14.2 Temperature scales
- Syllabus
- 9702–2028–2029
- Topic
- 14.2
- Level
- A2
A physical property that changes with temperature can be used as a thermometric property: calibrate measured property values against known temperatures, then infer an unknown temperature from its measured value after thermal equilibrium is reached.
| Official thermometric property | Typical instrument/condition |
|---|---|
| density of a liquid | density-based liquid thermometer; property must give a unique reading |
| volume of a gas at constant pressure | constant-pressure gas thermometer |
| resistance of a metal | metal/platinum resistance thermometer |
| e.m.f. of a thermocouple | thermocouple junction pair |
| Useful characteristic | Why it matters |
|---|---|
| monotonic, ideally near-linear | one property value maps unambiguously to temperature |
| reproducible and stable | calibration remains valid |
| sensitive over required range | small temperature changes are resolvable |
| low thermal mass / fast response when needed | reaches equilibrium without strongly disturbing or lagging the object |
A thermocouple's small sensing junction suits rapidly changing temperature. A bulky gas thermometer can be accurate for calibration but responds slowly and may disturb a small object. Water density is unsuitable over ranges where its variation is non-monotonic or one density corresponds to more than one temperature.
Do not replace the official liquid-density example with liquid volume, and do not omit 'constant pressure' for gas volume or 'metal' for resistance. Variation alone is insufficient without calibration, unique response and an appropriate range/time response.
The thermodynamic temperature scale is based on universal physical principles rather than a chosen material property; the kelvin is the SI unit.
A practical thermometer is calibrated to approximate this scale, but its raw property may be nonlinear or limited in range.
A gas, resistance and radiation thermometer can agree after calibration even though their measured properties differ.
The Celsius scale and a material’s expansion are convenient representations, not the fundamental definition of temperature.
Thermodynamic temperature T in kelvin relates to Celsius temperature θ by T=θ+273.15.
Kelvin is an absolute scale with the same degree size as Celsius but a different zero. Use kelvin in gas and thermodynamic equations unless instructed otherwise.
25 °C is 298.15 K; 0 °C is 273.15 K, not 0 K.
A temperature difference of 1 °C equals 1 K, but an absolute temperature of 1 °C is not 1 K.
Absolute zero is zero kelvin, the lowest limit of thermodynamic temperature; it corresponds to −273.15 °C.
It is a limiting state, not simply “no motion” in every quantum description. Use it as the zero of the absolute scale.
Cooling from 300 K to 150 K halves the absolute temperature even though Celsius readings do not behave as a ratio scale.
Negative Celsius temperatures can be physically valid, but temperatures below 0 K are not reached in the ordinary thermodynamic scale.