Pros and cons of dating objects with carbon 14 articles


09-Jul-2017 02:12

pros and cons of dating objects with carbon 14 articles-89

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The most common form of carbon in the atmosphere is carbon-12, which is a stable isotope of carbon.

An unstable form of carbon isotope, carbon-14, also known as radiocarbon, is formed when cosmic rays hit atoms in the upper atmosphere of the earth.

The method was developed by Willard Libby in the late 1940s and soon became a standard tool for archaeologists.

Libby received the Nobel Prize in Chemistry for his work in 1960.

How is it used * How does it work, from a nuclear / chemical perspective?

By measuring the ratio of the radio isotope to non-radioactive carbon, the amount of carbon-14 decay can be worked out, thereby giving an age for the specimen in question.

But that assumes that the amount of carbon-14 in the atmosphere was constant — any variation would speed up or slow down the clock.

The radiocarbon dating method is based on the fact that radiocarbon is constantly being created in the atmosphere by the interaction of cosmic rays with atmospheric nitrogen.

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The resulting radiocarbon combines with atmospheric oxygen to form radioactive carbon dioxide, which is incorporated into plants by photosynthesis; animals then acquire in a sample from a dead plant or animal such as a piece of wood or a fragment of bone provides information that can be used to calculate when the animal or plant died.Essay Carbon 14 Dating and over other 27,000 free term papers, essays and research papers examples are available on the website!Autor: people • June 13, 2011 • Essay • 470 Words (2 Pages) • 1,445 Views Carbon 14 Dating Intoduction Road workers in Eastern China dug up a 700 yr old mummy.The older a sample is, the less (the period of time after which half of a given sample will have decayed) is about 5,730 years, the oldest dates that can be reliably measured by this process date to around 50,000 years ago, although special preparation methods occasionally permit accurate analysis of older samples.