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.
Authors
- Huiqin Yun (ORCID: https://orcid.org/0009-0002-1225-1176)
- Xiang Jin (ORCID: https://orcid.org/0000-0001-5293-6335)
- Jianjun Zhao (ORCID: https://orcid.org/0000-0001-9619-5735)
- Ru Xing (ORCID: https://orcid.org/0009-0005-0204-7202)
- Zhendong Hao
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
- Type
- article
- Field-Weighted Citation Impact
- 0.00