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GRADE 8 · CHANGE IN STATE OF AGGREGATION

Melting, solidification and graphs

Melting temperature and energy of a phase change.

24 minutes5 theory cards
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Read the full lesson theory here without an account. In the interactive lesson, the same theory is presented as cards, followed by questions with feedback and practice problems. Your progress is saved.

Understanding step by step

We supply energy to ice at 0 °C. Less ice remains, but the thermometer still reads 0 °C. Why does energy enter while the familiar warming equation seems to give zero?

Energy enters, temperature stays constant0 °CQ > 0Where does the energy go?
Energy continues to enter a mixture of pure ice and water at normal atmospheric pressure. Ice floats near the surface; the thermometer bulb is immersed in the mixture and reads about 0 °C. Energy enters at unchanged temperature. We next investigate what it does.

A change of state

Watch an ice cube: melting removes its fixed shape, but water does not become a different substance. Melting is the change from solid to liquid; solidification is the reverse. Particle arrangement and the ability to exchange neighbours change, not the molecules' composition. Thermal motion alone cannot explain this; we must also account for interaction energy.

meltingCrystalLiquidsolidification
Melting changes the crystal into liquid; solidification returns it to the solid state. The upper arrow points towards liquid, the lower towards the crystal. Each diagram contains 12 identical particles: their arrangement changes, but particles do not disappear. Spacing is schematic and does not represent volume to scale.

The transition temperature

Pure ice and water can coexist near 0 °C at normal atmospheric pressure. This is the melting temperature: at that pressure, solid and liquid phases can be in equilibrium. It depends on the substance and pressure, so 0 °C is not a rule for every crystal. If some water freezes under the same equilibrium conditions, the change occurs at the same temperature.

At atmospheric pressureice≈ 0 °Clead≈ 327 °Ciron≈ 1538 °CAt this temperature, solid and liquidcan coexist
At normal atmospheric pressure, solid and liquid phases of a pure substance coexist near the indicated temperature. Values are rounded: about 0 °C for ice, 327 °C for lead and 1538 °C for iron. Changing the substance changes the transition temperature; pressure also matters.

Where does the energy go?

Where does energy go when the thermometer reading does not change? In a crystal, particles are held in ordered positions. Letting them exchange neighbours more freely requires changes in their arrangement and interactions. Energy goes into these changes during equilibrium melting. While both phases coexist at constant pressure, temperature does not rise. Once the last ice disappears, further energy transfer can warm the resulting water.

CrystalLiquidQlong-range orderno long-range orderSame temperature; Q > 0
During equilibrium melting of a pure crystal, supplied energy changes particle arrangement and interactions. At unchanged temperature, the average energy of thermal motion does not rise; motion continues in both states. Each diagram has 16 identical particles. Molecules are not destroyed, and spacing is schematic.

Read each graph segment

On a temperature-versus-supplied-heat graph, warming within one state gives a sloping segment: energy enters and temperature rises. During melting, energy keeps entering but the line is horizontal. Now imagine a temperature-versus-time graph T(t) after the heater is switched off: it can be horizontal without melting. Read a plateau together with the experimental conditions; time alone does not tell us how much energy was supplied.

T, КQ, ДжTплmeltingwarmingwarmingPure crystal; p = const
Schematic T(Q) graph for a pure crystal at constant pressure: first the solid warms, then melts at Tпл, then the liquid warms. Q is accumulated heat supplied in joules. The T axis is truncated; scales and stage durations are not specified. Q continues to increase along the plateau.

Energy per kilogram

Consider one kilogram of a substance already at its melting temperature. The energy needed to turn it into liquid is its specific latent heat of fusion λ, measured in J/kg. A larger λ requires more energy to melt the same mass. This differs from specific heat capacity: c concerns a temperature change, while λ concerns a change of state at the transition temperature.

For ice: λ ≈ 334 кДж/кг1 кг of ice0 °C334 кДж1 кг of water0 °CUnit of λ: Дж/кг
At normal atmospheric pressure, a kilogram of ice already at 0 °C becomes a kilogram of water at the same temperature. With λ = 334 кДж/кг, this requires 334 kJ. The arrow denotes a transition with energy input. Containers are identical; liquid water occupies less volume, while mass is conserved.

Calculate melting energy

If each kilogram needs λ joules, mass m needs Q = λm. Doubling mass doubles the heat; if only half the original substance melts, use that half's mass. At m = 0 no energy is needed for the transition itself. Solidifying the same mass under the same conditions releases the same energy magnitude, with negative Q for the substance. Units: Дж/кг · кг = Дж.

|Q| = λmMeltingSolidificationmmQ = +λmQ = −λmSame mass, substance and conditionsEqual magnitudes, opposite signs
Multiply specific latent heat of fusion λ by mass m. On the left, energy enters during melting, Q = +λm. On the right, the same mass of the same substance solidifies under the same conditions and releases energy, Q = −λm. Arrows are attached to the objects; the energy magnitudes are equal.

What if the ice starts colder?

