
An
isotope is a variation of a basic element. This means that one particular atom
can have different “flavors”. Isotope “flavors” of the same chemical element
always have the same number of protons (atomic number), but might have a
different number of neutrons in its nucleus than is typical. For example, one
of the most common elements is carbon. Three isotopes of carbon are carbon-12,
carbon-13, and carbon-14. The number after carbon represents the mass of each
isotope respectively. Each of these isotopes has 6 protons, therefore an atomic
number of 6. To determine the number of neutrons just subtract the atomic
number from each mass.
We
call carbon-13 the heavy isotope and carbon-12 the light isotope. “Lighter”
isotopes can run faster through chemical reactions and “heavier” ones lag
behind. Because the different isotopes move at different speeds through plants
and animals, the amounts of light and heavy isotopes can change. For instance,
plants use carbon dioxide in photosynthesis. The plant will use carbon dioxide
with carbon-12 faster than it will use carbon-13. Therefore, leaves in plants
have less carbon-13 in the, than in the carbon dioxide. This process is called isotope
fractionation.
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