This program calculates the energy available as heat or for chemical reactions and the specific heat production of six nuclides (26Al, 40K, 60Fe, 232Th, 235U, and 238U), which are geologically important as heat sources, especially in the context of the formation, evolution, and geodynamics of terrestrial planetary bodies.
Reference:
Ruedas, T. (2017): Radioactive heat production of six geologically important nuclides. Geochem. Geophys. Geosys., 18(9), 3530-3541, doi:10.1002/2017GC006997.