Weighted-Average Atomic Mass Calculator
Specialized for Mercury (Hg) and Other Element Analysis
Calculate the Weighted-Average Atomic Mass of Mercury
Edit the abundances or masses below to calculate the atomic weight. Default values represent natural Mercury (Hg).
| Isotope | Mass (u) | Abundance (%) | Weighted Contribution (u) |
|---|
Calculate the Weighted-Average Atomic Mass of Mercury
Understanding how to calculate the weighted-average atomic mass of mercury is fundamental for chemistry students, researchers, and lab technicians. Unlike simple averages, a weighted average accounts for the fact that not all isotopes of mercury (Hg) are equally common in nature. This calculator provides a precise method to determine the atomic mass based on specific isotopic compositions, which can vary slightly depending on the geological source of the sample.
What is the Weighted-Average Atomic Mass?
The weighted-average atomic mass is the mass of an element listed on the periodic table. It is not the mass of a single atom, but rather the average mass of all atoms of that element found in nature, weighted by their percent abundance.
For Mercury (Hg), there are seven stable isotopes naturally occurring. To calculate the weighted-average atomic mass of mercury accurately, one must consider the mass of each specific isotope and how frequently it appears (its abundance). This concept is crucial in stoichiometry, mass spectrometry, and environmental tracing.
Who uses this calculation?
- Chemists: For precise molar mass calculations in reactions.
- Geologists: To trace the origin of mercury samples via isotope ratios.
- Physics Students: To understand nuclear structure and stability.
Formula and Mathematical Explanation
The formula to calculate the weighted-average atomic mass of mercury is a summation of the products of each isotope's mass and its fractional abundance.
Atomic Mass = Σ (Isotope Mass × (Abundance % / 100))
Where:
• Σ means "sum of".
• Isotope Mass is the precise mass of the specific atom in atomic mass units (u).
• Abundance % is the percentage of that isotope found in nature.
| Variable | Meaning | Unit | Typical Range (Hg) |
|---|---|---|---|
| Mavg | Weighted Average Mass | u (amu) | 200.59 u |
| mi | Mass of Isotope i | u (amu) | 196 – 204 u |
| pi | Percent Abundance | % | 0.15% – 29.86% |
Practical Examples: Calculating Mercury's Mass
Example 1: Standard Natural Abundance
Consider a standard sample of Mercury. We want to calculate the weighted-average atomic mass of mercury using the three most abundant isotopes for simplicity (though our calculator uses all 7).
- Hg-200: 199.968 u (23.10%)
- Hg-202: 201.971 u (29.86%)
- Hg-199: 198.968 u (16.87%)
Calculation (Partial):
(199.968 × 0.2310) + (201.971 × 0.2986) + …
When all 7 isotopes are included, the sum equals approximately 200.59 u. This matches the standard atomic weight found on periodic tables.
Example 2: Enriched Mercury Sample
In nuclear physics or medical lighting, enriched mercury might be used. Suppose a sample is enriched to contain 90% Hg-198 (Mass ~197.97 u) and 10% Hg-202 (Mass ~201.97 u).
Calculation:
Mass = (197.97 × 0.90) + (201.97 × 0.10)
Mass = 178.173 + 20.197
Result: 198.37 u
This example shows how the average mass shifts significantly towards the most abundant isotope.
How to Use This Atomic Mass Calculator
Our tool allows you to calculate the weighted-average atomic mass of mercury quickly:
- Review Isotope Data: The calculator is pre-filled with standard IUPAC data for Mercury's 7 stable isotopes.
- Modify Values (Optional): If you are working with a specific non-standard sample, adjust the Abundance percentage or Mass values.
- Check Total Abundance: Ensure the "Total Abundance" equals 100%. The tool highlights this figure.
- Analyze Results: View the final atomic mass, the contribution table, and the abundance distribution chart.
Key Factors That Affect Atomic Mass Results
When you calculate the weighted-average atomic mass of mercury, several factors ensure accuracy:
- Geological Origin: Mercury samples from different mines (e.g., Almadén vs. Idrija) can have slight isotopic variations due to mass-dependent fractionation.
- Sample Purity: Contamination with other elements changes the bulk mass, though this calculator focuses purely on mercury isotopes.
- Significant Figures: Using precise isotope masses (to 4 decimal places) is vital. Rounding too early can introduce errors of ±0.01 u.
- Radiogenic Daughters: While Hg isotopes are stable, traces of radiogenic isotopes from other decays could theoretically alter mass in specific ores.
- Isotope Fractionation: Biological or chemical processes can slightly prefer lighter isotopes ($^{198}Hg$) over heavier ones ($^{204}Hg$), shifting the effective atomic mass in environmental samples.
- Experimental Error: Mass spectrometry limits determine the precision of the input "abundance" values.