An international collaboration of researchers recently detected and measured the half-life of the heaviest proton emitter, the 188At (astatine) isotope, which decayed by emitting a proton.
About Proton Emission:
Proton emission (also known as proton radioactivity) is a rare form of radioactive decay in which a proton is ejected from a nucleus.
Radioactive decay is the process of an unstable atom transitioning to a more stable form.
It may do so by releasing subatomic particles and energyor by capturing an orbital electron into the nucleus and releasing energy.
Proton emission can occur from high-lying excited states in a nucleus following a beta decay, in which case the process is known as beta-delayed proton emission, or can occur from the ground state (or a low-lying isomer) of very proton-rich nuclei, in which case the process is very similar to alpha decay.
Alpha decay is a type of radioactive decay in which an unstable nucleus emits an alpha particle. An alpha particle consists of 2 protons and 2 neutrons, which is the same as a helium nucleus (⁴₂He).
Beta decay occurs when a nucleus emits a beta particle, which can be an electron (β⁻) or a positron (β⁺).
For a proton to escape a nucleus, the proton separation energy must be negative - the proton is therefore unbound, and tunnels out of the nucleus in a finite time.
Proton emission is not seen in naturally-occurring isotopes; proton emitters can be produced via nuclear reactions, usually utilising some kind of particle accelerator.
The rate of proton emission is governed by the nuclear, Coulomb, and centrifugal potentials of the nucleus, where centrifugal potential affects a large part of the rate of proton emission.
The half-life of a nucleus with respect to proton emission is affected by the proton energy and its orbital angular momentum.
Half-life is the time that it takes for half of the original value of some amount of a radioactive element to decay.
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