Time range of radiocarbon dating

This discovery meant that there are three naturally occurring isotopes of carbon: Whereas carbon-12 and carbon-13 are stable isotopes, carbon-14 is unstable or radioactive.

Carbon-14 is produced in the upper atmosphere when cosmic rays bombard nitrogen atoms.

The ensuing atomic interactions create a steady supply of c14 that rapidly diffuses throughout the atmosphere.

Plants take up c14 along with other carbon isotopes during photosynthesis in the proportions that occur in the atmosphere; animals acquire c14 by eating the plants (or other animals).

These so-called "solid-carbon" dates were soon found to yield ages somewhat younger than expected, and there were many other technical problems associated with sample preparation and the operation of the counters.

Gas proportional counters soon replaced the solid-carbon method in all laboratories, with the samples being converted to gases such as carbon dioxide, carbon disulfide, methane, or acetylene.

The collagen fraction usually yields more reliable dates than the apatite fraction (see Dates on bones).

In addition to various pre-treatments, the sample must be burned and converted to a form suitable for the counter.

The objective of pre-treatment is to ensure that the carbon being analyzed is native to the sample submitted for dating.Many laboratories now use liquid scintillation counters with the samples being converted to benzene.All of these counter types measure the C-14 content by monitering the rate of decay per unit time.Bases may be used to remove contaminating humic acids.Some types of samples require more extensive pre-treatment than others, and these methods have evolved over the first 50 years of radiocarbon dating.

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Libby calculated the half-life of c14 as 5568 ± 30 years.

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