Abstract
The Europium rare-earth manganites, La0.7−xEuxSr0.3MnO3 (x = 0.0–0.7), were investigated by the technique of X-band electron paramagnetic resonance (EPR) in the temperature range from 30 to 500 K. As the temperature was lowered, the various samples made transitions from paramagnetic to ferromagnetic phases. Furthermore, coexistence of anywhere from two to three ferromagnetic phases in the various samples was found. The third ferromagnetic phase was observed only in the samples with x = 0.1, 0.2, 0.3. The Curie temperatures for the various samples were estimated from the characteristics of the variable-temperature EPR spectra. The EPR data indicated the presence of Griffiths phases in the samples with x = 0.2, 0.3, 0.4, 0.5, 0.6, from which the respective Griffiths temperatures were determined. The activation energies were estimated here from the EPR data using the hopping model. The EPR linewidth behavior is found to be consistent with that predicted by the bottlenecked spin-relaxation model. The perovskite La0.5Eu0.2Sr0.3MnO3 is potentially useful in the design of magnetocaloric refrigeration units as a working fluid, since its Curie temperature TC is found to be close to the room temperature. The various ferromagnetic components in the samples observed here have been resolved only by the technique of EPR, not possible by other techniques.
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1 Introduction
The manganites have the general formula A1−yByMnO3, where A is a rare-earth ion and B = Ca, Ba, Sr. The crystal structure of La1−xSrxMnO3 is shown in Fig. 1. They have been extensively studied by the techniques of electron paramagnetic resonance (EPR) and ferromagnetic resonance (FMR) [1,2,3,4,5,6,7,8,9,10,11,12,13,14,15,16,17,18,19,20,21,22,23,24,25,26,27,28,29,30,31,32,33,34,35]. Some of these studies have been focused on understanding the dynamics of spins near and above the ferromagnetic phase transition, the phase separation, manifestation of Jahn–Teller effect and occurrence of Griffiths phase [1,2,3,4,5,6,7,8, 12,13,14, 19,20,21,22,23]. Their transport, magnetic and structural properties depend on the presence of the rare-earth ions (A3+), e.g., La3+, Nd3+, and Eu3+, as well as the divalent ions (B2+) ions, e.g., Sr2+. Recently, Eremina et al. [22] reported studies on phase separation and Griffiths phase in La0.4−xEu0.6SrxMnO3. Investigations of structure, magnetic properties and magnetocaloric effect was carried out by Vadnala et al. [16, 33] on two series of substituted rare-earth manganite compounds:
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(1)
Eu3+-doped compounds La0.7−xEuxSr0.3MnO3 (x = 0.0, 0.1, 0.2, 0.3) [17, 18] and
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(2)
Nd3+-doped compounds La0.7−xNdxSr0.3MnO3 (x = 0.0, 0.1, 0.2, 0.3).
It is known that replacement of the trivalent Lanthanum ion with the divalent Strontium ion in La1−xSrxMnO3 compounds leads to a change in their behavior from exhibiting antiferromagnetic exchange to double exchange, achieving the maximum Curie temperature at the Strontium impurity concentration of 30%. Furthermore, the Curie temperature can be changed not only by replacing Lanthanum ions with divalent ions, but also by replacing them with rare-earth ions possessing different spins. The Europium ion contains 6 electrons on the outer shell: 4f 6, L = 3, S = 3, J = 0. It is expected that the exchange interactions between the rare-earth Europium ions and the iron group Manganese ions are absent and should, therefore, not affect the double exchange that is realized in strontium-doped manganites, in any way. The double-exchange (DE) interaction in the mixed rare-earth manganites La0.7−xEuxSr0.3MnO3 is affected by the substitution of the La3+ ion by the Eu3+ ion. The DE interaction increases when the Mn–O–Mn bond angle decreases due to the substitution of the La3+ ion with larger effective radius (1.032 Å) by the Eu3+ ion with smaller effective radius (0.95 Å). This decrease in the bond angle becomes larger the greater is the concentration, x, of the substituting Eu3+ ions. This implies that the DE interaction increases with increasing concentration. In addition, near the phase transitions in manganites, a phase stratification is observed, which manifests itself in the formation of ferromagnetic clusters in the paramagnetic matrix, associated with the formation of Griffiths phase. Using the technique of EPR, one can observe this phase stratification, which manifests itself as splitting into several lines in the EPR spectrum.
