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Heat production rates for the geologically important nuclides ${}^{26}$Al,${}^{40}$K, ${}^{60}$Fe, ${}^{232}$Th, ${}^{235}$U, and ${}^{238}$U arecalculated on the basis of recent data on atomic and nuclear properties. Therevised data differ by several per cent from some older values, but indicatethat more recent analyses converge toward values with an accuracy sufficientfor all common geoscience applications, although some possibilities forimprovement still remain, especially in the case of ${}^{40}$K and with regardto the determination of half-lives. A Python script is provided for calculatingheat production (https://github.com/trg818/radheat).

Radioactive heat production of six geologically important nuclides