The process of determining the average mass of an atom, taking into account the relative abundances of its isotopes, is fundamental to chemistry and physics. This calculation involves identifying the different isotopes present, their respective masses, and the percentage of each isotope found in a naturally occurring sample. For example, if an element has two isotopes, one with a mass of 10 amu and an abundance of 20%, and another with a mass of 12 amu and an abundance of 80%, the weighted average would be (10 0.20) + (12 0.80) = 11.6 amu.
Accurately establishing this value is crucial for various applications, from stoichiometric calculations in chemical reactions to understanding nuclear processes. Historically, accurate determination of this quantity has been essential for developing the periodic table and formulating fundamental laws of chemistry. It enables scientists to predict the behavior of elements and compounds in different environments and is a cornerstone of quantitative analysis in research and industry.