Open Access Article
Md. Rony Hossain
*ab,
Mst. Shamima Khanomb,
Prianka Mondal
c,
Akash Kumer Paulb and
Farid Ahmedb
aDepartment of Software Engineering, Daffodil International University, DSC, Birulia, Savar, Dhaka, 1216, Bangladesh. E-mail: rony.hossainb@gmail.com
bDepartment of Physics, Jahangirnagar University, Savar, Dhaka, 1342, Bangladesh
cDhaka University of Engineering & Technology, Gazipur, 1707, Bangladesh
First published on 27th April 2026
The present study employs density functional theory (DFT) within the CASTEP framework to systematically investigate the pressure-tunable structural, electronic and magnetic properties of A3CrO4 (A = Mg, Ca, Sr) alkali–metal oxides using GGA-PBE, GGA+U and GGA-PBEsol functionals. Structural optimization confirms that all A3CrO4 (A = Mg, Ca, Sr) compounds crystallize in the cubic P
3m space group, with ferromagnetic (FM) ordering consistently more stable than non-magnetic (NM) states across the entire pressure range of 0–30 GPa. Mg3CrO4 and Ca3CrO4 exhibit robust FM ground states with total magnetic moments of +4.0 to –4.1µB maintaining half-metallicity under hydrostatic pressures up to 30 GPa. In contrast, Sr3CrO4 undergoes a pressure-induced magnetic phase transition, with its magnetic moment reversing sign at 20–30 GPa, indicating a shift toward antiferromagnetic (AFM) or ferrimagnetic ordering. Elastic constant analysis confirms dynamic stability across the entire pressure range (0–30 GPa). While Mg3CrO4 remains brittle under compression, Ca3CrO4 and Sr3CrO4 exhibit pressure-induced ductility transitions, transforming from brittle to ductile behavior at higher pressures. Electronic structure calculations reveal persistent half-metallicity, with spin-down channels retaining wide band gaps and spin-up channels displaying metallic behavior. The application of Hubbard corrections (GGA+U) further validates the robustness of the electronic properties. The average sound velocity, Debye temperature, Debye frequency, melting temperature and Gruneisen parameter were analyzed under pressures of up to 30 GPa. Mg3CrO4 and Ca3CrO4 show a steady increase in sound velocity, Debye temperature, and frequency, indicating lattice stiffening, stronger bonding and enhanced thermal stability. In contrast, Sr3CrO4 exhibits anomalous behavior, with values rising up to 20 GPa but slightly decreasing at 30 GPa, consistent with its pressure-induced magnetic reversal. Melting temperatures increase significantly for all compounds, confirming their suitability for high-temperature and high-pressure applications. The interplay between pressure and functional analysis in these Cr-based compounds provides valuable insights for advancing spintronics and functional materials design.
Since the advent of spintronics in the early 1980s,14 half-metallic ferromagnetic (HMF) materials have garnered significant attention in both theoretical and experimental domains of materials science. The half-metallic nature was initially identified by de Groot and collaborators in semi-Heusler alloys such as NiMnSb and PtMnSb, marking a foundational advancement in spin-dependent electronic materials.14 Subsequent computational and experimental investigations have identified half-metallic behavior in a wide range of compounds beyond the initial semi-Heusler systems. Notable examples include rutile-type TiO2,15 spinel FeCr2O4,16 full Heusler Ti2CoSi,17 quadruple oxide perovskite CaCu3Fe2Re2O12,18 double perovskites La2CrNiO6,19 Sr2MnTaO6,20 Ba2YbTaO6,21 multiferroics RuCl2/Al2S3,22 RuBrF/Sc2CO223 zintl compounds EuMg2X2 (X = Sb and Bi)24 and XCr2Bi2 (X = Ca, Sr).25 Benjamin Balke et al.26 conducted a comprehensive study on the C 1b compound CoTi1−xMxSb (M = Fe, Mn, Cr, V) combining experimental techniques with first-principles calculations to demonstrate that selective substitution with 3d transition metals induces tunable half-metallic ferromagnetism, maintains crystalline stability, and achieves high Curie temperatures (>700 K) thereby highlighting the material's potential for spintronic applications. Seungho Seong et al. employed XMCD and XAS to investigate temperature-dependent mixed-valent states of Cr ions in CrO2 nanorods, providing direct experimental evidence of its half-metallic ferromagnetism.27 Recently, Samira Barouni et al. synthesized a nanoscale semiconductive perovskite, La0.25Sr0.75Sn0.4In0.25Ru0.35O3 (LSSIRuO), via co-doping of SrSnO3, demonstrating a narrowed band gap of 1.3 eV, robust conductivity, and low-temperature ferromagnetic ordering-highlighting its potential for optoelectronic, memory, and spintronic applications.28 Rasik Ahmad Parray et al. investigated a nanocrystalline Cr2NiAl inverse Heusler alloy synthesized via mechanical alloying, revealing a face-centered cubic XA/Xα structure, aggregated morphology, tunable electronic behavior, room-temperature soft ferromagnetism, and improved magnetic properties with higher annealing temperatures.29
Transition metal oxides, especially those with perovskite or related structures, have garnered significant attention due to their tunable electronic and magnetic properties.30–32 Chromium dioxide (CrO2), a well-known half-metallic ferromagnet, is a promising candidate for such applications due to its high Curie temperature and full spin polarization, though surface degradation remains a challenge.33 Similarly, other chromium-based compounds such as ZnCrO4 perovskites and Cr2O3 have been studied for their half-metallic ferromagnetism and spintronic applications.31,34 The precise engineering of these properties is crucial for advancing spintronic devices.35 Mohammed El Amine Monir et al.36 investigated X3FeO4 (X = Mg, Ca, Sr) using DFT, revealing ferromagnetic stability, semi-metallic behavior, and half-metallicity supported by elastic, electronic, and magnetic analyses. Their study also reported thermal parameters such as expansion coefficient, heat capacity, and Debye temperature, confirming the compounds’ potential for advanced applications.
