Radioactive heat production of six geologically important nuclides

Abstract

Heat production rates for the geologically important nuclides ${}^{26}$Al, ${}^{40}$K, ${}^{60}$Fe, ${}^{232}$Th, ${}^{235}$U, and ${}^{238}$U 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 ${}^{40}$K and with regard to the determination of half-lives. A Python script is provided for calculating heat production (https://github.com/trg818/radheat).

14 pages, 1 figure

References in corpus (2)

• Geophysical and geochemical constraints on geoneutrino fluxes from Earth's mantle
• Exploring the hidden interior of the Earth with directional neutrino measurements

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