Atomic Weight Formula:
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Atomic weight (also called relative atomic mass) is the average mass of atoms of an element, calculated using the relative abundance of isotopes in a naturally-occurring element. It accounts for all the natural isotopes of an element and their proportions.
The calculator uses the atomic weight formula:
Where:
Explanation: The atomic weight is a weighted average where each isotope's mass is multiplied by its natural abundance percentage (divided by 100), and all values are summed together.
Details: Atomic weight is fundamental in chemistry for stoichiometric calculations, determining molar masses of compounds, and understanding chemical reactions. It appears on the periodic table for each element.
Tips: Enter each isotope's mass in atomic mass units (amu) and its natural abundance percentage. Click "Add Another Isotope" for elements with multiple isotopes. Ensure abundance percentages sum to approximately 100% for accurate results.
Q1: Why isn't atomic weight a whole number?
A: Atomic weight is an average that accounts for different isotopes and their natural abundances, which rarely results in a whole number.
Q2: How is this different from mass number?
A: Mass number is the sum of protons and neutrons in a specific isotope (always a whole number), while atomic weight is the weighted average of all naturally occurring isotopes.
Q3: Why do some elements have atomic weights in brackets?
A: Brackets indicate the atomic weight is for the most stable isotope, as these elements have no stable isotopes and their compositions vary.
Q4: How often are standard atomic weights updated?
A: The IUPAC updates atomic weights biennially to reflect new measurements of isotopic abundances.
Q5: Can atomic weight vary in nature?
A: Yes, some elements (like lithium) show natural variation in isotopic composition, leading to slightly different atomic weights in different samples.