1.1 Industrial Applications
The strongly correlated manganite oxides studied here have various industrial applications, such as spintronic devices, magnetic refrigeration and infrared devices [36,37,38,39]. These materials exhibit colossal magnetoresistance effect in the presence of an external magnetic field. They are useful for development of magnetic data-storage devices [36,37,38]. Furthermore, at the ferromagnetic to paramagnetic transition temperature, most of the manganites exhibit high temperature coefficient of resistance and large change in magnetic entropy. The high temperature coefficient of resistance (TCR) of manganites is useful for infrared microbolometer detector applications [15, 39], whereas the large change in magnetic entropy with high relative cooling (RC) is useful for magnetic refrigeration [37]. The room temperature transition with high TCR (7.4%) was observed in Na0.5La0.2Sr0.3MnO3:Ag2O [15] and 3.36% in La0.7−xEuxSr0.3MnO3 [17], which are suitable for uncooled microbolometer applications. Similarly, Na0.7−xLaxSr0.3MnO3 [16] compounds, which exhibit a large change in magnetic entropy (~4.78 J/kg × K at 6 Tesla) with high relative cooling (281 J/kg), are suitable for magnetic refrigeration technology.
1.2 Motivation for the Present Study
Previous EPR investigations of the Eu-doped La0.7−xEuxSr0.3MnO3 (x = 0.4, 0.5, 0.6, 0.7) samples [35] did not include the samples with x = 0.1, 0.2 and 0.3. Furthermore, they did not carry out measurements at liquid helium and at very high temperatures, which did not lead to an accurate determination of the activation energies. This warrants a more detailed investigation of these compounds. The present paper reports a detailed variable-temperature EPR investigation of Eu-doped manganites La0.7−xEuxSr0.3MnO3 (x = 0.1, 0.2, 0.3, 0.4, 0.5, 0.6 and 0.7) in the extended temperature range, from 100 to 500 K for the samples with x = 0.1, 0.2, 0.3, 0.6 and for the samples with x = 0.7, 0.6, 0.5 from 5 to 100 K. The purpose of this paper is to carry out a comprehensive analysis of the ferromagnetic behavior of diluted manganites and the influence of inhomogeneity on their electronic properties from their variable-temperature EPR spectra.
By a detailed analysis of the features of the EPR lines in the paramagnetic region, one can determine the activation energy of the carriers, the temperature of ferromagnetic phase ordering and the Curie–Weiss temperature.
1.3 Organization of the Paper
A description of sample preparation is given in Sect. 2. It is followed by the details of EPR measurements and their interpretation for the Perovskites La0.7−xEuxSr0.3MnO3 (x = 0.1, 0.2, 0.3, 0.4, 0.5, 0.6 and 0.7) in Sect. 2.1. Section 2.2 describes the details of the EPR measurements on La0.7−xEuxSr0.3MnO3 (x = 0.1–0.7) and the determination of Curie temperatures from the EPR data. The details of Dysonian line shape exhibited by the EPR lines are given in Sect. 2.3. The dependence of the EPR linewidth on the Eu content in La0.7−xEuxSr0.3MnO3 (x = 0.1–0.7) samples is discussed in Sect. 2.4, which also includes estimation of Curie and Curie–Weiss temperatures for these Perovskites. Section 2.4.6 discusses the dependence of Curie temperature on Eu content. Observation of Griffith’s phase is presented in Sect. 2.5. Section 2.6 discusses the hopping conductivity and estimation of activation energies for the various samples. The conclusions are summarized in Sect. 3.
2 Sample Preparation and EPR Spectra
This section contains details of sample preparation and a discussion of the EPR data obtained on the family of the various rare-earth perovskites La0.7−xEuxSr0.3MnO3.
