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.
Potassium–argon dating
Potassium-40 is especially important in potassium–argon (K–Ar) dating. Argon is a gas that does not ordinarily combine with other elements. So, when a mineral forms – whether from molten rock, or from substances dissolved in water – it will be initially argon-free, even if there is some argon in the liquid. However, if the mineral contains traces of potassium, then decay of the 40K isotope present will create fresh argon-40 that will remain locked up in the mineral. Since the rate at which this conversion occurs is known, it is possible to determine the elapsed time since the mineral formed by measuring the ratio of 40K and 40Ar atoms contained in it. The argon in Earth's atmosphere is 99.6% 40Ar, but the argon in the Sun – and presumably in the primordial material that condensed into the planets – is mostly 36Ar, with less than 15% of 38Ar. It follows that most of Earth's argon derives from potassium-40 that decayed into argon-40, which eventually escaped to the atmosphere.
Contribution to natural radioactivity
The decay of 40K in Earth's mantle ranks third, after 232Th and 238U, in the list of sources of radiogenic heat. Less is known about the amount of radiogenic sources in Earth's outer and inner core, which lie below the mantle. It has been proposed, though, that significant core radioactivity (1–2 TW) may be caused by high levels of U, Th and K. Potassium-40 is the largest source of natural radioactivity in animals including humans. A 70 kg human body contains about 140 g (or 126 g) of potassium, hence about 140g × 0.0117% * (39.96/39.10) ≈ 16.7 mg of 40K; whose decay produces about 3,850 to 4,300 disintegrations per second (becquerel) continuously throughout the life of an adult person (and proportionally less in children). The normal potassium-40 concentration in the human body is equivalent to 55 Bq per kilogram, corresponding to an effective dose of 0.2 millisievert per year throughout the body. This is the largest source of internal radiation, followed by 0.12 mSv per year from the nuclides in the uranium and thorium decay series, and just 12 microsieverts per year from carbon-14.
Banana equivalent dose Potassium-40 is famous for its usage in the banana equivalent dose, an informal unit of measure, primarily used in general educational settings, to compare radioactive dosages to the amount received by eating one banana. If a banana weighing 120 grams has a concentration of 350 mg potassium per 100 grams, then it contains 420 mg. If the human body contains about 126 grams of potassium and this potassium gives an effective dose of 200 μSv per year (see above), then the potassium in a banana would theoretically add (0.420/126)200 ≈ 0.67 μSv per year, under the assumptions that all of the radiation produced by potassium-40 is absorbed in the body (mostly true, as most of the radiation is beta-minus radiation, which has a short range). If the biological half-life of potassium is taken as 38 days (this of course depends on how much potassium is ingested per day) then the effective dose integrated over time is (0.67)(38/365)/ln(2)⇔0.1 μSv, and this value is taken as the "banana equivalent dose'. At the estimated 0.1 μSv, one banana equivalent dose is around 1% of the average American's daily exposure to radiation. In actual fact, eating a banana will not add 0.1 μSv of dose, because the potassium concentration in the body is controlled, so it will not remain elevated for weeks.
See also Background radiation Isotopes of potassium
Notes
References
External links Table of radioactive isotopes, K-40 The Lund/LBNL Nuclear Data Search Potassium-40 Section, Radiological and Chemical Fact Sheets to Support Health Risk Analyses for Contaminated Areas
