Rare-earth elements share similar ground-state electronic properties, and their unique lanthanide contraction effect can lower the mixing enthalpy of rare-earth elements in high-entropy materials, which is of paramount importance for the fabrication of low-cost and high-performance high-entropy rare-earth intermetallic compounds. In this paper, the magnetization reversal mechanisms of rapidly quenched ribbons such as Nd<sub>11.76</sub>Fe<sub>82.36</sub>B<sub>5.88</sub> (NdFeB) and the relevant high-entropy rare-earth permanent magnet alloy compounds (La<sub>0.2</sub>Pr<sub>0.2</sub>Nd<sub>0.2</sub>Gd<sub>0.2</sub>Dy<sub>0.2</sub>)<sub>11.76</sub>Fe<sub>82.36</sub>B<sub>5.88</sub>and (La<sub>0.2</sub>Pr<sub>0.2</sub>Nd<sub>0.2</sub>Gd<sub>0.2</sub>Tb<sub>0.2</sub>)<sub>11.76</sub>Fe<sub>82.36</sub>B<sub>5.88</sub>were studied by analyzing the magnetization and demagnetization curves, supplemented by Henkel curves and magnetic viscosity coefficient <i>S</i>. Compared to the pure NdFeB sample, the inter-grain exchange coupling in high-entropy rare-earth permanent magnets is significantly enhanced, while the magnetic dipole interaction is weakened, indicating that the element diffusion mechanism in heavy rare-earth containing high-entropy materials homogenizes the sample, and significantly increases the coercivity. The mechanism of the coercivity is the nucleation of magnetization reversal domains in the grains of the hard magnetic phase. The magnetization mechanism is dominated by pinning at low magnetic fields and by nucleation at high magnetic fields, which is different from the magnetization mechanism of pure NdFeB and has some similarities with the self-pinning mechanism. The magnetic viscosity coefficient of (La<sub>0.2</sub>Pr<sub>0.2</sub>Nd<sub>0.2</sub>Gd<sub>0.2</sub>Dy<sub>0.2</sub>)<sub>11.76</sub>Fe<sub>82.36</sub>B<sub>5.88</sub> is larger than that of pure NdFeB. Due to the asynchrony of hard magnetic phase reversal and intergranular magnetic coupling in (La<sub>0.2</sub>Pr<sub>0.2</sub>Nd<sub>0.2</sub>Gd<sub>0.2</sub>Tb<sub>0.2</sub>)<sub>11.76</sub>Fe<sub>82.36</sub>B<sub>5.88</sub>, the magnetic viscosity coefficient is small with a large anisotropy field. This indicates that high-entropy samples reduce the magnetocrystalline anisotropy field barrier while increasing the magnetocrystalline coupling length. This suggests that the magnetization reversal of high-entropy rare-earth permanent magnet materials are significantly different from those of conventional rare earth permanent magnet materials and warrant further in-depth studies.
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