Revision notes · Particle model of matter
Internal energy and energy transfers
Internal energy4.3.2.1
Heating a system transfers energy to its particles, increasing the internal energy. This either raises the temperature of the system, or produces a change of state — but not both at the same time (see Changes of state and specific latent heat).
Temperature changes in a system and specific heat capacity4.3.2.2
| Equation | Units |
|---|---|
| ΔE = m × c × ΔT | ΔE (change in thermal energy) in J, m (mass) in kg, c (specific heat capacity) in J/kg°C, ΔT (temperature change) in °C |
A substance with a high specific heat capacity needs a lot of energy to change temperature — this is why it takes water a long time to heat up (and a long time to cool down) compared with many other materials.
Changes of state and specific latent heat4.3.2.3
| Equation | Units |
|---|---|
| E = m × L | E (energy) in J, m (mass) in kg, L (specific latent heat) in J/kg |
Energy is absorbed by a substance when it melts or evaporates, and released when it freezes or condenses. While a substance is actually changing state, all the energy transferred goes into breaking or forming the bonds between particles — none of it raises the temperature, so the temperature stays constant during the change of state itself.
On a graph of temperature against time for a substance being steadily heated from solid to gas, the temperature rises while it is fully solid, then stays flat while it melts (energy goes into changing state, not raising temperature), rises again while it is fully liquid, stays flat again while it boils (this flat section is usually longer, since evaporating takes more energy than melting), then rises again once it is fully gas.
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