1.4.1 (HL)—Entropy (S)
- Syllabus
- First assessment 2025
- Objective
- 1.4.1
- Level
- HL
S(gas)>S(liquid)>S(solid)
Entropy describes the dispersal of matter and available energy. For the reaction system, calculate ΔS° = ΣS°(products) − ΣS°(reactants), including every coefficient, and report J K⁻¹ mol⁻¹ for the reaction as written. System ΔS° is not the same as total entropy change of system plus surroundings; state the boundary before using entropy to discuss spontaneity.
Use phase and particle count to predict a likely sign before calculating: producing more gas particles usually increases dispersal. Treat that prediction as a check, not a replacement for the standard-entropy sum.
Worked entropy example: for HX2(g)+ClX2(g)2HCl(g), use S∘(HCl)=187, S∘(HX2)=131 and S∘(ClX2)=223JK−1mol−1. ΔS∘=2(187)−[131+223]=+20JK−1mol−1. The small positive value is plausible because gas moles are unchanged; the tabulated values, not gas count alone, determine the sign.
Representative question
Calculate the standard entropy change, ΔS⊖, of the reaction between carbon monoxide and chlorine to form phosgene. Use section 13 of the data booklet and the following data:
Standard entropy S⊖, of chlorine =223 J mol−1 K−1
Standard entropy S⊖, of phosgene =284 J mol−1 K−1
entropy change «= 284-223-198»
=−137≪ J mol−1 K−1≫
Retrieve the route: identify complete or incomplete combustion products, compare fuels and biofuels, balance fuel-cell half-equations, calculate ΔS° and ΔG°, then use ΔG, Q and K to reason about spontaneity and equilibrium.
Check products before balancing, evidence before evaluation, oxidation versus reduction, kelvin and unit consistency, the sign of ΔG, and whether Q is below, equal to, or above K.