2.1 Sample Preparation and Determination of the Ionic State of the Europium Ion in the Manganite Samples
The solid-state reaction route was used to synthesize La0.7−xEuxSr0.3MnO3 compounds, where x = 0.0–0.7 in the polycrystalline state, using high purity (more then 99.9%) chemicals La2O3, Eu2O3, SrCO3Nd2O3 and Mn2O3 (Sigma Aldrich) as starting materials, mixed in their stoichiometric ratios. The mixtures were ground for 3 h, then calcinated in successive intermediate grinding steps at 1000 °C, 1100 °C and 1200 °C in air for 12 h, subsequently made as pellets and sintered at 1300 °C for 12 h. A “PANanalytic X’pert Pro” was used for X-ray diffraction (XRD) analysis at room temperature. Mossbauer spectroscopy was used to confirm that the ionic state of the Europium ion in the mixed manganites studied here is trivalent, as discussed in “Appendix”.
2.2 EPR Measurements on La0.7−xEuxSr0.3MnO3 (x = 0.1–0.7)
The EPR spectra of the perovskite manganites La0.7−xEuxSr0.3MnO3 (LESMO hereafter), where x = 0.1–0.7, were rerecorded on an X-band (9.4 GHz) Bruker EMX/plus spectrometer, equipped with a liquid-nitrogen temperature controller RS 232 in the temperature range of 100–340 K, and a Varian E-12 spectrometer, equipped with a nitrogen gas temperature controller TC 232, in the temperature range of 300–600 K.
Figure 2 shows the temperature variations of the EPR lines for all the LESMO compounds in the temperature range 100–600 K, for the Eu concentrations x = 0.1–0.6 and from 5 to 340 K for the Eu concentration x = 0.7. To determine the phase-transition temperatures from the ferromagnetic to the paramagnetic state, the various EPR line shapes were simulated as superpositions of two to four Lorentzian lines (referred to as lines 1, 2, 3, 4 hereafter), depending upon the observed spectrum. The permissible number of lines necessary for a proper description of the spectrum was estimated by the method described in the appendix of the work of Demishev et al. [49]. Each such spectrum was characterized by its own line position, linewidth, and line intensity. Figure 3 shows the decomposition of the experimental EPR spectra for the samples La0.7−xEuxSr0.3MnO3 (x = 0.1–0.7) at 250 K as superposition of several simulated lines.
2.3 Dysonian Line Shape
The first derivative of the line shape P was fitted to the Dysonian line shape [40]:
where Bres is resonance magnetic field, ΔB is the linewidth, and α is the asymmetry parameters. Moreover, the value of |α|≤ 1, since the samples demonstrate a semiconductor character. The α parameter was zero for the ESR lines for La0.7−xEuxSr0.3MnO3 (x = 0.1; 0.2; 0.3; 0.4; 0.5; 0.6). As for the sample with x = 0.7, the alpha parameter was zero only for the ESR line at g = 2.
These overlapped theoretical lines were then fitted to the experimental ones, and the best-fit values of the resonance field, Bres, the absorption line width, ΔB, and the intensity I were estimated for each component EPR line of the spectrum. Thus, for each temperature with a step of 5 K, the values of Bres, ΔB and I were estimated (by Eq. 1) for the various component lines, as shown in Fig. 4 for the samples La0.7−xEuxSr0.3MnO3 (x = 0.1, 0.2, 0.3, 0.4, 0.5, 0.6, 0.7).
2.4 Estimation of Curie and Curie–Weiss Temperatures for the Perovskites La0.7−xEuxSr0.3MnO3 (x = 0.1–0.7)
As seen from Fig. 3, an overlap of several lines is necessary to describe the shape of the spectrum at low temperatures. However, above a certain temperature, only one line is observed in the experimental spectrum, which is the phase-transition temperature from an ordered state to a paramagnetic one. It depends on the relative concentrations of Lanthanum and Europium ions in the samples. When the Lanthanum ion (effective radius 1.032 Å) is increasingly replaced in the A-position in LESMO compounds by the Europium ion (effective radius 0.95 Å), i.e., as the concentration, x, of the Europium ion is increased, the ferromagnetic phase transition temperature, TC, was found to decrease, as seen from Table 1. From these plots, the transition temperatures from the ordered ferromagnetic state to the paramagnetic state (Curie temperatures) were estimated for the various samples, as shown in Fig. 5. To this end, the Curie temperature, TC, was determined from the temperature dependence of the derivative of the square of the integrated intensity with respect to temperature integral intensity of \(\partial I^2 /\partial T\) of line 1 and TC2, the ferromagnetic phase transition temperatures for line 2, was estimated from the critical points of these dependencies of line 2, listed in Table 1.
