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We present the results of new measurements of the basal-plane thermoelectric power S of highly oriented pyrolytic graphite between 1.3 and 300 K. In addition to the well-known large negative dip near 40 K, the curve of $S(T)$ reveals the presence of a second anomaly in the region below about 10 K. We show that this extra anomaly can be explained in terms of a phonon-drag effect acting on the H-point hole minority carriers. Such an interpretation is consistent with other experimental data.
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Ayache et al. (1980) studied this question.
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