What if the ice starts below 0 °C? Separate the process by what the thermometer and container show. First, the ice stays solid and warms, requiring cmΔT with the specific heat capacity of ice. Then water appears at the transition temperature, requiring λm. Add these contributions. The term λm does not also warm cold ice, and cmΔT cannot describe a segment where temperature stays constant while the state changes.

Two distinct stagesice −10 → 0 °CQ₁ = c · m · ΔTice → waterQ₂ = λ · mQ = Q₁ + Q₂One equation does not describe both stages
First bring cold ice to its melting temperature using the warming equation, then melt it using the phase-change equation. Calculate the two energies separately and add them.

Limits of the school model

A clear plateau describes a pure crystalline substance undergoing a nearly equilibrium transition at constant pressure. Rapid uneven heating, impurities or changing pressure can alter the experiment. An amorphous material such as glass softens differently and need not have this plateau. The model usefully separates warming from a phase change, but its features cannot be applied unchecked to every material or every horizontal graph.

Pure crystalAmorphous materialT, КQ, ДжT, КQ, Джmelting plateausofteningKnow the conditions before concluding
Schematic T(Q) graphs while energy is supplied: on the left, equilibrium melting of a pure crystal at constant pressure; on the right, gradual softening of an amorphous material. Axes are labelled without numerical scales. On a T(t) graph, a plateau can also mean thermal equilibrium without heating; the experimental conditions must be known.

Melting without a temperature rise

Melt 0.5 kg of ice already at 0 °C. λ = 334 кДж/кг. How much heat is needed?

λ = 334 кДж/кгice, 0,5 кгwater, 0,5 кг0 °C0 °CFind Q for complete meltingIce is already at the transition temperature
Turn the initial 0.5 kg of ice at 0 °C into 0.5 kg of water. The left panel shows the initial state, the right the required final state; a grey arrow denotes the transition. Find Q for complete melting with λ = 334 кДж/кг. Assume normal atmospheric pressure, no losses and negligible container heat capacity.

Worked example · 1

The ice is already at its melting temperature, so only the change of state is needed; there is no cmΔT warming stage here.

λ = 334 кДж/кгice, 0,5 кгwater, 0,5 кг0 °C0 °CNo initial warming neededCount only the transition: Q = λm
The same 0.5 kg of ice is already at 0 °C at the assumed pressure. There is no separate temperature change before the transition. Reaching the final state shown requires only melting, λm. The initial mass, temperature and λ are unchanged.

Worked example · 2

Each kilogram needs 334 kJ. For 0.5 kg, Q = λm = 334·0,5 = 167 кДж; kilograms cancel.

λ = 334 кДж/кгice, 0,5 кгwater, 0,5 кг0 °C0 °CQ = λm334 кДж/кг · 0,5 кг = 167 кДжкДж/кг · кг = кДж
Both states of the same portion remain shown, with mass 0.5 kg and λ = 334 кДж/кг. Complete conversion from ice to water requires Q = 334 кДж/кг · 0,5 кг = 167 кДж. Kilograms cancel, leaving kilojoules.

Worked example · 3

Half a kilogram needs half the energy needed for a kilogram. During the transition, the 167 kJ supplied changes the state while the mixture's temperature may remain 0 °C.

λ = 334 кДж/кгice, 0,5 кгwater, 0,5 кг0 °C0 °C167 кДжDuring the transition, T ≈ 0 °CAfter 167 кДж, all the ice has melted
In the same container, the initial 0.5 kg of ice at 0 °C becomes entirely water after receiving 167 kJ in this loss-free model. While ice and water coexist, temperature is about 0 °C. In the final state on the right, no ice remains; masses and conditions are unchanged.

Check the result

167 kJ. This melts 0.5 kg of ice at 0 °C but does not include later warming of the water.

Key idea · 1

During a phase change, internal energy changes even without a temperature change.

Key idea · 2

Q = λm applies to the mass that actually melts at the transition temperature.

Key idea · 3

Cold ice is warmed first and melted afterwards; the graph helps separate these stages.

What comes next

A liquid can become gas without boiling. Next we explore evaporation and humidity.

Basic Concepts

3 concepts

Melting and solidification

Melting changes a solid into a liquid; solidification is the reverse change.

For a pure crystalline substance, both processes at a given pressure occur at the same temperature.

Melting point

Temperature of phase equilibrium of solid and liquid states at a given pressure.

During equilibrium melting of a pure crystalline substance at constant pressure, energy changes particle arrangement and interactions while temperature stays constant. The molecules themselves are not destroyed. Pressure and impurities can change the transition temperature.

Heating graph

The graph shows how temperature changes with time, allowing us to identify warming and phase-change segments.

A sloping segment indicates temperature change. A horizontal segment while heat is still supplied may indicate a phase change. Constant temperature alone does not prove this: thermal equilibrium without heating also gives a horizontal line.

Physical quantities

1 magnitude

Specific latent heat of fusion

\lambda

Energy needed to melt a unit mass of a substance at its melting temperature.

Unit: joule per kilogram · \frac{\mathrm{Дж}}{\mathrm{кг}}

Lesson formulas

1 formula

Heat required for melting

Q = \lambda m

At constant temperature, the heat required for melting equals specific latent heat of fusion multiplied by mass.

Problems on this topic

Statements, answer options and the walkthrough.