As for the value of θCW, the Curie–Weiss temperature, it was determined by fitting (Eq. 2) the inverse integrated intensity, 1/I, to the Curie–Weiss law in the paramagnetic phase:
The fitted temperature variations of the first derivative of the square of the integral intensity and that of the inverse integral intensity are shown in Fig. 5 to determine TC and θCW, respectively, for the La0.7−xEuxSr0.3MnO3 (x = 0.1, 0.2, 0.3, 0.4, 0.5, 0.6, 0.7) samples. It is clearly seen from this figure that the phase-transition temperature, TC, decreases with increasing Europium concentration. As for θCW, considering the error bars, which is about 15% for each θCW, one can say that the Curie–Weiss temperature, θCW, also decreases with increasing Europium concentration, within error bars.
2.4.1 La0.6Eu0.1Sr0.3MnO3
The EPR spectrum of the La0.6Eu0.1Sr0.3MnO3 perovskite is shown in Fig. 2. It indicates that the Curie temperature is about 340 K, since below this temperature, a sharp decrease in the resonance field of the ferromagnetic line is observed. In the plot of the temperature dependence of the linewidth ΔB in Fig. 3a, a uniform broadening of both the ferromagnetic and paramagnetic lines below 340 K is seen. In the temperature range from 240 to 305 K, one more signal is observed, which is denoted as 3. This signal also appears in the EPR spectra for La0.7−xEuxSr0.3MnO3 perovskites with the Eu concentrations x = 0.2 and 0.3. This line is observed only in the temperature interval from \(T_{2C}^*\), referred to hereafter as the Curie temperature for line 2, to TC, as seen from Fig. 4. For the samples with x > 0.3, this line disappears as seen from Fig. 4. Interpretation of line 3 requires further study as this line is unexpected. However, it is noted that, in contrast to the ferromagnetic and paramagnetic signals, whose resonant fields increase with increasing temperature, the resonant field of this unknown signal decreases with increasing temperature, requiring further study.
2.4.2 La0.5Eu0.2Sr0.3MnO3
From the temperature dependence of the EPR spectrum in Fig. 3, it is seen that.
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(1)
the linewidth begins to increase sharply below 295 K as the temperature decreases, implying that the Curie temperature of this sample is about 295 K.
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(2)
the resonance fields for the two lines decrease sharply with decreasing temperature, starting from 300 K; and
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(3)
broadening of these lines is observed below 305 K. This indicates that the ferromagnetic transition occurs at about 300 K. Since the Curie temperature TC of the perovskite La0.5Eu0.2Sr0.3MnO3 is close to room temperature, it is potentially useful in the design of magnetocaloric refrigeration units as a working fluid.
2.4.3 La0.4Eu0.3Sr0.3MnO3
For this sample, it is observed that the linewidth begins to increase below 230 K as the temperature decreases (Fig. 4). A sharp decrease in the resonant field of this line is observed below 225 K (Fig. 4). In addition, at this temperature, there occurs a sharp broadening of the resonance lines of both the ferromagnetic and paramagnetic signals (Fig. 4). This indicates that the ferromagnetic phase transition temperature for this sample is 225 K. It is also noted that for the sample with the Eu concentration x = 0.3, 0.6 the third line, is still observed at room temperature, but its intensity is very low. On the other hand, this line is absent from the samples with the Eu concentrations of x = 0.4–0.5.
2.4.4 La0.3Eu0.4Sr0.3MnO3
For this sample, the unusual third line, as observed in the samples with x < 0.4, is no longer observed. Upon examining the temperature variation of the EPR spectra for this sample, it is seen that a significant line broadening occurs around 185 K, as seen in Fig. 4, which also shows that a sharp decrease in the resonant fields for the two observed EPR lines is seen as the temperature is decreased at approximately the same temperature (185 K).
