Atomic weight, often referred to as the average atomic mass, plays a crucial role in understanding why atomic masses on the periodic table do not match exactly with whole numbers for certain elements. Unlike the specific mass of a single isotope, the atomic weight considers:
- The relative abundance of each isotope in nature
- The individual mass of each isotope
This weighted average reflects the fact that most elements exist as a mixture of isotopes. To calculate it, you multiply the mass of each isotope by its relative abundance (expressed as a decimal), then sum these values. For example, since carbon mainly consists of Carbon-12 and Carbon-13, the atomic weight of carbon is calculated as follows:
\[Atomic \ Weight = (12 \times 0.9889) + (13 \times 0.0111) \approx 12.011\]
This value is what you see listed as the atomic weight in the periodic table, which gives a more practical representation of how the element behaves in the natural world.