14C is radioactive with a half-life of 5730 yr. It is produced in the upper atmosphere by bombardment of atmospheric 14N by neutrons from cosmic rays.
![]() Although present in too small an amount to change the average atomic mass of carbon, there is enough 14C in living organisms to produce a decay rate of 15.3 disintegrations per minute per gram of carbon. When organisms die, the carbon-14 in the atmosphere no longer keeps the ratio of 14C/12C constant, and the ratio goes down with time. Measuring the 14C/12C ratio in formerly living material allows us to determine its age up to about 25,000 years. |