What's inside an atom, why isotopes give non-whole-number masses, and how a mass spectrometer reveals an element's isotopic fingerprint.
This is the Higher Level lesson. The core S1.2.1–S1.2.2 (subatomic particles, isotopes, relative atomic mass) is shared with SL; the HL-only statement S1.2.3 — mass spectrometry carries a purple HL badge.
An atom has a tiny, dense nucleus of positively charged protons and neutral neutrons, surrounded by fast-moving negatively charged electrons. The atomic number (Z) is the number of protons; the mass number (A) is protons + neutrons.
| Particle | Relative charge | Relative mass | Location |
|---|---|---|---|
| Proton | +1 | 1 | Nucleus |
| Neutron | 0 | 1 | Nucleus |
| Electron | −1 | ≈ 1/1836 (negligible) | Outside the nucleus |
Isotopes are atoms of the same element (same protons) with different numbers of neutrons. The relative atomic mass (Aᵣ) is the weighted average of the isotope masses by their natural abundances:
Aᵣ = Σ (isotope mass × fractional abundance)
A mass spectrometer ionises the sample, accelerates the ions and separates them by mass-to-charge ratio (m/z). The result is a mass spectrum: each peak is an isotope. Peak position = isotope mass (m/z); peak height = relative abundance. Click a peak to read it, then calculate Aᵣ.
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