A nuclear reaction where a nucleus absorbs a neutron, often forming a heavier isotope.Neutron capture is a nuclear reaction in which an atomic nucleus absorbs a free neutron, forming a heavier isotope of the same element. This process is fundamental to nucleosynthesis — the creation of elements in stars — and is also a key mechanism in nuclear reactors and medical isotope production. Depending on the energy of the incoming neutron, the reaction can be fast (for high-energy neutrons) or slow (for thermal neutrons), leading to different outcomes in stellar evolution.
The concept was established in the 1930s following James Chadwick's discovery of the neutron in 1932. The s-process theory was developed by Margaret Burbidge, Geoffrey Burbidge, William Fowler, and Fred Hoyle in their seminal 1957 paper on stellar nucleosynthesis.
When a neutron approaches a nucleus, the strong nuclear force can bind it, releasing energy as gamma rays (radiative capture). The resulting isotope may be stable or radioactive. In stars, successive captures build heavier elements, with the 's-process' (slow) and 'r-process' (rapid) pathways explaining the abundance of elements up to bismuth and beyond.
Used in nuclear power generation (control rods and fuel breeding), production of medical radioisotopes like technetium-99m, and in neutron activation analysis for detecting trace elements in materials.
The r-process, which involves rapid neutron capture, is responsible for producing about half of the heavy elements in the universe, including gold and platinum, likely occurring in neutron star mergers.









