Abstract
Transverse magnetoresistivity measurements have been made on pure, polycrystalline α and β plutonium. The magnetoresistivity of both phases is negative at 5°K and low applied fields, and becomes positive at fields greater than 2000 G. The negative effect decreases with increasing temperature and is not dependent on sample texture. The higher-field results follow the H2 dependence found in "normal" metals. It is concluded that the negative effect is due to magnetic ordering, which results from sf exchange, and the Néel temperatures are near 20-30°K for both phases. The high-field data are consistent with earlier models in which the electrical conductivity is dominated by a small number of holes in the 7s band.

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