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General | |
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Symbol | 40K |
Names | potassium-40, 40K, K-40 |
Protons (Z) | 19 |
Neutrons (N) | 21 |
Nuclide data | |
Natural abundance | 0.0117(1)% |
Half-life (t1/2) | 1.251(3)×109 y |
Isotope mass | 39.96399848(21) Da |
Spin | 4− |
Excess energy | −33505 keV |
Binding energy | 341523 keV |
Parent isotopes | Primordial |
Decay products | 40Ca (β−) 40Ar (EC, γ; β+) |
Decay modes | |
Decay mode | Decay energy (MeV) |
β− | 1.31109 |
EC, γ | 1.5049 |
Isotopes of potassium Complete table of nuclides |
Potassium-40 (40K) is a long lived and the main naturally occurring radioactive isotope of potassium. Its half-life is 1.25 billion years. It makes up about 0.012% (120 ppm) of natural potassium.
Potassium-40 undergoes four different types 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, positron emission (β+ to 40Ar at 0.001% probability,[1] electron capture (EC) to 40Ar* followed by a gamma decay emitting a photon[Note 1] with an energy of 1.46 MeV at 10.3% probability and direct electron capture (EC) to the ground state of 40Ar at 0.1%.[2][3][4] Both forms of the electron capture decay release further photons,[Note 2] when electrons from the outer shells fall into the inner shells to replace the electron taken from there.
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.
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