1. Carbon-14 atoms produced in the upper atmosphere combine with oxygen to yield 14CO2, which slowly diffuses into the lower atmosphere, where it mixes with ordinary 12CO2 and is taken-up by plants during photosynthesis. When these plants are eaten, carbon-14 enters the food chain and is ultimately distributed evenly throughout all living organisms – so an equilibrium is established between the amount of C-14 consumed by the organism and the amount that is lost through exhalation of CO2 and excretion. In other words, the amount of C-14 in a living organism remains constant over time. Of course, when the organism dies, it ceases to take-up carbon-14, which very slowly decays back to nitrogen14 through slow nuclear decay. Therefore, the older a dead thing is, the less C-14 it has. Write the balanced nuclear equation for the radioactive decay of C-14 to N-14. 3.
2. What is the name of the process by which 14C is converted to 14N in the previous problem?
1. Carbon-14 atoms produced in the upper atmosphere combine with oxygen to yield 14CO2, which slowly diffuses into the lower atmosphere, where it mixes with ordinary 12CO2 and is taken-up by plants du...
Carbon 14 is a radioactive isotope produced in the upper atmosphere by cosmic rays. It has a half-life measured as 5730 : 40 years. Since plants and animals absorb carbon from the atmosphere, the percentage of carbon a living organism contains that is carbon 14 is equal to the percentage of carbon 14 in the atmosphere. When an organism dies, however (or when a layer of wood is laid down as bark in a tree), it ceases to absorb carbon....