Abstract

A comparative study is presented on magnetocaloric behavior in iron doped manganites La0.7A0.3Mn0.9Fe0.1O3 (A = Sr, Pb, Ba) prepared by a sol–gel technique and with Fe valence ascertained by the Mössbauer spectroscopy. For La0.7Sr0.3Mn0.9Fe0.1O3 sample, the maximum entropy change ΔS corresponding to a magnetic field variation of 1 T is found to be −0.82 J/kg K at 260 K resulting in a refrigerant capacity of 60 J/kg. The obtained results suggest that B-site Fe dopant actually disfavors the enhancement of the magnetocaloric effect in some perovskite manganites due to a weakening of the ferromagnetic double-exchange interaction between Mn3+ and Mn4+ ions of the original atomic structure.

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