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Impact of oxygen deficiencies on magnetic properties of La0.7250.275MnO3−δ compounds

W. Ben Jdidiaa, H. Gharsallahab, M. Smaria, M. Bejar*ac, E. K. Hlild and E. Dhahria
aLaboratoire de Physique Appliquée, Faculté des Sciences, Université de Sfax, Tunisia. E-mail: bejar_moez@yahoo.fr; Fax: +216 74 676609; Tel: +216 98 333 873
bInstitut Préparatoire aux Études d'Ingénieur, Université de Sfax, Tunisia
cFaculté des Sciences, Université de Monastir, Tunisia
dInstitut Néel, CNRS Université J. Fourier, BP166, 38042 Grenoble, France

Received 17th September 2025 , Accepted 18th March 2026

First published on 17th April 2026


Abstract

In this study, oxygen-deficient La0.7250.275MnO3−δ (δ = 0.00, 0.15, 0.25 and 0.35) compounds were synthesized using the sol–gel method. The elemental composition was confirmed by energy-dispersive X-ray spectroscopy (EDX) measurements, while X-ray photoelectron spectroscopy (XPS) measurements were employed to quantify and validate the oxygen deficiency levels. X-ray diffraction (XRD) analysis revealed that all samples crystallize with a rhombohedral structure in the R[3 with combining macron]c space group and exhibit nanometric crystallite sizes. Magnetic measurements demonstrated that the Curie temperature (TC) and magnetization (M) are strongly dependent on the oxygen deficiency (δ). The field-cooled/zero-field-cooled (FC/ZFC) magnetization curves reveal a pronounced magnetic irreversibility in all compounds, which becomes more marked as the δ value increases. This behavior is closely related to the enhancement of the magnetic anisotropy (MA) with increasing δ. Furthermore, analysis of the inverse magnetic susceptibility (χ−1(T)) shows clear deviations from the Curie–Weiss law at temperatures above the magnetic transition. These deviations are clearly observed for the compounds with δ = 0.00 and 0.15, become significantly weaker for δ = 0.25, and completely disappear for δ = 0.35. This evolution indicates that the magnetic inhomogeneities responsible for the non-Curie–Weiss behavior are progressively suppressed as δ increases, concomitant with strengthening of the magnetic anisotropy. Meanwhile, hysteresis loop measurements revealed a difference between the theoretical and experimental magnetization saturation values for the samples with δ = 0.00, 0.15 and 0.35. This disparity was assigned to a significant antiferromagnetic (AFM) contribution and to magnetic disorder on the nanoparticle surface. In contrast, the good agreement between the theoretical and experimental magnetic saturation for the compound with δ = 0.25 was attributed to the predominance of double exchange (DE) interactions.


1. Introduction

Manganites with the general formula R1−xAxMnO3, where R is a rare-earth element such as lanthanum and A is an alkaline-earth element, have been a hot area of research, generating significant scientific interest and attracting considerable attention from researchers due to their wide range of technological applications.1–6 These materials are widely used in the domains of magnetic refrigeration7–13 and gas sensing.14–16 Their outstanding properties result from complex electronic interactions, which are strongly influenced by several structural and chemical parameters. Among the key factors, the preparation method and annealing temperature play a major role in optimizing the properties of manganites.17–19 In particular, their magnetic characteristics are directly related to the image file: d5ra07059g-t1.tif ratio, which controls the DE mechanism. Multiple strategies have been proposed for adjusting this ratio, including substitution at the A-site with different elements.20,21

Beyond cationic substitution, other approaches have been explored, such as the creation of A-site vacancies.22,23 In this regard, the work of Dhahri et al.24,25 highlighted the introduction of oxygen deficiencies as another effective technique for modulating the magnetic properties of manganites.

Within this framework, these different methods equally demonstrate the existence of complex phenomena that influence the magnetic behavior of the materials. Among them, the SG behavior,26 the GP (ref. 27 and 28) and the AM (ref. 29) play a pivotal role. The emergence of these states is closely linked to several parameters, including the crystalline structure and crystallite size.30

Along this line, studies conducted by Mabrouki et al.31 focused on a series of manganites La0.83+0.2Mn0.4+2δ3+Mn0.6−2δ4+O3−δ2− with crystallite sizes of about 25 nm. Their work corroborated the presence of a GP in one of the compounds, notably attributed to a structural distortion that leads to the emergence of a significant proportion of the orthorhombic phase. Because the amount of Mn3+ ions becomes equal to 100% at a rate of 0.3, the oxygen deficiency for this series cannot be greater than δ = 0.25.

To gain better and deeper insight into the impact of the formation of oxygen deficiencies δ, in this study, we chose to tackle the structural and magnetic properties of oxygen-deficient compounds La0.7250.275MnO3. Increasing the A-site vacancy rate (0.275) can promote the creation of oxygen defects, leading to a value of δ = 0.35.

