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Details of carbon dating

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Radiocarbon dating also referred to as carbon dating or carbon dating is a method for determining the age of an object containing organic material by using the properties of radiocarbon , a radioactive isotope of carbon. The method was developed in the late s at the University of Chicago by Willard Libby , who received the Nobel Prize in Chemistry for his work in It is based on the fact that radiocarbon 14 C is constantly being created in the atmosphere by the interaction of cosmic rays with atmospheric nitrogen. The resulting 14 C combines with atmospheric oxygen to form radioactive carbon dioxide , which is incorporated into plants by photosynthesis ; animals then acquire 14 C by eating the plants. When the animal or plant dies, it stops exchanging carbon with its environment, and from that point onwards the amount of 14 C it contains begins to decrease as the 14 C undergoes radioactive decay.
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Is Carbon Dating Accurate?

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Carbon dating | scientific technology |

When we speak of the element Carbon, we most often refer to the most naturally abundant stable isotope 12 C. Although 12 C is definitely essential to life, its unstable sister isotope 14 C has become of extreme importance to the science world. Radiocarbon Dating is the process of determining the age of a sample by examining the amount of 14 C remaining against the known half-life, 5, years. The reason this process works is because when organisms are alive they are constantly replenishing their 14 C supply through respiration, providing them with a constant amount of the isotope. However, when an organism ceases to exist, it no longer takes in carbon from its environment and the unstable 14 C isotope begins to decay.
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Carbon Dating

There are many carbon atoms in our environment. The vast majority of these are 12 C pronounced "c twelve" , the stable isotope of carbon. However, cosmic radiation constantly collides with atoms in the upper atmosphere.
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Thank you for registering with Physics World If you'd like to change your details at any time, please visit My account. They say their study helps refine and calibrate the atmospheric radiocarbon record and provides insights into the causes of variations in atmospheric radiocarbon over time. The radioactive carbon isotope is absorbed from the atmosphere by living organisms and then starts to decay at a known rate once they die. Radiocarbon dating measures the residual levels of this isotope estimate the age of organic materials and it has transformed archaeology and climate science, and other research disciplines. As levels of carbon in the atmosphere fluctuate over time, to enable accurate dating the atmospheric carbon record needs to be calibrated against a calendar time-scale.
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