Argon (18Ar) has 26 known isotopes, from 29Ar to 54Ar, of which three are stable (36Ar, 38Ar, and 40Ar). On Earth, 40Ar makes up 99.6% of natural argon. The longest-lived radioactive isotopes are 39Ar with a half-life of 302 years, 42Ar with a half-life of 32.9 years, and 37Ar with a half-life of 35.01 days. All other isotopes have half-lives of less than two hours, and most less than one minute. Isotopes lighter than 38Ar decay to chlorine or lighter elements, while heavier ones beta decay to potassium. The naturally occurring 40K, with a half-life of 1.248×109 years, decays to stable 40Ar by electron capture (10.72%) and by positron emission (0.001%), and also to stable 40Ca via beta decay (89.28%). These properties and ratios are used to determine the age of rocks through potassium–argon dating. Despite the trapping of 40Ar in many rocks, it can be released by melting, grinding, and diffusion. Almost all argon in the Earth's atmosphere is the product of 40K decay, since 99.6% of Earth's atmospheric argon is 40Ar, whereas in the Sun and presumably in primordial star-forming clouds, argon consists of ~85% 36Ar, ~15% 38Ar and only trace 40Ar. Similarly, the ratio of the isotopes 36Ar:38Ar:40Ar in the atmospheres of the outer planets is measured to be 8400:1600:1. In the Earth's atmosphere, radioactive 39Ar (and to a lesser extent 37Ar) is made by cosmic ray activity, primarily from 40Ar. In the subsurface environment, 39Ar is also produced through neutron capture by 39K or 42Ca, with proton or alpha emission respectively; 37Ar was created in subsurface nuclear explosions similarly from 40Ca. The content of 39Ar in natural argon is measured to be of (8.6±0.4)×10−16 g/g, or (0.964±0.024) Bq/kg weight. The content of 42Ar (half-life 33 years) in the Earth's atmosphere, though it had previously been reported as a cosmogenic isotope, is lower than 6×10−21 of the element. Many endeavors require argon depleted in the cosmogenic isotopes, known as depleted argon and this may be obtained from underground sources that have been isolated from the atmosphere long enough for these isotopes to decay. 36Ar, in the form of argon hydride, was detected in the Crab Nebula supernova remnant during 2013. This was the first time a noble molecule was detected in outer space.
List of isotopes
See also Banana equivalent dose Daughter products other than argon
Isotopes of potassium Isotopes of chlorine Isotopes of sulfur Isotopes of phosphorus
References
External links Argon isotopes data from The Berkeley Laboratory Isotopes Projects