The objective of this study is to demonstrate the half-metallic nature of alkaline-earth chromates X3CrO4 (X = Mg, Ca, Sr) by analyzing their structural, electronic, and magnetic properties using DFT within the CASTEP framework under hydrostatic pressures ranging from 0 to 30 GPa. A central motivation is to investigate how the half-metallic gap evolves with applied pressure in Mg3CrO4, Ca3CrO4, and Sr3CrO4 employing GGA-PBE, GGA-PBEsol and GGA+U functionals. Understanding how variations in the alkaline-earth cation at the A-site influence these properties under pressure is key to designing new materials with enhanced performance for opto-spintronic applications. The paper is organized into the following sections: Computational details: outlines the methodology, Results and discussion: presents and interprets the structural, elastic, electronic, and magnetic findings, and Conclusions: summarizes the main outcomes.
3m space group shown in Fig. 1. The Wyckoff positions 3c (0, ½, ½), 1a (0, 0, 0), 3d (0, 0, ½) and 1b (½, ½, ½) in this crystal structure are occupied by A, B, O1 and O2 atoms, respectively.43 These structures are optimized in ferromagnetic (FM) and non-magnetic (NM) states to verify the most stable state. The Birch–Murnaghan equation of state (EOS) is a fundamental model used to describe the pressure–volume relationship of materials, particularly under high-pressure conditions, by expanding the solid's free energy as a polynomial in the Eulerian finite strain. The standard third-order Birch–Murnaghan EOS is well-defined for cubic materials.44 The present materials were simulated in FM and NM magnetic configurations in various exchange functionals to extract the ground state structural parameters by performing a least-squares fit of the crystal energy against the unit cell volume through the Birch–Murnaghan equation of state,45
![]() | (1) |
The terms E(V), V and B0
in this equation represent the ground state energy, unit cell volume, and the bulk modulus (pressure derivate of the bulk modulus), respectively. For all the compounds the optimized energy-volume curve in these different phases clearly indicates that the FM phase is significantly most stable as it holds the lowest energy in all approximations rather than the NM phase, as depicted in Fig. 3(a–i).
Variations in lattice parameters arise from the distinct treatment of the exchange–correlation term by different functionals. Hence, A3CrO4 (A = Mg, Ca, Sr) was geometrically optimized with GGA-PBE, GGA+U and GGA-PBEsol functionals and the values are reported in Table 3. As shown in Fig. 2(a and b), hydrostatic pressure strongly influences the lattice parameters and unit cell volumes across PBE, PBEsol and GGA+U calculations. Increasing pressure gradually reduces the lattice parameters by shortening interatomic distances. From Fig. 2(c), the lattice constant reductions are modest with GGA-PBEsol consistently predicting slightly lower compressibility relative to GGA-PBE and GGA+U. In Fig. 2(d) the volume reduction is significantly higher across all functionals. This comparative analysis highlights that while lattice constants provide a direct measure of contraction, volume reductions offer a more sensitive indicator of bulk compressibility, and functional choice introduces systematic variations that must be considered in high-pressure predictions.
