Nucleosynthesis is the process of creating new atomic nuclei from preexisting nucleons (protons and neutrons). The primordial preexisting nucleons were formed from the quark-gluon plasma of the Big Bang as it cooled below ten million degrees. This first process may be called nucleogenesis, the genesis of nucleons in the universe. The subsequent nucleosynthesis of the elements occurs primarily either by nuclear fusion or nuclear fission.
Historically Arthur Stanley Eddington first suggested in 1920 that stars obtain their energy by fusing hydrogen to helium, but this idea was not generally accepted because it lacked hard calculations for the conditions in stellar cores. Hans Bethe first gave a quantitative description of this process in the years immediately before World War II. Fred Hoyle's original work on nucleosynthesis of heavier elements in stars (including a detailed mechanistic analysis for the production of carbon) occurred just after World War II, but this work was in search of a way to produce heavier elements from hydrogen in stars, in the steady state model of cosmology. Subsequently, Hoyle's picture was expanded by creative contributions by E. Margaret Burbidge, Geoffrey Burbidge, William A. Fowler, Alistair G. W. Cameron, and Donald D. Clayton, and then by many others.
There are a number of astrophysical processes which are believed to be responsible for nucleosynthesis in the universe. The majority of these occur within the hot matter inside stars. The successive nuclear fusion processes which occur inside stars are known as hydrogen burning, helium burning, carbon burning, neon burning, oxygen burning and silicon burning. These processes are able to create elements up to iron and nickel (62Ni is the isotope with the highest binding energy). Heavier elements can be assembled within stars by a neutron capture process known as the s process or in explosive environments, such as supernovae, by a number of processes. Some of the more important of these include the r process which involves rapid neutron captures, the rp process which involves rapid proton captures and the p process (sometimes known as the gamma process) which involves photodisintegration of existing nuclei.
Theories of nucleosynthesis are tested by calculating isotope abundances and comparing with observed results. Isotope abundances are typically calculated by calculating the transition rates between isotopes in a network. Often these calculations can be simplified as a few key reactions control the rate of other reactions.
Astrophysics | Nuclear physics | Nucleosynthesis
Нуклеосинтез | Nukleosynthese | Nucléosynthèse | 핵합성 | Nukleoszintézis | Nucleosynthese | Nukleosynteza | Нуклеосинтез
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