This article is cited in
4 papers
Magnetism
Structure, phase transitions, $^{55}$Mn NMR, and magnetoresistive properties of La$_{0.6}$Sr$_{0.2}$Mn$_{1.2-y}$Cr$_y$O$_{3\pm\delta}$
A. V. Pashchenkoab,
V. P. Pashchenkoac,
A. G. Silchevad,
V. K. Prokopenkoa,
A. A. Shemyakova,
Yu. F. Revenkoa,
V. P. Komarovc,
S. V. Gorban'b a Galkin Donetsk Institute for Physics and Engineering, Donetsk
b Donetsk National University of Economics and Trade named after M. I. Tugan-Baranovsky, Donetsk
c Research Institute "Reactivelectron"
d Lugansk Taras Shevchenko National University
Abstract:
The structure and properties of lanthanum strontium manganite perovskites La
$_{0.6}$Sr
$_{0.2}$Mn
$_{1.2-y}$Cr
$_y$O
$_{3\pm\delta}$ (
$y$ = 0 – 0.3) sintered at 1430
$^\circ$C have been studied by X-ray, resistive, and magnetic (
$\chi_{\mathrm{ac}}$ and
$^{55}$Mn NMR) methods. The parameter of the rhombohedrally distorted
$(R\bar3c)$ perovskite structure decreases with increasing
$y$. The real perovskite structure contains point (anion and cation vacancies) and cluster-type nanostructure defects. The analysis of asymmetrically broadened
$^{55}$Mn NMR spectra has confirmed the high-frequency electron-hole exchange Mn
$^{3+}$ $\leftrightarrow$ Mn
$^{4+}$ and local inhomogeneity of their surrounding by other ions and point and cluster-type defects. An increase in the Cr content leads to an increase in the resistivity and the magnetoresistive effect and a decrease in the metal-semiconductor and ferromagnetic-paramagnetic phase transition temperatures (
$T_{ms}$ and
$T_c$) due to the distortion of the exchange interactions Mn
$^{3+}$ $\leftrightarrow$ Mn
$^{4+}$ by chromium ions, vacancies, and clusters. Introduction of Cr decreases the ferromagnetic component and increases the activation energy. The magnetoresistive effect near
$T_{ms}$ and
$T_c$ is caused by scattering of charge carriers from intercrystallite nanostructure inhomogeneities of the lattice, and the low-temperature effect is associated with the tunneling on mesostructural intercrystallite boundaries.
Received: 22.04.2010