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| Fig. 2 (a–d) Change in the lattice parameters and volume of cubic A3CrO4 compounds (A = Mg, Ca, Sr) under pressure (0–30 GPa) with different functionals. | ||
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| Fig. 3 Energy versus volume curve (a)–(i) for A3CrO4 compounds (A = Mg, Ca, Sr) under hydrostatic pressures (0–30 GPa) for FM (ferromagnetic) and NM (non-magnetic state). | ||
Any deviance from the optimal cubic structure can be assessed by the tolerance factor (t) that typically ranges from 0.81 to 1.11 for cubic perovskites.47 The Goldschmidt tolerance factor, t, is given as,
![]() | (2) |
| Category | Cubic |
|---|---|
| Values of descriptions | |
| Convergence | Energy tolerance: 1.0 × 10−6 a.u.; force tolerance: 1.0 × 10−4 a.u. |
| Exchange-correction functionals | PBE-GGA (Perdew–Burke–Ernzerhof), GGA-PBEsol and GGA+U |
| Plane-wave cutoffs | 500 eV |
| Smearing section | Occupations = smearing; method = Gaussian; width = 0.10 eV |
| K-points grid | 8 × 8 × 8 |
| Pseudopotentials | OTFG ultrasoft |
| Relativistic treatment | Koelling–Harmon |
| Spin treatment | Spin polarized (FM calculations) |
| Electronic minimization | Metallic treatment with density mixing; Pulay mixing scheme |
| Geometry optimization | Method = BFGS; max steps = 1000; force tolerance = 0.05 eV Å−1; stress tolerance = 0.1 GPa |
| Mg3CrO4 | Ca3CrO4 | Sr3CrO4 | ||||||||
|---|---|---|---|---|---|---|---|---|---|---|
| 0 GPa | 20 GPa | 30 GPa | 0 GPa | 20 GPa | 30 GPa | 0 GPa | 20 GPa | 30 GPa | ||
| GGA-PBE (FM-state) | Lattice constant a (Å) | 4.30 | 4.15 | 4.08 | 4.73 | 4.53 | 4.45 | 5.04 | 4.79 | 4.71 |
| Volume V (Å3) | 79.98 | 71.76 | 68.36 | 106.36 | 92.96 | 88.64 | 128.75 | 110.12 | 104.52 | |
| Energy E (eV) | −9239.78 | −9239.36 | −9238.86 | −7183.08 | −7182.47 | −7181.82 | −6798.26 | −6797.44 | −6796.60 | |
| Bulk modulus B (GPa) | 124.14 | 156.87 | 228.97 | 97.95 | 278.87 | 418.62 | 90.50 | 232.08 | 371.48 | |
| GGA-PBE (NM-state) | Lattice constant a (Å) | −9238.4 | −9238.03 | −9237.64 | −7181.15 | −7180.59 | −7179.97 | −6795.90 | −6795.21 | −6794.39 |
| Volume V (Å3) | 4.23 | 4.09 | 4.03 | 4.67 | 4.48 | 4.41 | 4.99 | 4.75 | 4.67 | |
| Energy E (eV) | 75.77 | 68.45 | 65.89 | 102.48 | 90.18 | 86.02 | 124.88 | 107.64 | 102.15 | |
| Bulk modulus B (GPa) | 96.82 | 536.12 | 815.04 | 140.92 | 232.05 | 338.43 | 68.32 | 227.22 | 368.05 | |
| Tolerance factor | 0.82 | 0.92 | 0.99 | |||||||
| Mg3FeO4 | Ca3FeO4 | Sr3FeO4 | ||||||||
| Other calculation | Lattice constant a (Å) | 4.2846 | 4.7446 | 5.0346 | ||||||
| Energy E (Ry) | −4350.3946 | −7230.8246 | −22 227.4146 |
|||||||
| Bulk modulus B (GPa) | 152.00346 | 108.9546 | 94.3646 | |||||||
| Mg3CrO4 | Ca3CrO4 | Sr3CrO4 | ||||||||
|---|---|---|---|---|---|---|---|---|---|---|
| Functional dependence | Lattice constant reduction in % | GGA-PBE | GGA-PBEsol | GGA+U | GGA-PBE | GGA-PBEsol | GGA+U | GGA-PBE | GGA-PBEsol | GGA+U |
| 5.12 | 5.38 | 5.09 | 5.92 | 5.36 | 6.11 | 6.55 | 6.23 | 6.91 | ||
| Volume reduction in % | GGA-PBE | GGA-PBEsol | GGA+U | GGA-PBE | GGA-PBEsol | GGA+U | GGA-PBE | GGA-PBEsol | GGA+U | |
| 14.56 | 13.94 | 14.11 | 16.67 | 15.65 | 16.99 | 18.82 | 17.44 | 19.31 | ||
Fig. 4 illustrates the band structures of A3CrO4 compounds (A = Mg, Ca, Sr) obtained using two different exchange–correlation functionals along high-symmetry paths. Across the entire pressure range (0–30 GPa), the spin down channel shows a wide semiconducting band gap. In contrast, in the spin up channel the valence conduction bands merge in the Fermi level confirming the metallic nature. Both show the half metallic nature of our investigated compounds.
![]() | ||
| Fig. 4 Band structure of the A3CrO4 compounds (A = Mg, Ca, Sr) under hydrostatic pressures (0–30 GPa) for GGA-PBE and GGA+U functionals. | ||
When the Hubbard correction GGA+U is applied, the band gap increases reflecting the tendency of semi-local GGA to underestimate band gaps and the improved accuracy of GGA+U. The systematic increase in band-gap values from GGA-PBE to GGA+U highlights the intrinsic limitation of semi-local functionals in underestimating band gaps because of the absence of derivative discontinuity in the exchange potential.50 The consistent GGA/GGA+U trend observed here confirms the robustness of the electronic structure calculations and supports the reliability of the predicted half metallic behavior of the A3CrO4 compounds (A = Mg, Ca, Sr) and hybrid functionals provide more accurate band-gap estimations, which are computationally demanding, making them less practical for large-scale property calculations on standard computing platforms. In contrast, GGA-PBE offers a good balance between efficiency and accuracy, and thus was used for all subsequent calculations, while GGA+U was employed primarily for band-gap correction and validation.
The total density of states (TDOS) describes the distribution of electronic energy levels per unit interval and serves as a key indicator of the overall electronic structure of a material.51 Fig. 5 shows the TDOS of the A3CrO4 compounds calculated using the GGA functional. All the investigated systems exhibit ferromagnetic ground states across the studied pressure range, where the spin-up channel exhibits metallic behavior and the spin-down channel is semiconducting, except for Sr3CrO4 at 30 GPa, where the characteristics are reversed, confirming its antiferromagnetic nature as evidenced by the Fermi level position. The unequal contributions from the two spin channels further validate their magnetic behavior. In addition, the TDOS reveals the band gaps of these compounds, which are consistent with the corresponding band structure results.
