What Calorimetry Measures
Energy changes accompanying chemical or physical processes are measured experimentally by calorimetry. The process is carried out in a vessel called a calorimeter, which is immersed in a known volume of a liquid — usually water. If the heat capacity of that liquid and the heat capacity of the calorimeter are known, the heat evolved or absorbed can be determined simply by tracking the temperature change of the assembly.
The NCERT text fixes one decisive idea: measurements are made under two different conditions, and the condition selects which thermodynamic quantity you obtain. At constant volume the heat exchanged is $q_V$, and at constant pressure it is $q_p$. These are not arbitrary labels — they connect directly to the first law of thermodynamics.
| Condition | Heat symbol | What it equals | Why |
|---|---|---|---|
| Constant volume ($\Delta V = 0$) | $q_V$ | $\Delta U$ | No expansion work, so $w = 0$ |
| Constant pressure | $q_p$ | $\Delta H$ | $H \equiv U + pV$ absorbs the $p\Delta V$ work |
The first law states $\Delta U = q + w$, where $w$ is the work done on the system. Holding the volume constant removes expansion work entirely, leaving the clean identity $\Delta U = q_V$. Holding the pressure constant instead routes the heat into the enthalpy, $q_p = \Delta H$. Calorimetry is, in essence, the art of building an apparatus that enforces one of these two conditions so that the measured heat is exactly the quantity wanted.
Heat Capacity and q = CΔT
The quantitative link between a thermometer reading and a heat quantity is the heat capacity. A substance with a large heat capacity requires a lot of energy to raise its temperature. For a calorimeter assembly the relevant quantity is the heat capacity $C$ of the whole device — vessel, water bath, stirrer and thermometer combined — measured in $\text{J K}^{-1}$ or $\text{kJ K}^{-1}$.
Once $C$ is known, the heat exchanged for any measured temperature change $\Delta T$ follows from the central calorimetric equation:
$$ q = C\,\Delta T $$
Heat released by the reacting system is captured by the calorimeter. Because heat lost by the system equals heat gained by the calorimeter, the two have equal magnitude but opposite signs: $q_{\text{system}} = -C\Delta T$.
The sign convention is worth pinning down. The calorimeter gains heat $+C\Delta T$, so the reacting system must have lost the same amount, $q_{\text{system}} = -C\Delta T$. For an exothermic reaction the temperature rises ($\Delta T > 0$), and $q_{\text{system}}$ comes out negative — exactly as it should, since heat has flowed out of the system.
ΔU at Constant Volume — Bomb Calorimeter
For chemical reactions, the heat absorbed at constant volume is measured in a bomb calorimeter. A heavy steel vessel — the bomb — is immersed in a stirred water bath, and the whole device is the calorimeter. The steel vessel sits in the water bath specifically to ensure that no heat is lost to the surroundings.
A combustible substance is burnt in pure dioxygen supplied inside the steel bomb. The heat released during the reaction is transferred to the water around the bomb, and the water's temperature is monitored. Because the bomb is sealed, its volume does not change, so the energy change is measured at constant volume. Crucially, no work is done even when gases are involved, because $\Delta V = 0$ inside the rigid vessel. Under these conditions the measured heat is $q_V$, which converts to $\Delta U$ through the known heat capacity using $q = C\Delta T$.
Bomb calorimeter (NCERT Fig. 5.7). The sealed steel bomb keeps the volume constant, so no expansion work is done and the heat transferred to the surrounding water gives $q_V = \Delta U$.
A bomb calorimeter measures ΔU, not ΔH
Examiners frequently describe combustion "in a bomb calorimeter" and then ask for the enthalpy of combustion. The bomb works at constant volume, so it gives $q_V = \Delta U$ directly. The enthalpy must be obtained afterwards through $\Delta H = \Delta U + \Delta n_g RT$.
Bomb (sealed, rigid) → $q_V = \Delta U$. Open vessel (atmospheric) → $q_p = \Delta H$.
