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  2. Neutron - Wikipedia

    en.wikipedia.org/wiki/Neutron

    Fusion reactors that generate neutrons are likely to create radioactive waste, but the waste is composed of neutron-activated lighter isotopes, which have relatively short (50–100 years) decay periods as compared to typical half-lives of 10,000 years [118] for fission waste, which is long due primarily to the long half-life of alpha-emitting ...

  3. Island of stability - Wikipedia

    en.wikipedia.org/wiki/Island_of_stability

    As of 2019, 251 nuclides are observed to be stable (having never been observed to decay); [9] generally, as the number of protons increases, stable nuclei have a higher neutron–proton ratio (more neutrons per proton). The last element in the periodic table that has a stable isotope is lead (Z = 82), [a] [b] with stability (i.e., half-lives of ...

  4. Marine biogeochemical cycles - Wikipedia

    en.wikipedia.org/wiki/Marine_biogeochemical_cycles

    Since liquid water flows, ocean waters cycle and flow in currents around the world. Since water easily changes phase, it can be carried into the atmosphere as water vapour or frozen as an iceberg. It can then precipitate or melt to become liquid water again. All marine life is immersed in water, the matrix and womb of life itself. [7]

  5. Free neutron decay - Wikipedia

    en.wikipedia.org/wiki/Free_neutron_decay

    Therefore, the half-life for this process (which differs from the mean lifetime by a factor of ln(2) ≈ 0.693) is 611 ± 1 s (about 10 min, 11 s). [3] [4] The beta decay of the neutron described in this article can be notated at four slightly different levels of detail, as shown in four layers of Feynman diagrams in a section below. n 0 → p ...

  6. Marine life - Wikipedia

    en.wikipedia.org/wiki/Marine_life

    Marine life, sea life or ocean life is the collective ecological communities that encompass all aquatic animals, plants, algae, fungi, protists, single-celled microorganisms and associated viruses living in the saline water of marine habitats, either the sea water of marginal seas and oceans, or the brackish water of coastal wetlands, lagoons ...

  7. Carbon-14 - Wikipedia

    en.wikipedia.org/wiki/Carbon-14

    Carbon-14 can also be produced by other neutron reactions, including in particular 13 C(n,γ) 14 C and 17 O(n,α) 14 C with thermal neutrons, and 15 N(n,d) 14 C and 16 O(n, 3 He) 14 C with fast neutrons. [28] The most notable routes for 14 C production by thermal neutron irradiation of targets (e.g., in a nuclear reactor) are summarized in the ...

  8. Radiocarbon dating - Wikipedia

    en.wikipedia.org/wiki/Radiocarbon_dating

    The calculation uses 8,033 years, the mean-life derived from Libby's half-life of 5,568 years, not 8,267 years, the mean-life derived from the more accurate modern value of 5,730 years. Libby's value for the half-life is used to maintain consistency with early radiocarbon testing results; calibration curves include a correction for this, so the ...

  9. Neutron radiation - Wikipedia

    en.wikipedia.org/wiki/Neutron_radiation

    Neutron radiation is a form of ionizing radiation that presents as free neutrons.Typical phenomena are nuclear fission or nuclear fusion causing the release of free neutrons, which then react with nuclei of other atoms to form new nuclides—which, in turn, may trigger further neutron radiation.