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 ΔU\Delta U. To track this constant-pressure heat directly, chemists define a new state function called enthalpy, HH, and ΔH\Delta H 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, CvC_v and CpC_p, linked by one clean equation for an ideal gas. This section builds H=U+PVH = U + PV into ΔH=ΔU+ΔngRT\Delta H = \Delta U + \Delta n_g RT for gas reactions, defines CvC_v and CpC_p, and derives Cp−Cv=RC_p - C_v = R — the two relations Unit V of CBSE Class 11 Chemistry expects you to use fluently in numericals.

The core insight

Enthalpy H=U+PVH = U + PV is the constant-pressure heat function, giving ΔH=ΔU+ΔngRT\Delta H = \Delta U + \Delta n_g RT for gas reactions, while Cp−Cv=RC_p - C_v = R 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:

H=U+PVH = U + PV

where: UU is internal energy, PP is pressure, and VV is volume — all state functions, so HH 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, ΔH=ΔU+PΔV\Delta H = \Delta U + P\Delta V, and it can be shown that this equals qpq_p, the heat exchanged at constant pressure. This is why ΔH\Delta H, not ΔU\Delta U, is the quantity tabulated for reaction enthalpies — it is exactly what a calorimeter open to the atmosphere measures. For reactions involving ideal gases, substituting PV=ngRTPV = n_gRT at constant temperature and pressure turns the volume term into a mole-number term:

ΔH=ΔU+Δng RT\Delta H = \Delta U + \Delta n_g\,RT

where: Δng\Delta n_g is (moles of gaseous products) minus (moles of gaseous reactants) — solids and liquids are not counted — R=8.314 J K−1mol−1R = 8.314\ \text{J K}^{-1}\text{mol}^{-1} is the gas constant, and TT is the temperature in kelvin.

Heat capacity CC is the heat needed to raise a system's temperature by 1 K:

C=qΔTC = \frac{q}{\Delta T}

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:

  • CvC_v (constant volume): Cv=(∂U∂T)VC_v = \left(\dfrac{\partial U}{\partial T}\right)_V, so qv=ΔU=CvΔTq_v = \Delta U = C_v\Delta T — all the heat goes into internal energy, none into work, because the volume cannot change.
  • CpC_p (constant pressure): Cp=(∂H∂T)PC_p = \left(\dfrac{\partial H}{\partial T}\right)_P, so qp=ΔH=CpΔTq_p = \Delta H = C_p\Delta T — some heat also does expansion work as the gas is free to push outward.

Because constant-pressure heating must additionally supply expansion work, CpC_p is always larger than CvC_v 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.

Figure
Two identical gas cylinders being warmed by one kelvin, one with a fixed piston at constant volume where all the heat raises internal energy, and one with a free piston at constant pressure where some heat also pushes the piston outward doing expansion work
Warming a gas by 1 K — constant volume versus constant pressure constant volume fixed piston heat q all heat raises U q = C_v ΔT constant pressure free piston piston rises heat q heat raises H, some does work q = C_p ΔT C_p is always greater than C_v for a gas
Derivation AFrom enthalpy to Cp minus Cv equals R

The goal is to start from the definition H=U+PVH = U + PV for an ideal gas and show, using only PV=nRTPV = nRT and the definitions of CvC_v and CpC_p as temperature derivatives, that for one mole of an ideal gas the two molar heat capacities differ by exactly the gas constant, Cp−Cv=RC_p - C_v = R, 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 PV=RTPV = RT: H=U+PV=U+RTH = U + PV = U + RT. This replaces the awkward PVPV product with a simple temperature term, because for an ideal gas PVPV depends only on TT, not on PP or VV separately.

Step 2. Differentiate with respect to temperature at constant pressure. Since RR is a constant, (∂H∂T)P=(∂U∂T)P+R\left(\dfrac{\partial H}{\partial T}\right)_P = \left(\dfrac{\partial U}{\partial T}\right)_P + R. For an ideal gas, internal energy UU depends only on temperature (not on volume or pressure), so (∂U∂T)P\left(\dfrac{\partial U}{\partial T}\right)_P is the same quantity as (∂U∂T)V\left(\dfrac{\partial U}{\partial T}\right)_V, which is by definition CvC_v.

Step 3. Substitute the definitions. The left side, (∂H∂T)P\left(\dfrac{\partial H}{\partial T}\right)_P, is by definition CpC_p. So Step 2 reads Cp=Cv+RC_p = C_v + R, which rearranges to Cp−Cv=RC_p - C_v = R.

