
The resistance of an atomic nucleus to radioactive decay, determined by its binding energy and structure.Nuclear stability refers to the resistance of an atomic nucleus to radioactive decay. It is determined by the balance between the strong nuclear force, which holds protons and neutrons together, and the electrostatic repulsion between protons. Stable nuclei have a specific ratio of neutrons to protons; deviations from this ratio make the nucleus unstable and prone to decay. The most stable nuclei are those with magic numbers of protons or neutrons, which correspond to closed shells in the nuclear shell model.
The concept of nuclear stability was developed in the 1930s with the discovery of the neutron and the formulation of the liquid drop model and the shell model. The magic numbers were identified by Maria Goeppert-Mayer and Hans Jensen in the 1940s and 1950s.
The binding energy per nucleon is a measure of stability — the higher it is, the more stable the nucleus. For light elements, stability increases with mass, peaking around iron-56. Beyond that, heavier nuclei are less stable and can undergo fission or alpha decay. The neutron-to-proton ratio also matters: too many neutrons lead to beta decay, while too few lead to positron emission or electron capture.
Understanding nuclear stability is crucial for nuclear energy, where fission of heavy nuclei releases energy, and for medical imaging, where unstable isotopes are used as tracers.
The element with the highest known stable nucleus is lead-208, which has 82 protons and 126 neutrons — both magic numbers, making it doubly magic and exceptionally stable.


















