Potassium-40

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Potassium-40
General
Name, symbol Potassium-40,40K
Neutrons 21
Protons 19
Nuclide data
Natural abundance 0.0117(1)%
Half-life 1.248(3)×109 y
Isotope mass 39.96399848(21) u
Spin 4
Excess energy −33505 keV
Binding energy 341523 keV

Potassium-40 (40K) is a radioactive isotope of potassium which has a very long half-life of 1.248×109 years. It makes up 0.012% (120 ppm) of the total amount of potassium found in nature.

Potassium-40 is a rare example of an isotope that undergoes all three types of beta decay. About 89.28% of the time, it decays to calcium-40 (40Ca) with emission of a beta particle, an electron) with a maximum energy of 1.33 MeV and an antineutrino. About 10.72% of the time it decays to argon-40 (40Ar) by electron capture, with the emission of a 1.460 MeV gamma ray and a neutrino. Very rarely (0.001% of the time) it will decay to 40Ar by emitting a positron+) and a neutrino.[1]

Potassium-argon dating[edit]

Decay scheme

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 any 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 found in Earth's atmosphere is 99.6% 40Ar; whereas the argon in the Sun — and presumably in the primordial material that condensed into the planets — is mostly 36Ar, with less than 15% of 40Ar. It follows that most of the terrestrial argon derives from potassium-40 that decayed into argon-40, which eventually escaped to the atmosphere.

Contribution to natural radioactivity[edit]

The evolution of Earth's radiogenic heat flow over time: contribution from 40K in red.

The radioactive decay of 40K in the Earth's mantle ranks third, after 232Th and 238U, as the source of radiogenic heat.

40K is the largest source of natural radioactivity in animals including humans. A 70 kg human body contains about 160 grams of potassium, hence about 0.000117 x 160 = 0.0187 grams of 40K; whose decay produces about 4,900 disintegrations per second (becquerels) continuously throughout the life of the body.[2][3]

See also[edit]

Notes and references[edit]

  1. ^ Engelkemeir, DW; KF Flynn; LE Glendenin (1962). "Positron Emission in the Decay of K40". Physical Review 126 (5): 1818. Bibcode:1962PhRv..126.1818E. doi:10.1103/PhysRev.126.1818. 
  2. ^ The number of radioactive decays per second in a given mass of 40K is the number of atoms in that mass, divided by the average lifetime of a 40K atom in seconds. The number of atoms in one gram of 40K is Avogadro's number 6.022×1023 (the number of atoms per mole) divided by the atomic weight of potassium-40 (39.96 grams per mole), which is about 0.1507×1023 per gram. As in any exponential decay, the average lifetime is the half-life divided by the natural logarithm of 2, or about 56.82×1015 seconds.
  3. ^ Supian Bin Samat et al (1997), activity of one gram of potassium, Phys. Med. Biol. volume 42 page 407, doi:10.1088/0031-9155/42/2/012

External links[edit]


Lighter:
potassium-39
Potassium-40 is an
isotope of potassium
Heavier:
potassium-41
Decay product of:
Decay chain
of potassium-40
Decays to:
argon-40, calcium-40, Stable