Chlorine-37
General | |
---|---|
Symbol | 37Cl |
Names | chlorine-37, 37Cl, Cl-37 |
Protons (Z) | 17 |
Neutrons (N) | 20 |
Nuclide data | |
Natural abundance | 24.23% |
Isotope mass | 36.965903 Da |
Isotopes of chlorine Complete table of nuclides |
Chlorine-37 (37
Cl
), is one of the
Remarkably, solar neutrinos were discovered by an experiment using a radiochemical method based on chlorine-37 transmutation.[2]
Neutrino detection
One of the historically important radiochemical methods of solar neutrino detection is based on inverse electron capture triggered by the absorption of an electron neutrino.[3] Chlorine-37 transmutes into argon-37 via the reaction[4]
- 37
Cl
+
ν
e → 37
Ar
+
e−
.
Argon-37 then de-excites itself via electron capture (half-life = 35 d) into chlorine-37 via the reaction
- 37
Ar
+
e−
→ 37
Cl
+
ν
e.
These last reactions involve
Occurrence
The representative terrestrial abundance of chlorine-37 is 24.22(4)% of chlorine atoms,
There is a known variation in the isotopic abundance of chlorine-37. This heavier isotope tends to be more prevalent in chloride minerals than in aqueous solutions such as sea water, although the isotopic composition of
See also
- Beta decay
- Neutrino detection
- Isotopic tracer
- Isotopes of chlorine
References
- ^ a b J.N. Bahcall (1969). "Neutrinos from the Sun". .
- ^ a b c
Sutton, Christine (1992). Spaceship Neutrino. OCLC 25246163.
chlorine-37 neutrino.
- ^
F.H. Shu (1982). The Physical Universe: An Introduction to Astronomy. University Science Books. p. 122. ISBN 978-0-935702-05-7.
chlorine 37 neutrino.
- ^ A.H. Snell, F. Pleasonton (1955). "Spectrometry of the Neutrino Recoils of Argon-37". .
- ISBN 978-981-238-244-3.
- ^