5/2) and Mn4+ or Mn3+ (S = 3/2 or S = 2) ions are different, due to the fact that these ions are distributed randomly, it is difficult to determine finite magnetization, if any, using thermal neutrons. The average magnetic moments of Fe/Mn in BSFMO (90 K) and BLFMO (4 K) are 1.11 (8) μB and 1.30 (3) μB respectively which are much lower than their respective theoretical values. Results from Rietveld refinement of neutron diffraction data have been summarized in Tables 1 and 2.
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Fig. 1 Room temperature (a) and low temperature (90 K) (b) neutron diffraction pattern of Bi0.5Sr0.5Fe0.5Mn0.5O3. Closed symbols are the experimental points, solid line represents calculated pattern and the Bragg's positions are indicated by ticks. Solid line below the pattern shows the difference between the experimental and calculated patterns. Red arrow shows the magnetic reflection (1b). Magnetic reflection has been zoomed for clarity. |
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Fig. 2 Neutron diffraction pattern of Bi0.5La0.5Fe0.5Mn0.5O3 at (a) room temperature and (b) at 4 K. |
Parameter | Bi0.5Sr0.5Fe0.5Mn0.5O3 | Bi0.5La0.5Fe0.5Mn0.5O3 | |||
---|---|---|---|---|---|
300 K | 90 K | 300 K | 4 K | ||
a/Å | 5.4817(2) | 5.4810(1) | 5.5275(1) | 5.5206(1) | |
c/Å | 13.4107(5) | 13.4029(3) | 13.5006(3) | 13.4808(2) | |
O x | 0.4693(2) | 0.4652(2) | 0.4537(3) | 0.5462(2) | |
Biso | Bi/Sr(La) | 2.05(5) | 1.79(3) | 2.27(5) | 1.89(4) |
Fe/Mn | 0.31(10) | 0.10(70) | 0.86(9) | 0.20(6) | |
O | 1.59(3) | 1.42(2) | 2.19(4) | 1.90(2) | |
χ2 | 3.99 | 6.80 | 8.36 | 9.61 | |
Rp | 25.4 | 16.4 | 24.4 | 21.7 | |
Rwp | 18.7 | 13.2 | 19.0 | 18.0 | |
RB | 7.01 | 5.06 | 11.0 | 9.90 | |
Rf factor | 6.76 | 4.69 | 9.50 | 7.49 |
Parameter | Bi0.5Sr0.5Fe0.5Mn0.5O3 | Bi0.5La0.5Fe0.5Mn0.5O3 | ||
---|---|---|---|---|
300 K | 90 K | 300 K | 4 K | |
Bi/Sr(La)—O (Å) | 2.909(1) × 3 | 2.931(1) × 3 | 2.508(2) × 3 | 2.506(1) × 3 |
2.573(2) × 3 | 2.550(2) × 3 | 2.770(2) × 6 | 2.766(1) × 6 | |
2.744(8) × 6 | 2.744(1) × 6 | |||
Fe/Mn—O (Å) | 1.945(1) × 6 | 1.946(2) × 6 | 1.969(1) × 6 | 1.966(1) × 6 |
Fe/Mn—O—Fe/Mn (°) | 170.071(10) × 4 | 168.744(2) × 4 | 165.064(9) × 4 | 165.13(1) × 4 |
It is important to verify the valence state of the B-site cations as it plays a significant role in determining properties. In LaMnO3, the valence state of the manganese ions depends on the synthesis conditions which determine stoichiometry of the compound.9 While the valence state of manganese in stoichiometric LaMnO3 is +3, the cation and/or oxygen non-stoichiometry leads to a mixed valence of Mn3+/Mn4+.19 As discussed below, our Mössbauer study confirms that the Fe ions are present in trivalent state. The valence state of manganese in the present compound can indirectly be inferred from the inspection of average Fe/Mn–O bond lengths in BSFMO and BLFMO (Table 2). It can be noticed that the average Fe/Mn–O bond length in the former (1.945(1) Å) is smaller than that in the latter (1.969(1) Å). Since Fe ions are present in trivalent in both the compounds, the smaller average Fe/Mn–O bond length suggests that Mn ions are present in the tetravalent state in BSFMO and in the trivalent state in BLMFO.
To probe different magnetic interactions as well as to verify the iron valence in Bi0.5Sr0.5Fe0.5Mn0.5O3, zero-field 57Fe Mössbauer spectra were recorded at different temperatures as shown in Fig. 3(a)–(d). The spectrum at 300 K is fitted to a doublet and the obtained values of isomer shift, δ = 0.295 mm s−1 and quadrupole shift, ε = 0.528 mm s−1 confirms the presence of iron in Fe3+ state.20 Low temperature spectra at 150, 80 and 10 K show six line patterns confirming the magnetic ordering. The hyperfine field is noticeably observed to increase for the spectra at and below 150 K. Due to the disorder of Fe3+ and Mn4+ ions at the B-site of the perovskite, the lines of Mössbauer spectra below the magnetic transition (TN) become broader. This indicates the presence of several subspectra which can be ascribed to various environments around octahedral Fe3+ ions due to random distribution of Mn4+ ions. Since the hyperfine parameters, namely, hyperfine field Bhf, isomer shift δ and quadrupole shift ε of these subspectra are not known a priori, we have fitted the Mössbauer spectra to a model based on a random distribution of Fe and Mn ions on the octahedral sites. The probability of an octahedral site having n nearest-neighbour Mn atoms was calculated using the binomial formula,21,22
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Fig. 3 (a)–(d) Mössbauer spectra of Bi0.5Sr0.5Fe0.5Mn0.5O3 collected at 10, 80, 150 and 300 K. Solid lines over the open symbols are fits to the experimental data and sub sextets corresponding to different environments around octahedral Fe site are also shown as lines. (e) Distribution of hyperfine fields indicating the enhancement of Fe–Mn interactions with lowering the temperature. |
To understand the behaviour of the magnetic interactions, the Mössbauer spectra at 10, 80 and 150 K were analyzed by a distribution of hyperfine field.25 The hyperfine field was varied in a smooth way over a certain range of values to reproduce the observed Mössbauer spectra. In the present analysis, individual Mössbauer spectra (each consisting of six Lorentzian-shaped lines) were calculated at discrete Bhf values (10 kOe apart) along the abscissas of the P(Bhf)versus Bhf curves and added to form a resultant pattern for comparison with the experimental Mössbauer spectrum. Fig. 3(e) shows the temperature dependence of hyperfine field distribution P(Bhf). As the temperature is lowered, a decrease in the broadening of distribution pattern below the Néel temperature indicates enhancement in the strength of the exchange interactions between Fe and Mn ions.