2.4.5 La0.7−xEuxSr0.3MnO3 (x = 0.5–0.7)
Using the same analysis as described above, the ferromagnetic phase-transition temperatures were determined for the two perovskites La0.2Eu0.5Sr0.3MnO3 and La0.1Eu0.6Sr0.3MnO3to be 110 K, and for Eu0.7Sr0.3MnO3 to be 55 K (Fig. 4). The estimated TC values for the samples with various Eu concentrations are listed in Table 1. A phase diagram was made, using the data listed in this table, as shown in Fig. 6, displaying the dependence of TC on the Eu concentration in the La0.7−xEuxSr0.3MnO3 perovskites, with x = 0.1–0.7. It is noted from this figure that the values TC for the Eu concentrations x = 0.1, 0.2 and 0.3 are in good agreement with the TC values reported in Ref. [18], where the TC values were determined by several methods: modified Arrott plots, Kouvel–Fischer technique, and critical isotherms.
It is noted that there are seen some differences in the Curie temperatures as derived from the EPR data and those listed in Ref. 18 for the samples, x = 0.1, 0.2 and 0.3. This is because different experimental methods were used in these two cases. Furthermore, although there were observed three phases in each of these samples, the Curie temperatures (shown in Table 1) were obtained from the behavior of only one phase. This accounts for the differences in the two sets of TC values.
2.4.6 Dependence of Curie Temperature on the Concentration of Eu
The transition from a paramagnetic insulating to a ferromagnetic metallic state observed in the rare-earth manganites A1−yByMnO3 is usually described within the framework of the double-exchange mechanism proposed by Zener [41, 42], where the mobile 3d eg electrons of the Mn3+ ions couple ferromagnetically to the localized 3d t2g core spins due to a strong Hund’s coupling [43]. Very important parameters in this model, which determine the value of the ferromagnetic phase transition temperature, here are the two Mn–O1–Mn and Mn–O2–Mn bond angles. According to the Double exchange model, the strength of the ferromagnetic interaction decreases with decreasing Mn–O–Mn bond angle, leading to a decrease in its TC. Therefore, a decrease in the Mn–O–Mn bond angle, which occurs as the Eu content increases, leads to a decrease in TC. The tendency to decrease the Mn–O–Mn bond angle is expected to continue for increase in the Eu content for x > 0.3 as x increases. Figure 6 and Tables 1 and 2 clearly show that the Curie temperature, TC, decreases with increasing Eu concentration, x.
2.5 Griffiths Phase
The nature of this phase can be understood in terms of Griffiths singularities arising due to the presence of correlated quenched disorder [44]. From the EPR point of view, the evidence of the formation of Griffiths phase is indicated by the appearance of an additional line, which shifts to low magnetic fields as the temperature decreases below the Curie temperature. In the presence of Griffith phase, the inverse temperature dependence of the magnetic susceptibility deviates from the Curie–Weiss law when measured in low magnetic fields and follows the Curie–Weiss law when measured in strong magnetic fields. In the perovskites La0.7−xEuxSr0.3MnO3, with x = 0.0–0.7, the Griffiths phase appears in the vicinity of 300 K and persists to temperatures as low as 110 K for x = 0.2–0.6. It indicates the transition to a ferromagnetic phase from the paramagnetic phase as the temperature is lowered, as observed for the resonance line at g = 2.0. Griffiths showed that there would develop essential singularities in the temperature region TC(p) < T < TG. Here p denotes the disorder parameter, TC(p) is the ferromagnetic ordering temperature, which is disorder-dependent, and TG is a new temperature scale, which corresponds to TC(1), the Curie temperature of the undiluted system, which is characterized by p = 1 [8].
The Griffiths phase temperature TG was determined here from the temperature dependence of the shift of the resonance field in the Griffiths phase from the resonance field in the paramagnetic phase, B–Bres (L1), as described in Ref. [8]:
The TG temperatures, as obtained by fitting to Eq. 3 for the various samples, are listed in Table 1. (In Eq. 3, L1 refers to line 1.)
