Nuclear Decay Quick Reference
Isotopes and Nuclear Stability
Isotopes: same proton number (Z), different neutron number (N).
Stability depends on N/Z ratio; some isotopes are stable, others decay.
All isotopes of elements with Z > 83 are unstable (radioactive).
Common decay modes:
Alpha decay: emission of an alpha particle (a helium-4 nucleus).
Effect:
Beta minus decay (β−): neutron converts to proton with emission of an electron and an antineutrino.
Effect:
Beta plus decay (β+ or positron emission): proton converts to neutron with emission of a positron and a neutrino.
Effect:
Electron capture (EC): proton captures an orbital electron turning into a neutron, emitting a neutrino.
Effect:
Gamma decay (γ): emission of a photon to shed excess energy; typically follows other decays.
Example thought question:
Which chlorine isotope is more likely to be unstable: or ?
Answer: is neutron-poor (N = A − Z = 16) compared to (N = 18); it is more unstable.
Most likely decay mode for the unstable chlorine isotope (33Cl): beta-plus emission (positron emission), often accompanied by neutrino emission, to move toward stability.
Primary decay:
(Electron capture is also possible if energetically allowed, giving )
Nuclear Decay Equations Practice
Write the balanced nuclear equation for the following decays:
1) Strontium-93 undergoes beta particle emission.
2) Zinc-52 undergoes electron capture.
3) Francium-217 undergoes alpha particle emission.
4) Indium-110 undergoes positron emission.
Notes on notation: Use Z, A in the superscripts and subscripts as shown; include neutrino terms for completeness. Equations can be written with or without the neutrino terms depending on the level of detail required.