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Volumn 97, Issue 23, 2010, Pages

Magnetic switch of polarization in epitaxial orthorhombic YMnO3 thin films

Author keywords

[No Author keywords available]

Indexed keywords

EPITAXIAL GROWTH; FERROELECTRICITY; MAGNETIC FIELDS; MANGANESE COMPOUNDS; POLARIZATION; THIN FILMS;

EID: 78650394845     PISSN: 00036951     EISSN: None     Source Type: Journal    
DOI: 10.1063/1.3523352     Document Type: Article
Times cited : (44)

References (21)
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    • Non-ferroelectric contributions to the hysteresis cycles in manganite thin films; A comparative study of measurement techniques
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    • I. Fina, L. F̀brega, E. Langenberg, X. Martí, F. Sánchez, M. Varela, and J. Fontcuberta, " Non-ferroelectric contributions to the hysteresis cycles in manganite thin films; A comparative study of measurement techniques.," J. Appl. Phys. JAPIAU 0021-8979 (submitted).
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    • Notice in Fig. that although the IPUND data are clearly irreversible, the features of a net switching current peak are not well visible; therefore one can not conclusively claim that the observed displacement charge measured corresponds to a ferroelectric polarization
    • Notice in Fig. that although the IPUND data are clearly irreversible, the features of a net switching current peak are not well visible; therefore one can not conclusively claim that the observed displacement charge measured corresponds to a ferroelectric polarization.
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    • Pole figures were collected to investigate the distribution of the intensity at an scattering angle of ∼25° corresponding to o-YMO (111) reflection, which is the most intense without any correspondence to substrate. Data revealed a strong texture o-YMO (100) and only a tiny amount of crystallites oriented o-YMO (010). The amount of the spurious texture is extremely low and does not exceed 1% of the total material.
    • Pole figures were collected to investigate the distribution of the intensity at an scattering angle of ∼25° corresponding to o-YMO (111) reflection, which is the most intense without any correspondence to substrate. Data revealed a strong texture o-YMO (100) and only a tiny amount of crystallites oriented o-YMO (010). The amount of the spurious texture is extremely low and does not exceed 1% of the total material.


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.