Using the data from Table 1, the TC(x) phase diagram, as a function of the concentration x, was plotted, showing the boundaries of Griffiths phase. Figure 6 shows a phase diagram describing the dependence of the ferromagnetic phase transition temperature on Eu concentration with the demarcation of the boundaries of the Griffiths phase in the perovskites La0.7−xEuxSr0.3MnO3, with x = 0.0–0.7. It is concluded from this figure that the Griffiths phase appears in the vicinity of 300 K and persists up to temperatures as low as 110 K for x = 0.2–0.6. As for the samples with x = 0.1 and x = 0.7, they do not exhibit any Griffiths phase due to their smaller than the required minimum disorder.
2.6 Hopping Conductivity and Estimation of Activation Energy for La0.7−xEuxSr0.3MnO3 Samples
Figures 7 and 8 show, respectively, the temperature variations of the linewidths of the EPR lines 1 and 2, observed in the samples La0.7−xEuxSr0.3MnO3.
The hopping conductivity of a sample affects significantly its EPR linewidth, ΔBpp [4, 45, 46]. The dependence of the linewidth on temperature in the paramagnetic region in the La0.7−xEuxSr0.3MnO3 samples is almost linear, as seen from Fig. 7. It is due to the small polaron-hopping conductivity as described below by Eq. 4 [9, 10]. The hopping rate limits the lifetime of the charge carriers, e.g., Mn4+ spins. In the paramagnetic state, the conductivity varies with the temperature as: σ(T) ∝ (1/T) × exp(− Eσ/kBT) due to the hopping motion of small polarons caused by the motion of charge carriers. Both the EPR linewidth and conductivity increase in proportion to the hopping rate. In the bottlenecked spin-relaxation model, the dependence of ΔBpp upon the temperature above Tmin in rare-earth manganites can be described, in similarity to the electrical conductivity in rare-earth manganites, by the following expression [4, 45, 46]:
where Ea is the activation energy for T > Tmin, and Tmin is the temperature at which the minimum of the EPR linewidth (ΔBpp min) is observed. The best-fit parameters for the activation energy, Ea, for these samples, as determined by applying the hopping model, where in one fits the EPR linewidth to Eq. 4, were here estimated. The dependence of the fitted values of Ea on the Eu content is shown in Fig. 9. It is seen from this figure that the activation energy, Ea, varies almost linearly for samples with x = 0.1–0.7 on the concentration of Eu ions, within an error of about 5–10%. The variations of the EPR linewidth with temperature of line 1 for the various samples are shown in Fig. 7. The activation energy Ea for La0.7−xEuxSr0.3MnO3 samples with x = 0.4, 0.5, 0.6, 0.7, as reported previously in [35], are very close to those obtained in the present work. The Ea values for the samples with x = 0.1, 0.2, 0.3 were estimated from the linear part of the temperature variations of the EPR linewidths in the high temperature region T > 300 K, as shown in Fig. 7 for line 1. It is also noted that Ea for the sample with x = 0.0 was estimated to be 0.33 eV (3820 K) from the temperature dependence of the EPR linewidth [14], included in Fig. 9, which also shows the Ea values derived from the polaron-hopping conductivity [17] for the samples with x = 0.1, 0.2, 0.3. It is noted that whereas the values obtained for the sample with x = 0.3, as obtained from the two models, agree with each other within error bars, those for the samples with x = 0.1, 0.2 show vast differences. In any case, our values show a continuous variation with the concentration, x, as one would expect, unlike those obtained from the polaron-hopping conductivity data.
It is noted that the activation energy as obtained here from the linewidth analysis differs markedly from that obtained from the temperature dependencies of the resistivity (Fig. 8), because the tunneling that is present in the resistivity between granules does not affect the EPR linewidth.
3 Concluding Remarks
The salient features of the EPR study on the family of La0.7−xEuxSr0.3MnO3 perovskites presented in this paper are as follows.
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1.
The present EPR investigations indicate that the activation energies for the La0.7−xEuxSr0.3MnO3 samples derived from the dependence of EPR linewidth on temperature, decreases almost linearly with x from x = 0.0 to x = 0.7.
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2.
The linewidths exhibit a pseudolinear temperature dependence in the paramagnetic region for the samples La0.7−xEuxSr0.3MnO3. This is consistent with the bottlenecked spin-relaxation model, especially for the samples characterized by the smallest disorder (x = 0.7, 0.6, 0.5).
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3.
