Observation of Ferroelectric Hysteresis Loop of Fe3O4 at 4.2 K
Hysteresis
DOI:
10.1143/jpsj.51.1335
Publication Date:
2005-07-13T13:52:36Z
AUTHORS (2)
ABSTRACT
The existence of ferroelectricity in magnetite has been established by determining the c -axis component spontaneous polarization at 4.2 K. ferroelectric D - E hysteresis loop was observed changing applied electric field stepwise 5 kV/cm intervals 10 s between -15 and 15 kV/cm. It found that, K, coercive is extremely high leakage current still prominent. switching process d 20
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