Negatively charged ions are produced when a free electron collides with an atom and is subsequently trapped inside the electric potential barrier, releasing any excess energy. The process is known as
electron capture ionization.
Positively charged ions are produced by transferring an amount of energy to a bound electron in a collision with charged particles (e.g. ions, electrons or positrons) or with photons. The threshold amount of the required energy is known as
ionization potential. The study of such collisions is of fundamental importance with regard to the few-body problem (see article on
few-body systems), which is one of the major unsolved problems in physics.
Kinematically complete experiments,
[2] i.e. experiments in which the complete momentum vector of all collision fragments (the scattered projectile, the recoiling target-ion, and the ejected electron) are determined, have contributed to major advances in the theoretical understanding of the few-body problem in recent years.
Adiabatic ionization is a form of ionization in which an electron is removed from or added to an
atom or
molecule in its lowest
energy state to form an ion in its lowest energy state.
[3]
The
Townsend discharge is a good example of the creation of positive ions and free electrons due to ion impact. It is a cascade reaction involving
electrons in a region with a sufficiently high
electric field in a gaseous medium that can be ionized, such as
air. Following an original ionization event, due to such as ionizing radiation, the positive
ion drifts towards the
cathode, while the free electron drifts towards the
anode of the device. If the electric field is strong enough, the free electron gains sufficient energy to liberate a further electron when it next collides with another molecule. The two free electrons then travel towards the anode and gain sufficient energy from the electric field to cause impact ionization when the next collisions occur; and so on. This is effectively a chain reaction of electron generation, and is dependent on the free electrons gaining sufficient energy between collisions to sustain the avalanche.
[4]