Potassium-40

Common card · No. 223552

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...

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