Abstract
Lattice thermal conductivity is a sensitive probe of distortions of the translational invariance of crystalline materials. Crossplane thermal conductivity, , was studied by the 3ω technique in superlattices, comprising orthorhombic charge/orbital ordered manganite and cubic . The manganite/titanite superlattices show a peak in just above the charge order transition temperature with a pronounced thermal hysteresis. This ordering peak in is successively suppressed with decreasing layer thickness. Our results demonstrate a minor effect of the interface density on , primarily visible below . In contrast, much higher changes in evolve close to , due to interface-induced effects on charge and orbital ordering. Our results suggest that the ordering peak in is a result of lattice softening above the phase transition which is modified by thickness-dependent misfit strain.
- Received 28 May 2018
- Revised 5 October 2018
DOI:https://doi.org/10.1103/PhysRevB.98.195114
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