Pressure induced canted ferromagnetic order in La1.32Sr1.68Mn2O7 layered manganite
被引:3
作者:
Kumaresavanji, M.
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机构:
Ctr Brasileiro Pesquisas Fis, Rua Dr Xavier Sigaud 150, Urca, RJ, BrazilCtr Brasileiro Pesquisas Fis, Rua Dr Xavier Sigaud 150, Urca, RJ, Brazil
Kumaresavanji, M.
[1
]
Reis, M. S.
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机构:
Univ Aveiro, CICECO, Aveiro, PortugalCtr Brasileiro Pesquisas Fis, Rua Dr Xavier Sigaud 150, Urca, RJ, Brazil
Reis, M. S.
[2
]
Xing, Y. T.
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Ctr Brasileiro Pesquisas Fis, Rua Dr Xavier Sigaud 150, Urca, RJ, BrazilCtr Brasileiro Pesquisas Fis, Rua Dr Xavier Sigaud 150, Urca, RJ, Brazil
Xing, Y. T.
[1
]
Fontes, M. B.
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Ctr Brasileiro Pesquisas Fis, Rua Dr Xavier Sigaud 150, Urca, RJ, BrazilCtr Brasileiro Pesquisas Fis, Rua Dr Xavier Sigaud 150, Urca, RJ, Brazil
Fontes, M. B.
[1
]
机构:
[1] Ctr Brasileiro Pesquisas Fis, Rua Dr Xavier Sigaud 150, Urca, RJ, Brazil
[2] Univ Aveiro, CICECO, Aveiro, Portugal
来源:
INTERNATIONAL CONFERENCE ON MAGNETISM (ICM 2009)
|
2010年
/
200卷
关键词:
DOUBLE EXCHANGE;
CRYSTAL;
D O I:
10.1088/1742-6596/200/5/052013
中图分类号:
T [工业技术];
学科分类号:
08 ;
摘要:
The electrical resistance, magnetization and magnetoresistance of La1.32Sr1.68Mn2O7 layered manganite have been studied under hydrostatic pressure and magnetic field. At ambient pressure, the temperature dependence of the magnetization shows a ferromagnetic to paramagnetic transition at 118 K. Close to this transition, we have also observed a metal-insulator transition at T = T-MI(1) in the temperature dependence of the resistivity rho(T) measurement. The increasing pressure enhances a second metal-insulator transition T-MI(2) at a critical pressure 6 <= P-C <= 7 kbar. With further increasing pressure, both the T-MI(1) and T-MI(2) shift to high temperatures and the peak resistivity suppresses abruptly. We could not observe any transition correspond to T-MI(2) in the temperature dependence of the magnetization up to 10.2 kbar. A large negative tunneling magnetoresistance was observed around T-C in the field dependence of the rho(T) curves and the pressure reduces magnetoresistance ratio significantly. From our results, we argue that the increasing pressure induces a canted ferromagnetic order which leads to a ferromagnetic insulating phase at low temperature.