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chlorine-36

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Also known as Cl-36, 36Cl

Chlorine-36 (36Cl) is a radioactive isotope of chlorine whose half-life is 301,000 years; it decays primarily (98%) by beta-minus decay to 36Ar, and the balance by electron capture to 36S. This cosmogenic isotope occurs in natural chlorine alongside the two stable isotopes.

Wikidata facts

Subclass of
chlorine
Mass
35.968306822
Image
Chlorine-36.svg
Show 8 more facts
atomic number
17
neutron number
19
decays to
sulfur-36
half-life
301000.0
spin quantum number
2.0
parity quantum number
1
mass excess
-29522.005
binding energy
306789.516
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Encyclopedic overview

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Chlorine-36 (36Cl) is a radioactive isotope of chlorine whose half-life is 301,000 years; it decays primarily (98%) by beta-minus decay to 36Ar, and the balance by electron capture to 36S. This cosmogenic isotope occurs in natural chlorine alongside the two stable isotopes.

Trace amounts of radioactive 36Cl exist in the environment, in a ratio of about to 1 with respect to the stable chlorine isotopes. This 36Cl/Cl ratio is sometimes abbreviated as R36Cl. This corresponds to a concentration of approximately .

Excerpted from Wikipedia’s “chlorine-36” article, available under the CC BY-SA 4.0 licence.

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