Homestake experiment
The Homestake experiment (sometimes referred to as the Davis experiment or Solar Neutrino Experiment and in original literature called Brookhaven Solar Neutrino Experiment or Brookhaven 37Cl (Chlorine) Experiment)
Methodology
The experiment took place in the
The reaction threshold is 0.814 MeV, i.e. the neutrino should have at least this energy to be captured by the 37Cl nucleus.
Because 37Ar has a half-life of 35 days, every few weeks, Davis bubbled helium through the tank to collect the argon that had formed. A small (few cubic cm) gas counter was filled by the collected few tens of atoms of 37Ar (together with the stable argon) to detect its decays. In such a way, Davis was able to determine how many neutrinos had been captured.[3][4]
Conclusions
Davis' figures were consistently very close to one-third of Bahcall's calculations. The first response from the scientific community was that either Bahcall or Davis had made a mistake. Bahcall's calculations were checked repeatedly, with no errors found. Davis scrutinized his own experiment and insisted there was nothing wrong with it. The Homestake experiment was followed by other experiments with the same purpose, such as
See also
- antineutrino)
- Sanford Underground Research Facility
References
- from the original on 2017-08-15.
- S2CID 119501801.
- ISBN 978-0-471-97285-3.
- doi:10.1086/305343.