ΔG° and K
The standard Gibbs free energy change and the equilibrium constant are related simply:
R = 8.314 J/(mol·K), and T is in kelvins. When ΔG° is given in kJ/mol, multiply by 1000 to convert it to J/mol first. From this relationship:
| ΔG° | K | At equilibrium |
|---|---|---|
| < 0 | > 1 | products favored |
| = 0 | = 1 | comparable amounts |
| > 0 | < 1 | reactants favored |
K depends exponentially on ΔG°. At 25 °C, every change of RT ln 10 ≈ 5.7 kJ/mol in ΔG° changes K by a factor of 10, so a ΔG° just a few tens of kJ/mol from zero gives a very large or very small K.
Drag ΔG° to see K and the shares of A and B at equilibrium, then look at some real reactions (data: OpenStax Appendix G):
The effect of temperature
ΔG° changes with temperature (ΔG° = ΔH° − TΔS°), and so does K. For an exothermic reaction (ΔH° < 0), heating makes ΔG° larger and K smaller; for an endothermic reaction, heating makes K larger. This matches the conclusion from Le Châtelier’s principle (U7.9).
Example 1: K from ΔG°
Find K at 25 °C for H₂(g) + I₂(g) ⇌ 2HI(g). ΔfG° (kJ/mol): I₂(g) 19.3, HI(g) 1.7.
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ΔG° from free energies of formation. Products minus reactants; H₂(g) is an element in its standard state, so ΔfG° = 0 (in kJ):
In joules: −1.59 × 10⁴ J (R is in J, so ΔG° must be too).
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Find ln K. Use ΔG° = −RT ln K with T = 298 K:
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Find K.
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Check the sign. ΔG° < 0 goes with K > 1. Consistent.
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Compare with Unit 7. This reaction has K = 50 at 400 °C, smaller than at 25 °C. K falling as temperature rises means the forward reaction is exothermic (ΔH° = −9.5 kJ), consistent with Le Chatelier’s principle.
Example 2: ΔG° from K
At 25 °C, Ksp for AgCl is 1.6 × 10⁻¹⁰ (OpenStax Appendix J). Find ΔG° for AgCl(s) ⇌ Ag⁺(aq) + Cl⁻(aq).
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Write the formula. For a dissolving equilibrium, K is Ksp:
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Work out ln K first.
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Substitute. In J:
That is .
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Check the sign. Ksp ≪ 1, so ln Ksp is negative; times the minus sign, ΔG° is positive. Consistent.
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Connect to solubility. ΔG° > 0 and K ≪ 1: dissolving AgCl is unfavorable under standard conditions, very little dissolves at equilibrium, and that is why it is only slightly soluble.
- ΔG° = −30 kJ/mol
ΔG° < 0.
- ΔG° = +20 kJ/mol
ΔG° > 0.
- ΔG° = −0.3 kJ/mol
K = e0.12 ≈ 1.1.
- ΔG° = +45 kJ/mol
K is about 10−8.
- ΔH° = −50 kJ, ΔS° = −100 J/K, T = 1000 K
ΔG° = −50 + 100 = +50 kJ.
- ΔH° = +40 kJ, ΔS° = +200 J/K, T = 400 K
ΔG° = 40 − 80 = −40 kJ.
- ΔG° = +0.4 kJ/mol at 500 K
K = e−0.096 ≈ 0.91.
- ΔG° = −100 kJ/mol
K is about 10¹⁷.
Common mistakes
Mistake 1: “ΔG° = 0 means the reaction is at equilibrium.” ΔG° = 0 means K = 1. The sign of equilibrium is ΔG = 0 (without the °), when Q = K.
Mistake 2: “Use log instead of ln, or ΔG° in kJ with R in J.” The formula uses the natural log, ln; R is in J/(mol·K), so convert ΔG° to J/mol.
Mistake 3: “A reaction with ΔG° > 0 has no product at equilibrium.” K < 1 only means there is less product than reactant. With ΔG° = +5 kJ/mol, for example, K ≈ 0.13, which is still a fair amount of product.
