Heat, temperature & internal energy
- Heat flows from a hotter body to a cooler one — never the reverse — until thermal equilibrium (equal temperature, no net flow) is reached.
- Internal energy = sum of the randomly distributed kinetic and potential energies of all particles in a body.
- Internal energy increases when a system is heated or has work done on it (and vice versa).
Specific heat capacity
SHC: energy needed to raise 1 kg of a substance by 1 °C.
Q = mcΔθ
- Q = heat supplied (J) m = mass (kg)
- c = specific heat capacity (J kg⁻¹ °C⁻¹ or K⁻¹)
Water's high c (4200 J kg⁻¹ °C⁻¹) vs. copper (385) means water heats and cools far more slowly for the same energy transfer — this is why water is used in heating/cooling systems.
Mixing method: assuming no losses, heat lost by the hotter substance equals heat gained by the cooler one — m₁c₁(θ₁−θ_f) = m₂c₂(θ_f−θ₂).
Measuring SHC: simple method
Immersion heater warms a known mass; record I, V, t, θᵢ and θ_f.
Record current, p.d., time and temperature change to find Q=IVt=mcΔθ.
Limitation: heat lost to the surroundings, and heat absorbed by the container/insulation itself, both give a systematically too-high value of c.
Measuring SHC: continuous flow method
Water flows steadily through a heated tube; two flow rates eliminate heat loss.
Taking two measurements at the same Δθ (different flow rates) means the heat lost to surroundings, E, is identical both times and cancels on subtraction:
c = (IVt − I₂V₂t₂) / [Δθ(m − m₂)]
Advantage: eliminates the systematic heat-loss error of the simple method — no need to know the heat capacity of the apparatus.