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Structural and magnetic properties in the nonstoichiometric perovskite-type oxides La0.67Sr0.150.18MnO3−δ

机译:非化学计量钙钛矿型氧化物La 0.67 Sr 0.15 0.18 MnO 3-δ的结构和磁性

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Due to many novel phenomena such as colossal magnetoresistance (CMR), magnetocaloric effect (MCE) and possible applications to magnetic devices, hole-doped lanthanum manganites La1−xAxMnO3 family (here A is divalent element such as Ca, Sr, Ba, Pb and etc.) have been intensively studied [1–2]. Their potential for application is based on coupling of spin and charge orders of freedom. Controlling the oxygen content in manganites is crucial in order to obtain well defined magnetic and transport properties [3]. Oxygen content in manganites can be well adjusted experimentally by varying the thermal treatments which is most likely to form the oxygen vacancies in the unit cell. On the other hand, a change of oxygen content may also cause a change in lattice constant. Therefore, one may expect that the properties of manganites with varied oxygen content would be as interesting as those of manganites based on A-site doping.
机译:由于许多新现象,例如巨大的磁阻(CMR),磁热效应(MCE)以及在磁性器件中的可能应用,带孔掺杂的锰镧镧La1 -x A x MnO 3 族(这里的A是二价元素,例如Ca,Sr,Ba,Pb等)已被深入研究[1-2]。它们的应用潜力基于自旋和电荷自由度的耦合。为了获得明确定义的磁性和运输性能,控制锰中的氧含量至关重要[3]。通过改变最有可能在晶胞中形成氧空位的热处理,可以通过实验很好地调节锰矿中的氧含量。另一方面,氧含量的变化也可能引起晶格常数的变化。因此,人们可能希望改变含氧量的锰矿的特性与基于A位置掺杂的锰矿的特性一样有趣。

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