Thermal equilibrium and temperature scales, kinds of thermometer, linear, area and volume expansion of solids, and the expansion of liquids.
Heat flows from a hotter body to a colder one until both reach the same temperature. They are then in thermal equilibrium. If A and B are each in equilibrium with C, they are in equilibrium with each other (the zeroth law of thermodynamics). A thermometer reads its own temperature, which equals the body's once they are in equilibrium.
The SI temperature is the thermodynamic (kelvin) temperature $T$. The Celsius temperature is $\theta = T - 273.15$, usually taken as $T = \theta + 273$. Absolute zero is $0\ \text{K} = -273\ ^\circ\text{C}$. A change of $1\ \text{K}$ equals a change of $1\ ^\circ\text{C}$.

Any property that changes steadily with temperature can make a thermometer. Examples are the length of a liquid column, the pressure of a gas at constant volume, electrical resistance and the emf of a thermocouple.
| Thermometer | Good for |
|---|---|
| mercury- or alcohol-in-glass | everyday use, simple and direct |
| constant-volume gas | the standard; very accurate, but large and slow |
| platinum resistance | accurate over a wide range |
| thermocouple | small, fast response, very high temperatures, remote reading |
A thermometer for the method of mixtures should have a range just covering the temperatures expected and the smallest suitable least count.
Example: In a 2023 Paper II question a student had to choose between thermometers of ranges $0$–$50\ ^\circ\text{C}$, $-10$–$110\ ^\circ\text{C}$ and $0$–$360\ ^\circ\text{C}$ for an experiment at room temperature with ice. The best choice has the smallest least count while still covering $0\ ^\circ\text{C}$ to room temperature.
Most solids expand when heated because their atoms vibrate with larger amplitude about positions slightly further apart. $$\Delta l = l_0,\alpha,\Delta\theta, \qquad \Delta A = A_0,\beta,\Delta\theta, \qquad \Delta V = V_0,\gamma,\Delta\theta$$ with $\beta \approx 2\alpha$ and $\gamma \approx 3\alpha$ for an isotropic solid. $\alpha$ is the linear expansivity, unit $\text{K}^{-1}$.
Example: A steel tape calibrated at $20\ ^\circ\text{C}$ reads $50.00\ \text{m}$ at $40\ ^\circ\text{C}$ ($\alpha = 2 \times 10^{-5}\ \text{K}^{-1}$). Each "metre" of the tape is now longer by a factor $1 + \alpha\Delta\theta = 1.0004$. So the true length is $50.00 \times 1.0004 = 50.02\ \text{m}$. (A 2023 Paper I question.)

A liquid has only volume expansivity. Its container expands too. So what you see, the apparent expansion, is less than the real expansion: $$\gamma_{real} = \gamma_{apparent} + \gamma_{container}$$ The density of a liquid falls with temperature: $\rho_\theta = \dfrac{\rho_0}{1 + \gamma\Delta\theta}$.
Anomalous expansion of water: between $0\ ^\circ\text{C}$ and $4\ ^\circ\text{C}$ water contracts on heating, so it is densest at $4\ ^\circ\text{C}$. In winter the water at $4\ ^\circ\text{C}$ sinks to the bottom of a lake, and ice forms on the top and insulates the water below. Fish survive.
Photo credits: Laboratory thermometer-01.jpg by Lilly_M, CC BY-SA 3.0; Bobina Bimetálica termostato.jpg by Shorenster, CC BY-SA 3.0.