{"title":"多晶 La0.6Sr0.4Fe1-xCuxO3-δ 的弹性和磁性能","authors":"Boren Xue, Xuenong Ying, Xiaomei Lu","doi":"10.1002/pssb.202400218","DOIUrl":null,"url":null,"abstract":"Perovskite La<jats:sub>0.6</jats:sub>Sr<jats:sub>0.4</jats:sub>Fe<jats:sub>1−<jats:italic>x</jats:italic></jats:sub>Cu<jats:sub><jats:italic>x</jats:italic></jats:sub>O<jats:sub>3−<jats:italic>δ</jats:italic></jats:sub> (<jats:italic>x</jats:italic> = 0, 0.05, 0.1, and 0.2) polycrystalline samples have been synthesized in air and investigated by X‐Ray diffraction, scanning electron microscope, magnetization, and mechanical spectroscopy. An antiferromagnetic transition is observed around 300 K, while no corresponding anomaly is observed in the mechanical spectrum, indicating the absence of conventional magnetoelastic coupling. For La<jats:sub>0.6</jats:sub>Sr<jats:sub>0.4</jats:sub>FeO<jats:sub>3</jats:sub>, an internal friction peak (P1) presents around 140 K and shifts to lower temperatures with increasing Cu‐doping content. Meanwhile, a magnetic anomaly is also observed around P1 peak temperature. As explained, the P1 peak is related to the freezing of the ferroelastic domain walls, and the mechanical energy dissipation is induced by the lagging variation of the octahedral tilting under the alternating stress. This work suggests a peculiar magnetic property of the octahedra within ferroelastic domain walls.","PeriodicalId":20406,"journal":{"name":"Physica Status Solidi B-basic Solid State Physics","volume":"46 1","pages":""},"PeriodicalIF":1.5000,"publicationDate":"2024-07-22","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Anelastic and Magnetic Properties of Polycrystalline La0.6Sr0.4Fe1−xCuxO3−δ\",\"authors\":\"Boren Xue, Xuenong Ying, Xiaomei Lu\",\"doi\":\"10.1002/pssb.202400218\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"Perovskite La<jats:sub>0.6</jats:sub>Sr<jats:sub>0.4</jats:sub>Fe<jats:sub>1−<jats:italic>x</jats:italic></jats:sub>Cu<jats:sub><jats:italic>x</jats:italic></jats:sub>O<jats:sub>3−<jats:italic>δ</jats:italic></jats:sub> (<jats:italic>x</jats:italic> = 0, 0.05, 0.1, and 0.2) polycrystalline samples have been synthesized in air and investigated by X‐Ray diffraction, scanning electron microscope, magnetization, and mechanical spectroscopy. An antiferromagnetic transition is observed around 300 K, while no corresponding anomaly is observed in the mechanical spectrum, indicating the absence of conventional magnetoelastic coupling. For La<jats:sub>0.6</jats:sub>Sr<jats:sub>0.4</jats:sub>FeO<jats:sub>3</jats:sub>, an internal friction peak (P1) presents around 140 K and shifts to lower temperatures with increasing Cu‐doping content. Meanwhile, a magnetic anomaly is also observed around P1 peak temperature. As explained, the P1 peak is related to the freezing of the ferroelastic domain walls, and the mechanical energy dissipation is induced by the lagging variation of the octahedral tilting under the alternating stress. This work suggests a peculiar magnetic property of the octahedra within ferroelastic domain walls.\",\"PeriodicalId\":20406,\"journal\":{\"name\":\"Physica Status Solidi B-basic Solid State Physics\",\"volume\":\"46 1\",\"pages\":\"\"},\"PeriodicalIF\":1.5000,\"publicationDate\":\"2024-07-22\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Physica Status Solidi B-basic Solid State Physics\",\"FirstCategoryId\":\"101\",\"ListUrlMain\":\"https://doi.org/10.1002/pssb.202400218\",\"RegionNum\":4,\"RegionCategory\":\"物理与天体物理\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q3\",\"JCRName\":\"PHYSICS, CONDENSED MATTER\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Physica Status Solidi B-basic Solid State Physics","FirstCategoryId":"101","ListUrlMain":"https://doi.org/10.1002/pssb.202400218","RegionNum":4,"RegionCategory":"物理与天体物理","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q3","JCRName":"PHYSICS, CONDENSED MATTER","Score":null,"Total":0}
引用次数: 0
摘要
我们在空气中合成了透辉石 La0.6Sr0.4Fe1-xCuxO3-δ(x = 0、0.05、0.1 和 0.2)多晶样品,并通过 X 射线衍射、扫描电子显微镜、磁化和机械光谱进行了研究。在 300 K 附近观察到了反铁磁性转变,而在机械光谱中没有观察到相应的异常,这表明不存在传统的磁弹性耦合。对于 La0.6Sr0.4FeO3,一个内摩擦峰(P1)出现在 140 K 左右,并随着铜掺杂含量的增加而向更低的温度移动。同时,在 P1 峰温度附近还观察到磁异常。据解释,P1 峰与铁弹性域壁的冻结有关,而机械能耗散则是由交变应力下八面体倾斜的滞后变化引起的。这项研究表明,铁弹性畴壁内的八面体具有奇特的磁性。
Anelastic and Magnetic Properties of Polycrystalline La0.6Sr0.4Fe1−xCuxO3−δ
Perovskite La0.6Sr0.4Fe1−xCuxO3−δ (x = 0, 0.05, 0.1, and 0.2) polycrystalline samples have been synthesized in air and investigated by X‐Ray diffraction, scanning electron microscope, magnetization, and mechanical spectroscopy. An antiferromagnetic transition is observed around 300 K, while no corresponding anomaly is observed in the mechanical spectrum, indicating the absence of conventional magnetoelastic coupling. For La0.6Sr0.4FeO3, an internal friction peak (P1) presents around 140 K and shifts to lower temperatures with increasing Cu‐doping content. Meanwhile, a magnetic anomaly is also observed around P1 peak temperature. As explained, the P1 peak is related to the freezing of the ferroelastic domain walls, and the mechanical energy dissipation is induced by the lagging variation of the octahedral tilting under the alternating stress. This work suggests a peculiar magnetic property of the octahedra within ferroelastic domain walls.
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