Enthalpy and Heat Capacity
Chemists rarely run reactions in sealed, rigid boxes — they run them in open flasks and beakers sitting under the atmosphere, at constant pressure, not constant volume. At constant pressure some of the heat released or absorbed by a reaction goes into pushing back (or being pushed by) the atmosphere as gases expand or contract, so the heat measured is not quite the same as the change in internal energy . To track this constant-pressure heat directly, chemists define a new state function called enthalpy, , and becomes the number printed in every thermochemistry table. Alongside enthalpy sits a second everyday idea: how much heat does it take to warm something up? That is heat capacity, and because a gas can be warmed at constant volume or at constant pressure, it comes in two flavours, and , linked by one clean equation for an ideal gas. This section builds into for gas reactions, defines and , and derives — the two relations Unit V of CBSE Class 11 Chemistry expects you to use fluently in numericals.
Enthalpy is the constant-pressure heat function, giving for gas reactions, while links the two heat capacities of an ideal gas because constant-pressure heating must also supply expansion work.
The core idea
Most reactions happen in open vessels at constant atmospheric pressure. At constant pressure, heat absorbed by the system splits between raising internal energy and doing expansion work against the atmosphere, so a state function that captures "heat at constant pressure" directly is genuinely useful. That function is enthalpy:
where: is internal energy, is pressure, and is volume — all state functions, so is a state function too, depending only on the current state of the system, not on how it got there. For a process at constant pressure, , and it can be shown that this equals , the heat exchanged at constant pressure. This is why , not , is the quantity tabulated for reaction enthalpies — it is exactly what a calorimeter open to the atmosphere measures. For reactions involving ideal gases, substituting at constant temperature and pressure turns the volume term into a mole-number term:
where: is (moles of gaseous products) minus (moles of gaseous reactants) — solids and liquids are not counted — is the gas constant, and is the temperature in kelvin.
Heat capacity is the heat needed to raise a system's temperature by 1 K:
Two heat capacities matter because the "1 K rise" can happen at constant volume or constant pressure, and the heat needed is different in each case:
- (constant volume): , so — all the heat goes into internal energy, none into work, because the volume cannot change.
- (constant pressure): , so — some heat also does expansion work as the gas is free to push outward.
Because constant-pressure heating must additionally supply expansion work, is always larger than for a gas; the two are equal only for near-incompressible solids and liquids where volume barely changes with temperature. Molar heat capacity is per mole of substance; specific heat capacity is per unit mass — always check which one a problem is quoting before you substitute.
The goal is to start from the definition for an ideal gas and show, using only and the definitions of and as temperature derivatives, that for one mole of an ideal gas the two molar heat capacities differ by exactly the gas constant, , explaining numerically why constant-pressure heating always costs more energy than constant-volume heating for the same temperature rise.
Step 1. Write enthalpy for one mole of ideal gas using : . This replaces the awkward product with a simple temperature term, because for an ideal gas depends only on , not on or separately.
Step 2. Differentiate with respect to temperature at constant pressure. Since is a constant, . For an ideal gas, internal energy depends only on temperature (not on volume or pressure), so is the same quantity as , which is by definition .
Step 3. Substitute the definitions. The left side, , is by definition . So Step 2 reads , which rearranges to .
Step 4. Check the numbers from the worked example below. With for a monatomic gas, — a roughly increase, all of it the extra energy needed to push back the atmosphere as the gas expands while being warmed at constant pressure. Result: for one mole of an ideal gas, verified against the worked example's , .
Worked example
Problem: For at , . Find . Separately, an ideal monatomic gas has ; find and the heat needed to warm of it by at constant pressure.
Step 1. Count gas moles on each side. Products: mol . Reactants: mol mol mol. So .
Step 2. Apply with , : .
Step 3. Add to : . The gas contracts (4 mol gas becomes 2 mol), so the surroundings do work on the shrinking system, and the reaction releases slightly more heat at constant pressure than the bare suggests.
Step 4. Now the heat capacity part. Using : . Then .
Final answer: for the ammonia synthesis, and of heat is needed to warm of the gas by at constant pressure (with ).
Common traps
- Computing from all species, including solids and liquids — only gaseous species count; a pure solid or liquid product contributes zero.
- Flipping the sign of — it is always (products) minus (reactants), so a reaction that produces fewer moles of gas gives a negative and .
- Assuming in general — this only holds approximately for solids and liquids with negligible expansion; for an ideal gas exactly.
- Mixing up heat capacity (extensive, scales with amount) with molar or specific heat capacity (intensive, per mole or per gram) — always confirm the units before plugging into or .
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Why do we need enthalpy at all if internal energy already tracks energy changes?
Internal energy is the total energy change, but most reactions happen in open vessels at constant atmospheric pressure, where the system also does or absorbs expansion work as gas volume changes. A calorimeter open to the air measures the heat exchanged, , which equals , not . Enthalpy is simply the state function built to match what is actually measured in ordinary lab conditions, so tabulated reaction data is reported as .
Do I need to worry about Δn_g if a reaction has no gases at all?
No — if every species in the reaction is a solid or liquid, , and because there is essentially no volume change to do expansion work against. The correction only matters when gases are involved and the total moles of gas change across the reaction, which is common in combustion and synthesis reactions like the ammonia example.
Is Cp − Cv = R only true for monatomic gases like the worked example?
No — the relation holds for one mole of any ideal gas, monatomic or polyatomic, because the derivation only uses , , and the fact that an ideal gas's internal energy depends on temperature alone. What differs between monatomic and polyatomic gases is the actual value of itself (more atoms means more ways to store energy, so is larger), but the gap between and stays exactly either way.