2003
DOI: 10.1016/s0304-8853(03)00201-4
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Staircase effect in metamagnetic transitions of charge and orbitally ordered manganites

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Cited by 90 publications
(95 citation statements)
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“…These observations are also identical to the behavior of phase-separated manganites and Gd 5 Ge 4 . 11,15,17,20 In the case of manganites, the different crystal structures of the FM and AFM phases in the phase-separated state is responsible for the sweep rate dependence. The sweep rate dependence of the step behavior is a signature of martensitic strains in the system.…”
Section: Resultsmentioning
confidence: 99%
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“…These observations are also identical to the behavior of phase-separated manganites and Gd 5 Ge 4 . 11,15,17,20 In the case of manganites, the different crystal structures of the FM and AFM phases in the phase-separated state is responsible for the sweep rate dependence. The sweep rate dependence of the step behavior is a signature of martensitic strains in the system.…”
Section: Resultsmentioning
confidence: 99%
“…[14][15][16][17][18][19][20] Among the intermetallics, Gd 5 Ge 4 is known to show many similarities with the oxides. 11,23 Though there are several factors thought to be responsible for the multistep behavior, the most striking and accepted reason common to the oxide materials and the intermetallics seems to be the martensitic transition driven by the applied field.…”
Section: Discussionmentioning
confidence: 99%
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“…Two small samples were cut out from the crystal in order to perform the different measurements: a cube of about 10 mm 3 for the magnetization and transport measurements, and a parallelepiped of about 40 mm 3 for the SANS measurements. Prior to characterizations, the purity of the sample was checked by energy dispersive spectroscopy, X-ray, electron and neutron diffraction.…”
Section: Methodsmentioning
confidence: 99%
“…The present features could also correspond to the pseudo CE-type AFM to FM transition. 23 In the disordered (due to size reduction) manganites, the slight mismatch in the unit cell parameters of competing FMM and AFI-CO phases generates a notable strain at the interface regions, creating a situation similar as for the strain accommodation observed in classical Martensite phase transition, 24 which may explain the current behaviour.…”
Section: B Pulse Field Magnetic Propertiesmentioning
confidence: 91%