The properties of Sr1−xYxCoO3−δ layered cobaltites are determined by synchrotron X-ray and neutron powder diffraction studies, by measurements of magnetic and magnetotransport properties. It is shown that the crystal structure changes from tetragonal P4/mmm (ap × ap × 2ap) to monoclinic A2/m (4√2ap × 2√2ap×4ap up to the magnetic ordering temperature and 2√2ap ×2√2ap × 4ap above) through the intermediate tetragonal I4/mmm (2ap × 2ap × 4ap) with alternating layers of CoO6 and CoO4+δ. The basic magnetic structure is G-type antiferromagnetic with Co3+ ions in a high spin/low spin (HS/LS) state mixture in both structural layers. The Co3+ magnetic moments in the CoO6 and CoO4+δ layers are 1.5 μB/Co and 2 μB/Co for x = 0.1 and 1.8 μB/Co and 2.7 μB/Co for x = 0.2, respectively. The antiferromagnetic–“ferromagnetic” transition in compounds with x > 0.2 is associated with the structural and orbital disorder. Magnetic transitions are accompanied by structural phase transitions. The presence of the ferromagnetic component is associated with the monoclinic distortions and canting of magnetic moments in anion-deficient layers due to orbital ordering. A sharp drop of the magnetization for x > 0.2 is caused by the LS Co3+ stabilization and orbital disordering. No spontaneous magnetization is found for compounds with x > 27%.
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