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Topic 2 of 6 · 3 of 6 modules ready

Thermal physics

The particle model of matter and how heating changes temperature, state and size.

Modules

  1. A plain aerosol spray can lying on the dashboard of a parked car, in strong sunshine under the windscreen.

    Module 2 · syllabus 2.1.2, 2.1.3, 2.2.1 · 3 parts

    Gas pressure and temperature

    Why can a sealed can burst when it gets hot?

    Trap some air in a syringe joined to a pressure gauge and squeeze it to smaller and smaller volumes, with a magnifier showing a model of its particles. Then lock the plunger, cool the air with ice and warm it on a hotplate, and extend the graph to find where the pressure would reach zero.

    1. Squeezing a gas Gas pressure from particles hitting the walls, as a force per unit area; squeezing a gas at a steady temperature, and pV = constant with its graphs
    2. Heating a gas at a fixed volume Heating a gas at a fixed volume, in particle terms; the kelvin scale and T = θ + 273
    3. Thermal expansion Thermal expansion of solids, liquids and gases, why gases expand most, and where expansion is useful or a problem

    Experiment Squeeze trapped air · then lock it, cool it and warm it

Syllabus statements for this topic · for teachers · 45 statements

Core for every pupil · Supplement also for Extended entry. Paraphrased from the Cambridge IGCSE Physics 0625 syllabus (2026–2028); check the official syllabus for exact wording.

2.1.1 States of matter

  • 2.1.1.1Properties of solids, liquids and gasesC
  • 2.1.1.2Names of the changes of stateC

2.1.2 Particle model

Covered in Gas pressure and temperature

  • 2.1.2.1Particle arrangement, separation and motion; particle diagramsC
  • 2.1.2.2Particle motion, temperature and absolute zeroC
  • 2.1.2.3Gas pressure from particle collisions with wallsC
  • 2.1.2.4Random motion of suspended specks supports the particle modelC
  • 2.1.2.5Brownian motion explained by random molecular collisionsC
  • 2.1.2.6Particle forces, distances and motion set propertiesS
  • 2.1.2.7Gas pressure as collision force per unit areaS
  • 2.1.2.8Fast light molecules move visible specks; atoms versus specksS

2.1.3 Gases and the absolute scale of temperature

Covered in Gas pressure and temperature

  • 2.1.3.1Gas pressure with temperature or volume, in particle termsC
  • 2.1.3.2Kelvin and Celsius; T = θ + 273C
  • 2.1.3.3pV = constant at fixed temperature, with its graphS

2.2.1 Thermal expansion of solids, liquids and gases

Covered in Gas pressure and temperature

  • 2.2.1.1Thermal expansion of solids, liquids and gasesC
  • 2.2.1.2Everyday uses and problems of thermal expansionC
  • 2.2.1.3Why gases expand most and solids leastS

2.2.2 Specific heat capacity

Covered in Specific heat capacity

  • 2.2.2.1Temperature rise increases internal energyC
  • 2.2.2.2Temperature rise as higher average particle kinetic energyS
  • 2.2.2.3Specific heat capacity; c = ΔE/(mΔθ)S
  • 2.2.2.4Measuring specific heat capacity of a solid and liquidS

2.2.3 Melting, boiling and evaporation

Covered in Melting, boiling and evaporation

  • 2.2.3.1Melting and boiling: energy in, temperature steadyC
  • 2.2.3.2Melting and boiling points of waterC
  • 2.2.3.3Condensation and solidification in particle termsC
  • 2.2.3.4Evaporation as escape of faster surface particlesC
  • 2.2.3.5Evaporation cools the remaining liquidC
  • 2.2.3.6Boiling versus evaporationS
  • 2.2.3.7Temperature, surface area and airflow affect evaporationS
  • 2.2.3.8Cooling an object by an evaporating liquidS

2.3.1 Conduction

  • 2.3.1.1Experiments comparing thermal conductors and insulatorsC
  • 2.3.1.2Conduction by lattice vibrations and free electronsS
  • 2.3.1.3Why gases and most liquids conduct poorlyS
  • 2.3.1.4Many solids conduct moderately wellS

2.3.2 Convection

  • 2.3.2.1Convection transfers energy in liquids and gasesC
  • 2.3.2.2Convection from density changes; demonstration experimentsC

2.3.3 Radiation

  • 2.3.3.1Thermal radiation is infrared; all objects emit itC
  • 2.3.3.2Radiation transfer needs no mediumC
  • 2.3.3.3Surface colour and texture versus infrared emission and absorptionC
  • 2.3.3.4Steady temperature: energy out equals energy inS
  • 2.3.3.5Unequal energy rates warm or cool an objectS
  • 2.3.3.6Earth's temperature and its radiation balanceS
  • 2.3.3.7Experiments comparing infrared emittersS
  • 2.3.3.8Experiments comparing infrared absorbersS
  • 2.3.3.9Emission rate with surface temperature and areaS

2.3.4 Consequences of thermal energy transfer

  • 2.3.4.1Everyday transfers: pans and room heatingC
  • 2.3.4.2Combined transfers: coal fire, car radiatorS