4 research outputs found

    Phonon thermal transport shaped by strong spin-phonon scattering in a Kitaev material Na2_2Co2_2TeO6_6

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    The recent report of a half-quantized thermal Hall effect in the Kitaev material α\alpha-RuCl3_3 has sparked a strong debate on whether it is generated by Majorana fermion edge currents or whether other more conventional mechanisms involving magnons or phonons are at its origin. A more direct evidence for Majorana fermions which could be expected to arise from a contribution to the longitudinal heat conductivity Îșxx\kappa_{xx} at T→0T\rightarrow0 is elusive due to a very complex magnetic field dependence of Îșxx\kappa_{xx}. Here, we report very low temperature (below 1~K) thermal conductivity (Îș\kappa) of another candidate Kitaev material, Na2_2Co2_2TeO6_6. The application of a magnetic field along different principal axes of the crystal reveals a strong directional-dependent magnetic-field (B\bf B) impact on Îș\kappa. We show that no evidence for mobile quasiparticles except phonons can be concluded at any field from 0~T to the field polarized state. In particular, severely scattered phonon transport is observed across the B−TB-T phase diagram, which is attributed to prominent magnetic fluctuations. Cascades of phase transitions are uncovered for all B\bf B directions by probing the strength of magnetic fluctuations via a precise record of Îș\kappa(BB). Our results thus rule out recent proposals for itinerant magnetic excitations in Na2_2Co2_2TeO6_6, and emphasise the importance of discriminating true spin liquid transport properties from scattered phonons in candidate materials

    Melting Curves of Triolein Polymorphs

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    High‐pressure treatment is a promising option for improving mechanical properties and processing parameters of fat‐containing products. To identify optimum processing windows, melting curves, crystallization kinetics, and pathways for transferring the optimized structures to atmospheric pressure need to be known. Here, we provide melting curves of different polymorphic forms of triolein in the industrially relevant pressure range. The melting points of different polymorphic forms are detected optically in thin samples during stepwise changes of pressure or temperature. For cross‐nucleated spherulites, this method allows determining the respective melting points of nuclei and overgrown structures. Tracing the melting curves to atmospheric pressure confirms previous identification of the polymorphic forms at high pressure and enables identifying a previously reported but undefined structure as the ÎČ2‐form. Employing Raman spectroscopy, it is confirmed that the polymorph remained unaltered during the pressure release. With increasing pressure, the melting curves of the different polymorphic forms approach each other until they successively merge at the highest pressure levels studied
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