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nucleosynthesis

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Nucleosynthesis is the set of nuclear processes leading to the formation of chemical elements. Primordial nucleosynthesis (the first few minutes after the Big Bang) produced hydrogen (~75% by mass), helium (~25%), and traces of lithium. Stellar nucleosynthesis occurs in two stages: burning of light elements (up to iron) in stellar cores and explosive synthesis (heavier than iron) during supernovae and neutron star mergers. Main reactions: pp-chain, CNO cycle, triple-alpha process, s-process (slow neutron capture), r-process (rapid neutron capture).

History

In the 1940s–1950s, scientists George Gamow, Ralph Alpher and others proposed that the elements originated in the hot early universe. But it later turned out that most elements were created in stars. In 1957, the famous B²FH paper was published, which described in detail the processes of stellar nucleosynthesis.

How it works

In the center of a star, temperatures of millions of degrees cause nuclei to collide and fuse, releasing energy, like compressed springs releasing their stored force when joined together. The star successively burns hydrogen, then helium, carbon and so on, until iron is formed. Iron is 'nuclear ash', further fusion yields no energy. Then the core collapses, and the star explodes, creating elements heavier than iron.

💡 The element technetium, which has no stable isotopes and is almost absent on Earth, has been detected in the spectra of giant stars — this is direct evidence that stars continuously produce new nuclei.
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Scientists
Fred HoyleMargaret BurbidgeRalph Alpher
Related tags
big bangcarboncosmic dustheliumkilonovaneutron starnuclear fusionstar formation
Laws
mass–energy equivalencetriple-alpha process (Hoyle process)

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