Abstract
Low temperature nuclear orientation thermometry, in particular γ-ray anisotropy thermometry, is discussed both from a theoretical and practical point of view. Detailed information is given on the most often used γ-ray anisotropy thermometers, along with a comprehensive description of the γ-ray anisotropy technique. The 60Co in (hcp) cobalt single crystal γ-ray anisotropy thermometer is discussed in considerable detail since it is used more frequently in comparison experiments with other primary thermometers. Recent experimental results using γ-ray anisotropy thermometers are also reviewed.
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