Magnetocaloric effect in manganites

The magnetocaloric effect (MCE) in La_{1 ? x} Sr _x MnO₃, Sm_0.55Sr_0.45MnO₃, and PrBaMn₂O₆ compounds is studied. The maximum values of MCE (??T _max) determined by a direct method in the second and third compositions and in La_0.9Sr_0.1MnO₃ are found to be much lower than those calculated from the change of the magnetic part of entropy in the Curie temperature (T _C) and the Néel temperature (T _N) range. The negative contribution of the antiferromagnetic (AFM) part of a sample in the La_{1 ? x} Sr _x MnO₃ system at 0.1 ?? x ?? 0.3 decreases ??T _max and changes the ??T(T) curve shape, shifting its maximum 20?C40 K above T _C. Lower values of ??T _max are detected in the range T _C = 130?142 K in polycrystalline and single-crystal Sm_0.55Sr_0.45MnO₃ samples cooled in air. If such samples were cooled in an oxygen atmosphere (which restores broken Mn-O-Mn bonds and, thus, increases the volume of CE-type AFM clusters), the maximum in the temperature dependence of MCE is located at T _N (243 K) for CE-type AFM clusters. A magnetic field applied to a sample during the MCE measurements transforms these clusters into a ferromagnetic (FM) state, and both types of clusters decompose at T = T _N. The PrBaMn₂O₆ composition undergoes an AFM-FM transition at 231 K, and the temperature dependence of its MCE has a sharp minimum at T = 234 K, where MCE is negative, and a broad maximum covering T _C. The absolute values of MCE at both extrema are several times lower than those calculated from the change in the magnetic entropy. These phenomena are explained by the presence of a magnetically heterogeneous FM-AFM state in these manganites.