An example of radiochemical dating is carbon-14 dating, which is used to determine the age of organic materials. It measures the ratio of carbon-14, a radioactive isotope, to carbon-12 in a sample. As carbon-14 decays at a known rate (its half-life is about 5,730 years), scientists can estimate how long it has been since the organism died. This method is particularly useful for dating artifacts, fossils, and other biological remains up to about 50,000 years old.
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Radiochemical yield is calculated by dividing the radioactivity of the desired product by the total radioactivity introduced at the start of the reaction, and then multiplying by 100 to get a percentage yield. The formula for radiochemical yield is: Radiochemical yield (%) = (radioactivity of desired product / total radioactivity introduced) x 100.
Robert Allan Overholt has written: 'A study of coprecipitation using radiochemical techniques' -- subject(s): Precipitation (Chemistry), Radiochemistry, Radiochemical analysis
Carbon-14 is an example of radioactive dating.
Carbon 14 dating is the best known example of radiometric dating, but there are many others. Another example of radiometric dating is the dating of the age of geological formations on earth. The oldest known rocks on the earth that have been analyzed, have been dated back some 4.404 billion years.
fossils.
Examples: - chemistry of water in nuclear reactors - separation of new artificial elements - radiochemical polymerization
Radioactive
Radioactive
It would appear not as my copy of "The Radiochemical Manual" does not list any available isotopes of it.
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Charles K. Garrett has written: 'Radiochemical studies of the interaction of energetic pions with complex nuclei'