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| Fig. 5 (a–c) Total density of states (TDOS) of A3CrO4 compounds (A = Mg, Ca, Sr) under hydrostatic pressures (0–30 GPa). | ||
| μ = 4Ooxygen + Cr + 3A (Mg, Ca, Sr) | (3) |
Table 4 provides the spin magnetic moments µB for A-site cations (A = Mg, Ca, Sr), chromium (Cr) and oxygen (O) anions in the A3CrO4 family under varying hydrostatic pressures (0, 20, 30 GPa) and using three distinct functionals GGA-PBE, GGA-PBEsol and GGA+U. These calculations provide critical insights into the magnetic behavior of these chromate perovskite-related materials and their potential for spintronic applications, especially under pressure-induced modifications. Understanding these properties is vital for the design of materials with tunable magnetic responses.52,53 For Mg- and Ca-based compounds the data consistently indicate a ferromagnetic (FM) alignment with positive total magnetic moments approximately +4µB to +4.1µB observed across all pressures and DFT functionals. This behavior is consistent with Cr3+ (d3, high-spin, S = 3/2) ions, where the magnetic moments of the Cr and O atoms align to produce a net ferromagnetic state. Such ferromagnetic coupling in chromite is often mediated by superexchange interactions and hybridization effects.54–56 The A-site cations (Mg and Ca) exhibit small positive magnetic moments, while the Cr ions contribute the dominant positive moment, generally ranging from 3.18µB to 3.78µB, depending on the specific compound, pressure and functional. The oxygen anions also contribute positive moments, suggesting a degree of spin polarization induced by their interaction with the Cr ions.
| Mg3CrO4 | Ca3CrO4 | Sr3CrO4 | ||||||||
|---|---|---|---|---|---|---|---|---|---|---|
| 0 GPa | 20 GPa | 30 GPa | 0 GPa | 20 GPa | 30 GPa | 0 GPa | 20 GPa | 30 GPa | ||
| GGA-PBE | µA | 0.21 | 0.21 | 0.21 | 0.24 | 0.30 | 0.30 | 0.27 | −0.27 | −0.30 |
| µCr | 3.52 | 3.45 | 3.18 | 3.64 | 3.53 | 3.48 | 3.79 | −3.64 | −3.59 | |
| µO | 0.36 | 0.44 | 0.44 | 0.12 | 0.24 | 0.28 | −0.08 | −0.08 | −0.12 | |
| µtotal | 4.09 | 4.10 | 3.83 | 4.00 | 4.07 | 4.06 | 4.00 | −3.99 | −4.01 | |
| GGA-PBEsol | µA | 0.21 | 0.21 | 0.18 | 0.27 | 0.30 | 0.30 | −0.27 | −0.30 | −0.33 |
| µCr | 3.50 | 3.27 | 3.06 | 3.60 | 3.48 | 3.37 | −3.74 | −3.60 | −3.56 | |
| µO | 0.36 | 0.44 | 0.44 | 0.16 | 0.28 | 0.28 | 0.04 | −0.12 | −0.16 | |
| µtotal | 4.07 | 3.92 | 3.68 | 4.03 | 4.06 | 3.95 | −3.97 | −4.02 | −4.05 | |
| GGA-GGA+U | µA | 0.21 | 0.21 | 0.24 | 0.27 | 0.30 | 0.30 | 0.27 | 0.30 | 0.30 |
| µCr | 3.63 | 3.54 | 3.50 | 3.78 | 3.65 | 3.61 | 3.96 | 3.78 | 3.74 | |
| µO | 0.20 | 0.32 | 0.36 | 0.08 | 0.04 | 0.08 | −0.32 | −0.12 | −0.08 | |
| µTotal | 4.04 | 4.07 | 4.10 | 4.13 | 3.99 | 3.99 | 3.91 | 3.96 | 3.96 | |
In contrast, Sr3CrO4 exhibits a notable and intriguing pressure-induced magnetic transition. At 0 GPa, under the GGA-PBE functional Sr3CrO4 shows a positive total magnetic moment of approximately +4µB. However, as pressure increases to 20 GPa and further to 30 GPa, the total magnetic moments reverse sign, becoming approximately −4µB and −4.01µB respectively under the GGA-PBE and GGA-PBEsol functionals, as demonstrated in Fig. 6. This sign reversal suggests a shift from an initial ferromagnetic ordering to an antiferromagnetic (AFM) or ferrimagnetic ordering where the dominate magnetic moments align antiparallel to their initial orientation.57 This transition is particularly significant as it implies that the magnetic properties of Sr3CrO4 can be manipulated by external pressure, offering potential avenues for mechanically controlled spin or switchable spintronics materials.58 Such pressure-driven transitions have been observed in other transition metal oxides, impacting their electronic and magnetic structures.54,59 The phenomenon in Sr3CrO4 is similar to pressure-induced spin-state transitions in iron-based oxides, which can lead to novel functionalities.60
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| Fig. 6 The magnetic moments µB for the cubic A3CrO4 compounds (A = Mg, Ca, Sr) under hydrostatic pressures (0–30 GPa) using different exchange correlation functionals. | ||
In Table 4, GGA+U generally yields more stable positive magnetic moments for all compounds with the total magnetic moments consistently around +4µB to +4.1µB. This suggests that the on-site Coulomb correction stabilizes the high spin d3 state of Cr3+ making it less susceptible to charge transfer effects or spin collapse under pressure.61,62 For Sr3CrO4, while PBE and PBEsol show a moment reversal, GGA+U consistently maintains a positive magnetic moment across all pressures indicating a more robust ferromagnetic state predicted by this functional. This highlights the importance of accurately treating electron corrections in such systems, as the magnetic ground state can be sensitive to the chosen theoretical framework.
