A rapid neutron-capture process in astrophysics that synthesizes heavy elements like gold and platinum.The r-process, or rapid neutron-capture process, is the astrophysical mechanism responsible for creating about half of all elements heavier than iron, including gold, platinum, and uranium. It occurs in extreme environments where atomic nuclei are bombarded with neutrons so quickly that they are absorbed before the resulting unstable nucleus has time to decay. This process builds up heavy elements step by step, each neutron capture pushing the nucleus further up the periodic table.
The r-process was first proposed in 1957 by Margaret Burbidge, Geoffrey Burbidge, William Fowler, and Fred Hoyle in their landmark paper on stellar nucleosynthesis, with independent contributions from Alastair Cameron the same year.
In a dense neutron-rich environment, a seed nucleus (like iron) captures neutrons in rapid succession, becoming heavier and more neutron-rich. These neutron-rich nuclei are unstable and undergo beta decay, converting a neutron into a proton and emitting an electron. This increases the atomic number, creating a new element. The cycle repeats, climbing the periodic table until fission limits halt further growth. The required conditions—enormous neutron fluxes—are found in neutron star mergers and certain supernovae.
Understanding the r-process helps astronomers interpret elemental abundances in old stars and galaxies, and guides searches for gravitational wave counterparts like kilonovae.
The gold in your jewelry was likely forged in the collision of two neutron stars billions of years ago.