2. Sample preparation and characterization

2.1. Synthesis and novelty of the approach

While the controlled creation of oxygen vacancies in La1−xSrxMnO3−δ compounds using titanium metal as an oxygen getter is a well-established method developed in our laboratory, the present study introduces significant advancements. These advancements concern both the synthesis of the parent compound and the extent of the oxygen deficiency explored. The primary novelty lies in the use of the sol–gel method to synthesize the initial La0.7250.275MnO3 powder, as opposed to the conventional solid–state reaction employed by Abdelmoula et al.32 This wet-chemical route ensures superior chemical homogeneity, a finer particle size, and higher reactivity of the precursor powder. Consequently, this leads to more uniform and controlled incorporation of oxygen vacancies during the subsequent reduction step. Furthermore, we extend the investigation to a much wider range of oxygen deficiencies, up to δ = 0.35, compared to the previously studied limit of δ ≤ 0.15. This allows us to probe new physical regimes and property modifications in this colossal magnetoresistance material.

2.2. Sol–gel synthesis of the parent compound

The starting compound La0.7250.275MnO3 was synthesized using the sol–gel technique. The nitrate precursors La(NO3)3·6H2O and Mn(NO3)2·4H2O were dissolved in distilled water in stoichiometric quantities (eqn (1)); ethylene glycol and citric acid were added to ensure solution homogeneity.
 
(0.725)La(NO3)3·6H2O + Mn(NO3)2·4H2O → La0.7250.275MnO3 + Gaz (1)

The solution was slowly evaporated at 70 °C for 2 h in order to remove excess water and then heated to 180 °C to from a viscous gel. This gel was dried at 350 °C for 5 h to yield a solid precursor. The obtained powder was thoroughly ground and subjected to a stepwise calcination process at 450, 600 and finally 800 °C each for six hours to promote crystallization and remove organic residues.

2.3. Controlled creation of oxygen vacancies

The phase-pure La0.7250.275MnO3 powder, as confirmed by XRD, was then used to prepare oxygen-deficient samples, La0.7250.275MnO3−δ. This was achieved using the titanium getter method, following a protocol adapted from our previous work. A precise amount of the powder was sealed under vacuum in a quartz ampoule together with titanium metal chips.

The amount of titanium was calculated to achieve target oxygen deficiency values of δ = 0.15, 0.25, and 0.35, according to the reaction:32

 
image file: d5ra07059g-t2.tif(2)

The sealed ampoule was heated at 600 °C for 13 days to ensure thermodynamic equilibrium and homogeneous oxygen diffusion throughout the sample volume. The actual oxygen deficiency, δ, was determined gravimetrically using a high-precision ultra-microbalance:31

 
image file: d5ra07059g-t3.tif(3)
where Δm denotes the mass difference before and after reduction; Mmol is the molar mass of the stoichiometric compound; mused indicates the initial mass of the powder and MO is the atomic mass of oxygen.

The measured δ values were in excellent agreement with the target values, with an error of 10−4, confirming the accuracy and reproducibility of the process.31

2.4. Structural, chemical, and magnetic characterization

The elemental composition and homogeneity of the samples were verified by energy dispersive X-ray spectroscopy (EDX). The chemical states and surface purity were investigated by X-ray photoelectron spectroscopy (XPS) using a monochromatic Al Kα source (1486.6 eV).

The crystal structure and phase purity of all samples (before and after reduction) were characterized at room temperature by X-ray diffraction (XRD) using a BRUKER D8 diffractometer equipped with a CuKα1 radiation source (λ = 1.5406 Å). Data were collected over the 2θ range of 25–90° with a step size of 0.02°.

The magnetic properties were investigated using a BS2 magnetometer at the Néel Institute in Grenoble, France. Magnetization measurements were performed as a function of the temperature and applied magnetic field up to 5 T.

3. Results and discussion

3.1. EDX study

To validate the elemental composition of the prepared compounds, we employed EDX. The spectra displayed in Fig. 1 revealed characteristic peaks corresponding to all constituent elements (La, Mn and O) of the La0.7250.275MnO3−δ compounds, confirming no significant elemental losses during the various preparation steps. The presence of carbon (C) in the sample spectrum can be attributed to the carbon tape used before the EDX analysis.
image file: d5ra07059g-f1.tif
Fig. 1 Typical scanning electron micrographs: EDX spectra of La0.7250.275MnO3−δ (δ = 0.00, 0.15, 0.25 and 0.35) compounds measured at room temperature.

The measured atomic percentages, reported in Table 1, are close to the nominal values, which confirms the success of the preparation. This table reveals that the experimental La/Mn ratio values are very close to the theoretical ones. Additionally, EDX mapping demonstrates that the lanthanum (La), manganese (Mn), and oxygen (O) are uniformly distributed in the samples (Fig. 2).