The oxygen anion moments provide further insights into the electron structure and bonding. In Mg3CrO4 and Ca3CrO4 the positive oxygen moments increase with pressure under GGA-PBE and GGA-PBEsol. This increase reflects enhanced covalency and p–d hybridization between oxygen and chromium under compression. Similar observations have been made in other transition-metal oxides like NiO and CoO, where pressure strengthens the hybridization between oxygen 2p and transition metal 3d orbitals leading to greater spin polarization of the oxygen sublattice.63
In Sr3CrO4 however, the oxygen moments also reverse their sign under PBE and PBEsol with increasing pressure, aligning with the overall change in the total magnetic moment. This suggests that the oxygen sublattice actively participated in the pressure-induced magnetic transition, rather than merely reflecting the Cr moments. The magnetic properties of Cr-containing perovskites are generally complex due to the competition between direct exchange and superexchange interactions and the influence of the structural distortions.64–67
Overall, materials with tunable spin polarization could be employed in pressure-sensitive magnetic sensors, data storage devices, and spin valves where mechanical strain dictates the magnetic state.68,69
![]() | (4) |
Since A3CrO4 (A = Mg, Ca, Sr) is a cubic structure with a high degree of symmetry, the elastic constant reduces to three independent elastic constants: C11, C12, and C4472 as reported in Table 5. The following is an expression of the conventional mechanical stability conditions in cubic crystals at equilibrium in terms of elastic constants,73,74
| C44 > 0, C11 > |C12|, C11 + 2C12 > 0 | (5) |
| Born stability at P = 0 (GPa) | Dynamical stability | Stability | ||||||
|---|---|---|---|---|---|---|---|---|
| Compounds | Pressure P (GPa) | C11 | C44 | C11 + 2C12 | Stable | |||
| Mg3CrO4 | 0 | 239.07 | 110.75 | 447.29 | 134.96 | 447.29 | 110.75 | Stable |
| 20 | 343.78 | 114.08 | 492.88 | 249.68 | 492.88 | 94.08 | Stable | |
| 30 | 478.14 | 117.29 | 680.70 | 245.58 | 680.70 | 87.29 | Stable | |
| Ca3CrO4 | 0 | 214.37 | 74.05 | 339.65 | 151.73 | 339.65 | 74.05 | Stable |
| 20 | 391.87 | 72.90 | 581.09 | 183.66 | 581.09 | 52.90 | Stable | |
| 30 | 466.44 | 74.19 | 657.38 | 245.97 | 657.38 | 44.19 | Stable | |
| Sr3CrO4 | 0 | 177.63 | 53.55 | 273.53 | 129.68 | 273.53 | 53.55 | Stable |
| 20 | 362.99 | 48.90 | 529.83 | 176.15 | 529.83 | 28.90 | Stable | |
| 30 | 444.05 | 42.07 | 638.57 | 219.53 | 638.57 | 12.07 | Stable | |
The equations for mechanical stability under pressure are given by,75
![]() | (6) |
As reported in Table 6, all investigated compounds satisfy both the Born and dynamical stability criteria, thereby confirming their reliability under the studied conditions.
| Mg3CrO4 | Ca3CrO4 | Sr3CrO4 | ||||||||
|---|---|---|---|---|---|---|---|---|---|---|
| 0 GPa | 20 GPa | 30 GPa | 0 GPa | 20 GPa | 30 GPa | 0 GPa | 20 GPa | 30 GPa | ||
| Elastic constants | C11 (GPa) | 239.07 | 343.78 | 478.14 | 214.37 | 391.87 | 466.44 | 177.63 | 362.99 | 444.05 |
| C12 (GPa) | 104.11 | 74.55 | 101.28 | 62.64 | 94.61 | 95.47 | 47.95 | 83.42 | 97.26 | |
| C44 (GPa) | 110.75 | 114.08 | 117.29 | 74.05 | 72.90 | 74.19 | 53.55 | 48.90 | 42.07 | |
| Bulk modulus B (GPa) | 149.09 | 164.29 | 226.9 | 113.21 | 193.69 | 219.12 | 71.17 | 176.61 | 212.85 | |
| Poisson ratio v | 0.24 | 0.20 | 0.24 | 0.22 | 0.284 | 0.288 | 0.23 | 0.31 | 0.37 | |
| Shear modulus G (GPa) | 90.79 | 121.89 | 141.94 | 74.77 | 97.37 | 108.16 | 45.07 | 75.67 | 77.47 | |
| Young modulus Y (GPa) | 226.41 | 293.17 | 352.36 | 183.84 | 250.20 | 278.64 | 111.65 | 198.64 | 207.28 | |
| Anisotropy factor A | 0.30 | 0.84 | 0.62 | 0.97 | 0.49 | 0.39 | 1.53 | 0.34 | 0.24 | |
| Pugh ratio B/G | 1.64 | 1.34 | 1.59 | 1.51 | 1.98 | 2.02 | 1.57 | 2.33 | 2.74 | |
| Kleinman parameter | 0.56 | 0.36 | 0.36 | 0.44 | 0.39 | 0.35 | 0.54 | 0.38 | 0.37 | |
| Nature | Brittle | Brittle | Brittle | Brittle | Ductile | Ductile | Brittle | Ductile | Ductile | |
| Other calculation46 | Mg3FeO4 | Ca3FeO4 | Sr3FeO4 | |||||||
| C11 | 254.61 | 244.81 | 181.69 | |||||||
| C12 | 102.51 | 57.60 | 51.81 | |||||||
| C44 | 117.35 | 101.21 | 88.62 | |||||||
| Bulk modulus B (GPa) | 153.21 | 120.01 | 95.10 | |||||||
| Poisson ratio v | 0.23 | 0.17 | 0.17 | |||||||
| Shear modulus G (GPa) | 98.62 | 98.09 | 78.24 | |||||||
| Anisotropy factor A | 1.54 | 1.08 | 1.36 | |||||||
