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The origin of bulk magnetoresistivity in manganites

机译:锰矿中体磁电阻率的起源

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On substitution of Ca2+ for La3+ in LaMnO3, the compound La1-xCaxMnO3 becomes a ferromagnetic metal for 0.18 less than or equal to x < 0,5, The hopping of an electron from Mn3+ to O2- is associated with simultaneous hop from the latter to Mn4+, The probability of the hopping by this double exchange is highest when both hopping electrons have the same spin orientation, requiring Mn ions to be ordered ferromagnetically, The metallic behavior is synergistically associated with the ferromagnetic order through electron hopping, The resistivity increases considerably near the Curie temperature (T-C) and application of a magnetic field causes a dramatic decrease in resistivity due to regeneration of metallicity, The origin of this colossal magnetoresistivity is rather enigmatic and has attracted lot of attention from researchers, We have addressed this problem using emission Mossbauer spectroscopy where the local probe Co-57/Fe-57 substituting Mn atoms senses the microscopic behavior of the material. We find that the long-range ferromagnetic order breaks down anomalously below T-C and the material degenerates into small spin clusters which fluctuate rapidly and which exhibit superparamagnetic-like behavior. On a time scale of 10(-8) s, the spin clusters exhibit minimal lattice distortions, These spin clusters survive well above T-C and would constitute very effective scattering centers for charge carriers due to their rapid fluctuations. On application of an external magnetic field, the small magnetic clusters coalesce to form larger ones with more ordered spins, and the material shows enhanced conductivity through percolation, We also observe superparamagnetic-like behavior below T-C in the pyrochlore, Tl2Mn2(Co-57)O-7, which does not exhibit double exchange electron hopping, It seems that the breakup into small rapidly fluctuating ferromagnetic spin clusters near T-C (exhibiting superparamagnetic-like behavior) is a prerequisite for observing bulk magnetoresistivity, (C) 2000 Academic Press [References: 51]
机译:用Ca2 +代替LaMnO3中的La3 +时,化合物La1-xCaxMnO3变成铁磁性金属,其x小于或等于x <0.5时为0.18。电子从Mn3 +跃迁至O2-与从后者跃迁至O2-有关。 Mn4 +,当两个跳跃电子都具有相同的自旋取向时,通过双交换发生跳跃的可能性最高,这要求Mn离子具有铁磁有序性,通过电子跳跃,金属行为与铁磁有协同作用,在附近,电阻率显着增加由于金属的再生,居里温度(TC)和磁场的施加会导致电阻率急剧下降。这种巨大的磁阻现象的起源颇为神秘,引起了研究人员的广泛关注,我们已经使用Mossbauer发射解决了这个问题光谱中用局部探针Co-57 / Fe-57取代Mn原子来感测m的微观行为空中我们发现,远距离铁磁序在温度低于T-C时异常分解,并且材料退化为小的自旋簇,该簇快速波动并且表现出超顺磁性的行为。在10(-8)s的时间尺度上,自旋簇表现出最小的晶格畸变。这些自旋簇在T-C以上生存,并且由于其快速波动而对电荷载流子构成非常有效的散射中心。在外部磁场的作用下,小的磁团簇聚结形成更大的,具有更多有序自旋的团簇,并且该材料通过渗滤显示出增强的电导率。我们还观察到在烧绿石中,TC以下的超顺磁行为,Tl2Mn2(Co-57) O-7,不表现出双交换电子跳跃,似乎在TC附近分裂成小的快速波动的铁磁自旋簇(表现出超顺磁性)是观察体磁电阻率的先决条件,(C)2000 Academic Press [References :51]

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