Atomic mass calculation involves taking into account each isotope’s atomic mass and its relative abundance. The average atomic mass is calculated using a weighted mean, considering both of these factors. Here's how the process unfolds:
- Multiply the atomic mass of each isotope by its relative abundance (expressed as a fraction).
- Add all these values together. The sum is the average atomic mass of the element.
- This calculated value explains why the atomic mass isn't a simple average of isotope masses—it accounts for abundance.
This method explains the atomic mass results in decimals, rather than whole numbers. A practical example: For sulfur, with most isotopes having a mass near 32, the calculation yields about 32 for its atomic mass. In contrast, chlorine’s isotopes significantly differ, resulting in an average atomic mass of 35.453. Knowing how to calculate and interpret the atomic mass allows for better comprehension of isotopic variations and their significance in chemical science.