| Pugh ratio B/G | 1.53 | 1.22 | 1.21 | |||||||
| Kleinman parameter | 0.54 | 0.38 | 0.43 | |||||||
| Nature | Brittle | Brittle | Brittle | |||||||
The formulations associated with the calculations of bulk modulus (B), shear modulus (G), Young's modulus (E), anisotropy (A), Poisson's ratio (v), Pugh's ratio (B/G), plasticity measurement (B/C44), and Kleinman parameter (ς) were computed using the following expressions, respectively,76–80
![]() | (7) |
![]() | (8) |
![]() | (9) |
![]() | (10) |
![]() | (11) |
![]() | (12) |
![]() | (13) |
![]() | (14) |
The elastic constants C11, C12 and C44 provide fundamental insights into a material's response to external stress. For all three investigating compounds C11 significantly increases with pressure, as shown in Fig. 7(a), indicating enhanced resistance to uniaxial compression. This trend is typical for solids under pressure, as interatomic distances decrease, leading to stronger bonds and a stiffer lattice.81 The increase in C12 and C44 also suggests increased resistance to shear deformation and improved shear stiffness under compression. The positive values of elastic constants across all the pressures satisfied the Born stability criteria of these cubic structures under the investigated conditions.
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| Fig. 7 (a–d) Variations in the elastic constants Cij, Young's modulus, Bulk modulus and Poisson's ratio of the A3CrO4 compounds (A = Mg, Ca, Sr) under hydrostatic pressures of 0–30 GPa. | ||
The bulk modulus representing resistance to volume change, consistently increases with pressure for all the compounds shown in Fig. 7(c). This indicates that all three compounds become significantly stiffer and less compressible under elevated pressure. The Young's modulus which measures stiffness also increases with pressure, reinforcing the observation of enhanced mechanical rigidity. Among the investigated compounds the Mg3CrO4 compounds are dominant throughout the pressure range shown in Fig. 7(b). These findings suggest that these chromates could potentially maintain their structural integrity in high-pressure environments making them candidates for applications requiring mechanically robust materials.60
Poisson's ratio, an elastic constant that describes how a material deforms sideways in response to longitudinal force, is also known as the transverse deformation coefficient. Poisson's ratio is a characteristic with a minimum value of approximately 0.2682 in most metals. A Poisson's ratio greater than 0.25 suggests predominantly ionic bonding in the compound, whereas a value below 0.25 indicates predominantly covalent bonding.83 The Poisson's ratio values indicate that Mg3CrO4 (v < 0.25) exhibits predominantly covalent bonding, whereas Ca3CrO4 and Sr3CrO4 (v > 0.25 at higher pressures) show a transition toward ionic bonding characteristics, consistent with their enhanced ductility under compression. For Mg3CrO4, Poisson's ratio fluctuates between 0.20 and 0.24 suggesting it remains relatively brittle. Ca3CrO4 shows an increase from 0.22 to 0.288 indicating a potential shift towards more ductile behavior at higher pressures. Notably, the Sr3CrO4 compound significantly increases from 0.23 at 0 GPa to 0.37 at 30 GPa pointing towards enhanced ductility under compression, as shown in Fig. 7(d). Ductile materials have potential applications in flexible electronics as well as photovoltaic cells, as the ability to sustain mechanical deformation without fracturing is needed.84 This increasing ductility with pressure is a desirable characteristic for materials used in extreme conditions where resistance to fracture is critical.60 Recent studies confirm that in perovskite oxides, applied pressure can induce a shift from covalent to ionic bonding, which enhances ductility and mechanical resilience critical for applications such as solid oxide fuel cells, thermoelectric, and spintronics.85,86 Agouri et al.87 demonstrated through first-principles calculations on PbXO3 (X = Ge, Si) perovskites that applied pressure induces a progressive shift from covalent to ionic bonding, thereby enhancing ductility and mechanical stability for energy applications. Similarly, Rahman et al.88 reported pressure-induced transitions in Ba3SbI3 perovskites, where bonding changes under compression were directly linked to improved ductility and optoelectronic performance.
