Abstract

The crystal and magnetic structures ofTbBaCo1.9Fe0.1O5.43 have been studied by neutron diffraction and magnetizationmeasurements. It is shown that spontaneous magnetization develops atTN = 305 Kand decreases abruptly below 200 K. The crystal structure is described in the space group Pmmm, ona 2ap*ap*2ap unit cell. It was shown that the extra oxygen vacancies are located mainly in the pyramidalsublattice, thus making tetrahedra. Magnetic structure in the high-temperaturemagnetic phase consists of ferromagnetic and G-type antiferromagnetic components,while in the low-temperature phase only the G-type component exists with a2ap*2ap*2ap magnetic unit cell. The ferromagnetic component results from canting magnetic moments ofCo3+ ions which were found to be predominantly in the high-spin statein pyramids. The refined values of the magnetic moments of theCo3+ ions in the octahedra indicate a mixed high–low-spin state. It is assumed thatnon-collinear magnetic structure results from a concurrence between positiveand negative exchange interactions as well as magnetocrystalline anisotropy inthe pyramidal sublattice. Using the concept of non-collinear magnetic structure,the giant anisotropic magnetoresistive effect in layered cobaltites is explained.

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