Effect of pressure and magnetic field on the phase transitions in lanthanum-deficient manganites

V. Dyakonov, I. Fita, E. Zubov, V. Pashchenko, V. Mikhaylov, Yu. Bukhantsev, H. Szymczak
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Abstract

We report on the pressure, field and temperature dependencies of magnetization and resistance in manganites of (La1-xCax)1-yMn1+y O3 type. The M(T) dependencies is established to exhibit the following peculiarities: the first is connected with the paramagnet (PM)-ferromagnet (FM) transition at 267 K; the peak of M(T) dependence eat 263K is presumable due to an existence of AFM clusters; an anomaly in magnetization is connected with the FM-canted phase transition at 42K and the large irreversibility in the field-cooled and zero field- cooled magnetization. As field is increased above 200 Oe, the sign of the M(T) anomaly changes, namely, the M(T) magnetization increases with increasing field at 42K. The character of M(T) dependencies does not change under pressure. However, both the Curie temperature, Tc, and the resistance peak corresponding to metal-insulator transition shift in the direction of high temperatures with increasing pressure. A pressure stabilizes the ferromagnetic metallic phase. The temperature of the FM-canting phase transition does not change under pressure. The magneto resistance effect increase by 15 percent under pressure of 12.6 kbar.
压力和磁场对缺镧锰矿石相变的影响
我们报道了(La1-xCax)1-yMn1+ yo3型锰矿石磁化和电阻的压力、场和温度依赖关系。建立了M(T)依赖性,以显示以下特性:第一个与267 K时的顺磁体(PM)-铁磁体(FM)跃迁有关;由于AFM簇的存在,M(T)依赖性峰值约为263K;磁化强度的异常与42K时的fm倾斜相变以及场冷和零场冷磁化的大不可逆性有关。在200 Oe以上,随着磁场的增大,M(T)异常的符号发生变化,即在42K处,M(T)磁化强度随磁场的增大而增大。M(T)依赖性的特征在压力下不改变。但随着压力的增加,居里温度Tc和金属-绝缘子转变对应的电阻峰都向高温方向移动。压力使铁磁性金属相稳定。在压力作用下,相变温度不发生变化。在12.6 kbar的压力下,磁阻效应增加了15%。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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