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Isotopic abundance is significant as it determines the average atomic mass of an element.
Isotopic abundance refers to the amount of each different isotope of an element that exists in nature. Each element can have several isotopes, which are atoms with the same number of protons but different numbers of neutrons. This means they have the same atomic number but different mass numbers. The isotopic abundance of an element is usually expressed as a percentage, indicating the proportion of each isotope in a sample of the element.
The significance of isotopic abundance lies in its impact on the average atomic mass of an element. The atomic mass listed on the periodic table for each element is not simply the mass of one atom of that element. Instead, it is a weighted average that takes into account the masses of all the element's naturally occurring isotopes and their relative abundances.
For example, carbon has two stable isotopes, carbon-12 and carbon-13. Carbon-12 makes up about 98.9% of all naturally occurring carbon, while carbon-13 accounts for the remaining 1.1%. Therefore, the average atomic mass of carbon is close to 12, but not exactly 12, due to the small contribution from carbon-13.
Understanding isotopic abundance is also crucial in fields such as geochemistry and environmental science. For instance, the ratios of different isotopes can provide information about the age of rocks or the source of certain pollutants. Therefore, isotopic abundance is not only significant in determining the average atomic mass of an element, but also in various scientific research and applications.
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