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  2. Beta decay - Wikipedia

    en.wikipedia.org/wiki/Beta_decay

    An example of electron emission (β − decay) is the decay of carbon-14 into nitrogen-14 with a half-life of about 5,730 years: 14 6 C → 14 7 N + e − + ν e. In this form of decay, the original element becomes a new chemical element in a process known as nuclear transmutation.

  3. List of radioactive nuclides by half-life - Wikipedia

    en.wikipedia.org/wiki/List_of_radioactive...

    This is a list of radioactive nuclides (sometimes also called isotopes), ordered by half-life from shortest to longest, in seconds, minutes, hours, days and years. Current methods make it difficult to measure half-lives between approximately 10 −19 and 10 −10 seconds.

  4. Isotopes of cadmium - Wikipedia

    en.wikipedia.org/wiki/Isotopes_of_cadmium

    For two of them, natural radioactivity was observed, and three others are predicted to be radioactive but their decays have not been observed, due to extremely long half-lives. The two natural radioactive isotopes are 113 Cd (beta decay, half-life is 8.04 × 10 15 years) and 116 Cd (two-neutrino double beta decay, half-life is 2.8 × 10 19 years).

  5. Isotopes of cobalt - Wikipedia

    en.wikipedia.org/wiki/Isotopes_of_cobalt

    Naturally occurring cobalt, Co, consists of a single stable isotope, 59 Co (thus, cobalt is a mononuclidic element). Twenty-eight radioisotopes have been characterized; the most stable are 60 Co with a half-life of 5.2714 years, 57 Co (271.811 days), 56 Co (77.236 days), and 58 Co (70.844 days).

  6. Isotopes of thorium - Wikipedia

    en.wikipedia.org/wiki/Isotopes_of_thorium

    Thorium (90 Th) has seven naturally occurring isotopes but none are stable. One isotope, 232 Th, is relatively stable, with a half-life of 1.405×10 10 years, considerably longer than the age of the Earth, and even slightly longer than the generally accepted age of the universe.

  7. Carbon-13 - Wikipedia

    en.wikipedia.org/wiki/Carbon-13

    Bulk carbon-13 for commercial use, e.g. in chemical synthesis, is enriched from its natural 1% abundance. Although carbon-13 can be separated from the major carbon-12 isotope via techniques such as thermal diffusion, chemical exchange, gas diffusion, and laser and cryogenic distillation, currently only cryogenic distillation of methane (boiling point −161.5°C) or carbon monoxide (b.p. − ...

  8. Spontaneous fission - Wikipedia

    en.wikipedia.org/wiki/Spontaneous_fission

    [4]: 484 Spontaneous fission does not favour equal-mass fragments, and no convincing explanation has been found to explain this. [4]: 484 In rare instances (0.3%), three or more fission fragments may be created. [10] Ternary products are usually alpha-particles, though can be as massive as oxygen nuclei. [2]: 46

  9. Radium - Wikipedia

    en.wikipedia.org/wiki/Radium

    Its immediate decay product is the dense radioactive noble gas radon (specifically the isotope 222 Rn), which is responsible for much of the danger of environmental radium. [14] [b] It is 2.7 million times more radioactive than the same molar amount of natural uranium (mostly uranium-238), due to its proportionally shorter half-life. [15] [16]