The bulk to shear modulus ratio (B/G) is another important indicator of ductility. A B/G ratio greater than 1.75 often correlates with ductile behavior while values less than 1.75 suggest brittleness. Both Mg3CrO4 compounds generally maintain B/G ratios below or around 1.75 indicating brittle behavior. In contrast, the B/G ratio of Ca3CrO4 and Sr3CrO4 compounds transit from brittle characteristics at 0 GPa and from 20 GPa to 30 GPa further supporting its transition to a ductile state under high pressure.
The Kleinman parameter is crucial for understanding the nature of interatomic forces with a material, particularly distinguishing between bond-stretching and bond bending contributions to the elastic response. A Kleinman parameter closer to 0 indicates that bond-bending forces are more significant, while a value closer to 1 suggests a predominance of bond-stretching forces. The calculated Kleinman parameters for Mg3CrO4, Ca3CrO4, and Sr3CrO4 reveal a consistent decrease with increasing hydrostatic pressure (0–30 GPa). At ambient conditions, values around 0.44–0.56 indicate a balanced contribution of bond stretching and bond bending to the elastic response. However, under compression, the parameters drop toward 0.35–0.37, signifying that bond bending becomes increasingly dominant suggesting a significant shift in the materials elastic behaviour: bond bending becomes increasingly dominant over bond stretching under compression.89 This trend aligns with literature reports on perovskite oxides and halide crystals, where pressure enhances orbital overlap and shortens bond lengths, thereby favoring angular distortions over bond elongation. The persistence of stable Kleinman parameters across all pressures confirms the dynamical stability of these chromates, while the shift toward bond bending suggests enhanced mechanical flexibility. Such behavior is particularly relevant for piezoelectric and optoelectronic applications, where internal atomic displacements strongly influence polarization, optical absorption, and carrier transport.
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| Mg3CrO4 | Ca3CrO4 | Sr3CrO4 | |||||||
|---|---|---|---|---|---|---|---|---|---|
| 0 GPa | 20 GPa | 30 GPa | 0 GPa | 20 GPa | 30 GPa | 0 GPa | 20 GPa | 30 GPa | |
| Debye temperature θD | 731.37 | 831.93 | 890.97 | 621.89 | 691.73 | 717.48 | 445.70 | 489.67 | 480.74 |
| Average sound velocity | 5252.09 | 5766.36 | 6085.84 | 4875.50 | 5204.24 | 5314.84 | 3721.06 | 3898.81 | 3765.56 |
| Debye frequency ωD | 15.2 | 17.3 | 18.6 | 12.96 | 14.42 | 14.95 | 9.28 | 10.19 | 10.02 |
| Melting temperature Tm | 1965.90 | 2584.73 | 3378.80 | 1819.92 | 2868.95 | 3309.66 | 1248.19 | 2698.27 | 3177.33 |
| Gruneisen parameter | 1.066 | 1.003 | 1.058 | 1.041 | 1.23 | 1.28 | 1.05 | 1.16 | 1.20 |
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| Fig. 8 (a–d) Variations in Debye temperature, average sound velocity, Debye frequency, and melting temperature of A3CrO4 compounds (A = Mg, Ca, Sr) under hydrostatic pressures of 0–30 GPa. | ||
The average sound velocity is directly related to the stiffness of the materials and speed at which phonons propagate through the lattice. From Table 7 and Fig. 8(d) the average sound velocity of Mg3CrO4 and Ca3CrO4 consistently increases with pressure. This trend indicates a stiffening of the crystal lattice and stronger interatomic bonds under compression which is consistent with the general increase in elastic moduli observed in such materials under pressure. Higher sound velocities typically correlate with higher Debye temperature and melting temperatures, suggesting improved thermal stability and mechanical integrity at elevated pressures. In contrast Sr3CrO4 exhibits a more complex behavior where the average sound velocity increases from 3721.06 at 0 GPa to 3898.81 at 20 GPa but then slightly decrease to 3765.56 at 30 GPa. This anomaly might be indicative of a pressure induced change in its electronic and magnetic configurations potentially related to the magnetic reversal observed in previously analyses for Sr3CrO4 under higher pressures.
