Magnetic Studies on Gd-doped Perovskite Manganese Oxide Pr<sub>0.87</sub>Ca<sub>0.13</sub>MnO<sub>3</sub>

Perovskite manganese oxide doped with rare earth elements has great potential in magnetic refrigeration. Due to the prohibition of freon refrigerants and the greenhouse effect, the green and pollution-free magnetic refrigeration technology has been widely studied. Pr<sub>(0.87-<italic>x</italic>)</sub>Gd<sub><italic>x</italic></sub>Ca<sub>0.13</sub>MnO<sub>3</sub>(<italic>x</italic> = 0,0.05,0.10,0.15)series polycrystalline samples were produced by high temperature solid phase reaction method. The effects of doping amounts of Gd<sup>3+</sup> on the structure, magnetic properties of parent Pr<sub>0.87</sub>Ca<sub>0.13</sub>MnO<sub>3</sub> samples were systematically investigated. The spatial point group of Pr<sub>(0.87-<italic>x</italic>)</sub>Gd<sub><italic>x</italic></sub>Ca<sub>0.13</sub>MnO<sub>3</sub>(<italic>x</italic> = 0, 0.05,0.10,0.15)series polycrystalline samples is the orthorhombic system Pnma, with the addition of Gd<sup>3+</sup>, lattice parameters (a, b, c) are gradually decreasing. This trend can be attributed to the partial substition of Gd<sup>3+</sup> (ionic radius: 0.0938 nm) for Pr<sup>3+</sup> (ionic radius: 0.099 nm), which has a smaller ionic radius. All samples in this series exhibit the typical characteristics of preformed cluster phase. The absolute values of the maximum magnetic entropy change (|??| ) are 4.26962 J·kg<sup>-1</sup>·K<sup>-1</sup>(<italic>x</italic> =0)、4.89822 J·kg<sup>-1</sup>·K<sup>-1</sup>(<italic>x</italic> =0.05)、6.26870 J·kg<sup>-1</sup> ·K<sup>-1</sup>(<italic>x</italic> = 0.1)、5.92600 J·kg<sup>-1</sup> ·K<sup>-1</sup>(<italic>x</italic> = 0.15), respectively. The adiabatic temperatures (Δ<italic>T</italic><sub><italic>ad</italic></sub> ) were 3.76 K, 4.49 K, 6.52 K, and 6.39 K, respectively. All Arott display positive slopes, a characteristic that persists in the vicinity of the Curie temperature (<italic>T</italic><sub>C</sub>), indicating that the paramagneticferromagnetic transformation in all samples are second-order phase transitions. The results show that the critical behavior of Pr<sub>0.87</sub>Ca<sub>0.13</sub>MnO<sub>3</sub> and Pr<sub>0.72</sub>Gd<sub>0.15</sub>Ca<sub>0.13</sub>MnO<sub>3</sub> samples is more similar to the mean field model, and the critical behavior of Pr<sub>0.82</sub>Gd<sub>0.05</sub>Ca<sub>0.13</sub>MnO<sub>3</sub> samples is more similar to the 3D Heisenberg model. The phase transition critical behavior of Pr<sub>0.77</sub>Gd<sub>0.1</sub>Ca<sub>0.13</sub>MnO<sub>3</sub> samples is more similar to the three-critical model.

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Publication Details

Journal
Chinese Rare Earths
Published
2025-12-01
DOI
https://doi.org/10.3724/s1004-0277.202506011
Primary Topic
Magnetic and transport properties of perovskites and related materials
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article
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article

Magnetic Studies on Gd-doped Perovskite Manganese Oxide Pr0.87Ca0.13MnO3

Huiqin Yun, Xiang Jin, Jianjun Zhao, Ru Xing et al.
Chinese Rare Earths
Magnetic and transport properties of perovskites and related materials
article

Magnetic Studies on Gd-doped Perovskite Manganese Oxide Pr0.87Ca0.13MnO3

Huiqin Yun, Xiang Jin, Jianjun Zhao, Ru Xing, Zhendong Hao
article en

Abstract

Perovskite manganese oxide doped with rare earth elements has great potential in magnetic refrigeration. Due to the prohibition of freon refrigerants and the greenhouse effect, the green and pollution-free magnetic refrigeration technology has been widely studied. Pr<sub>(0.87-<italic>x</italic>)</sub>Gd<sub><italic>x</italic></sub>Ca<sub>0.13</sub>MnO<sub>3</sub>(<italic>x</italic> = 0,0.05,0.10,0.15)series polycrystalline samples were produced by high temperature solid phase reaction method. The effects of doping amounts of Gd<sup>3+</sup> on the structure, magnetic properties of parent Pr<sub>0.87</sub>Ca<sub>0.13</sub>MnO<sub>3</sub> samples were systematically investigated. The spatial point group of Pr<sub>(0.87-<italic>x</italic>)</sub>Gd<sub><italic>x</italic></sub>Ca<sub>0.13</sub>MnO<sub>3</sub>(<italic>x</italic> = 0, 0.05,0.10,0.15)series polycrystalline samples is the orthorhombic system Pnma, with the addition of Gd<sup>3+</sup>, lattice parameters (a, b, c) are gradually decreasing. This trend can be attributed to the partial substition of Gd<sup>3+</sup> (ionic radius: 0.0938 nm) for Pr<sup>3+</sup> (ionic radius: 0.099 nm), which has a smaller ionic radius. All samples in this series exhibit the typical characteristics of preformed cluster phase. The absolute values of the maximum magnetic entropy change (|??| ) are 4.26962 J·kg<sup>-1</sup>·K<sup>-1</sup>(<italic>x</italic> =0)、4.89822 J·kg<sup>-1</sup>·K<sup>-1</sup>(<italic>x</italic> =0.05)、6.26870 J·kg<sup>-1</sup> ·K<sup>-1</sup>(<italic>x</italic> = 0.1)、5.92600 J·kg<sup>-1</sup> ·K<sup>-1</sup>(<italic>x</italic> = 0.15), respectively. The adiabatic temperatures (Δ<italic>T</italic><sub><italic>ad</italic></sub> ) were 3.76 K, 4.49 K, 6.52 K, and 6.39 K, respectively. All Arott display positive slopes, a characteristic that persists in the vicinity of the Curie temperature (<italic>T</italic><sub>C</sub>), indicating that the paramagneticferromagnetic transformation in all samples are second-order phase transitions. The results show that the critical behavior of Pr<sub>0.87</sub>Ca<sub>0.13</sub>MnO<sub>3</sub> and Pr<sub>0.72</sub>Gd<sub>0.15</sub>Ca<sub>0.13</sub>MnO<sub>3</sub> samples is more similar to the mean field model, and the critical behavior of Pr<sub>0.82</sub>Gd<sub>0.05</sub>Ca<sub>0.13</sub>MnO<sub>3</sub> samples is more similar to the 3D Heisenberg model. The phase transition critical behavior of Pr<sub>0.77</sub>Gd<sub>0.1</sub>Ca<sub>0.13</sub>MnO<sub>3</sub> samples is more similar to the three-critical model.

Chinese Rare EarthsVol. 46(6)
Openalex Percentile: Top 72%
Magnetic and transport properties of perovskites and related materials
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