Table 1 Atomic percentages of La0.7250.275MnO3−δ (δ = 0.00; 0.15; 0.25 and 0.35) compounds
δ   La (%) Mn (%) O (%) La/Mn
0.00 Theoretical values 15.34395 21.16401 63.49204 0.72500
Obtained values 15.45808 21.28083 63.26109 0.72639
Relative error 0.74 0.55 0.36 0.19
0.15 Theoretical values 15.84703 21.85791 62.29506 0.72500
Obtained values 15.78851 21.90552 62.30597 0.72075
Relative error 0.37 0.22 0.02 0.59
0.25 Theoretical values 16.20115 22.34636 61.45249 0.72500
Obtained values 16.05115 22.37335 61.57550 0.71742
Relative error 0.93 0.12 0.20 1.05
0.35 Theoretical values 16.57146 22.85713 60.57141 0.72500
Obtained values 16.36760 22.58966 61.04274 0.72456
Relative error 1.23 1.17 0.78 0.66



image file: d5ra07059g-f2.tif
Fig. 2 EDX mappings of O, Mn and La in La0.7250.275MnO3−δ (δ = 0.00, 0.15, 0.25 and 0.35) compounds at room temperature.

3.2. XPS study

The XPS survey spectra of the La0.7250.275MnO3−δ (δ = 0.00, 0.15, 0.25 and 0.35) compounds were analyzed using Casa XPS software (version 2.3.25). The Shirley background was applied for all Mn 2p spectra to account for inelastic electron loss. Peak fitting was performed using a mixed Gaussian–Lorentzian (GL (30)) lineshape, and the full width at half maximum (FWHM) was constrained to remain within ±10% for all Mn oxidation states to ensure consistency and physical relevance.

These spectra show only La, Mn, O, and adventitious C (Fig. 3a).33 There are no detectable contaminants. All fittings exhibit excellent agreement between the experimental (red) and fitted (black) spectra, with residual standard deviation (STD) values ranging from 2.42 to 2.68, indicating high-quality fits and consistent fitting parameters across all compounds. These findings validate the strength and reproducibility of the Mn 2p analysis, confirming the reliability of the extracted Mn3+/Mn4+ ratios addressed in the main text.


image file: d5ra07059g-f3.tif
Fig. 3 XPS profiles of La0.7250.275MnO3−δ (δ = 0.00, 0.15, 0.25 and 0.35) compounds: (a) survey, (b–e) Mn 2p deconvolution, and (f) Mn 2p multiplet splitting.

The C 1s peak at 284.8 eV was used as a reference for all of the spectra. We looked at the Mn core levels to figure out how the Mn3+/Mn4+ balance changed in the La0.7253+0.275Mn0.175+2δ3+Mn0.825−2δ4+O3−δ2− (δ = 0.00, 0.15, 0.25 and 0.35) compounds. For A-site-deficient perovskites La0.7250.275MnO3−δ, charge neutrality requires m3+ + m4+ = 1, where m3+ = 0.175 + 2δ and m4+ = 0.825 − 2δ stand for the molar fraction of Mn3+ and Mn4+, respectively. High-resolution Mn 2p spectra (Fig. 3b−e) were modeled using Gaussian–Lorentzian lineshapes.34 The spin–orbit splitting of (11.6 ± 0.1) eV for all species and all compounds was fixed.35 The peaks were attributed to Mn3+ (2p3/2 ≈ 640.6 − 641.1 eV) and Mn4+ (2p3/2 ≈ 641.7 − 642.8 eV). Weak shake-up/charge-transfer satellites were added at a fixed offset (∼6 eV) as a constant fraction of the parent but were not included in the quantification.36 The full width at half maximum was restricted within the oxidation state and fixed across the series. The quantification ratios were determined from the main 2p3/2 components. The experimentally derived image file: d5ra07059g-t4.tif ratios (Table 2) increased monotonically with δ: 0.22 (δ = 0.00), 0.79 (δ = 0.15), 1.78 (δ = 0.25), and 5.05 (δ = 0.35).37 The data as a whole adhered to the charge-balance trend, and there was a modest deficit in Mn3+ at the highest δ. Converting the ratios to bulk descriptors gave average Mn valences image file: d5ra07059g-t5.tif of 3.82, 3.56, 3.36, and 3.17 for δ = 0.00, 0.15, 0.25, and 0.35, respectively.38 Using the inverse relation image file: d5ra07059g-t6.tif,39 we obtained δXPS ≈ 0.003, 0.133, 0.232 and 0.330, in excellent agreement with the nominal series. The Mn 3s spectra (Fig. 3f) were examined for multiplet splitting ΔE, which increased with increasing Mn reduction.40

