Setting temperature effect in polycrystalline exchange-biased IrMn/CoFe bilayers J. Appl. Phys. 113, 17D704 (2013) Effect of Ni substitution on Y-type barium ferrite J. Appl. Phys. 113, 17D906 (2013) Magnetic interactions and reversal mechanisms in Co nanowire and nanotube arrays J. Appl. Phys. 113, 093907 (2013) Effect of Mn substitution on the magnetic and magneto-transport properties of Fe3−xMnxSi (0≤x≤1.25) alloys J. Appl. Phys. 113, 093904 (2013) Critical behaviors in double-exchange ferromagnets Pr1−xPbxMnO3 J. Appl. Phys. 113, 17E110 (2013) Additional information on J. Appl. Phys.

Manganites with the formula La 1−x Ca x MnO 3 for 0.2 < x < 0.5 undergo a magnetic field driven transition from a paramagnetic to ferromagnetic state, which is accompanied by changes in the lattice and electronic structure. An isotropic expansion of the La 0.75 Ca 0.25 MnO 3 cell at the phase transition has been observed experimentally. It is therefore expected that there will be a large entropy change at the transition due to the first order nature. However, the maximum obtained value for the entropy change in Ca-doped manganites merely reaches a moderate value in the field of a permanent magnet. The present theoretical work aims to shed light on this discrepancy. A combination of finite temperature statistical mechanics and first principles theory is applied to determine individual contributions to the total entropy change of the system by treating the electronic, lattice and magnetic components independently. Hybrid-exchange density functional (B3LYP) calculations and Monte Carlo simulations are performed for La 0.75 Ca 0.25 MnO 3 . Through the analysis of individual entropy contributions, it is identified that the electronic and lattice entropy changes oppose the magnetic entropy change. The results highlighted in the present work demonstrate how the electronic and vibrational terms can have a deleterious effect on the total entropy change. * romi.korotana09@alumni.imperial.ac.uk