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- Topic 9 · Thermodynamics
- Internal Energy and Specific Heat Capacity
Internal Energy and Specific Heat Capacity
Heat a pan of water and its temperature rises steadily — until it boils, when the temperature stops rising even though you keep supplying energy. Explaining both stages needs one idea: , the total kinetic and potential energy of the particles in a substance.
What you'll be able to do
- Define internal energy as the sum of random kinetic and potential energies of particles
- Use and describe how to measure specific heat capacity
- Use for changes of state
- Explain absolute zero and convert between Celsius and kelvin
Internal energy and temperature
The of a substance is the sum of the randomly distributed kinetic and potential energies of all its particles.
The kinetic part comes from particles moving and vibrating. The potential part comes from the forces between them, and depends on how far apart they are.
is a measure of the average kinetic energy of the particles, not of the total internal energy. A bath of warm water has more internal energy than a cup of boiling water, though it is at a lower temperature.
Energy flows by heating from a region of higher temperature to one of lower temperature, until they reach .
Tip — Say "randomly distributed" in the definition of internal energy. The ordered kinetic energy of a moving object does not count.
Absolute zero and the kelvin scale
is the temperature at which particles have the minimum possible internal energy. It is , or .
The kelvin scale starts at absolute zero, and one kelvin is the same size as one degree Celsius. So a temperature change is numerically the same on both scales.
Any equation involving gases or particle energy needs temperatures in kelvin. Heating equations only use , so Celsius is fine there.
Specific heat capacity
The of a substance is the energy needed to raise the temperature of 1 kg by 1 K, with no change of state. Its unit is .
Water has a very high value, about , which is why it is used in heating systems and why coastal climates are mild.
To measure it, heat a known mass with an electrical heater in an insulated block, measuring the energy supplied with a joulemeter or from , and plot temperature against time. The gradient gives . Using the gradient avoids errors from the initial lag while the heater warms up.
Example 1A 2.0 kW kettle heats 1.5 kg of water from C to C. Ignoring losses, how long does it take? Use .
Latent heat and changes of state
During melting or boiling, energy is supplied but the temperature stays constant. The energy increases the energy of the particles as bonds are broken or weakened; their average kinetic energy does not change.
The is the energy needed to change the state of 1 kg without changing temperature. Fusion refers to melting; vaporisation to boiling.
Latent heat of vaporisation is much larger than of fusion. Melting only loosens the structure, but boiling separates particles completely and does work pushing back the atmosphere as the gas expands.
Example 1How much energy is needed to turn 0.40 kg of ice at C into water at C? .
Tip — On a heating curve, sloping sections use and flat sections use . Split multi-stage problems at every change of state.
Equation recap
Common mistakes to avoid
Key takeaways
- Internal energy is the sum of random kinetic and potential energies of particles.
- Temperature measures average particle kinetic energy; 0 K is absolute zero.
- for a change in temperature.
- for a change of state at constant temperature.
- During a change of state, potential energy changes but kinetic energy does not.
Test yourself
Answer a few questions, then review anything you missed.
Keep practising
Start with the quiz above to check the key ideas. You can also choose another topic from the practice library.