Average Atomic Mass Calculator

Calculate the weighted average atomic mass from isotope masses and abundances. Supports 2-6 isotopes with automatic normalization and visual abundance charts.

Element Presets

For comparison
Average Atomic Mass
35.4529 amu
Weighted average of all isotopes
Accepted Value
35.4530 amu
Difference: -0.00013 amu
Percent Error
-0.0004%
Excellent agreement
Molar Mass
35.4529 g/mol
Numerically equal to average atomic mass
Number of Isotopes
2
Abundances total: 100.00%
Dominant Isotope
34.969 amu
75.77% abundance

Isotope Abundance Breakdown

75.8%
24.2%

Contribution Table

IsotopeMass (amu)Abundance (%)FractionContribution (amu)
Isotope 134.969075.7700.7577026.49601
Isotope 236.966024.2300.242308.95686
Total100.001.0000035.45287
Planning notes, formulas, and examples

About the Average Atomic Mass Calculator

Every element on the periodic table lists an atomic mass that is the weighted average of its naturally occurring isotopes. For example, carbon's atomic mass of 12.011 amu comes from 98.93% ¹²C (12.000 amu) and 1.07% ¹³C (13.003 amu). Calculating this average is a fundamental chemistry skill.

The weighted average is computed by multiplying each isotope's mass by its fractional abundance, then summing the products. This process relates directly to mass spectrometry data, where the mass spectrum shows peaks at each isotope's mass with heights proportional to relative abundance.

This calculator supports up to six isotopes and automatically normalizes abundances if they don't sum to 100%. It shows each isotope's contribution to the total, a visual abundance breakdown, and comparison with the periodic table value. It's ideal for general chemistry homework, mass spectrometry analysis, and understanding why atomic masses aren't whole numbers.

When This Page Helps

Essential for general chemistry courses, mass spectrometry data analysis, and understanding isotopic composition. The visual breakdown makes it easy to see how each isotope contributes to the overall atomic mass.

How to Use the Inputs

  1. Select an element preset or start from scratch.
  2. Enter the mass (amu) and percent abundance for each isotope.
  3. Add additional isotopes (up to 6) as needed.
  4. Abundances are auto-normalized if they don't sum to 100%.
  5. View the weighted average atomic mass and each isotope's contribution.
  6. Compare your result against the accepted periodic table value.
  7. Use the abundance chart to visualize isotopic composition.
Formula used
Average Atomic Mass = Σ (fractional abundance_i × isotopic mass_i)\n\nwhere fractional abundance = percent abundance / 100\n\nFor two isotopes:\nM_avg = f₁ × m₁ + f₂ × m₂ (f₁ + f₂ = 1) This keeps planning practical and lowers the chance of preventable errors.

Example Calculation

Result: 35.453 amu

Chlorine has two stable isotopes. Average = 0.7577 × 34.969 + 0.2423 × 36.966 = 26.496 + 8.957 = 35.453 amu, matching the periodic table value.

Tips & Best Practices

  • The most abundant isotope usually has a mass number closest to the rounded atomic mass.
  • If the atomic mass is closer to one isotope's mass, that isotope is more abundant.
  • Monoisotopic elements (only one stable isotope) have integer-like atomic masses: Au = 196.97, Na = 22.99.
  • Mass spectrometry is the primary experimental method for determining isotopic abundances.
  • Radioactive isotopes aren't included in standard atomic mass calculations.
  • IUPAC periodically updates atomic weights as new abundance measurements are published.

How Mass Spectrometry Determines Atomic Mass

A mass spectrometer ionizes atoms, accelerates them through magnetic and electric fields, and separates them by mass-to-charge ratio. The resulting spectrum directly shows which isotopes exist and their relative abundances. Modern instruments can measure isotopic masses to six decimal places.

Notable Isotopic Compositions

Hydrogen is unique: its isotopes differ by 100% and 200% in mass (¹H, ²H, ³H). Chlorine's two-isotope pattern is visible in mass spectra of chlorinated compounds. Lead's atomic mass varies geographically because radiogenic lead (from U and Th decay) changes the isotopic mix.

Isotope Effects in Chemistry

Heavier isotopes form slightly stronger bonds (lower zero-point energy), leading to kinetic and equilibrium isotope effects. This is measurable for hydrogen/deuterium (up to 7× rate difference) and detectable for ¹²C/¹³C and ¹⁶O/¹⁸O ratios in biochemistry and geochemistry.

Sources & Methodology

Last updated:

Frequently Asked Questions

  • Fractional abundance is the decimal form of percent abundance (e.g., 75.77% = 0.7577). Both are equivalent; the calculator accepts percentages for convenience.