Table 2 Mn 2p peak-fitting parameters and image file: d5ra07059g-t18.tif experimental ratio for La0.7250.275MnO3−δ (δ = 0.00; 0.15; 0.25 and 0.35) compounds
δ Mn2p3/2
Mn4+ Mn3+

image file: d5ra07059g-t19.tif

0.00 641.7246 eV 640.5665 eV 0.22
47.99% 10.58%
0.15 641.8508 eV 640.6083 eV 0.79
33.05% 26.17%
0.25 642.0356 eV 640.9182 eV 1.77
23.12% 41.06%
0.35 642.1317 eV 641.0571 eV 5.05
10.25% 51.80%


Mn 3s multiplet splitting (ΔE3s) was determined from the energy separation between both well-resolved 3s peaks (peak-to-peak distance) in the deconvoluted spectra. This separation originated from exchange coupling between the 3s core hole and 3d valence electrons. The measured ΔE values were directly taken from the experimental spectra after baseline correction, not from the fitted envelopes, ensuring minimal fitting bias. The experimental values of 5.293, 5.549, 5.627, and 5.534 eV at δ = 0.00, 0.15, 0.25, and 0.35 followed the Mn 2p-derived reduction (Mn4+ → Mn3+) and exhibited no characteristics of Mn2+.41 The slight non-monotonicity in the region between δ = 0.25 and 0.35 (≈0.09 eV) is within standard experimental scatter (charging/background selections) and does not affect the trend. This small non-monotonic variation can lie within the instrumental energy uncertainty (±0.1 eV) of the XPS setup. However, it may also reflect a minor contribution from local inhomogeneity or mixed-valence Mn3+/Mn4+ domains, which are typical of oxygen-deficient manganite. Such subtle effects are consistent with prior studies on La–Mn–O systems, exhibiting variable oxygen stoichiometry.42–44

Throughout the series, the Mn 2p binding energies vary subtly, trending to lower energies with increasing δ, and the relative Mn3+ peak area increases at the cost of that of Mn4+, both of which are clear signs of reduction caused by oxygen vacancies.45 The survey spectra verify the chemical purity, and the Mn 3s splittings independently verify the evolution of the Mn valence derived from Mn 2p fitting. Altogether, the findings confirm the controlled oxygen non-stoichiometry in La0.7250.275MnO3−δ and offer a quantitative connection between δ, the Mn3+/Mn4+ ratio, and the average Mn valence.

3.3. Structural study

X-ray diffraction analysis revealed that all La0.7250.275MnO3−δ (δ = 0.00, 0.15, 0.25 and 0.35) compounds crystallize in the rhombohedral phase with R[3 with combining macron]c space group, as confirmed by Rietveld refinement using the FullProf program (Fig. 4). The space group assignment was further verified by comparison with the JCPDS database (card number 96-153-3630) with the assistance of Match 4 software.
image file: d5ra07059g-f4.tif
Fig. 4 Observed (red) and calculated (black solid line) spectra and their difference patterns (blue) and the Bragg positions (green) of La0.7250.275MnO3−δ (δ = 0.00, 0.15, 0.25 and 0.35) compounds.

The refinement results are displayed in Table 3. Accordingly, this table presents the crystallite sizes (DSC) determined from the XRD data using (eqn (4)):46

 
image file: d5ra07059g-t7.tif(4)
where θ refers to the diffraction angle of the most intense peak, β corresponds to the full width at half-maximum (FWHM) of this peak, k = 0.9 stands for the shape factor of the crystallites assumed to be spherical and λ denotes the wavelength of the radiation.

Table 3 Results of Rietveld refinement of XRD diffractograms of La0.7250.275MnO3−δ (δ = 0.00, 0.15, 0.25 and 0.35) compounds
δ 0.00 0.15 0.25 0.35
a (Å) 5.515(5) 5.509(7) 5.531(8) 5.536(2)
c (Å) 13.360(4) 13.353(2) 13.380(6) 13.388(0)
V3) 58.664(6) 58.510(0) 59.101(8) 59.227(5)
dMn–O (Å) 1.963(1) 1.959(2) 1.971(4) 1.975(1)
〈Mn–O–Mn〉 (°) 163.539(5) 164.432(0) 162.200(0) 161.343(4)
DSC (nm) 36.448(0) 38.337(0) 39.061(0) 39.796(2)
W/W0 0.093(3) 0.094(1) 0.091(9) 0.091(1)
χ2 1.51 1.60 1.77 1.71


The crystallite size grows monotonically as the oxygen deficiency increases. The increase in the crystallite size is attributed to the increase in the average radius rB of the B-site, determined using (eqn (5)):

 
rB = (0.175 + 2δ)rMn3+ + (0.825 − 2δ)rMn4+ (5)
In fact, the creation of oxygen deficiencies in La0.7253+0.275Mn0.175+2δ3+Mn0.825−2δ4+O3−δ2− entails the partial reduction of Mn4+ ions (rMn4+ = 0.53 Å) to Mn3+ ions, which have a larger ionic radius (rMn3+ = 0.65 Å).

