Effect of Eu Doping and Partial Oxygen Isotope Substitution on Magnetic Phase Transitions in (Pr1-yEuy)0.7Ca0.3CoO3 Cobaltites

被引:5
作者
Babushkina, N. A. [1 ]
Taldenkov, A. N. [1 ]
Streltsov, S. V. [2 ,3 ]
Kalinov, A. V. [4 ]
Kuzmova, T. G. [5 ]
Kamenev, A. A. [5 ]
Kaul, A. R. [5 ]
Khomskii, D. I. [6 ]
Kugel, K. I. [7 ]
机构
[1] IV Kurchatov Atom Energy Inst, Natl Res Ctr, Moscow 123182, Russia
[2] Russian Acad Sci, Inst Met Phys, Ural Branch, Ekaterinburg 620990, Russia
[3] Ural Fed Univ, Ekaterinburg 620002, Russia
[4] All Russian Elect Engn Inst, Moscow 111250, Russia
[5] Moscow MV Lomonosov State Univ, Dept Chem, Moscow 119991, Russia
[6] Univ Cologne, Phys Inst 2, D-50937 Cologne, Germany
[7] Russian Acad Sci, Inst Theoret & Appl Electrodynam, Moscow 125412, Russia
基金
俄罗斯基础研究基金会;
关键词
INTERMEDIATE-SPIN STATE; METAL TRANSITION; LACOO3; MANGANITES; EXCHANGE;
D O I
10.1134/S1063776114010026
中图分类号
O4 [物理学];
学科分类号
0702 ;
摘要
We study experimentally and theoretically the effect of Eu doping and partial oxygen isotope substitution on the transport and magnetic characteristics and spin-state transitions in (Pr1-yEuy)(0.7)Ca0.3CoO3 cobaltites. The Eu doping level y is chosen in the range of the phase diagram near the crossover between the ferromagnetic and spin-state transitions (0.10 < y < 0.20). We prepared a series of samples with different degrees of enrichment by the heavy oxygen isotope O-18, namely, with 90, 67, 43, 17, and 0% of O-18. Based on the measurements of the ac magnetic susceptibility chi(T) and electrical resistivity rho(T), we analyze the evolution of the sample properties with a change of the Eu and O-18 content. It is demonstrated that the effect of increasing the O-18 content on the system is similar to that of increasing the Eu content. The band structure calculations of the energy gap between t(2g) and e(g) bands including the renormalization of this gap due to the electron-phonon interaction reveals the physical mechanisms underlying this similarity.
引用
收藏
页码:266 / 278
页数:13
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