RADIOACTIVE HEATING

Some atomic nuclei are not stable. If they are allowed to sit, they will spontaneously break apart into smaller nuclei releasing particles and energy. For example, the isotope is not stable. (Oh, wait, the 13 says that the Aluminum nucleus contains 13 protons and the 26 says that the Aluminum nucleus contains 26 protons and neutrons, that is, the nucleus contains 26 - 13 = 13 neutrons.) The Aluminum decays as

breaks up into + positron + energy

This process has a half-life of 720,000 years. The half-life is the amount of time over which the probability is 1/2 that the nucleus will decay. Some important short half-life radioactive nuclei are to with t = 0.72 M years
to with t = 16 M years

Some important long half-life radioactive nuclei are to , with t = 1.25 B years
to with t = 14 B years
to with t = 0.7 B years
to with t = 4.5 B years

The shorter half-life nuclei add to the initial heating of the planets while the longer half-life nuclei add to the current heating of the interiors of the planets (the interiors of some of the Terrestrial planets are still quite hot.