3.4. Magnetic study

Subsequently, we measured M as a function of temperature (T) in ZFC and FC modes, under an applied magnetic field of 0.05 T, for the La0.7253+0.275Mn0.175+2δ3+Mn0.825−2δ4+O3−δ2− (δ = 0.00, 0.15, 0.25 and 0.35) compounds (Fig. 5). The curves acquired in FC mode display a PM/FM transition, which is detected at the TC, with values of 255, 265, 220 and 215 K, for δ = 0.00, 0.15, 0.25 and 0.35, respectively. This temperature was determined from the dM/dT curves presented in the inset of Fig. 5. For the δ = 0.15 sample, we first observed a slight increase in the temperature following a slight improvement in the Mn–O–Mn angle and a reduction in the Mn–O distance, leading to an increase in the one-electron bandwidth (W) calculated using eqn (6)31 and presented in Table 3:
 
image file: d5ra07059g-t8.tif(6)
where W0 indicates a positive constant, dMn–O indicates the Mn–O distance and γ refers to the Mn–O–Mn angle.

image file: d5ra07059g-f5.tif
Fig. 5 ZFC/FC magnetization versus temperature under an applied field of 0.05 T for La0.7250.275MnO3−δ (δ = 0.00, 0.15, 0.25 and 0.35) compounds. Insets: The variation of image file: d5ra07059g-t23.tif versus temperature.

Following the decrease in the Mn–O–Mn angle and the increase in the Mn–O distance, the decrease in W for the two other compounds (δ = 0.25 and δ = 0.35) is accompanied by a significant drop in TC.

However, it is inferred from Fig. 5 that the M(T) curves in the ZFC and FC modes have different characteristics that are affected by temperature. For temperatures above the irreversibility temperature (Ti), both curves overlap, indicating reversible magnetic behavior. The Ti temperature corresponds to the point at which the FC and ZFC curves begin to diverge, marking a separation between the two measurement modes. It is observed that Ti decreases with increasing oxygen deficiency (Table 4).

Table 4 Blocking temperature (TB), irreversibility temperature (Ti), Curie temperature (TC), anisotropy constant, anisotropy energy and Stoner–Wohlfarth field of La0.7250.275MnO3−δ (δ = 0.00, 0.15, 0.25 and 0.35) compounds
δ 0.00 0.15 0.25 0.35
TB (K) 80 85 120 130
Ti (K) 245 248 210 195
TC (K) 255 264 220 215
image file: d5ra07059g-t20.tif 0.152 0.128 0.139 0.268
image file: d5ra07059g-t21.tif 0.567 0.478 0.519 1
Anisotropy energy (KV′) (10−20 J) 2.845 3.023 4.269 4.628
V′ (107 Å3) 2.535 2.950 3.120 3.300
Anisotropy constant (K) (106 J m−3) 1.491 1.506 2.087 2.220
Stoner–Wohlfarth field µ0HSW (T) 1.103 1.144 1.332 1.761


For the T > Ti region, M varies identically with temperature, whether during heating or cooling. This implies that the effect of the thermal cycle does not influence M.

At low temperatures (T < Ti), the magnetic behavior becomes irreversible, indicating the existence of MA. Below this temperature, the spins freeze into a disordered state, generating irreversible SG/CG behavior, which is characteristic of materials exhibiting magnetic frustration as well as competing interactions.47 In numerous studies, researchers have identified divergence between the FC and ZFC modes as a result of this behavior.48–50 According to Pillai et al.,51 the ZFC curve indicates competition between the ferromagnetic (FM) and antiferromagnetic (AFM) interactions, which are of the DE and super-exchange types, respectively. AFM interactions are more prominent when the relative difference between the FC and ZFC curves is larger. This behavior can also be assigned to the presence of surface inhomogeneities related to spin disorder or MA, for compounds with nanometric crystallites sizes.52

This irreversibility between the FC and ZFC curves can be characterized by the relative difference between M in the FC and ZFC modes image file: d5ra07059g-t9.tif at 5 K (Table 4). This deviation is 15.2%, 12.8%, 13.9% and 26.8%, respectively, for δ = 0.00, 0.15, 0.25 and 0.35. Based on the values of image file: d5ra07059g-t10.tif, we can assert that for compounds with δ = 0.00, 0.15 and 0.25, the divergence of the ZFC and FC curves remains relatively stable, suggesting a similar magnetic behavior within this composition range. For the compound with δ = 0.25, a notable increase of over 41% in the MA energy is detected. One might have expected an intensification of the SG/CG behavior, but this is not the case. Indeed, the SG/CG behavior results from competition between FM and AFM contributions. From this perspective, this observation can be attributed to strengthening of the DE interactions, which regulate the magnetic behavior in such a way that the FC/ZFC gap remains constant, suggesting weakening of the SG/CG behavior.

