Latent heat

Ice at 0°C and water at 0°C feel equally cold — same thermometer reading, same temperature — yet melting that ice takes a surprisingly large amount of heat while the thermometer refuses to move at all. Where does the heat go if not into raising the temperature? It goes into prying apart the molecules themselves. In a solid, molecules sit locked in a fixed, ordered arrangement; melting means breaking enough of those bonds that they can slide past one another as a liquid. That bond-breaking energy is latent heat — "latent" because it stays hidden from the thermometer even as it is absorbed or released. This article builds the two formulas ICSE expects — Q=mcΔTQ = mc\Delta T for ordinary heating and Q=mLQ = mL for a change of state — shows how they combine in the classic steam-into-water numerical, and reads the flat plateaus of a heating curve as the graphical signature of latent heat at work.

The core insight

Latent heat Q=mLQ = mL is the heat absorbed or released during a change of state at constant temperature, distinct from sensible heat Q=mcΔTQ = mc\Delta T which changes temperature without changing state — and ICSE numericals routinely chain both in one problem.

The core idea

Why the thermometer doesn't move. Heat supplied to a solid at its melting point does not speed up molecular vibration (which is what a rising temperature actually measures); instead it goes entirely into overcoming the intermolecular forces holding the solid's ordered lattice together. Once every particle has broken free into the looser liquid arrangement, any further heat resumes raising the temperature. The same logic applies at the boiling point, only now the bonds must be broken almost completely, separating molecules so far apart that they become a gas.

Specific latent heat. The specific latent heat LL of a substance is the heat required to change the state of unit mass of it, at constant temperature:

Q=mLQ = mL

where: QQ is heat supplied or released (J), mm is mass (kg or g), and LL is specific latent heat (J/kg or J/g), a fixed property of the substance and the particular change of state. Two named values are prescribed by the syllabus. Specific latent heat of fusion, LfL_f, is the heat to convert unit mass of solid to liquid at the melting point (or released on freezing); for ice, Lf≈336 J/g=3.36×105 J/kgL_f \approx 336\ \text{J/g} = 3.36\times10^5\ \text{J/kg}. Specific latent heat of vaporisation, LvL_v, is the heat to convert unit mass of liquid to vapour at the boiling point (or released on condensation); for steam, Lv≈2268 J/g≈2.27×106 J/kgL_v \approx 2268\ \text{J/g} \approx 2.27\times10^6\ \text{J/kg}. Notice LvL_v is nearly seven times LfL_f for water — vaporisation separates molecules completely, while fusion only loosens their fixed positions, so vaporisation is by far the costlier change.

Melting point vs boiling point. The melting point is the fixed temperature at which a solid turns to liquid; impurities lower it, and increased pressure lowers ice's melting point specifically. The boiling point is the fixed temperature at which a liquid turns to vapour throughout its bulk; increased pressure raises it, which is exactly why a pressure cooker — sealed, so pressure builds — cooks food faster than an open pan.

Evaporation vs boiling. Evaporation happens only at a liquid's exposed surface, at any temperature, and proceeds slowly and gradually. Boiling happens throughout the entire liquid, but only at one fixed temperature — the boiling point. Treating the two as interchangeable is a common and penalised mix-up.

The heating curve. Heat a solid steadily and plot temperature against time: the graph climbs (solid warming), then runs perfectly flat at the melting point while latent heat of fusion is absorbed and the solid liquefies, then climbs again (liquid warming), then runs flat again at the boiling point while latent heat of vaporisation is absorbed, and finally climbs once more as vapour is superheated. The two flat plateaus, at fixed temperatures despite continuous heat input, are the graph's unmistakable signature of a change of state.

Figure
Heating curve of ice showing temperature rising then a flat plateau at the melting point then rising again then a flat plateau at the boiling point
Heating curve: flat plateaus mark latent heat heat supplied / time temperature melting: solid to liquid boiling: liquid to vapour solid warms liquid warms vapour warms m.p. b.p.
Derivation ATotal heat to melt ice and warm the water

Find the total heat required to convert 50 g of ice at 0°C completely into water at 0°C, and then further heat that water to 30°C, taking Lf(ice)=336 J/gL_f(\text{ice}) = 336\ \text{J/g} and c(water)=4.2 J/g ⋅ Kc(\text{water}) = 4.2\ \text{J/g}\,\cdot\,\text{K}, by adding a latent-heat stage and a sensible-heat stage in sequence.

Step 1. The ice melts at constant temperature, so this stage uses only the latent heat formula, with no ΔT\Delta T term at all:

Q1=mLf=50×336=16,800 JQ_1 = mL_f = 50 \times 336 = 16{,}800\ \text{J}

Step 2. The resulting water at 0°C is then heated to 30°C, a change of temperature with no change of state, so this stage uses the sensible heat formula:

Q2=mcΔT=50×4.2×30=6300 JQ_2 = mc\Delta T = 50 \times 4.2 \times 30 = 6300\ \text{J}

Step 3. The two stages happen one after another on the same 50 g of substance, so the total heat is simply their sum:

Qtotal=Q1+Q2=16,800+6300=23,100 J=23.1 kJQ_{\text{total}} = Q_1 + Q_2 = 16{,}800 + 6300 = 23{,}100\ \text{J} = 23.1\ \text{kJ}

Step 4. Notice that melting the ice (Step 1) alone costs more heat than raising the melted water's temperature by a full 30°C (Step 2) — this is the essence of why latent heat is called "large": breaking molecular bonds is energetically expensive even though the thermometer shows no change at all during that stage.

