The nucleus of carbon 14 contains 6 protons and 8 neutrons, as opposed to the 6 and 6 found in ordinary carbon 12. The imbalance makes carbon 14 a radioisotope with a half-life of 5,700 years, and an emitter of beta particles. This radioactive isotope of carbon is called radiocarbon.
The carbon 14 found in nature is constantly being regenerated by cosmic rays hitting the atmosphere. The rate at which the regeneration takes place has gone virtually unchanged for centuries; a feature which depends on the flux of particles bombarding the earth, and the strength of the magnetic field capable of diverting them. This magnetic shield, and consequently the particle flux, has slowly changed over time, and the quantity of carbon 14 formed on Earth changes with it.
Incoming cosmic rays create atoms of carbon 14 by colliding with nuclei in the upper atmosphere, liberating neutrons. These neutrons in turn interact with nuclei of nitrogen in the air, replacing one of the 7 protons nitrogen contains with an extra neutron. The resulting atom, now containing 6 protons and 8 neutrons, is one of carbon 14
Carbon gases formed with carbon 14 are chemically indistinguishable from gases with the ordinary isotope of carbon, carbon 12. The radioactive atom is absorbed by plants and living matter in the same way as its non-radioactive isotope ; in every thousand billion (ten to the power of twelve) atoms of carbon 12, there will be on average one atom of carbon 14.
This tiny ratio exists in all molecules involving carbon atms, including all living matter. This is why carbon 14, along with potassium 40, accounts for almost all the natural radioactivity of our body.
When a living organism dies, the radioactive carbon is no longer absorbed, and the ratio of carbon 14 present begins to decrease. The amount still present in a sample of what was once a living creature can thus be used to determine its age.
Carbon 14 can also be used as a radioactive marker.
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