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- W1980278312 abstract "Abstract Magnetisation and susceptibility measurements have been performed on the oxygen isotope-substituted manganite Pr 0.7 Ca 0.3 Mn 16–18 O 3 in pulse magnetic fields up to 35 T in the temperature range 78–300 K. It was found that the charge-ordering transition temperature T CO ≈210 K and temperature of antiferromagnetic ordering T AFM ≈125 K in this narrow band manganite are independent on isotope content. The magnetic-field-induced transition into ferromagnetic state was observed in both isotope-substituted samples at temperatures T FM . Isotope substitution has been proved to have a significant impact on the critical field H C of this transition. We found that magnetisation curves are qualitatively different for both isotopic samples. The sample with natural oxygen has the positive derivative d H C /d T on the whole T–H plane. In compound with 18 O, H C is shifted to the higher fields ( H C ∼20 T), being nearly temperature-independent at T >120 K. As the temperature decreases ( T T AFM ), this transition disappears and a more complicated behaviour arises at magnetic fields 6–14 T." @default.
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- W1980278312 date "2004-04-01" @default.
- W1980278312 modified "2023-10-18" @default.
- W1980278312 title "Magnetic phase diagram of oxygen isotope-substituted Pr0.7Ca0.3Mn16–18O3" @default.
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- W1980278312 doi "https://doi.org/10.1016/j.physb.2004.01.026" @default.
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