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55Mn NMR Study of the Field-Controlled Magnetic Phase Separation in (La0.25Pr0.75)0.7Ca0.3MnO3 with Different Oxygen Isotope Content
Strongly Correlated Electrons · Submitted 20 Sep 2002
abstract compiled · 2026-09-23 · no language-model review
The authors' main claim Its relative fraction can be controlled by external magnetic field and the resulting magnetic structure in the PS region is discussed.
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The abstract, sentence by sentence
An influence of the 16O-18O isotope substitutions on magnetic state of perovskite-type manganite (La0.25Pr0.75)0.7Ca0.3MnO3 is studied by 55Mn NMR. Successive cycling with an isochronal exposure at different magnetic fields up to H=8T is used to study the field-induced transition from antiferromagnetic insulating (AFI) state to the ferromagnetic metal (FMM) one in the 18O-enriched sample. After exposure at H>H_{cr} \sim 5.3T the NMR spectrum of the 18O-sample evidences for magnetic phase separation (PS) resulted in the coexisting AFI and FMM domains. Further increase of exposing field leads to a progressive growth of the FMM phase at the expense of AFI domains. Its relative fraction can be controlled by external magnetic field and the resulting magnetic structure in the PS region is discussed. Anomalous T-dependence of the 55Mn nuclear spin-lattice relaxation rate is revealed in the FMM state of both 16O-and 18O-enriched samples. The manifestation of the Pr magnetic ordering at T \sim 40K is considered.
background contribution method result interpretation main claim
| # | sentence | role | the authors' own work | states the main conclusion | strength |
|---|---|---|---|---|---|
| s0 | An influence of the 16O-18O isotope substitutions on magnetic state of perovskite-type manganite (La0.25Pr0.75)0.7Ca0.3MnO3 is studied by 55Mn NMR. | contribution 0.97 | 0.92 | 0.05 | asserted 0.97 |
| s1 | Successive cycling with an isochronal exposure at different magnetic fields up to H=8T is used to study the field-induced transition from antiferromagnetic insulating (AFI) state to the ferromagnetic metal (FMM) one in the 18O-enriched sample. | method 0.99 | 0.94 | 0.07 | asserted 0.98 |
| s2 | After exposure at H>H_{cr} \sim 5.3T the NMR spectrum of the 18O-sample evidences for magnetic phase separation (PS) resulted in the coexisting AFI and FMM domains. | result 1.00 | 0.94 | 0.37 | asserted 0.94 |
| s3 | Further increase of exposing field leads to a progressive growth of the FMM phase at the expense of AFI domains. | result 1.00 | 0.91 | 0.16 | asserted 1.00 |
| s4 | Its relative fraction can be controlled by external magnetic field and the resulting magnetic structure in the PS region is discussed. | interpretation 0.61 | 0.75 | 0.24 | asserted 0.94 |
| s5 | Anomalous T-dependence of the 55Mn nuclear spin-lattice relaxation rate is revealed in the FMM state of both 16O-and 18O-enriched samples. | result 1.00 | 0.95 | 0.08 | asserted 1.00 |
| s6 | The manifestation of the Pr magnetic ordering at T \sim 40K is considered. | result 0.89 | 0.74 | 0.05 | asserted 0.70 |
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Original abstract
An influence of the 16O-18O isotope substitutions on magnetic state of perovskite-type manganite (La0.25Pr0.75)0.7Ca0.3MnO3 is studied by 55Mn NMR. Successive cycling with an isochronal exposure at different magnetic fields up to H=8T is used to study the field-induced transition from antiferromagnetic insulating (AFI) state to the ferromagnetic metal (FMM) one in the 18O-enriched sample. After exposure at H>H_{cr} \sim 5.3T the NMR spectrum of the 18O-sample evidences for magnetic phase separation (PS) resulted in the coexisting AFI and FMM domains. Further increase of exposing field leads to a progressive growth of the FMM phase at the expense of AFI domains. Its relative fraction can be controlled by external magnetic field and the resulting magnetic structure in the PS region is discussed. Anomalous T-dependence of the 55Mn nuclear spin-lattice relaxation rate is revealed in the FMM state of both 16O-and 18O-enriched samples. The manifestation of the Pr magnetic ordering at T \sim 40K is considered.
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