Average Atomic Mass Calculator
Calculate an element's weighted mean isotopic mass from isotope masses and natural abundances, with a transparent contribution table and a validated Excel workbook.
Isotope inputs
Live result
Isotope contribution breakdown
| Isotope | Abundance | Isotopic mass (u) | Contribution (u) | Share of weighted sum |
|---|---|---|---|---|
| Isotope 1 | 75.7600% | 34.968852682 | 26.492402792 | 74.7256% |
| Isotope 2 | 24.2400% | 36.965902602 | 8.960534791 | 25.2744% |
How to use the average atomic mass calculator
What this calculator does
This calculator finds the weighted mean mass of an element's isotopes. It multiplies each isotope's mass by its fractional abundance and adds the products. The result is expressed in unified atomic mass units, symbol u (often written amu in classroom materials). It is an exact weighted-average identity for the numbers entered, but it does not identify an unknown element, measure a sample, or guarantee that a laboratory specimen has the same isotope distribution as a published natural-abundance table.
When to use it
Use it to check general-chemistry homework, reproduce a periodic-table atomic weight from isotope data, compare a sample's measured isotope mix with a natural reference, or explore how enrichment changes the weighted mean. For reference data, consult the NIST chlorine isotope composition table, which lists isotope masses and representative compositions.
How to calculate
- The calculator opens with a complete chlorine demonstration and an immediately available validated XLSX workbook.
- Choose Number of isotopes from 2 through 10. Only the selected rows participate.
- Choose Abundance format. Percent entries must total 100; fractional entries must total 1. Switching formats converts the values already entered.
- Replace each Abundance and Isotopic mass (u) value. Results and the contribution table update live.
- Read Average atomic mass, verify Total abundance, and inspect each row's Contribution (u).
- Select Download Excel to export the current validated model. Reset clears the demonstration values and disables export until a complete valid set is entered again.
Input guide
Number of isotopes is a required integer selector from 2 to 10. A value of 2 is suitable for chlorine. Increasing it reveals more required isotope rows; hidden rows are excluded. Abundance format is a required mode selector. Choose Percent (%) for values such as 75.76, or Fraction (0 – 1) for 0.7576. Do not mix the two formats, use scientific notation, or type a percent sign into the field. Each visible Abundance 1 – 10 is a required nonnegative decimal. A higher abundance gives that isotope more influence. Each visible Isotopic mass 1 – 10 (u) is a required positive decimal, such as 34.968852682. A higher mass raises the average in proportion to its abundance. Commas are accepted only as thousands separators in unambiguous U.S. notation; decimal-comma input such as 1,5 is rejected rather than interpreted as 15.
Output guide
Average atomic mass is the weighted mean in u. Total abundance is a validation check and must equal 100.0000% within a very small numerical tolerance. Weighted sum repeats the unrounded weighted total so the calculation is auditable. The header pills show the active isotope count, normalized abundance total, and readiness state. In the table, Abundance shows the normalized percent, Isotopic mass (u) is the entered mass, Contribution (u) is abundance fraction times mass, and Share of weighted sum shows how much of the final weighted total comes from that row. A zero abundance is allowed and produces a zero contribution; a zero or negative mass is invalid.
Worked example
The startup example uses chlorine-35 at 34.968852682 u with 75.76% abundance and chlorine-37 at 36.965902602 u with 24.24% abundance. The calculation is:
(0.7576 × 34.968852682) + (0.2424 × 36.965902602) = 35.4529375826 u
This value lies inside the current chlorine standard atomic-weight interval published by the Commission on Isotopic Abundances and Atomic Weights. Small differences from a textbook's rounded answer usually come from using rounded isotope masses or abundances.
Formula and interpretation
For isotopes indexed from 1 to n, the model is A = Σ(fᵢmᵢ), where fᵢ is fractional abundance and mᵢ is isotopic mass. Percentages are divided by 100 before multiplication. Because the fractions sum to one, the result must fall between the smallest and largest entered mass whenever all abundances are nonnegative. That bound is a useful error check. The CIAAW chlorine overview also explains why standard atomic weights can reflect natural variation rather than one universal decimal for every sample.
Average atomic mass is related to molar mass numerically, but the concepts use different scales: atomic mass describes one atom in u, while molar mass describes one mole in grams per mole. Published atomic weights may be conventional values or intervals because isotope ratios can vary among natural materials. For classroom exercises, use the isotope values supplied by the problem rather than silently substituting a periodic-table value.
Common mistakes
- Entering 75.76 in Fraction mode instead of 0.7576.
- Using mass numbers 35 and 37 when precise isotope masses are required.
- Forgetting that abundances must sum to 100% or 1.
- Rounding every row before adding; keep full precision until the final display.
- Assuming a standard atomic weight exactly describes every natural or enriched sample.