Radiation Information - Carbon Dating

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Radiation Information

Carbon Dating

          Radiocarbon dating has been one of the most significant discoveries in 20th century science. Renfrew (1973) said 'the radiocarbon revolution'. Oakley (1979) said, “its development meant an almost complete re-writing of the evolution and cultural emergence of the human species.”

The radiocarbon method was developed by a team of scientists led by ProfessorWillard F. Libby of the University of Chicago

         Today, there are over 130 radiocarbon dating laboratories <http://www.radiocarbon.org/Info/> around the world producing radiocarbon assays for the scientific community. The C14 technique has been and continues to be applied and used in many, many different jobs including hydrology, atmospheric science, oceanography, geology, palaeoclimatology, archaeology and biomedicine.

       There are three principal isotopes of carbon which occur naturally - C12, C13 (both stable) and C14 (unstable or radioactive). One carbon 14 atom exists in nature for every 1,000,000,000,000 C12 atoms in living material. The radiocarbon method is based on the rate of decay of the radioactive or unstable carbon isotope 14 (14C), which is formed in the upper atmosphere through the effect of cosmic ray neutrons upon nitrogen 14. The reaction is:

14N + n => 14C + p

(Where n is a neutron and p is a proton).

         Libby, Anderson and Arnold (1949) first discovered that this decay occurs at a constant rate. They found that after 5568 years, half the C14 in the original sample will have decayed and after another 5568 years, half of that remaining material will have decayed, and so on. The half-life is the name given to this value which Libby measured at 5568 per 30 years. This became known as the Libby half-life. After 10 half-lives, there is a very small amount of radioactive carbon in a sample. At about 50 - 60 000 years, then, the technique can’t be used  (beyond this time, other radiometric techniques must be used for dating). By measuring the C14 concentration of a sample whose age is not known, it is possible to tell the countrate or number of decay events per gram of Carbon. By comparing this with modern levels of activity (1890 wood corrected for decay to 1950 AD) and using the measured half-life it becomes possible to calculate a date for the death of the sample.

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Power Generation

      Nuclear power plants are fuelled by uranium, a naturally occurring element found in the Rocky Mountains and in countries such as Canada, Australia and South Africa. The nearly infinite energy that is stored in uranium atoms makes nuclear power possible.

       The interaction between three "heavy" elements - two types of uranium and a form of plutonium -- creates a chain reaction that can be harnessed to generate electricity. The nuclear reaction generates heat that is used to boil water to create steam to drive a turbine to generate electricity. Like ...

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