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Low-temperature quasi-adiabatic magnetization reversal of rare-earth ising metamagnets

机译:稀土变磁超磁体的低温准绝热磁化反转

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The magnetization and magnetically induced elastic strains of rare-earth Ising antiferromagnets DyAlO3 and TbAlO3 are shown to exhibit an unusual behavior associated with low-temperature metamagnetic phase transitions. As an external magnetic field is applied and then removed slowly, the state of the magnetic system in these compounds follows quite different paths on the H-T diagram. Small alternating-sign variations in the field magnitude cause the magnetic system to switch reversibly from one path to another, which is accompanied by sharp changes in the magnetization and elastic strains. The observed anomalies are shown to be due to the magnetization process being quasi-adiabatic in character in the compounds under study. This fact should be taken into account in interpreting the data on the magnetization and magnetostriction in Ising antiferromagnets undergoing metamagnetic transitions at low temperatures. Experimentally, quasi-adiabatic magnetization makes it possible to determine the critical fields for metamagnetic transitions very exactly and to investigate the H-T phase diagram at temperatures that are far below the minimum temperature of a helium bath and are unattainable under strictly isothermal conditions. (c) 2005 Pleiades Publishing, Inc.
机译:稀土Ising反铁磁体DyAlO3和TbAlO3的磁化和磁感应弹性应变显示出与低温亚磁相变有关的异常行为。当施加外部磁场然后缓慢去除磁场时,这些化合物中磁系统的状态遵循H-T图上的完全不同的路径。磁场大小的微小交替符号变化会导致磁性系统从一条路径可逆地切换到另一条路径,并伴随着磁化强度和弹性应变的急剧变化。结果表明,观察到的异常是由于所研究化合物的磁化过程具有准绝热特性。在解释有关在低温下经历亚磁性跃迁的伊辛反铁磁体的磁化和磁致伸缩数据时,应考虑到这一事实。在实验上,准绝热磁化使得可以非常精确地确定亚磁跃迁的临界场,并研究在远低于氦浴最低温度且在严格等温条件下无法达到的温度下的H-T相图。 (c)2005年Pleiades Publishing,Inc.

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