Measurements of thermal conductivity versus temperature and magnetic field are reported for perovskite manganites that exhibit ferromagnetic (FM), charge-ordering (CO), antiferromagnetic, and/or structural phase transitions. The data reveal a dominant lattice contribution to the heat conductivity with κ~1-2 W/mK near room temperature. The rather low values, implying a phonon mean free path on the order of a lattice spacing, are shown to correlate with static local distortions of the MnO₆ octahedra. Modifications of the local structure are responsible for abrupt anomalies in the zero-field {κ} at the FM, CO, and structural transitions, and for colossal magnetothermal resistance near the FM transition.
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Cohn et al. (1997) studied this question.
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