Published by Patrick Mutisya · 14 days ago
When an unstable nucleus decays it can emit one of three kinds of radiation:
Alpha particles are helium‑4 nuclei consisting of two protons and two neutrons.
Beta particles are high‑speed electrons (β⁻) or positrons (β⁺) emitted from the nucleus.
Gamma rays are high‑energy photons emitted from the excited nucleus after an α or β transition.
The ability of radiation to ionise atoms depends on two main factors:
Combining these factors gives the following hierarchy of ionising power:
| Radiation Type | Kinetic Energy (MeV) | Electric Charge (e) | Ionising Power (relative) | Penetration Ability |
|---|---|---|---|---|
| Alpha (α) | \$4\text{–}8\$ | +2 | Very high – dense ionisation over a short path | Very low |
| Beta (β⁻ / β⁺) | \$0.1\text{–}2\$ (continuous) | –1 / +1 | Medium – less dense than α but higher than γ | Medium |
| Gamma (γ) | \$0.1\text{–}10\$ (photon energy) | 0 | Low – ionises mainly by secondary electrons (Compton, photoelectric) | High |
Kinetic energy: Alpha particles, despite having similar or slightly higher kinetic energies than beta particles, carry much more mass. Their large mass means they lose energy rapidly through collisions, creating a dense ionisation track. Gamma photons, being massless, travel at the speed of light and interact less frequently, so each interaction deposits less energy.
Electric charge: Charged particles (α and β) experience Coulomb forces with electrons in matter, directly stripping electrons and producing ion pairs. The magnitude of the charge influences how strongly they attract or repel electrons; a +2 charge (α) exerts a stronger force than a ±1 charge (β). Gamma rays have no charge, so ionisation occurs only indirectly via secondary processes (photoelectric effect, Compton scattering, pair production), which are less efficient per unit path length.