Calculate the standard entropy change for a chemical or physical process based on the absolute entropies (standard molar entropies) of the species involved.
The entropy change for a process can be calculated from the absolute entropies of the species involved before and after the process occurs. The equation is on the AP sheet:
ΔS°reaction = Σ S°(products) − Σ S°(reactants)
Same "products minus reactants" pattern as ΔH°f (6.8) and ΔG°f (9.3), each weighted by the stoichiometric coefficient.
One critical difference from enthalpy: entropies are absolute, not relative to a reference. A perfect crystal at 0 K has S = 0, and every substance above that has a positive absolute entropy. So unlike ΔH°f, S° for an element in its standard state is not zero — S° for O₂(g) is 205.0 J·mol⁻¹·K⁻¹, and it must be included in your sum.
Units. Entropies are quoted in J·mol⁻¹·K⁻¹, while enthalpies are in kJ/mol. That factor of 1000 is the single most common arithmetic error in Unit 9, because ΔG° = ΔH° − TΔS° requires them in the same units. Convert before subtracting.
Patterns in tabulated S° values that let you sanity-check an answer:
Calculate ΔS° for 2 NO(g) + O₂(g) → 2 NO₂(g). S° values (J·mol⁻¹·K⁻¹): NO(g) = 210.8, O₂(g) = 205.0, NO₂(g) = 240.1. Does the sign agree with a qualitative prediction?
Qualitative prediction first: gas moles go from 2 + 1 = 3 to 2. Fewer gas particles means less dispersal, so ΔS° should be negative.
Products: 2 × 240.1 = 480.2 J·mol⁻¹·K⁻¹
Reactants: 2 × 210.8 + 1 × 205.0 = 421.6 + 205.0 = 626.6 J·mol⁻¹·K⁻¹
ΔS° = 480.2 − 626.6 = −146.4 J·mol⁻¹·K⁻¹
The sign matches the prediction ✓. Note that O₂ contributed 205.0 rather than zero — a reminder that absolute entropies of elements are not zero.
To use this in ΔG° = ΔH° − TΔS°, first convert: ΔS° = −0.1464 kJ·mol⁻¹·K⁻¹.