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S1.1 - Introduction to the particulate nature of matter S1.2 - The nuclear atom S1.3 - Electron configurations S1.4 - Counting particles by mass - The mole S1.5 - Ideal gases S2.1 - The ionic model S2.2 - The covalent model S2.3 - The metallic model S2.4 - From models to materials S3.1 - The periodic table - Classification of elements S3.2 - Functional groups - Classification of organic compounds R1.1 - Measuring enthalpy changes R1.2 - Energy cycles in reactions R1.3 - Energy from fuels R1.4 - Entropy and spontaneity AHL R2.1 - How much? The amount of chemical change R2.2 - How fast? The rate of chemical change R2.3 - How far? The extent of chemical change R3.1 - Proton transfer reactions R3.2 - Electron transfer reactions R3.3 - Electron sharing reactions R3.4 - Electron-pair sharing reactions

S1.2 - The nuclear atom

1.2.1 Nuclear Atom and Sub-Atomic Particles 1.2.2 Isotopes and Atomic Mass 1.2.3 Mass Spectrometry and Isotopes (AHL)

Mass Spectrometry and Isotopes HL Only

Specification Reference S1.2.3

Quick Notes:

  • Mass spectrometry is used to identify isotopes of an element and determine their relative abundances.
  • Each peak in a mass spectrum represents an isotope.
  • The height or area of each peak shows the abundance of that isotope.
  • The relative atomic mass (Ar) of the element is calculated as a weighted average of the isotope masses and their abundances.
  • You are not required to know how a mass spectrometer works — focus on interpreting the spectra.

Full Notes:

What Is Mass Spectrometry?

Mass spectrometry is an analytical technique used to:

How a mass spectrometer works has been outlined in more detail here, however you are not required to know any detail about this, only how to interpret and use mass spectra produced.

Interpreting a Mass Spectrum

A mass spectrum is a graph with:

IB Chemistry mass spectrum diagram showing isotope peaks with mass-to-charge ratio and relative abundance axes.

Each peak corresponds to a different isotope of the element.

The m/z value for each peak tells you the mass number of that isotope (assuming a 1+ ion charge).

The height (or area) of the peak tells you how much of it is present in a sample.

Calculating Relative Atomic Mass (Ar)

To find the relative atomic mass, you calculate a weighted average using the isotopic masses and their abundances.

Steps:

  1. Multiply the mass of each isotope by its % abundance.
  2. Add all the results together.
  3. Divide by 100.

Example: Chlorine has two peaks in its mass spectra, from two isotopes:

Use this formula: Ar = (Σ (isotopic mass × % abundance)) / 100

IB Chemistry chlorine mass spectrum showing two peaks at 35 and 37 with relative abundances 75% and 25%.

Ar = (35 × 75 + 37 × 25) / 100 = (2625 + 925) / 100 = 35.5

Summary

Linked Questions

Structure 3.2 – Linked Course Question

How does the fragmentation pattern of a compound in the mass spectrometer help in the determination of its structure?

When a compound is ionised in a mass spectrometer, some molecular ions break apart into smaller charged fragments. Each fragment corresponds to a specific part of the molecule, producing characteristic peaks at different m/z values. By analysing these peaks and matching them to known fragment masses, chemists can identify structural features such as alkyl groups, functional groups, or branching patterns. Together with the molecular ion peak (M⁺), the fragmentation pattern acts like a structural fingerprint that helps deduce the molecule’s overall structure.