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Fig. 4 ZFC–FC curves under magnetic field of 100 Oe for Bi0.5Sr0.5Fe0.5Mn0.5O3 showing magnetic anomalies at 30, 114 and 226 K. Inset shows ZFC–FC curves for Bi0.5La0.5Fe0.5Mn0.5O3 at 50 Oe. |
Magnetic isotherms of BSFMO recorded at different temperatures are shown in Fig. 5. At 5 K, the curve is slanted S-shaped with small coercive field of 400 Oe. At lower fields, the shape of the isotherm is related to the glassiness and is similar to that of observed similar compounds. At high fields, the curve shape changes to that of antiferromagnetic systems. This indicates that at high field the glassy feature disappears as all the frozen moments are forced to align towards the applied field. At 75 K, the isotherm shape changes with a higher coercive field value of 700 Oe which indicates a weak ferromagnetic behavior arising due to the canting of antiferromagnetic spins. The difference in the shape is related to the weak anomaly at 30 K in the ZFC data. At room temperature, a linear hysteresis curve is observed confirming the paramagnetic state. Magnetic isotherm (not shown) of Bi0.5La0.5Fe0.5Mn0.5O3 at low temperature (at 5 K) shows weak ferromagnetic behavior which does not saturate but has a much higher coercive field (3100 Oe) than that of the Sr doped compound (400 Oe).
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Fig. 5 Magnetic isotherms of Bi0.5Sr0.5Fe0.5Mn0.5O3 at 5, 75, 150 and 300 K. |
In order to understand the nature of magnetic interactions associated with three anomalies in BSFMO, we have performed ac susceptibility measurements and the results are shown in Fig. 6. Weak frequency dependence in the anomaly of real part of the ac susceptibility χ′ is observed in the vicinity of 40 and 105 K. The peak positions shift to higher temperature with increasing frequency. The imaginary part, χ′′ on the other hand, shows frequency dependent peaks near the magnetic anomalies. At the Néel temperature, χ′′ shows sharp peak which are frequency independent. These features along with the dc magnetization and Mössbauer data confirm the glassy nature of this system in which the competing magnetic interactions are present below a characteristic temperature. As the glassy state occurs below TN, it can either be associated with a reentrant spin glass (RSG) or with a cluster glass (CG) behavior.26,27 In a RSG, where the glassy nature persists into a long range ferromagnetic or antiferromagnetic order, the magnetic anomaly lies well below the paramagnetic to ferromagnetic/antiferromagnetic transition temperature. On the other hand, in a CG, where a set of clusters shows short range ordering below a characteristic temperature, a strong irreversibility in the ZFC–FC curves is observed below the magnetic ordering temperature. In the present case, the ZFC–FC in dc magnetization data shows a large irreversibility starting below the Néel temperature and also frequency dependent anomalies in χ′ lie closer to the Néel temperature which confirms the cluster glass phenomenon. The peak shift in the low temperature anomaly near 40 K is not very clear with frequency which is due to broad anomalies and existence of cluster glass state above this temperature. As both dc and ac magnetic measurements suggest that the anomaly near 40 K does not represent a long range magnetic ordering, this is assigned to a spin glass effect similar to that of Bi0.5La0.5Fe0.5Mn0.5O3.16 Glassy features in a magnetic system results from the competing magnetic interactions due to disorder arrangement of magnetic ions or geometric frustration. In the present compound, three superexchange interactions between Fe and Mn ions exist, Fe3+–O–Fe3+, Fe3+–O–Mn4+ and Mn4+–O–Mn4+. According to the Goodenough–Kanamori rules, coupling of Fe–O–Fe and Mn–O–Mn superexchange interactions are antiferromagnetic whereas Fe–O–Mn is ferromagnetic. Thus the glassy nature might be arising due to the competing magnetic interactions due to the disordered magnetic ions in the same crystallographic site. It should be noted that, spin glass and/or cluster glass effect, induced by disorder is well known in doped manganites.4,5,28 The glassy state in Bi0.5Sr0.5Fe0.5Mn0.5O3 is far more complex than in the La doped compound due to difference in sizes between the magnetic ions, Fe3+/Mn3+ and Fe3+/Mn4+ ions, which further increases disorder. Also, the possibility of oxygen non-stoichiometry in the compound though small, cannot be neglected which can lead to the presence of Mn3+ ions and contribute to the complex glassy nature. Thus our Mössbauer and magnetic studies suggest that the title compound BSFMO orders antiferromagnetically at 226 K and below the Néel temperature, the random and competing magnetic interactions lead to freezing of local magnetic moment of the clusters in random orientations which finally leads to a spin glass state at low temperature.
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Fig. 6 Ac susceptibility data of Bi0.5Sr0.5Fe0.5Mn0.5O3 plotted against temperature for different frequencies. |
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