However, for the compound with δ = 0.35, a significant increase in this divergence is observed, indicating strengthening of the anisotropy and magnetic disorder effects.

These findings become clearer by comparing the coefficient image file: d5ra07059g-t11.tif for the different compounds with that of δ = 0.35. In fact, calculation of image file: d5ra07059g-t12.tif (Table 4) leads us to a difference that does not exceed 57% for the compounds with δ = 0.00, 0.15 and 0.25, compared to that of δ = 0.35.

Through analyzing these curves, the blocking temperatures (TB) of the La0.7250.275MnO3−δ (δ = 0.00, 0.15, 0.25 and 0.35) compounds were determined and are outlined in Table 4. TB is defined as the temperature below which the magnetic moments of a disordered system become frozen and can no longer follow thermal variations on experimental timescales.53 In this respect, for temperatures below TB, the magnetic anisotropy energy outweighs the thermal agitation energy. For such temperatures, the measurement time (τm = 155 s) is less than the Néel relaxation time τN, which follows the Arrhenius law (eqn (7)). Thus, the magnetic moment is frozen, as indicated by the following equation:

 
image file: d5ra07059g-t13.tif(7)
where K denotes the magnetic anisotropy constant, kB refers to the Boltzmann constant, τ0 corresponds to the relaxation time for a zero-energy barrier, and V′ expresses the particle volume indicated by: image file: d5ra07059g-t14.tif, where DSC denotes the crystallite size.

Using the Arrhenius law (eqn (7)), when τN = τm, i.e. for T = TB, the anisotropy energy (KV′)47 was determined. Knowing the values of the volume V′, we were able to determine the value of the magnetic anisotropy constant K. The values of KV′, V′ and K are summarized in Table 4.

The data in Table 4 suggest that a rise in the oxygen deficiency (δ) correlates with an increase in the crystallite size, which in turn leads to a larger particle volume, accompanied by a rise in the magnetic anisotropy constant K and consequently KV′ value.

Compared to the anisotropy energy obtained for the compound with δ = 0.00, the rise for the compound with δ = 0.15 is still rather small. For this reason, the FC/ZFC gap remains almost the same compared to that for δ = 0.00, indicating that the SG/CG behavior did not change at δ = 0.15. This stability has a direct consequence on the increase in the spontaneous magnetization compared to that for δ = 0.00. This improvement is ascribed to the increase in the proportion of Mn3+, thereby reinforcing the DE interactions in the case where δ = 0.15.

For the compound with δ = 0.25, a notable increase of over 41% in the magnetic anisotropy energy is detected. One might have expected an intensification of the SG/CG behavior, but this is not the case. Indeed, the SG/CG state results from competition between the FM and AFM contributions. From this perspective, this observation can be attributed to strengthening of the DE interactions, which regulate the magnetic behavior in such a way that the FC/ZFC gap remains constant, suggesting weakening of the SG/CG behavior. It is widely recognized that the DE reaches its highest efficiency when the Mn3+/Mn4+ ratio is approximately 7/3.54,55

In the case of the compound with δ = 0.35, the DE mechanism becomes much less important than in the case for δ = 0.25. This reduction in the DE interaction is accompanied by an increase in the magnetic anisotropy energy, resulting in stronger SG/CG behavior and subsequently a widening of the FC/ZFC gap.

This monotonic evolution of the magnetic anisotropy energy is confirmed by the evolution of the Stoner–Wohlfarth field, provided by eqn (8):56

 
image file: d5ra07059g-t15.tif(8)
where, K indicates the uniaxial magnetic anisotropy constant (Table 4), Msat refers to the experimental saturation magnetization (Fig. 7 and Table 5), µ0 denotes the vacuum permeability and µ0HSW stands for the field required to reverse the magnetization in the direction of the easy magnetization axis. In other words, it corresponds to the field required to overcome the magnetic anisotropy.

