Sign in to save

Bookmark this page so you can find it later.

Sign in to save

Bookmark this page so you can find it later.

Heating and cooling curves show how the temperature of a substance changes as heat is added or removed. They matter because they connect energy, temperature, and phase changes in one simple graph. A typical heating curve rises during warming within one phase, then becomes flat during melting or boiling.

A cooling curve has the same ideas in reverse as a substance releases energy and changes from gas to liquid to solid.

During a sloped part of the curve, added or removed heat changes the average kinetic energy of the particles, so the temperature changes. During a flat plateau, the energy changes the particle arrangement and intermolecular forces instead of changing temperature. The heat needed for a phase change is calculated with q = mΔHfus or q = mΔHvap, while heating within one phase uses q = mcΔT.

Reading the curve carefully helps identify the phase, the phase change, and which equation to use.

Key Facts

  • Temperature changes only on sloped segments of a heating or cooling curve.
  • Temperature stays constant during a phase change because energy changes potential energy, not average kinetic energy.
  • Heating within one phase uses q = mcΔT.
  • Melting or freezing uses q = mΔHfus.
  • Boiling or condensing uses q = mΔHvap.
  • For the same substance, ΔHvap is usually greater than ΔHfus because separating particles into a gas requires more energy.

Vocabulary

Heating curve
A graph showing how the temperature of a substance changes as heat is added.
Cooling curve
A graph showing how the temperature of a substance changes as heat is removed.
Heat of fusion
The energy required to melt a unit mass or mole of a substance at its melting point.
Heat of vaporization
The energy required to vaporize a unit mass or mole of a substance at its boiling point.
Plateau
A flat part of a heating or cooling curve where temperature stays constant during a phase change.

Common Mistakes to Avoid

  • Using q = mcΔT during a plateau is wrong because ΔT = 0 during a phase change, so latent heat equations must be used instead.
  • Thinking the substance stops absorbing heat on a flat segment is wrong because heat is still being used to overcome or form intermolecular attractions.
  • Confusing melting point with boiling point is wrong because the lower plateau is usually melting or freezing and the higher plateau is usually boiling or condensing.
  • Ignoring the direction of the curve is wrong because heating adds energy while cooling removes energy, even if the phase-change temperatures are the same.

Practice Questions

  1. 1 A 50.0 g sample of ice at 0°C melts completely. If the heat of fusion of water is 334 J/g, how much heat is absorbed?
  2. 2 A 25.0 g sample of liquid water warms from 20.0°C to 80.0°C. If c = 4.18 J/g°C, how much heat is absorbed?
  3. 3 On a heating curve, a substance reaches a flat segment at 100°C while heat continues to be added. Explain what is happening to the particles and why the temperature does not rise.