Thermal conductivity of pure and Mg-doped CuGeO3 in the incommensurate phase
Abstract
The thermal conductivity of Cu1-xMgxGeO3 is measured in magnetic fields up to 16 T. At the transition field Hc to the high-field incommensurate (I) phase, abruptly decreases. While of the pure CuGeO3 is enhanced with the application of higher magnetic fields, an anomalous plateau feature shows up in the (H) profile in the I phase of the Mg-doped samples which includes antiferromagnetic ordering (I-AF phase). With the help of specific heat data, taken supplementally for the identical samples, the above features are well understood that phonons are strongly scattered by spin solitons and that in the I phase is governed by their spatial distribution. In particular, the plateau feature in the doped samples suggests "freezing" of the solitons, in which antiferromagnetism must be playing an essential role because this feature is absent at temperatures above TN.
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