Potassium-40

Potassium-40 (40K) is a long lived and the main naturally occurring radioactive isotope of potassium, with a half-life of 1.248 billion years. It makes up about 117 ppmTooltip parts-per-million of natural potassium, making that mixture very weakly radioactive. The half-life is much shorter than the age of Earth, meaning this fraction was significantly larger earlier in Earth's history. Potassium-40 undergoes four different paths of radioactive decay, including all three main types of beta decay: Electron emission (β−) to 40Ca with a decay energy of 1.31 MeV at 89.6% probability Electron capture (EC) to 40Ar* followed by a gamma decay emitting a photon with an energy of 1.46 MeV at 10.3% probability Direct electron capture (EC) to the ground state of 40Ar at 0.1% probability Positron emission (β+) to 40Ar at 0.001% probability Both forms of the electron capture decay release further photons, when electrons from the outer shells fall into the inner shells to replace the electron taken from there. The total energy for the decay to argon is 1.51 MeV. The EC decay of 40K explains the large abundance of argon (nearly 1%) in the Earth's atmosphere, as well as prevalence of 40Ar over other isotopes.