Radiocarbon Dating

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Radiocarbon Dating


Radiocarbon dating is a chemical analysis used to determine the age of organic materials based on their content of the radioisotope carbon-14, to estimate the age of carbon-bearing materials up to about 58,000 to 62,000 years. Archaeology and other human sciences use radiocarbon dating to prove or disprove theories. Over the years, carbon 14 dating has also found applications in geology, hydrology, geophysics, and atmospheric science. Not all materials can be radiocarbon dated. Most, if not all, organic compounds can be dated. Samples that have been radiocarbon dated since the inception of the method include , twigs, seeds, ,  and , among others. When plants during photosynthesis they include a certain amount of 14C, the isotope in the atmosphere matches the same level approximately. Through photosynthesis Carbon dioxide is taken in by the plant, which is also ingested by animals, therefore every living organism is continually exchanging carbon-14 with its surrounding area as long as it lives. On the other hand when the organism dies the exchanges stops, so the amount of carbon-14 slowly decreases by radioactive beta decay with a half-life of 5,730+-40 years, half-life is the period of time it takes for the amount of a substance undergoing decay to decrease by half.

There are three main types of techniques which are used to measure carbon-14 content of any given sample: gas proportional counting, liquid scintillation counting, and accelerator mass spectrometry. Firstly counting proportional counting is a conventional radiometric dating technique, which counts the quantity of beta particles that are produced by a given sample. A product of radiocarbon decay is beta particles. Measurement of the carbon in the gas proportional counters takes place after it is converted to carbon dioxide. Secondly there liquid scintillation counting which is another radiocarbon dating technique, this was well known in the 1960s.In the process of this method the sample is presented in a liquid form then a scintillator is added. Furthermore the scintillator produces a flash of light when it meets with a beta particle. Between two photomultipliers a sample passed between them, the count can only be made when both devices register the flash of light. The last technique is accelerator mass spectrometry, which is a modern technique of radiocarbon dating method, it is seen as the most effective way of measuring radiocarbon content. This method does not count the beta particles however it does of the number of carbon atoms, the carbon 14 is measured directly unlike the carbon 12 and 13.

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The studies by Rutherford and Holmes on the age of the earth by radiometric dating. Radiometric dating has been ongoing since the year 1905; it was invented by Ernest Rutherford a method that might possibly determine the age of the earth. Radiometric dating is a method used to age materials such as rocks etc. it is the principal source of information about the absolute age of rocks and other geological features, this includes the age of the earth, furthermore it can be ...

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