The EPR studies on Eu-doped La0.7−xEuxSr0.3MnO3 samples reveal the coexistence of two ferromagnetic phases in the samples with x = 0.4, 0.5, 0.6, 0.7, whereas, in the samples with x = 0.1, 0.2 and 0.3, a coexistence of three ferromagnetic phases is found.
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4.
The Curie temperatures for the manganites La0.7−xEuxSr0.3MnO3 have been estimated here from the behavior of their respective ferromagnetic components in their EPR spectra.
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5.
According to the Double exchange model, as the concentration of the Eu3+ ions increases, the strength of the ferromagnetic interaction decreases due to decrease in the Mn–O–Mn bond angle, leading to a decrease in its TC, as shown in Table 1.
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6.
The Griffiths temperatures for the various samples La0.7−xEuxSr0.3MnO3 have been estimated here from their respective EPR spectra.
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7.
The present investigations indicate that the perovskite La0.5Eu0.2Sr0.3MnO3 is potentially useful in the design of magnetocaloric refrigeration units as a working fluid, since its Curie temperature is close to the room temperature.
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8.
The disordered solid solutions of the manganites La0.7−xEuxSr0.3MnO3 are highly inhomogeneous. Their ferromagnetic components have been discerned here by the technique of EPR, not possible by other techniques.
Data Availability
No datasets were generated or analysed during the current study. The data that support the findings of this study are available from the corresponding author upon a reasonable request.
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Acknowledgements
S. Asthana acknowledges financial support by project numbers UGC-DAE (CRS/2021-22/03/553) and SERB (CRG/2020/001509) for fabrication of the samples investigated in this paper. Electron spin resonance measurements were performed with the financial support from the government assignment for FRC Kazan Scientific Center of RAS.
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This work was partially supported by S. Asthana’s project numbers UGC-DAE (CRS/2021-22/03/553) and SERB (CRG/2020/001509).
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IIF, AVS, IVY and DVM made all the EPR measurements reported here. AVP made the Mossbauer measurements reported here. RME, along with SIA, prepared the preliminary version of the manuscript. SA and SV prepared the samples investigated here. All authors helped in the interpretation of the various parts of the data reported here. SKM was responsible for verifying all the interpretations of the data, adding additional information required to enhance the impact of the research presented in the paper, checking the English, and for preparing the final version of the manuscript.
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Appendix: Mossbauer Spectroscopy of La0.6Eu0.1Sr0.3MnO3 and Eu0.7Sr0.3MnO3
Appendix: Mossbauer Spectroscopy of La0.6Eu0.1Sr0.3MnO3 and Eu0.7Sr0.3MnO3
It is well known from the isomer-shift data that there is manifested a large separation (more than 10 mm/s) between the compounds containing Eu2+ and Eu3+ ions. This is due to different shielding of the closed-shell s-electrons by the 46 and 4f5 configurations [47, 48]. It is well known that the valence of the Europium ion in the manganite Eu1−xSrxMnO3 is 3 + [22]. Mössbauer spectroscopy was used in the present work to check the degree of oxidation by the measurement of the isomer shifts of the Eu ion in the manganites with different concentration, x = 0.1 and 0.7 of the Eu ion. Figure 10 shows typical absorption lines obtained for the samples with x = 0.1 and 0.7. The spectra were taken in transmission mode at 295 K using a MS-2201 spectrometer with a 151Sm2O3 source of 285 MBq radioactivity. The absorber thickness of the samples was 25 mg × Eu/cm2. The isomer-shift values, δeff = −0.5 ± 0.1 mm/s and δeff = −0.4 ± 0.1 mm/s, were determined with respect to the absorber Eu2O3 at T = 295 K for the samples La0.6Eu0.1Sr0.3MnO3 and Eu0.7Sr0.3MnO3, respectively. These measured isomer shifts confirm unequivocally the trivalent state of the Europium ion in the samples.
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Yatsyk, I., Mamedov, D.V., Shestakov, A.V. et al. EPR Studies of Rare-Earth Manganites La0.7−xEuxSr0.3MnO3 (x = 0.1–0.7). Appl Magn Reson 55, 1199–1219 (2024). https://doi.org/10.1007/s00723-024-01694-4
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DOI: https://doi.org/10.1007/s00723-024-01694-4