The Debye temperature (θD) is a key parameter relating to the maximum vibration frequency of atoms in a crystal lattice, and is directly linked to material stiffness and thermal conductivity. Although not directly measurable, θD can be reliably estimated from elastic modulus data using the following expressions,90
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As presented in Table 7 and Fig. 8(a), the Debye temperature generally increases with pressure indicating a stiffening of the lattice and potentially improved thermal stability. J. Zhang et al.91 and L. Zhang et al.92 reported that the Debye temperature increases with applied pressure, thereby confirming the suitability of these compounds for high-temperature applications. The results in Table 7 clearly demonstrate that the Debye temperature (θD) of A3CrO4 compounds increases with applied pressure, consistent with previous reports. For Mg3CrO4, θD rises from 731.37 K at 0 GPa to 890.97 K at 30 GPa, representing a substantial increase of 159.6 K. Similarly, Ca3CrO4 shows an increase from 621.89 K to 717.48 K, while Sr3CrO4 increases from 445.70 K to 480.74 K over the same pressure range. This systematic enhancement of θD under compression indicates stronger interatomic bonding and greater lattice rigidity, confirming the suitability of these compounds for high-temperature applications, in agreement with previous results. At 30 GPa, Sr3CrO4 exhibits a reduction in Debye temperature, unlike Mg3CrO4 and Ca3CrO4. While Mounaim Bencheikh et al.93 attributed decreases in θD at constant pressure to thermal expansion and lattice softening, this mechanism is unlikely under compression where volume expansion is suppressed. The more probable origin is a pressure-induced change in the magnetic state of Sr3CrO4 which modifies vibrational modes and reduces θD highlighting the role of magneto-elastic coupling in its lattice dynamics. Among them the Mg-based compounds exhibit the highest Debye temperatures among the materials studied, indicating stronger interatomic bonding and superior phonon-mediated thermal conductivity.93
The melting temperature plays a critical role in determining the thermal stability, performance, and applicability of materials across various scientific and industrial domains, including alloy design, nanoparticle stability, and high-temperature technologies.94 The melting temperature (Tm) is calculated using the following relationship.95
| Tm = 553 + 5.91C11 | (19) |
As illustrated in Table 7 and Fig. 8(c), the melting temperature Tm is consistently predicted to increase significantly with pressure for all chromates. The calculated melting temperatures (Tm) of A3CrO4 compounds show a clear increasing trend with pressure, reflecting enhanced lattice stability under compression. For Mg3CrO4, Tm rises from 1965.90 K at 0 GPa to 3378.80 K at 30 GPa. Ca3CrO4 exhibits a similar increase, from 1819.92 K to 3309.66 K, while Sr3CrO4 shows the most pronounced change, from 1248.19 K to 3177.33 K over the same pressure range. These results indicate that hydrostatic compression significantly strengthens interatomic bonding, thereby elevating the melting point.96 The systematic increase in Tm confirms the suitability of these compounds for high-temperature applications, consistent with literature reports that pressure enhances thermal stability in oxide materials.97 This strong correlation between pressure and melting temperature suggests that these materials can withstand much higher temperatures at elevated pressures which is a critical consideration for high temperature and high-pressure applications. Such high melting points are characteristic of robust ceramic materials.60
The Debye frequency (ωD) is a measure of the maximum vibrational frequency of atoms in a crystal lattice serving as a fundamental parameter in solid-state physics for understanding thermal properties. The Debye frequency for a given solid is calculated using the following expression.94
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From Table 7 and Fig. 8(b), the Debye frequency of Mg3CrO4 increases from 15.2 THz at 0 GPa to 18.6 THz at 30 GPa. Similarly, the Debye frequency of Ca3CrO4 also shows an increase from 12.96 THz to 14.95 THs. This increase signifies an enhanced stiffness of the phonon nodes under pressure implying a stronger lattice that can sustain higher frequency vibrations. Fr Sr3CrO4 the Debye frequency increases from 9.28 THz at 0 GPa to 10.19 THz at 20 GPa but then slightly decrease to 10.02 THz at 30 GPa, mirroring the trend observed in its average sound velocity. This behavior reinforces the hypothesis of pressure induced events affecting the lattice dynamics of Sr3CrO4.98 Materials with higher Debye frequencies are generally expected to have higher thermal conductivities and specific heats making these chromates potentially suitable for applications requiring efficient heat dissipation of thermal insulation under specific conditions.
Table 7 also reports the Gruneisen parameter (γ), which quantifies the anharmonicity of the lattice vibrations and the relationship between thermal expansion and changes in vibrational frequencies with volume. It is a parameter for understanding a materials thermal expansion coefficient and its response to temperature changes under pressure. This parameter is derived from Poisson's ratio using the following relationship.99
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The calculated values for investigated compounds under pressure remain close to unity, indicating moderate anharmonicity. A positive Gruneisen parameter implies that phonon frequencies increase upon compression, which is typical for most solids. The variations in this parameter provide insights into how each material's thermal properties will respond to external pressure, influencing applications where thermal stability and dimensional changes are critical. The observed increase in γ with pressure for Ca3CrO4 and Sr3CrO4 is consistent with literature reports by Mounaim Bencheikh et al.93 showing that compression amplifies anharmonic lattice responses by modifying phonon frequencies. In contrast, Mg3CrO4 shows only weak variation, suggesting greater anharmonic stability under hydrostatic compression. Overall, the results confirm that pressure enhances anharmonic effects in A3CrO4 compounds, while the magnitude of γ remains within the range typical for stable oxide materials. For instance, materials with low Gruneisen parameters tend to have low thermal expansion coefficients, desirable for precision components operating over wide temperature ranges.100
The observed pressure induced magnetic transition in our investigated compounds in the magnetic data discussed previously alongside the elastic property changes further emphasizes the intricate interplay between structural, electronic, elastic, thermodynamics and magnetic degrees of freedom in these materials.
In conclusion, the variations in average sound velocity, Debye frequency, and Gruneisen parameter with pressure provide a comprehensive picture of the lattice dynamics and thermal behavior of Mg3CrO4, Ca3CrO4 and Sr3CrO4. The consistent stiffening and enhanced thermal stability observed in Mg3CrO4 and Ca3CrO4 make them promising for high-pressure and high-temperature applications. The anomalous behavior of Sr3CrO4, particularly the decrease in sound velocity and Debye frequency at higher pressures, suggests a pressure-induced phenomenon that requires further investigation, potentially leading to new applications in pressure-tunable functional materials. These findings contribute to the broader understanding of complex oxides and their potential in advancing materials science and engineering.
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