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Temperature · Subtopic 2 of 2

Specific Heat Capacity and Latent Heat

Specific heat capacity cc is the energy needed per unit mass per unit temperature rise: Q=mcΔθQ=mc\Delta\theta. Water's cc is about 42004200 J kg⁻¹ K⁻¹. Specific latent heat LL is the energy needed per unit mass to change state at constant temperature: Q=mLQ=mL. Vaporisation needs much more energy than melting because molecules must be completely separated and push back the atmosphere.

Cambridge 9702 Paper 4Edexcel YPH11 WPH15AQA 7408 Paper 2≈ 35 minRevision 5 · updated 2026-10-27
Section 1 of 14

Learning objectives

  • Define specific heat capacity and use Q=mcΔθQ=mc\Delta\theta.
  • Describe an electrical method to measure cc and its errors.
  • Define specific latent heat of fusion and vaporisation; use Q=mLQ=mL.
  • Explain why LvL_v is much greater than LfL_f.
Pause and think

Steam at 100100 °C gives a much worse burn than the same mass of boiling water at 100100 °C. Why?

Section 2 of 14

Core idea

Start hereIce in a drink

An ice cube keeps a drink cold far longer than the same mass of 0 °C water. Melting the ice soaks up a large amount of energy without any temperature change. That's latent heat.

The big idea

E=mcΔθE=mc\Delta\theta (temperature change); E=mLE=mL (state change, constant temperature).

1. The heating curve

Heating curve: steady heater, 0.5 kg ice from −20 °C
2004006008001000120014001600−20204060801001200energy supplied (kJ)temperature (°C)melting: mL_f = 167 kJboiling: mL_v = 1130 kJmcΔθ = 210 kJ
The boiling plateau is much longer than melting: separating particles completely needs far more energy than loosening them.
E=mcΔθE=mLE=mc\Delta\theta\qquad E=mL
where
cc
specific heat capacity (J kg⁻¹ K⁻¹).
LL
specific latent heat (J kg⁻¹).
Worked exampleIce from −20 °C to water at 0 °C

0.5 kg; cice=2100c_{\text{ice}}=2100, Lf=3.34×105L_f=3.34\times10^5.

Goal
Total energy.
Strategy
Warm, then melt.
  1. 0.5×2100×20=21000 J0.5\times2100\times20=21000\text{ J}
    Warm the ice to 0 °C.
  2. 0.5×3.34×105=167000 J0.5\times3.34\times10^5=167000\text{ J}
    Melt at 0 °C.
  3. 188000 J188000\text{ J}
    Add.
Answer1.88×1051.88\times10^5 J.
✓ CheckMelting dominates ✓.

2. Measuring c

Worked exampleElectrical method

1.0 kg aluminium; heater 12 V, 4.0 A, 300 s; rise 15.6 K.

Goal
cc.
Strategy
VIt=mcΔθVIt=mc\Delta\theta.
  1. E=12×4.0×300=14400 JE=12\times4.0\times300=14400\text{ J}
    Electrical energy.
  2. c=144001.0×15.6=923c=\frac{14400}{1.0\times15.6}=923
    J kg−1^{-1} K−1^{-1}.
Answer923923 J kg−1^{-1} K−1^{-1}.
✓ CheckHeat losses make this an overestimate: insulate ✓.
Key takeawayWhy Lv>LfL_v>L_f Melting loosens bonds; boiling separates molecules completely and pushes back the atmosphere.
Pause and think

Boil off 0.2 kg at 100 °C (Lv=2.26×106L_v=2.26\times10^6)?

Summary

  • mcΔθmc\Delta\theta on slopes; mLmL on plateaus.
Key words
Specific latent heat
Energy per kg to change state.
HistoryBlack's hidden heat. In the 17601760s Joseph Black noticed that melting ice absorbs heat without getting warmer, calling it "latent" (hidden) heat. His student James Watt used the idea to make steam engines far more efficient by condensing steam in a separate chamber.
Fun factWhy coastal cities are mild. Water's specific heat capacity is about five times that of rock and sand. Oceans warm and cool slowly, so seaside cities like Karachi have much smaller temperature swings between summer and winter than inland cities like Jacobabad.
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