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  2. 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. − ...

  3. δ13C - Wikipedia

    en.wikipedia.org/wiki/Δ13C

    Foraminifera samples. In geochemistry, paleoclimatology, and paleoceanography δ 13 C (pronounced "delta thirteen c") is an isotopic signature, a measure of the ratio of the two stable isotopes of carbon— 13 C and 12 C—reported in parts per thousand (per mil, ‰). [1]

  4. Isotopes of carbon - Wikipedia

    en.wikipedia.org/wiki/Isotopes_of_carbon

    Carbon (6 C) has 14 known isotopes, from 8 C to 20 C as well as 22 C, of which 12 C and 13 C are stable.The longest-lived radioisotope is 14 C, with a half-life of 5.70(3) × 10 3 years. . This is also the only carbon radioisotope found in nature, as trace quantities are formed cosmogenically by the reactio

  5. Table of nuclides - Wikipedia

    en.wikipedia.org/wiki/Table_of_nuclides

    Isotopes are nuclides with the same number of protons but differing numbers of neutrons; that is, they have the same atomic number and are therefore the same chemical element. Isotopes neighbor each other vertically. Examples include carbon-12, carbon-13, and carbon-14 in the table above.

  6. Isotopic signature - Wikipedia

    en.wikipedia.org/wiki/Isotopic_signature

    Similarly, marine fish contain more 13 C than freshwater fish, with values approximating the C 4 and C 3 plants respectively. The ratio of carbon-13 and carbon-12 isotopes in these types of plants is as follows: [11] C 4 plants: −16‰ to −10‰ CAM plants: −20‰ to −10‰ C 3 plants: −33‰ to −24‰

  7. Carbon - Wikipedia

    en.wikipedia.org/wiki/Carbon

    It belongs to group 14 of the periodic table. [13] Carbon makes up about 0.025 percent of Earth's crust. [14] Three isotopes occur naturally, 12 C and 13 C being stable, while 14 C is a radionuclide, decaying with a half-life of 5,700 years. [15] Carbon is one of the few elements known since antiquity. [16]

  8. 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 include jumping up and down make it difficult to measure half-lives between approximately 10 −19 and 10 −10 seconds.

  9. Carbon-13 nuclear magnetic resonance - Wikipedia

    en.wikipedia.org/wiki/Carbon-13_nuclear_magnetic...

    The major isotope of carbon, the 12 C isotope, has a spin quantum number of zero and so is not magnetically active and therefore not detectable by NMR. 13 C, with a spin quantum number of 1/2, is not abundant (1.1%), whereas other popular nuclei are 100% abundant, e.g. 1 H, 19 F, 31 P.