CDS Physics · Heat and Thermodynamics
Change of State and Gases
Latent heat and why evaporation cools, the triple point of water, what the ideal gas model assumes, and how the common thermodynamic processes are named.
Why this matters
Five CDS questions from 2017 (II) to 2026 (I). Two turn on latent heat in daily life, one on the triple point of water, and two on how gases behave: the ideal gas and the Joule-Thomson process.
Concept 1 of 2: Latent heat, evaporation and the triple point
Definition
Heat and change of state:
- Latent heat: heat taken in or given out during a change of state, at constant temperature. .
- Latent heat of fusion of ice: about J/kg. Latent heat of vaporisation of water: about J/kg, nearly seven times larger.
- Evaporation happens at any temperature, from the surface only, and cools what is left behind. It is faster with more surface area, more wind, higher temperature and drier air.
- Cotton in summer: cotton soaks up sweat and spreads it thin, so the sweat evaporates fast and takes latent heat from the body.
- Triple point of water: the one temperature and pressure at which ice, liquid water and water vapour exist together: 273.16 K and about 611 Pa (about 0.006 atmosphere).
Heat for a change of state
- Qheat taken in or given out, in joules
- mmass that changes state, in kg
- Llatent heat of fusion or of vaporisation, in J/kg
Worked example
Practice this conceptself-check · 4 quick reps
The same idea in a real exam question:
Example 1 · Heat and Thermodynamics · Change of State and Gases
Latent heat changes the state, not the temperature
The triple point is 273.16 K, not 273.15 K or 0 K
Concept 2 of 2: The ideal gas and thermodynamic processes
Definition
What the ideal gas model assumes:
- Molecules have negligible size and no forces act between them, so the gas has no potential energy of attraction.
- Collisions are perfectly elastic.
- Molecular speeds are spread over a range (the Maxwell distribution), so the molecules do not all have the same speed or kinetic energy.
- The average kinetic energy depends only on the absolute temperature.
Processes are named by what stays constant:
- Isothermal: temperature. Isobaric: pressure. Isochoric: volume. Adiabatic: no heat enters or leaves.
- Isoenthalpic: enthalpy. The Joule-Thomson (throttling) expansion, a gas forced through a porous plug, keeps enthalpy constant and is used to cool gases to very low temperatures.
| Process | What stays constant |
|---|---|
| Isothermal | Temperature |
| Isobaric | Pressure |
| Isochoric | Volume |
| Adiabatic | No heat flows in or out of the gas |
| Joule-Thomson throttling | Enthalpy (an isoenthalpic process) |
Practice this conceptself-check · 4 quick reps
The same idea in a real exam question:
Example 2 · Heat and Thermodynamics · Change of State and Gases
Equal average energy does not mean equal speeds
Isochoric is volume, isobaric is pressure
Summary — formulas & gotchas at a glance
A revision cheat-sheet for the formulas and gotchas above. Click any concept name to jump back to its full explanation.
Formulas (1)
- Latent heat, evaporation and the triple point
Heat for a change of state
Reference tables (1)
The ideal gas and thermodynamic processes5 rows
| Process | What stays constant |
|---|---|
| Isothermal | Temperature |
| Isobaric | Pressure |
| Isochoric | Volume |
| Adiabatic | No heat flows in or out of the gas |
| Joule-Thomson throttling | Enthalpy (an isoenthalpic process) |
Watch out for (4)
- Latent heat changes the state, not the temperature→ Latent heat, evaporation and the triple point
- The triple point is 273.16 K, not 273.15 K or 0 K→ Latent heat, evaporation and the triple point
- Equal average energy does not mean equal speeds→ The ideal gas and thermodynamic processes
- Isochoric is volume, isobaric is pressure→ The ideal gas and thermodynamic processes
Test yourself on a real paper
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