Table 5 Theoretical and experimental values of magnetization saturation Msat of La0.7250.275MnO3−δ (δ = 0.00, 0.15, 0.25 and 0.35) compounds
δ Theoretical Mthesat (µB/Mn) Experimental Mexpsat (µB/Mn)

image file: d5ra07059g-t22.tif

0.00 3.17 2.85 10
0.15 3.47 2.77 20
0.25 3.67 3.33 9
0.35 3.87 2.68 30


Fig. 6 traces the evolution of (χ−1) as a function of temperature (T), under a magnetic field (µ0H) of 0.05 T. For the compound with δ = 0.00, the χ−1(T) curve deviates from the Curie–Weiss law above TC, suggesting the presence of the GP.57–61 Numerous studies have reported an analogous behavior, validating the existence of GP. The latter is marked by the presence of FM clusters integrated in the paramagnetic (PM) phase, as reported in multiple studies.42,43 To confirm this hypothesis, it is highly needed to analyze the behavior of the χ−1(T) curve under higher magnetic fields. As highlighted, for δ = 0.00, the application of a magnetic field (µ0H) of 2 T can suppress the curvature observed above TC.


image file: d5ra07059g-f6.tif
Fig. 6 Temperature dependence of inverse susceptibility (χ−1) measured under an applied magnetic field (µ0H) of 0.05 T for La0.7250.275MnO3−δ (δ = 0.00, 0.15, 0.25 and 0.35) compounds. Insets: Curves recorded under (δ = 0.00)µ0H = 2 T, (δ = 0.15)µ0H = 2 T and (δ = 0.25)µ0H = 1 T showing that the deviation from the Curie–Weiss law is progressively suppressed, indicating the disappearance of the Griffiths phase.

For the compound with δ = 0.15, a similar behavior is observed. Indeed, the GP is present and can be suppressed by µ0H = 2 T. However, for the compound with δ = 0.25, the GP becomes weak and an applied magnetic field of about 1 T is sufficient to eliminate it. Although the anisotropy energy (KV′) is very high for this compound, it does not have such a significant impact on the SG/CG behavior or the GP. As a result, we can assert that the DE interactions in this compound substantially control the magnetic interactions. This keeps the lattice well organized and prevents the SG/CG state as well as GP from being properly established in the lattice. In contrast, for the δ = 0.35 compound, with a further increase in KV′, we notice that the SG/CG behavior becomes more important than in all other compounds, while GP becomes almost non-existent. This is confirmed through the shape of χ−1(T) curve, which becomes almost linear and follows the Curie Weiss law. Thus, it may be deduced that the SG/CG behavior is strengthened and GP is weakened as MA increases.

The structural, electronic, and magnetic characteristics of the La0.7250.275MnO3−δ series are closely interrelated, providing a coherent framework for understanding the observed magnetic behavior. XRD analysis reveals a rhombohedral lattice with subtle distortions that increase with increasing oxygen deficiency, while XPS measurements indicate a systematic variation in the Mn3+/Mn4+ ratio corresponding to δ. These lattice distortions modify the Mn–O–Mn bond angles and lengths, thereby tuning the DE interactions responsible for ferromagnetism. Simultaneously, the change in the Mn oxidation states alter the number of itinerant electrons, directly affecting the TC and saturation magnetization. The combination of these structural and electronic inhomogeneities promotes magnetic frustration and anisotropy, which underpin the emergence of SG/CG behavior and influence the development of the GP. Although the χ−1(T) curves initially suggest a GP for δ = 0.00 and 0.15, this alone is insufficient evidence; the GP is supported by the presence of locally correlated FM clusters arising from lattice distortions and oxygen-induced electronic variations. Its progressive weakening with increasing δ correlates with the suppression of the GP, strengthening of the SG/CG behavior, and stronger XPS signals. Thus, the observed magnetic transitions reflect the intimate coupling between the lattice, charge, and spin degrees of freedom in oxygen-deficient manganites, demonstrating that structural and electronic changes jointly dictate the evolution of both glassy and cluster-like magnetic phenomena.

Hysteresis loops are a fundamental feature for characterizing the magnetic properties of materials, particularly saturation magnetization and the MA effect. Through analyzing these loops (Fig. 7), it is possible to assess the influence of magnetic interactions and structural effects on the alignment of moments under an external field.


image file: d5ra07059g-f7.tif
Fig. 7 Applied magnetic field-dependence of the magnetization at 10 K for La0.7250.275MnO3−δ (δ = 0.00, 0.15, 0.25 and 0.35) compounds.

In the current work, we compared the theoretical and experimental values of the magnetization saturation (Msat) of La0.7250.275MnO3−δ (δ = 0.00, 0.15, 0.25 and 0.35) compounds (Table 5).

The theoretical magnetization saturation value (Mthesat) was determined using eqn (9):

 
Mthesat = (0.175 + 2δ) × µMn3+ + (0.825 − 2δ) × µMn4+ (9)
where µMn3+ = 4µB and µMn4+ = 3µB (ref. 31) represent the magnetic moments of Mn3+ and Mn4+ ions, respectively, expressed in µB (Bohr magnetons).

