This MCQ module is based on: Spontaneity Second Law
Spontaneity Second Law
This assessment will be based on: Spontaneity Second Law
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Spontaneity, Entropy and Gibbs Free Energy
5.15 Spontaneity — What Drives a Process?
A spontaneous process is one that has a natural tendency to occur without any external aid. Examples: water flowing downhill, iron rusting, ice melting at 25 °C, two gases mixing.
Some spontaneous processes are exothermic (combustion of methane, ΔH = −890 kJ/mol) and some are endothermic (NH₄Cl dissolving in water, ΔH = +14 kJ/mol). So enthalpy alone cannot predict spontaneity. We need another driving force.
5.16 Entropy (S)
The missing ingredient is entropy (S) — a measure of the disorder or randomness of a system. The higher the disorder, the higher the entropy.
5.16.1 Predicting the Sign of ΔS
| Process | ΔS | Reason |
|---|---|---|
| Solid → Liquid (melting) | + | More positions available |
| Liquid → Gas (vaporisation) | ++ (very large) | Huge increase in volume/disorder |
| Gas → Liquid (condensation) | − | Order increases |
| Reaction increases moles of gas | + | e.g., 2KClO₃ → 2KCl + 3O₂ |
| Reaction decreases moles of gas | − | e.g., N₂ + 3H₂ → 2NH₃ |
| Mixing of two gases | + | More ways to arrange |
| Increase in temperature | + | More kinetic states accessible |
5.17 The Second Law of Thermodynamics
Even an exothermic reaction with ΔS_system < 0 can be spontaneous if the surroundings gain enough entropy: ΔS_surr = −ΔH/T > 0, and the total can be positive.
5.17.1 Third Law of Thermodynamics
5.18 Gibbs Free Energy (G)
For chemists working at constant T and P (typical lab/industrial conditions), it is inconvenient to compute ΔS_universe (need data on the surroundings). The American physicist J. W. Gibbs defined a new state function:
Why is this useful? Multiplying ΔS_universe by −T gives: \[-T\Delta S_\text{universe} = \Delta H_\text{system} - T\Delta S_\text{system} = \Delta G_\text{system}\] So ΔG measures the increase of disorder of the universe, but using only system properties!
5.18.1 Criteria for Spontaneity
| ΔG | Process |
|---|---|
| < 0 (negative) | Spontaneous in forward direction |
| = 0 | Equilibrium |
| > 0 (positive) | Non-spontaneous forward (reverse is spontaneous) |
5.18.2 Sign Combinations of ΔH and ΔS
| ΔH | ΔS | ΔG = ΔH − TΔS | Spontaneity |
|---|---|---|---|
| − (exo) | + (disorder ↑) | Always − | Spontaneous at all T (e.g., 2H₂O₂ → 2H₂O + O₂) |
| + (endo) | − (disorder ↓) | Always + | Never spontaneous (e.g., 3O₂ → 2O₃) |
| − (exo) | − (disorder ↓) | − at low T | Spontaneous only at LOW T (e.g., water freezing) |
| + (endo) | + (disorder ↑) | − at high T | Spontaneous only at HIGH T (e.g., NH₄Cl dissolving, decomposition reactions) |
5.19 Standard Free Energy & Equilibrium Constant
The standard Gibbs free energy change Δ_rG° is related to the equilibrium constant K by:
\[\Delta_r G^\circ = -RT \ln K = -2.303\,RT\,\log K\]| Δ_rG° | K | Direction at standard state |
|---|---|---|
| < 0 | K > 1 | Products favoured |
| = 0 | K = 1 | Equal amounts |
| > 0 | K < 1 | Reactants favoured |
🎯 Interactive: ΔG Spontaneity Predictor
Set ΔH and ΔS for a reaction. Slide T to see when the reaction becomes spontaneous (ΔG < 0).
ΔG = ΔH − TΔS = −10.20 kJ
SPONTANEOUS (forward) ✓
Switch-over T (T_eq = ΔH/ΔS) = 400 K
Setup: For ice → liquid water at 1 atm: ΔH_fus = +6.01 kJ/mol, ΔS_fus = +22.0 J K⁻¹ mol⁻¹.
(a) T = 263 K: ΔG = 6010 − 263×22 = 6010 − 5786 = +224 J. Non-spontaneous — ice stays frozen.
(b) T = 273 K: ΔG = 6010 − 273×22 = 6010 − 6006 ≈ 0. Equilibrium — ice and water coexist (this is the melting point!).
(c) T = 283 K: ΔG = 6010 − 283×22 = 6010 − 6226 = −216 J. Spontaneous — ice melts.
Key insight: The melting point is precisely the temperature where ΔG = 0, i.e., T_m = ΔH/ΔS. Below it, freezing wins; above it, melting wins. ΔG = 0 is the natural definition of phase equilibrium.
Worked Example 5.7: Spontaneity at 298 K
For the reaction N₂(g) + 3H₂(g) → 2NH₃(g), ΔH° = −92.4 kJ and ΔS° = −198.3 J K⁻¹. Is the reaction spontaneous at 298 K? Above what temperature does it become non-spontaneous?
Switch-over temperature (ΔG° = 0): T = ΔH°/ΔS° = (−92400)/(−198.3) = 466 K (≈ 193 °C).
Above 466 K, ΔG° becomes positive — reaction becomes non-spontaneous. This is why industrial NH₃ synthesis uses high pressure to compensate for moderate temperatures (~700 K).
Worked Example 5.8: K from ΔG°
For a reaction at 298 K, Δ_rG° = −13.6 kJ/mol. Calculate the equilibrium constant K. (R = 8.314 J K⁻¹ mol⁻¹)
−13600 = −2.303 × 8.314 × 298 × log K
−13600 = −5705 × log K
log K = 2.383 → K = 10²·³⁸³ ≈ 242
A modest negative ΔG° (~13 kJ) gives K ~ 240, which is product-favoured but not overwhelmingly so.
🎯 Competency-Based Questions
Q1. The criterion of spontaneity at constant T and P is: L1 Remember
Q2. Predict the sign of ΔS for: I₂(s) → I₂(g). L2 Understand
Q3. NH₄Cl dissolves in water with ΔH = +14 kJ/mol but the process is spontaneous at room temperature. Explain. L4 Analyse
Q4. The standard ΔG° for a reaction at 300 K is +5.706 kJ. Calculate K. L3 Apply
Q5. HOT (Evaluate): Life involves building highly ordered structures (proteins, DNA) — apparently violating the second law! How is this reconciled? L5 Evaluate
🧠 Assertion–Reason Questions
Choose: (A) Both true, R explains A. (B) Both true, R doesn't explain A. (C) A true, R false. (D) A false, R true.
A: Spontaneous processes have negative ΔG.
R: Spontaneous processes always release heat.
A: The entropy of a perfectly crystalline solid is zero at 0 K.
R: At 0 K, only one microstate is accessible (all atoms locked in place).
A: A reaction with ΔH > 0 and ΔS > 0 becomes spontaneous at high temperature.
R: The TΔS term grows in magnitude with T, eventually overcoming ΔH.