Step 4. Check the numbers from the worked example below. With Cv=12.5 J K−1mol−1C_v = 12.5\ \text{J K}^{-1}\text{mol}^{-1} for a monatomic gas, Cp=12.5+8.314=20.8 J K−1mol−1C_p = 12.5 + 8.314 = 20.8\ \text{J K}^{-1}\text{mol}^{-1} — a roughly 67%67\% increase, all of it the extra energy needed to push back the atmosphere as the gas expands while being warmed at constant pressure. Result: Cp−Cv=RC_p - C_v = R for one mole of an ideal gas, verified against the worked example's Cv=12.5C_v = 12.5, Cp=20.8 J K−1mol−1C_p = 20.8\ \text{J K}^{-1}\text{mol}^{-1}.

Worked example

Problem: For N2(g)+3H2(g)→2NH3(g)\text{N}_2(g) + 3\text{H}_2(g) \rightarrow 2\text{NH}_3(g) at 298 K298\ \text{K}, ΔU=−91.8 kJ mol−1\Delta U = -91.8\ \text{kJ mol}^{-1}. Find ΔH\Delta H. Separately, an ideal monatomic gas has Cv=12.5 J K−1mol−1C_v = 12.5\ \text{J K}^{-1}\text{mol}^{-1}; find CpC_p and the heat needed to warm 2.0 mol2.0\ \text{mol} of it by 15 K15\ \text{K} at constant pressure.

Step 1. Count gas moles on each side. Products: 22 mol NH3\text{NH}_3. Reactants: 11 mol N2+3\text{N}_2 + 3 mol H2=4\text{H}_2 = 4 mol. So Δng=2−4=−2\Delta n_g = 2 - 4 = -2.

Step 2. Apply ΔH=ΔU+ΔngRT\Delta H = \Delta U + \Delta n_g RT with R=8.314 J K−1mol−1R = 8.314\ \text{J K}^{-1}\text{mol}^{-1}, T=298 KT = 298\ \text{K}: ΔngRT=(−2)(8.314)(298)=−4955 J mol−1=−4.955 kJ mol−1\Delta n_g RT = (-2)(8.314)(298) = -4955\ \text{J mol}^{-1} = -4.955\ \text{kJ mol}^{-1}.

Step 3. Add to ΔU\Delta U: ΔH=−91.8+(−4.955)=−96.8 kJ mol−1\Delta H = -91.8 + (-4.955) = -96.8\ \text{kJ mol}^{-1}. 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 ΔU\Delta U suggests.

Step 4. Now the heat capacity part. Using Cp=Cv+RC_p = C_v + R: Cp=12.5+8.314=20.8 J K−1mol−1C_p = 12.5 + 8.314 = 20.8\ \text{J K}^{-1}\text{mol}^{-1}. Then qp=nCpΔT=(2.0)(20.8)(15)=624 Jq_p = nC_p\Delta T = (2.0)(20.8)(15) = 624\ \text{J}.

Final answer: ΔH=−96.8 kJ mol−1\Delta H = -96.8\ \text{kJ mol}^{-1} for the ammonia synthesis, and 624 J624\ \text{J} of heat is needed to warm 2.0 mol2.0\ \text{mol} of the gas by 15 K15\ \text{K} at constant pressure (with Cp=20.8 J K−1mol−1C_p = 20.8\ \text{J K}^{-1}\text{mol}^{-1}).

Common traps

  • Computing Δng\Delta n_g from all species, including solids and liquids — only gaseous species count; a pure solid or liquid product contributes zero.
  • Flipping the sign of Δng\Delta n_g — it is always (products) minus (reactants), so a reaction that produces fewer moles of gas gives a negative Δng\Delta n_g and ΔH<ΔU\Delta H < \Delta U.
  • Assuming Cp=CvC_p = C_v in general — this only holds approximately for solids and liquids with negligible expansion; for an ideal gas Cp−Cv=RC_p - C_v = R 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 q=nCΔTq = nC\Delta T or q=mcΔTq = mc\Delta T.

Ask the tutor: Stuck on when to use CvC_v versus CpC_p, or how to compute Δng\Delta n_g for a tricky reaction — ask the AI tutor to walk through a fresh example with you.

Why do we need enthalpy at all if internal energy already tracks energy changes?

Internal energy ΔU\Delta U 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, qpq_p, which equals ΔH\Delta H, not ΔU\Delta U. Enthalpy is simply the state function built to match what is actually measured in ordinary lab conditions, so tabulated reaction data is reported as ΔH\Delta H.

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, Δng=0\Delta n_g = 0, and ΔH≈ΔU\Delta H \approx \Delta U because there is essentially no volume change to do expansion work against. The ΔngRT\Delta n_g RT 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 Cp−Cv=RC_p - C_v = R holds for one mole of any ideal gas, monatomic or polyatomic, because the derivation only uses H=U+PVH = U + PV, PV=RTPV = RT, 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 CvC_v itself (more atoms means more ways to store energy, so CvC_v is larger), but the gap between CpC_p and CvC_v stays exactly RR either way.

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