Phase Changes & Phase Diagrams
Why boiling water stays at 100 C, where the heat 'disappears' to, and how one map charts every state of a substance.
Put a pot of water on to boil and watch a thermometer in it. The temperature climbs steadily to 100 C β and then stops dead, even though the burner is still roaring. Where is all that energy going, if not into raising the temperature? The answer reveals what a phase change really is.
The changes of state
Matter shifts between solid, liquid and gas as you add or remove energy. Each transition has a name:
- Melting (solid → liquid) and freezing (liquid → solid)
- Vaporisation (liquid → gas) and condensation (gas → liquid)
- Sublimation (solid → gas directly) and deposition (gas → solid directly)
Which way you go depends on whether you add heat (toward gas) or remove it (toward solid). What holds particles together in the first place is their intermolecular forces — stronger forces mean higher melting and boiling points.
The heating curve: steps and plateaus
Heat a block of ice steadily and plot temperature against energy added. You don't get a straight ramp. You get a staircase: sloped sections where the temperature rises, separated by flat plateaus where it doesn't move at all.
The sloped parts are the ice, then water, then steam simply warming up. The plateaus are the phase changes: melting (at 0 C) and boiling (at 100 C for water at 1 atm). During a plateau, every joule of energy goes into breaking particles apart, not into making them move faster — so the temperature holds steady.
- Temperature is constant during a phase change. While ice melts, both the ice and the water sit at 0 C. The heat isn't 'missing' — it's going into breaking bonds, not raising temperature.
- Boiling is not the same as evaporation. Evaporation happens only at the surface, at any temperature. Boiling happens throughout the liquid once its vapour pressure equals the surrounding pressure.
- The water is already at its boiling point, so this is a pure phase change: q = m × L.
- q = 10.0 g × 2260 J/g.
- = 22 600 J = 22.6 kJ — all of it going into separating the molecules into vapour, at a steady 100 C.
The phase diagram: a map of states
A phase diagram plots pressure (vertical) against temperature (horizontal) and shades in which state is stable under each combination. Lines divide the regions; crossing a line is a phase change. Two special points stand out.
Why water is the weird one
On most phase diagrams the solid-liquid line tilts slightly to the right (more pressure favours the solid). Water's tilts to the left: increase the pressure on ice and it can melt. That is because ice is less dense than liquid water — the reason ice floats, and a quirk that keeps lakes liquid beneath a frozen surface.
- The ice is at its melting point, so this is a phase change: q = m × L.
- q = 50.0 g × 334 J/g = 16 700 J.
- Convert to kilojoules: 16 700 J ÷ 1000 = 16.7 kJ. The temperature stays at 0 C throughout.
Check your understanding
- Phase changes: melting/freezing, vaporisation/condensation, sublimation/deposition.
- A heating curve has sloped sections (warming) and flat plateaus (phase changes).
- Latent heat changes state at CONSTANT temperature: q = m*L (fusion or vaporisation).
- A phase diagram maps state versus pressure and temperature; lines are phase changes.
- Triple point = all three phases coexist; critical point = liquid and gas merge.