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Calorimetry — Notes

5 sections 4 min readBeta

1. Heat, temperature, heat capacity and specific heat capacity

  • Heat: energy flowing from hot to cold; unit J (1 cal ≈ 4.2 J). Temperature: degree of hotness; unit K (°C in practice; a change of 1 °C = 1 K).
  • Heat capacity CC: heat to raise the temperature of a body by 1 K; unit J K⁻¹; depends on mass and material.
  • Specific heat capacity cc: heat to raise 1 kg by 1 K; unit J kg⁻¹ K⁻¹; depends only on material. Water 4200, ice 2100, aluminium 900, copper 400.
  • C=mcC = mc; Q=mc ΔTQ = mc\,\Delta T.
Table of specific heat capacities
Substancec (J kg⁻¹ K⁻¹)
Water4200
Ice2100
Copper400

Formulas

  • Heat for a temperature change
    Q=mc ΔTQ = mc\,\Delta T
  • Heat capacity
    C=mcC = mc

Key terms

Heat capacity

The heat required to raise the temperature of a body by one kelvin.

Specific heat capacity

The heat required to raise the temperature of unit mass of a substance by one kelvin.

2. Method of mixtures

Principle: when hot and cold bodies are mixed and no heat is lost to the surroundings, heat lost by the hot body = heat gained by the cold body.

m1c1(T1−T)=m2c2(T−T2)m_1 c_1 (T_1 - T) = m_2 c_2 (T - T_2) (+ mcalccal(T−T2)m_{cal} c_{cal} (T - T_2) for the calorimeter).

A calorimeter is a thin polished copper vessel (low heat capacity, good conductor, polished to reduce radiation) in an insulating jacket, with stirrer and thermometer.

Table of the two sides of a mixture
Hot bodyCold body
Loses heatGains heat
T₁ → TT₂ → T

Formulas

  • Mixtures
    m1c1(T1−T)=m2c2(T−T2)m_1 c_1 (T_1 - T) = m_2 c_2 (T - T_2)

Key terms

Principle of method of mixtures

Heat lost by the hot body equals heat gained by the cold body, provided no heat is exchanged with the surroundings.

Calorimeter

A vessel, usually of polished copper in an insulating jacket, used to measure heat exchanged.

3. High specific heat capacity of water

Water warms and cools slowly. Consequences and uses:

  • Sea breeze by day (land hotter), land breeze at night (sea warmer).
  • Coastal climates are moderate; inland deserts have extreme days and nights.
  • Coolant in car radiators, power stations; hot-water bottles.
  • Farmers flood fields on frosty nights; water gives out heat as it cools.
  • Body temperature stays steady (body is mostly water).
Table of effects of water’s high specific heat capacity
EffectReason
Sea breeze by dayLand heats faster
Land breeze at nightLand cools faster
Radiator coolantAbsorbs much heat per degree

Key terms

Sea breeze

A cool daytime wind blowing from the sea to the land, because land heats faster than water.

4. Change of state and latent heat of fusion

A pure substance changes state at a fixed temperature (ice melts at 0 °C at normal pressure). Heat absorbed during melting separates the molecules and does not raise the temperature.

Specific latent heat of fusion LL: heat to change 1 kg of solid at its melting point into liquid at the same temperature. Ice: L=336 000 J kg−1L = 336\,000\ \text{J kg}^{-1} (336 J g⁻¹). Q=mLQ = mL.

Heating curve (ice → steam): sloping parts Q=mcΔTQ = mc\Delta T; flat parts at 0 °C (melting) and 100 °C (boiling) are latent heat.

Table of heating curve parts and formulae
Part of curveFormula
Ice warmingmc_ice ΔT
MeltingmL
Water warmingmc_water ΔT

Formulas

  • Heat for melting
    Q=mLQ = mL

Key terms

Specific latent heat of fusion

The heat required to convert unit mass of a solid at its melting point into liquid at the same temperature.

Melting point

The fixed temperature at which a pure solid changes into liquid at a given pressure.

5. Everyday effects of latent heat of fusion

  • Ice at 0 °C cools better than water at 0 °C: each kilogram absorbs 336 000 J to melt before warming.
  • Snow on mountains melts slowly, so rivers keep flowing in summer.
  • Ponds and lakes freeze slowly: a lot of heat must be removed first.
  • Frozen food and ice-cream stay cold longer.
  • Freezing water gives out heat: trays of water in a cellar protect stored vegetables from frost.
Table comparing ice and water at zero degrees as coolants
Coolant at 0 °CHeat absorbed per kg before warming
Water0
Ice336 000 J

Key terms

Latent heat

Heat absorbed or given out during a change of state without any change in temperature.

Exam tips

Common mistakes

  • Using grams with c in J kg⁻¹ K⁻¹.
  • Forgetting to warm the melted ice after it melts.
  • Saying temperature rises while ice melts.
  • Mixing up heat capacity (J K⁻¹) and specific heat capacity (J kg⁻¹ K⁻¹).

How marks are usually awarded

  • Mixture problems (3–4 marks): heat lost written, heat gained written, equation, answer with unit.
  • Explanations (1–2 marks): name specific heat capacity or latent heat and say what it does.