Electrical transport in charge-ordered Fe2OBO3: Resistive switching and pressure effects

被引:12
作者
Akrap, Ana [1 ,2 ]
Angst, Manuel [3 ,4 ,5 ]
Khalifah, Peter [6 ]
Mandrus, David [3 ,7 ,8 ]
Sales, Brian C. [3 ]
Forro, Laszlo [1 ]
机构
[1] Ecole Polytech Fed Lausanne, Inst Phys Mat Complexe, CH-1015 Lausanne, Switzerland
[2] Brookhaven Natl Lab, Condensed Matter Phys & Mat Sci Dept, Upton, NY 11973 USA
[3] Oak Ridge Natl Lab, Div Mat Sci & Technol, Oak Ridge, TN 37831 USA
[4] Forschungszentrum Julich GmbH, Inst Festkorperforsch, JCNS, D-52425 Julich, Germany
[5] Forschungszentrum Julich GmbH, JARA FIT, D-52425 Julich, Germany
[6] Brookhaven Natl Lab, Dept Chem, Upton, NY 11973 USA
[7] Univ Tennessee, Dept Mat Sci, Knoxville, TN 37996 USA
[8] Univ Tennessee, Div Technol, Knoxville, TN 37996 USA
来源
PHYSICAL REVIEW B | 2010年 / 82卷 / 16期
基金
瑞士国家科学基金会;
关键词
DRIVEN PHASE-TRANSITION; DENSITY-WAVE; MANGANITES; SOLIDS;
D O I
10.1103/PhysRevB.82.165106
中图分类号
T [工业技术];
学科分类号
08 ;
摘要
The pressure-temperature-electric field phase diagram of Fe2OBO3 is studied under ambient and high pressure using resistivity and thermoelectric power measurements. The onset of the incommensurate charge order at T-CO=340 K does not depend on pressure up to at least 2 GPa. The temperature of the transition to the commensurate charge order is increased by similar to 10 K/GPa. High pressure stabilizes the commensurate phase. We find evidence for resistive switching in the incommensurate phase, which may be linked to the dynamics of the charge-order domain boundaries.
引用
收藏
页数:7
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