Probing phase coexistence and stabilization of the spin-ordered ferrimagnetic state by calcium addition in theY(Ba1−xCax)Co2O5.5layered cobaltites using neutron diffraction

Abstract

We study the effects of a partial substitution of Ba with the smaller cation Ca in the layered cobaltites YBaCo{sub 2}O{sub 5+{delta}} for {delta}{approx_equal}0.5. Neutron thermodiffractograms are reported for the compounds YBa{sub 0.95}Ca{sub 0.05}Co{sub 2}O{sub 5.5} (x{sub Ca}=0.05) and YBa{sub 0.90}Ca{sub 0.10}Co{sub 2}O{sub 5.5} (x{sub Ca}=0.10) in the temperature range 20 K{<=}T{<=}300 K, as well as high-resolution neutron diffraction experiments at selected temperatures for the samples x{sub Ca}=0.05, x{sub Ca}=0.10, and the parent compound x{sub Ca}=0. We have found the magnetic properties to be strongly affected by the cationic substitution. Although the ''122'' perovskite structure seems unaffected by Ca addition, the magnetic arrangements of Co ions are drastically modified: the antiferromagnetic (AFM) long-range order is destroyed, and a ferrimagnetic phase with spin state order is stabilized below T{approx}290 K. For the sample with x{sub Ca}=0.05 a fraction of AFM phase coexists with the ferrimagnetic one below T{approx}190 K, whereas for x{sub Ca}=0.10 the AFM order is completely lost. The systematic refinement of the whole series has allowed for a better understanding of the observed low-temperature diffraction patterns of the parent compound YBaCo{sub 2}O{sub 5.5}, which had not yet been clarified. A two-phase scenario is proposed for the x{sub Ca}=0 compoundmore » which is compatible with the phase coexistence observed in the x{sub Ca}=0.05 sample.« less