For the δ = 0.00 compound, the experimental and theoretical values of the saturation magnetization are equal to 2.85 and 3.17µB/Mn, respectively (Table 5). We thus infer a relative difference between these two values equal to 10%. The MA cannot account for this difference since a µ0HSW field of 1.103 T (Table 4) is able to overcome this anisotropy while the field reaches 5 T. It can be accordingly concluded that 10% of the magnetic moments do not contribute to the saturation magnetization, which can be explained by the core–shell model.62 In this regard, it is worth noting that this model applies in the case of compounds that have nanometric crystallites. In this model, the core is ferromagnetically ordered while the shell is either totally or partially disordered, i.e., the spins are in a state of paramagnetism or ferrimagnetism.31 Thus, the real experimental saturation magnetization (Mexpsat) value can be obtained using the following relation:47

 
Mexpsat = ρshell Mshell + (1 − ρshell) Mcore (10)
where ρshell = 10% stands for the shell magnetization fraction, Mshell and Mcore refer to the contributions of the shell and the core to the magnetization, respectively.

Within the core, Mn3+ and Mn4+ ions are parallel to each other, and Mcore is specified in terms of:

 
Mcore = 0.175 × µMn3+ + 0.825 × µMn4+ = 3.17µB/Mn (11)

Departing from the experimental magnetic saturation Mexpsat, we estimate the shell magnetization fraction as follows:

 
image file: d5ra07059g-t16.tif(12)

The gap between the experimental Mexpsat value and the theoretical Mthesat increases and reaches 20% for the compound with δ = 0.15. Since the crystallite sizes of both δ = 0.00 and δ = 0.15 compounds are nearly identical, the core–shell model cannot adequately account for this discrepancy, which is significantly larger than that for the δ = 0.00 compound. Similarly, with the δ = 0.00 compound, the MA cannot explain the extra 10% discrepancy from that found for the δ = 0.00 compound, since a µ0HSW field of 1.144 T is able to exceed this anisotropy (Table 4), while the field reaches 5 T. Thus, this additional 10% gap can be assigned to the persistence of a robust AFM component within this compound.

For the δ = 0.25 compound, as pointed out previously, the DE interactions become dominant, implying that the FM order in this compound is very stable and no AFM order has a chance to establish itself. The magnetic field is significantly higher than the µ0HSW field, which amounts to 1.332 T (Table 4). It is, therefore, able to align almost all the moments, which explains the good agreement between the theoretical and experimental values of Msat, with a relative difference equal to 9%. As stated for the case of the compound with δ = 0.00, this difference can be ascribed to the core–shell model.

For the δ = 0.35 compound, a high saturation magnetization was expected (Mthesat = 3.87µB/Mn) (eqn (9)), but this is not the case. The discrepancy between the experimental and theoretical values is about 30%. The MA cannot explain this difference since the µ0HSW field, which amounts to 1.761 T, is consistently smaller than the applied field (Table 4). Thus, this discrepancy can be attributed to the contribution of the core–shell model (of about 10%) as well as the robust AFM component (of about 20%).

4. Conclusion

The impact of oxygen deficiencies on the magnetic properties of oxygen-deficient La0.7250.275MnO3−δ (δ = 0.00, 0.15, 0.25 and 0.35) compounds was examined. Careful scrutiny was given to the compounds' compositions, structural properties, and magnetic properties. Energy dispersive X-ray spectroscopy (EDX) measurements confirmed the elemental composition of the compounds. XPS measurements corroborated that oxygen deficiency (δ) was created in the desired proportions. The determined image file: d5ra07059g-t17.tif ratio is very close to the theoretical ratio, confirming the successful preparation of the compounds. Structural analysis demonstrated that all compounds include crystallites with nanometric dimensions.

A deviation from Curie–Weiss's law in the compounds with δ = 0.00 and 0.15 was proven by inverse magnetic susceptibility χ−1(T) analysis. It was found that this behavior weakens for compounds with δ = 0.25 and vanishes for the compound with δ = 0.35. On the other hand, it was inferred that for the compound with δ = 0.25, the magnetic interactions were influenced by the double-exchange (DE) mechanism, which reached its maximum for this compound.

Ultimately, a discrepancy between the experimental and predicted magnetization saturation values was detected based on the hysteresis loops.

A substantial antiferromagnetic component, especially for the compounds with δ = 0.15 and 0.35, explains this disparity.

As a future perspective, an analysis of the progression of competition among the different magnetic interactions in the magnetic network as a function of the applied magnetic field can be conducted in subsequent studies.

Conflicts of interest

The authors declare that they have no known competing financial interests or personal relationships that could have appeared to influence the work reported in this paper.

Data availability

All data supporting this manuscript, including EDX mapping, X-ray diffraction data and magnetic measurement curves, are in the supplementary information (SI). Supplementary information is available. See DOI: https://doi.org/10.1039/d5ra07059g.

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