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Charge ordered ferromagnetic phase in manganites

dc.citation.epage0en_US
dc.citation.issue14en_US
dc.citation.spage0en_US
dc.citation.volume67en_US
dc.citation.woscount11en_US
dc.contributor.authorMinh-Tien, Ten_US
dc.contributor.department電子物理學系zh_TW
dc.contributor.departmentDepartment of Electrophysicsen_US
dc.date.accessioned2019-04-03T06:38:13Z
dc.date.available2019-04-03T06:38:13Z
dc.date.issued2003-04-11en_US
dc.description.abstractA mechanism for charge ordered ferromagnetic phase in manganites is proposed. The mechanism is based on the double exchange in the presence of diagonal disorder. It is modeled by a combination of the Ising double-exchange and the Falicov-Kimball model. Within the dynamical mean-field theory the charge and spin correlation function are explicitly calculated. It is shown that the system exhibits two successive phase transitions. The first one is the ferromagnetic phase transition, and the second one is a charge ordering. As a result a charge ordered ferromagnetic phase is stabilized at low temperature.en_US
dc.identifier.doi10.1103/PhysRevB.67.144404en_US
dc.identifier.issn2469-9950en_US
dc.identifier.journalPHYSICAL REVIEW Ben_US
dc.identifier.urihttp://dx.doi.org/10.1103/PhysRevB.67.144404en_US
dc.identifier.urihttps://ir.lib.nycu.edu.tw/handle/11536/27963
dc.identifier.wosnumberWOS:000182718400034en_US
dc.language.isoen_USen_US
dc.titleCharge ordered ferromagnetic phase in manganitesen_US
dc.typeArticleen_US

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