ΔH at Constant Pressure — Coffee-Cup Calorimeter
Most chemical reactions of interest are not carried out at constant volume but in flasks or test tubes open to the atmosphere, that is, at constant pressure. To measure these, a constant-pressure calorimeter is used — at the school-laboratory level a simple insulated "coffee-cup" vessel open to the atmosphere. Because the pressure stays constant (atmospheric), the heat absorbed or evolved is $q_p$, and we know that $\Delta H = q_p$ at constant pressure.
This heat at constant pressure is also called the heat of reaction or enthalpy of reaction, $\Delta_r H$. In an exothermic reaction the system loses heat to the surroundings, so $q_p$ is negative and $\Delta_r H$ is negative; in an endothermic reaction heat is absorbed, $q_p$ is positive and $\Delta_r H$ is positive.
Constant-pressure (coffee-cup) calorimeter, NCERT Fig. 5.8. Open to the atmosphere, it measures $q_p$, which equals the reaction enthalpy $\Delta_r H$.
The whole apparatus logic rests on the definitions of $C$, $C_p$ and $C_V$. Revise Enthalpy and Heat Capacity before you tackle calorimetric problems.
Bridging ΔU and ΔH
Since enthalpy is defined as $H = U + pV$, a change at constant pressure gives $\Delta H = \Delta U + p\Delta V$. For a reaction involving ideal gases, the ideal gas law lets us replace $p\Delta V$ by a tidy expression. Writing $pV_A = n_A RT$ for the gaseous reactants and $pV_B = n_B RT$ for the gaseous products at constant temperature and pressure,
$$ p\,\Delta V = p(V_B - V_A) = (n_B - n_A)RT = \Delta n_g RT $$
where $\Delta n_g$ is the number of moles of gaseous products minus the number of moles of gaseous reactants. Substituting gives the bridge equation:
$$ \Delta H = \Delta U + \Delta n_g RT $$
This is the equation that turns a bomb-calorimeter $\Delta U$ into the enthalpy $\Delta H$, and vice versa. When no gaseous moles change ($\Delta n_g = 0$) the two are identical, $\Delta H = \Delta U$. The difference is also negligible for systems of only solids and liquids, because such phases barely change volume on heating; it becomes significant only when the number of gas-phase moles changes.
| Reaction | $\Delta n_g$ | Relation |
|---|---|---|
| $\ce{C(graphite) + O2(g) -> CO2(g)}$ | $1 - 1 = 0$ | $\Delta H = \Delta U$ |
| $\ce{H2(g) + 1/2 O2(g) -> H2O(l)}$ | $0 - 1.5 = -1.5$ | $\Delta H = \Delta U - 1.5RT$ |
| $\ce{CaCO3(s) -> CaO(s) + CO2(g)}$ | $1 - 0 = +1$ | $\Delta H = \Delta U + RT$ |
Worked Examples
$1\,\text{g}$ of graphite is burnt in a bomb calorimeter in excess of oxygen at $298\ \text{K}$ and $1$ atm:
$$\ce{C(graphite) + O2(g) -> CO2(g)}$$
During the reaction the temperature rises from $298\ \text{K}$ to $299\ \text{K}$. If the heat capacity of the bomb calorimeter is $20.7\ \text{kJ K}^{-1}$, what is the enthalpy change for the reaction at $298\ \text{K}$ and $1$ atm?
Step 1 — heat gained by the calorimeter. With $C_V$ the heat capacity, the calorimeter absorbs $q = C_V\,\Delta T$.
Step 2 — heat from the reaction. Heat lost by the system equals heat gained by the calorimeter, so it has the same magnitude but the opposite sign:
$$ q = -\,C_V\,\Delta T = -\,20.7\ \text{kJ K}^{-1} \times (299 - 298)\ \text{K} = -20.7\ \text{kJ} $$
The negative sign confirms the reaction is exothermic. Thus $\Delta U$ for combustion of $1\,\text{g}$ of graphite is $-20.7\ \text{kJ}$.
Step 3 — per mole. The molar mass of carbon is $12.0\ \text{g mol}^{-1}$, so for $1$ mole:
$$ \Delta U = \frac{-20.7\ \text{kJ}}{1\ \text{g}} \times 12.0\ \text{g mol}^{-1} = -2.48 \times 10^{2}\ \text{kJ mol}^{-1} $$
Step 4 — convert to ΔH. Here $\Delta n_g = 1 - 1 = 0$, so $\Delta H = \Delta U = -2.48 \times 10^{2}\ \text{kJ mol}^{-1}$.
