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Part 3 of 3

Cooling it back down

On a cold morning, the inside of the kitchen window is covered with drops of water. Outside, the pond has turned to ice. Nobody poured water on the window. Where did it come from? In this part you'll follow the changes in reverse: gas to liquid, then liquid to solid. You'll read cooling curves and use melting and boiling points to predict the state of any substance.

A cold morning in a warm kitchen. The kettle adds water vapour to the air; drops form on the inside of the cold window. Outside, the pond is frozen. (enlarge)

Condensing: gas to liquid

The air in a kitchen always contains some water vapour, a gas. The kettle adds more. When water molecules in the air hit the cold glass, they lose energy and slow down. Forces of attraction pull them close together, and they form drops of liquid. A gas changing into a liquid is condensing, also called condensation. Like evaporation, this happens far below 100 °C.

Pure water vapour behaves differently. Cool steam (water vapour with no air mixed in) at normal atmospheric pressure, and it condenses at 100 °C, its boiling point. The temperature then stays at 100 °C until all of it has condensed: boiling in reverse. Water vapour mixed with air condenses on any surface that is cold enough: evaporation in reverse.

50 g of pure steam cooled at a steady rate: the experiment run backwards. The temperature stays at 100 °C while the steam condenses and at 0 °C while the water freezes. (enlarge)

Trap: “The water on the outside of a cold glass leaked through it.” Glass doesn't let water through. Water vapour from the air condensed on the cold surface. That's where the drops on the glass in part 1 came from.

Trap: “The white cloud above a kettle is a gas.” Water vapour is invisible. The white cloud is tiny drops of liquid water that have already condensed in the cooler air.

Freezing: liquid to solid

Now cool liquid water. Its molecules move more and more slowly. At 0 °C they settle into fixed positions in a regular pattern, and the water becomes ice. A liquid changing into a solid is freezing.

For a pure substance, the freezing point is the same temperature as its melting point. Water freezes, and ice melts, at 0 °C. Which one happens depends on whether the water is losing or gaining energy.

The cooling curve

Melt some stearic acid, a waxy solid, in a test tube. Then let it cool in air and record its temperature every minute. Predict the shape of the graph before you look.

Stearic acid cooling in air. The temperature falls, stays at 69 °C while the liquid freezes, then falls again as the solid cools. (enlarge)

Did you predict a flat part? The temperature falls, stays at 69 °C for several minutes, then falls again. The flat part is freezing. The tube is still losing energy to the cooler room. But as the particles move into fixed positions, forces of attraction pull them together, and energy is released. That energy replaces what the tube loses, so the temperature stays constant until all the liquid has frozen.

Key idea: Flat parts on heating and cooling curves are changes of state. On heating, energy is taken in to overcome forces between particles. On cooling, energy is released as forces pull the particles together.

Which state at a given temperature?

Melting and boiling points tell you the state of a substance at any temperature.

  • Below its melting point, it's a solid.
  • Between its melting point and its boiling point, it's a liquid.
  • Above its boiling point, it's a gas.
A temperature line for mercury. Below its melting point of −39 °C it is a solid; between −39 °C and its boiling point of 357 °C it is a liquid; above 357 °C it is a gas. At 25 °C mercury is a liquid. (enlarge)

Trap: “Its boiling point is above room temperature, so it must be a liquid.” Check the melting point too. Iron boils far above room temperature, but it also melts far above room temperature, so it's a solid.

The five changes of state

Taking in energy moves a substance up: melting, then boiling or evaporating. Giving out energy moves it down: condensing, then freezing. (enlarge)

Melting and freezing link solids and liquids. Boiling, evaporating and condensing link liquids and gases. In every one, the particles themselves stay the same; their separation, arrangement and motion change.

Worked example

Reading a cooling curve

Use the stearic acid curve. What is its freezing point, what is in the tube at 6 minutes, and why is the temperature constant there?

The flat part is at 69 °C, so the freezing point is 69 °C. At 6 minutes the temperature is on the flat part: freezing is under way, so liquid and solid stearic acid are both present. The temperature stays constant because energy released as particles are pulled into fixed positions replaces the energy lost to the room. Its melting point is also 69 °C: the same temperature, reached by heating instead of cooling.

Worked example

Solid, liquid or gas at 25 °C?

Mercury melts at −39 °C and boils at 357 °C. Is it a solid, a liquid or a gas at 25 °C?

Compare 25 °C with each point, as on the temperature line above. It's above the melting point, so mercury isn't a solid. It's below the boiling point, so mercury isn't a gas. Between the two, mercury is a liquid: the silvery liquid metal once used in thermometers.

Case closed

Condensing is the reverse of boiling and evaporating; freezing is the reverse of melting. On a cooling curve, a flat part shows a change of state: energy released as particles are pulled together keeps the temperature steady. To find the state at any temperature, compare it with the melting point and the boiling point.

About this model

Real cooling curves bend, because a warm sample loses heat more slowly as it nears room temperature. Some liquids cool a little below their freezing point before crystals start to form; our figures leave this out. The steam curve assumes energy is removed at a steady rate, like the hotplate run backwards.

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Scope and sources

Cambridge IGCSE Chemistry 0620 · 2026–2028 v2 · Original learning materials.

Distinguishing properties and particle structure of solids, liquids and gases; melting, boiling, evaporating, freezing and condensing; heating and cooling curves explained with kinetic particle theory (1.1.1–1.1.3, Supplement 1.1.5). The experiment heats one ideal 50 g ice sample; freezing and condensing are taught with figures and practice. Gas volume with temperature and pressure (1.1.4, 1.1.6) comes in a later module.

Apparatus, amounts and times in the experiment are illustrative. Real practical work follows a teacher-approved safety method.

Official Cambridge syllabus