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Chlorine-36 (36 Cl) is an isotope of chlorine. Chlorine has two stable isotopes and one naturally occurring radioactive isotope, the cosmogenic isotope 36 Cl. Its half-life is 301,300 ± 1,500 years. [1] 36 Cl decays primarily (98%) by beta-minus decay to 36 Ar, and the balance to 36 S. [1]
36 Cl has seen use in other areas of the geological sciences, forecasts, and elements. In chloride-based molten salt reactors the production of 36 Cl by neutron capture is an inevitable consequence of using natural isotope mixtures of chlorine (i.e.
Chlorine is a chemical element; it has symbol Cl and atomic number 17. The second-lightest of the halogens, ... The most stable chlorine radioisotope is 36 Cl.
Chlorine-36 is the radioactive isotope produced in many nuclear facilities as byproduct waste. [3] Its half-life of 3.01 × 10 5 years , mobility in the pedosphere , and ability to be taken up by organisms has made it an isotope of high concern among researchers. [ 3 ]
The residence time of 36 Cl in the atmosphere is about 1 week. Thus, as an event marker of 1950s water in soil and ground water, 36 Cl is also useful for dating waters less than 50 years before the present. 36 Cl has seen use in other areas of the geological sciences, including dating ice [37] and sediments.
Sodium-22 and chlorine-36 are commonly used to study ion transporters. However, sodium-22 is hard to screen off and chlorine-36, with a half-life of 300,000 years, has low activity. However, sodium-22 is hard to screen off and chlorine-36, with a half-life of 300,000 years, has low activity.
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26.36 thorium-216: 26.8 meitnerium-268: 27 astatine-193m2: 27 lawrencium-251: 27 actinium-208m: 28 astatine-193: 28 manganese-68: 28 sodium-28: 30.5 actinium-207: 31 neon-27: 32 bismuth-187: 32 polonium-192: 32.2 astatine-217: 32.3 uranium-234m: 33.5 curium-244m1: 34 bohrium-260: 35 radon-218: 35 neptunium-226: 35 thorium-212: 36 moscovium-287: ...
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