Quick check
At 25 °C a reaction has ΔG° = +11.4 kJ/mol. K is about:
−ΔG°/RT = −11400 ÷ (8.314 × 298) = −4.6, so K = e−4.6 ≈ 0.010.
At 25 °C a reaction has K = 2.0 × 10⁸. What is ΔG°?
ΔG° = −8.314 × 298 × ln(2.0 × 10⁸) J = −4.74 × 10⁴ J = −47.4 kJ. B uses log; D treats J as kJ.
At some temperature a reaction has ΔG° = 0. Which statement is correct?
ΔG° = −RT ln K = 0, so ln K = 0 and K = 1.
At 25 °C, ΔG° for reaction 1 is 11.4 kJ/mol more negative than for reaction 2. K₁ is about how many times K₂?
Each 5.7 kJ/mol is a factor of 10, so 11.4 kJ/mol is a factor of 10² = 100.
A reaction has ΔH° = +50 kJ and ΔS° = +100 J/K. At what temperature is K = 1?
K = 1 when ΔG° = 0, so T = 50 ÷ 0.100 = 500 K; above 500 K, K > 1.
Which quantity equals zero when a reacting system reaches equilibrium?
At equilibrium Q = K, so ΔG = ΔG° + RT ln Q = 0; ΔG° is generally not zero.
AP-style free response
Above the iodine crystals in a sealed bottle there is faint violet iodine vapor: I₂(s) ⇌ I₂(g). Data: for I₂(g), ΔfG° = 19.3 kJ/mol and ΔfH° = 62.4 kJ/mol; S° (J·mol⁻¹·K⁻¹) I₂(s) 116.1, I₂(g) 260.7 (OpenStax Appendix G).
(a) Write the Kp expression for this equilibrium.
(b) Calculate ΔG° at 25 °C.
(c) Calculate Kp at 25 °C, and state what it represents here.
(d) Assuming ΔH° and ΔS° don’t change with temperature, calculate the temperature at which Kp = 1.
(e) The bottle is opened in a fume hood, and iodine vapor keeps escaping. Compare Q with K, and describe what happens to the iodine crystals.
Model answer and scoring
(a) Kp = P(I₂) (the solid is left out of the expression).
(b) ΔG° = 19.3 − 0 = +19.3 kJ.
(c) Kp = e−19300/(8.314 × 298) = e−7.79 = 4.1 × 10⁻⁴. It is the equilibrium vapor pressure of iodine at 25 °C, about 4.1 × 10⁻⁴ bar: ΔG° > 0, so there is little I₂(g) at equilibrium.
(d) ΔS° = 260.7 − 116.1 = 144.6 J/K, so T = 62.4 ÷ 0.1446 = 432 K.
(e) The escaping vapor lowers P(I₂), so Q < K; the equilibrium shifts toward I₂(g), and the crystals keep subliming and shrinking.
Scoring: (a) expression; (b) ΔG°; (c) Kp and its meaning; (d) ΔS° and temperature; (e) Q < K and the conclusion.
Summary
- ΔG° = −RT ln K: ΔG° < 0 ↔ K > 1, ΔG° = 0 ↔ K = 1, ΔG° > 0 ↔ K < 1.
- At 25 °C, every change of about 5.7 kJ/mol in ΔG° changes K by a factor of 10.
- Temperature affects K through ΔG° = ΔH° − TΔS°: heating raises K for an endothermic reaction and lowers it for an exothermic one.
AP tip: When using ΔG° = −RT ln K, show the unit conversion (kJ → J) and use ln, not log. In qualitative questions, stating the link, such as “ΔG° < 0, so K > 1,” is enough.
Enrichment (nonstandard conditions): For any composition, ΔG = ΔG° + RT ln Q. When Q < K, ΔG < 0 and the reaction proceeds forward; when Q = K, ΔG = 0 and the system is at equilibrium.