14.2 Temperature scales

Syllabus
9702–2028–2029
Topic
14.2
Level
A2

Learning objectives

Calibrate a temperature-dependent physical property as a thermometer

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.

Thermodynamic temperature is defined independently of any particular thermometric substance

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.

Convert between kelvin and Celsius using T(K)=θ(°C)+273.15

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 0 K, the lower limit of the thermodynamic temperature scale

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.