Reaction equilibria
You already know how to write or for a reaction and predict which way Le Chatelier's principle pushes it — that is CBSE/JEE-level equilibrium. What you have not yet seen is why takes the form it does, why it depends on temperature alone and never on pressure or concentration, or why heating an exothermic reaction reliably lowers . CY11001 answers all three from a single starting point: the chemical potential expression carried over from the previous article. Writing the equilibrium condition in terms of species activities produces the general equilibrium constant , and differentiating with respect to produces the van't Hoff equation — a genuine derivative that replaces the qualitative "system opposes the change" heuristic with an equation you can actually compute.
The thermodynamic equilibrium constant follows from and depends on temperature alone, and differentiating this relation gives the van't Hoff equation , which turns Le Chatelier's temperature rule into a computable derivative.
The core idea
From chemical potential to . The equilibrium condition for a reaction is that the weighted sum of chemical potentials of products equals that of reactants, each weighted by its stoichiometric coefficient (negative for reactants, positive for products). Substituting the general form — where is the species activity, a dimensionless "effective concentration" referenced to a standard state ( for an ideal gas, for a dilute solute) — and rearranging gives with
where: is the activity of species and its stoichiometric coefficient. Because every on the right of is a standard chemical potential — fixed once is fixed, independent of how much of each species is actually present — itself is a function of alone. This is the fact CBSE states but CY11001 proves: changing pressure, volume or concentration shifts the equilibrium composition to keep satisfied, but never changes itself.
The van't Hoff equation. Differentiate with respect to and use the Gibbs-Helmholtz relation :
where: is the standard reaction enthalpy (assumed roughly constant over the temperature range considered) and . Integrating between two temperatures gives the working form used in calculations:
This is structurally identical to the integrated Clausius-Clapeyron equation from phase equilibrium, because both descend from the same mathematics.
Le Chatelier's rule, now a sign. For an exothermic reaction (), the van't Hoff equation gives , so falls as rises — heating disfavours products. For an endothermic reaction (), rises with . The qualitative CBSE rule is exactly this sign, now derived rather than asserted.
The goal is to show, using only the chain rule and the Gibbs-Helmholtz relation already established for , that the temperature dependence of the equilibrium constant is governed by a single derivative , and that this derivative — not a qualitative appeal to "the system resists change" — is the correct thermodynamic content behind Le Chatelier's temperature rule.
Step 1. Start from the relation between and standard Gibbs energy, , and rearrange it to isolate : . Written this way, is a constant () times the very quantity whose temperature derivative the Gibbs-Helmholtz relation already gives.
Step 2. Differentiate both sides with respect to at constant pressure. . This step is purely mechanical differentiation of Step 1; no new physics has entered yet.
Step 3. Substitute the Gibbs-Helmholtz relation, , applied to the reaction quantities and : . This is the van't Hoff equation.
Step 4. Integrate assuming is roughly constant over to . gives , the working integrated form. Reading the sign directly: if (exothermic) and , the bracket is negative, so the two negatives cancel and is negative — falls on heating, exactly the exothermic Le Chatelier rule, now obtained as an algebraic consequence rather than assumed.
Worked example
For , at 500 K and (exothermic, roughly constant over the range). Estimate at 600 K, and use the answer to find the degree of dissociation regime it implies is favoured.
Step 1. Apply the integrated van't Hoff equation with K, , K. .
Step 2. Evaluate the bracket. , , so the difference is .
Step 3. Combine. , so and .
Step 4. Interpret via the dissociation link. Since falls by roughly two orders of magnitude on heating, the equilibrium extent of the reverse reaction (ammonia decomposing back to and ) is strongly favoured at 600 K compared with 500 K — consistent with the general degree-of-dissociation relation derived for a dissociating gas-phase equilibrium: a smaller at fixed forces a smaller equilibrium for the forward process, i.e. less product. Answer: , roughly of its value at 500 K, obtained purely from — the quantitative version of "heating an exothermic reaction disfavours products."
Competitive stretch
Suppose instead you were given at both 500 K and 600 K but not — could you recover it? Yes: the same integrated van't Hoff equation is linear in the unknown once , , and are known, so it can be solved by rearrangement rather than integration. Using the two values already found, at K and at K, rearrange for : , recovering the same used to construct the problem — the check that the van't Hoff equation is a genuinely invertible relation between and the pair of equilibrium constants, exactly the way two points on a straight line fix its slope.
Common traps
- Believing itself changes when reactant is added or pressure is changed — is a function of only; what changes is relative to , or (for pressure and volume changes) the equilibrium composition/extent that still satisfies the fixed , never itself.
- Applying the integrated van't Hoff equation across a temperature range where is not roughly constant, such as one spanning a phase change of a reactant — the constant- assumption can fail over wide ranges, exactly as in Clausius-Clapeyron.
- Reversing the sign rule under exam pressure: an increase in increases for endothermic reactions () and decreases for exothermic reactions — students commonly remember it backwards.
- Forgetting that built from activities is dimensionless by construction (each activity already divides by or ); plugging a quoted with explicit pressure units directly into produces a dimensionally meaningless logarithm.
Ask the tutor: If you want Le Chatelier's pressure and concentration rules derived thermodynamically the same way the temperature rule was derived here, ask the AI tutor to work through the -versus- argument for those cases too.
If K only depends on temperature, why does adding more reactant shift the equilibrium at all?
Adding reactant does not change , but it does change the reaction quotient , which is computed the same way as but from the current (non-equilibrium) activities. Immediately after adding reactant, , so the reaction proceeds forward until the new composition again satisfies . The system moves to a new equilibrium composition; the value of itself never moves, because is fixed by the standard chemical potentials at that temperature only.
Why does the van't Hoff equation look so similar to Clausius-Clapeyron?
Both are integrated forms of the same underlying mathematical statement, , applied to two different equilibria. For phase equilibrium, is the enthalpy of the phase change and the "equilibrium constant" is effectively the vapour pressure; for reaction equilibrium, is the reaction enthalpy and the constant is . The shared Gibbs-Helmholtz origin is why both integrate to the same functional form.
How do I know when the constant-delta-H assumption in the integrated van't Hoff equation is safe to use?
It is safe when the temperature range is narrow enough, and free of any phase change of a reactant or product, that does not vary appreciably — typically a few tens of kelvin for problems at this level. Over wider ranges, itself depends on through the heat capacities of reactants and products, and the simple integrated form used in the worked example above would need a correction term. Unless a problem explicitly signals a wide range or a phase change, treat as constant, exactly as with Clausius-Clapeyron.