Worked example

Steam at 100°C of mass 10 g is passed into 200 g of water at 20°C in a calorimeter of negligible heat capacity. Find the final temperature of the water, assuming the steam fully condenses and no heat is lost to the surroundings, taking Lv(steam)=2268 J/gL_v(\text{steam}) = 2268\ \text{J/g} and c(water)=4.2 J/g ⋅ Kc(\text{water}) = 4.2\ \text{J/g}\,\cdot\,\text{K}.

Step 1. The steam first condenses to water at 100°C (releasing latent heat), and that condensed water then cools from 100°C down to the final temperature TT (releasing sensible heat), so the heat released has two parts:

Qreleased=msteamLv+msteamc(100−T)=(10×2268)+(10×4.2)(100−T)=22,680+42(100−T)Q_{\text{released}} = m_{\text{steam}}L_v + m_{\text{steam}}c(100 - T) = (10 \times 2268) + (10 \times 4.2)(100-T) = 22{,}680 + 42(100-T)

Step 2. The original 200 g of water simply warms from 20°C to TT, a purely sensible-heat gain:

Qgained=mwaterc(T−20)=200×4.2×(T−20)=840(T−20)Q_{\text{gained}} = m_{\text{water}}c(T - 20) = 200 \times 4.2 \times (T-20) = 840(T-20)

Step 3. With no heat lost to surroundings, heat lost equals heat gained, so equate the two expressions and solve for TT:

22,680+42(100−T)=840(T−20)22{,}680 + 42(100-T) = 840(T-20)
26,880−42T=840T−16,80026{,}880 - 42T = 840T - 16{,}800
43,680=882T⇒T≈49.5°C43{,}680 = 882T \quad\Rightarrow\quad \boxed{T \approx 49.5°\text{C}}

Step 4. Only 10 g of steam, against 200 g of water twenty times its mass, still pushes the final temperature up from 20°C to about 49.5°C — the huge latent heat released on condensation dominates the mixture, which is exactly why steam burns are far more severe than hot-water burns at the same starting temperature.

Competitive stretch

If the same 10 g had arrived as boiling water at 100°C instead of steam, only the sensible-heat term would apply: 10×4.2×(100−T)=840(T−20)10 \times 4.2 \times (100-T) = 840(T-20) gives T≈21.8°CT \approx 21.8°\text{C} — dramatically cooler than the steam case, isolating just how much of the 49.5°C rise above came from the latent heat of condensation alone.

Common traps

  • Forgetting the condensation or melting step in mixed problems — when steam meets water, students often apply only Q=mcΔTQ=mc\Delta T to the steam and skip the much larger Q=mLvQ=mL_v term for condensation; always check whether a state change happens before or after the temperature change.
  • Assuming latent heat causes a temperature rise — by definition temperature stays constant throughout melting or boiling, and all the heat goes into changing state, exactly what the flat plateau on a heating curve shows.
  • Mixing up fusion and vaporisation values — Lf(ice)≈336 J/gL_f(\text{ice}) \approx 336\ \text{J/g} is much smaller than Lv(steam)≈2268 J/gL_v(\text{steam}) \approx 2268\ \text{J/g}, because vaporisation must separate molecules completely while fusion only loosens their fixed arrangement.
  • Treating evaporation and boiling as the same process — evaporation is a slow surface-only process at any temperature, while boiling occurs throughout the liquid at one fixed temperature; do not use the two words interchangeably.

Ask the tutor: Want to try a trickier combined problem, like ice starting below 0°C being converted all the way to steam — ask for a step-by-step walkthrough.

Why does steam at 100°C cause worse burns than boiling water at the same 100°C

Steam carries its sensible heat just like boiling water does, but it also carries an enormous extra amount of latent heat of vaporisation, about 2268 J/g, which is released the instant it condenses on your skin. That condensation happens before the resulting hot water even starts cooling, so steam delivers far more total energy to the same spot in the same time than boiling water at the identical 100°C reading.

If latent heat does not change temperature then where does the energy actually go

It goes into doing work against the intermolecular forces holding particles in their more ordered arrangement, effectively increasing the potential energy of the molecular arrangement rather than the kinetic energy of molecular motion. Since temperature is a measure of average kinetic energy, not potential energy, the thermometer reading does not move even though the substance has clearly absorbed real energy, evident from how much heat is needed and from the state actually changing.

In a mixed problem, how do I know whether to use Q equals mL or Q equals mcΔT for a given stage

Ask whether the substance is changing state or changing temperature during that stage. If ice at 0°C is turning into water at 0°C, that is a state change at constant temperature, so use Q = mL. If water at 0°C is then warming to 30°C with no state change, that is sensible heat, so use Q = mcΔT. Long ICSE numericals usually need both formulas applied to different stages of the same substance, added together.

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