Trace radioisotope
From Wikipedia, the free encyclopedia
A trace radioisotope is a radioisotope that occurs naturally in trace amounts (i.e. extremely small). This natural formation can be from the decay of heavier nuclei such as uranium-235 decaying into thorium-231. Natural occurrence of radioisotopes can also be driven by cosmic rays. This is the method that creates hydrogen-3 and carbon-14. Isotopes with half-lives greater than about 80 million years also remain in trace amounts from the formation of the Earth. Potassium-40 and vanadium-50 fit into this category.
 |
This chemistry article is a stub. You can help Wikipedia by expanding it. |
