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Magnetization and M?ssbauer study of double layer perovskites La1.5Ca1.5Mn2 ? x Fe x O7 prepared by sol–gel method

机译:双层钙钛矿La1.5 Ca1.5 Mn2α的磁化和M?ssbauer研究溶胶-凝胶法制备的x Fe x O7

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Magnetization and M?ssbauer studies have been made for understanding magnetic behavior of three double perovskite systems La1.5Ca1.5Mn2 ? x Fe x O7 corresponding to x = 0.05, 0.10 and 0.50. These have been prepared following sol–gel route. Substitution of Fe does not lead to any major change in the tetragonal cell but increased iron leads to greater distortion in octahedral site. The three samples undergo paramagnetic–ferromagnetic transition. Curie temperature (T c) for the system with 0.05 Fe is ~150 K which is lower than (190 K) for the system without iron; with 0.50 Fe T c goes below 50 K. Iron goes as Fe3 + and replaces Mn in ab plane. With increasing Fe the valence states of Mn get re-distributed in a way that number of the Jahn–Teller ions Mn3 + increases and that of the pairs of Mn3 + –O–Mn4 + experiencing double exchange decreases.
机译:已经进行磁化和Msssbauer研究来理解三种双钙钛矿体系La1.5 Ca1.5 Mn2?的磁行为。 x Fe x O7 对应于x = 0.05、0.10和0.50。这些是按照溶胶-凝胶法制备的。 Fe的取代不会导致四边形细胞发生任何重大变化,但是铁的增加会导致八面体位置更大的变形。这三个样品经历顺磁性-铁磁性转变。具有0.05 Fe的系统的居里温度(T c )为〜150 K,低于没有铁的系统的(190 K); Fe T c 的含量为0.50时低于50K。铁随着Fe3 + 的存在而在ab平面中取代Mn。随着Fe含量的增加,Mn的价态以Jahn–Teller离子Mn3 + 的数量增加,而Mn3 + –O–Mn4 +对的数量增加。 >两次交换减少。

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