If water vapour is assumed to be a perfect gas, the molar enthalpy change for vaporisation of $1$ mol of water at $1$ bar and $100\,^{\circ}\text{C}$ is $41\ \text{kJ mol}^{-1}$. Calculate the internal energy change when (i) $1$ mol of water is vaporised at $1$ bar pressure and $100\,^{\circ}\text{C}$.
$$\ce{H2O(l) -> H2O(g)}$$
Step 1 — rearrange the bridge equation. From $\Delta H = \Delta U + \Delta n_g RT$,
$$ \Delta U = \Delta H - \Delta n_g RT $$
Step 2 — find $\Delta n_g$. One mole of gaseous water is produced from liquid water, so $\Delta n_g = +1$.
Step 3 — substitute. With $T = 373\ \text{K}$ and $R = 8.314\times10^{-3}\ \text{kJ K}^{-1}\text{mol}^{-1}$:
$$ \Delta U = 41\ \text{kJ mol}^{-1} - (1)(8.314\times10^{-3})(373)\ \text{kJ mol}^{-1} $$
$$ \Delta U = 41 - 3.10 = 37.9\ \text{kJ mol}^{-1} $$
The internal energy change is smaller than the enthalpy change because part of the $41\ \text{kJ}$ goes into the expansion work done by the newly formed vapour against the atmosphere.
Keep the units of R consistent
In $\Delta H = \Delta U + \Delta n_g RT$, if energies are in kJ then $R$ must be $8.314\times10^{-3}\ \text{kJ K}^{-1}\text{mol}^{-1}$. Mixing $R = 8.314\ \text{J K}^{-1}\text{mol}^{-1}$ with kJ energies inflates the correction term a thousandfold — a classic silent error.
Energies in kJ → $R = 8.314\times10^{-3}\ \text{kJ K}^{-1}\text{mol}^{-1}$. Count only gaseous species in $\Delta n_g$.
Constant-V vs Constant-p — Summary
The two measurement modes are best contrasted side by side. The choice of apparatus is dictated entirely by whether the volume or the pressure is held fixed, and this in turn fixes whether the measured heat is $\Delta U$ or $\Delta H$.
| Feature | Constant volume | Constant pressure |
|---|---|---|
| Apparatus | Bomb calorimeter (sealed steel bomb) | Coffee-cup / open calorimeter |
| Held fixed | Volume ($\Delta V = 0$) | Pressure (atmospheric) |
| Expansion work | $w = 0$ | $w = -p\Delta V$ |
| Heat measured | $q_V$ | $q_p$ |
| Quantity obtained | $\Delta U = q_V$ | $\Delta H = q_p = \Delta_r H$ |
| Working relation | $q_V = C_V\,\Delta T$ | $q_p = C_p\,\Delta T$ |
| Conversion | $\Delta H = \Delta U + \Delta n_g RT$ | |
Whichever route is used, the experimental skeleton is identical: calibrate the calorimeter to know its heat capacity, run the process, read the temperature change, and apply $q = C\Delta T$. The thermodynamics enters only in deciding what that $q$ represents and, if necessary, converting between $\Delta U$ and $\Delta H$.
Calorimetry in one screen
- Calorimetry measures heat from a temperature change using $q = C\Delta T$, where $C$ is the heat capacity of the calorimeter assembly.
- At constant volume $w = 0$, so $q_V = \Delta U$ — measured in a sealed bomb calorimeter.
- At constant pressure $q_p = \Delta H = \Delta_r H$ — measured in an open constant-pressure (coffee-cup) calorimeter.
- Heat lost by the system equals heat gained by the calorimeter: $q_{\text{system}} = -C\Delta T$ (negative ⇒ exothermic).
- Convert between the two with $\Delta H = \Delta U + \Delta n_g RT$; when $\Delta n_g = 0$, $\Delta H = \Delta U$.
- $\Delta H \approx \Delta U$ for solids and liquids; the difference matters only when gaseous moles change.