inverse beta การใช้

Geoneutrinos from 40 K decay have energies below the threshold and cannot be detected using inverse beta decay reaction.
However, protons are known to transform into neutrons through the process of electron capture ( also called inverse beta decay ).
Instead, fifteen years later in 1956, Frederick Reines and Clyde Cowan detected the neutrino through a different method involving the inverse beta-decay reaction.
All other cerium isotopes are inverse beta decay or electron capture to isotopes of lanthanum, while that of the heavier isotopes is beta decay to isotopes of praseodymium.
Inverse beta decay may also sometimes refer to the interaction of an electron and proton, creating a neutrino and neutron, although this process is normally referred to as electron capture.