Heat production rates for the geologically important nuclides 26Al,
40K, 60Fe, 232Th, 235U, and 238U are
calculated on the basis of recent data on atomic and nuclear properties. The
revised data differ by several per cent from some older values, but indicate
that more recent analyses converge toward values with an accuracy sufficient
for all common geoscience applications, although some possibilities for
improvement still remain, especially in the case of 40K and with regard
to the determination of half-lives. A Python script is provided for calculating
heat production (https://github.com/trg818/radheat).Comment: 14 pages, 1 figur