This MCQ module is based on: Law Mass Action Kc Kp
Law Mass Action Kc Kp
This assessment will be based on: Law Mass Action Kc Kp
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Law of Mass Action, Kc and Kp
6.5 Law of Chemical Equilibrium — Law of Mass Action
In 1864, the Norwegian chemists Cato Guldberg and Peter Waage proposed the Law of Mass Action:
For the elementary reaction aA + bB → cC + dD:
Forward rate: r_f = k_f [A]^a [B]^b
Reverse rate: r_r = k_r [C]^c [D]^d
At equilibrium, r_f = r_r, so:
\[k_f[A]^a[B]^b = k_r[C]^c[D]^d \quad\Rightarrow\quad \frac{k_f}{k_r} = \frac{[C]^c[D]^d}{[A]^a[B]^b} = K_c\]6.6 Equilibrium Constant K_c
6.6.1 Significance of the Magnitude of K
| K range | Implication | Example |
|---|---|---|
| K > 10³ | Reaction nearly complete (products dominate) | 2H₂ + O₂ → 2H₂O at 298 K (K ≈ 10⁸⁰) |
| 10⁻³ < K < 10³ | Significant amounts of both reactants and products | H₂ + I₂ ⇌ 2HI at 700 K (K ≈ 50) |
| K < 10⁻³ | Reaction barely occurs (reactants dominate) | N₂ + O₂ ⇌ 2NO at 298 K (K ≈ 5 × 10⁻³¹) |
6.6.2 Properties of K
- K depends only on temperature, not on initial concentrations or pressure (for ideal systems).
- K for the reverse reaction = 1/K_forward.
- If a reaction is multiplied by n, K becomes K^n.
- For a sum of reactions, K_total = K₁ × K₂ × … (multiplication rule).
6.7 Equilibrium Constant K_p (Gas-Phase Reactions)
For reactions involving gases, partial pressures are often more convenient than concentrations:
6.7.1 Relationship between K_p and K_c
From ideal gas law, p = (n/V) RT = c RT. Substituting:
\[\boxed{K_p = K_c (RT)^{\Delta n_g}}\]where Δn_g = (moles of gaseous products) − (moles of gaseous reactants), and R = 0.0831 L·bar K⁻¹ mol⁻¹ (or 0.0821 L·atm K⁻¹ mol⁻¹).
| Reaction | Δn_g | Relation |
|---|---|---|
| H₂(g) + I₂(g) ⇌ 2HI(g) | 0 | K_p = K_c |
| N₂(g) + 3H₂(g) ⇌ 2NH₃(g) | −2 | K_p = K_c (RT)⁻² |
| PCl₅(g) ⇌ PCl₃(g) + Cl₂(g) | +1 | K_p = K_c (RT)¹ |
| 2NO₂(g) ⇌ N₂O₄(g) | −1 | K_p = K_c (RT)⁻¹ |
6.7.2 Units of K
K is sometimes treated as dimensionless (when concentrations/pressures are divided by their standard values 1 mol/L or 1 bar). Strictly, it can have units depending on Δn:
| Δn | Units of K_c | Units of K_p |
|---|---|---|
| 0 | dimensionless | dimensionless |
| +1 | mol L⁻¹ | bar (or atm) |
| −1 | L mol⁻¹ | bar⁻¹ |
| +2 | mol² L⁻² | bar² |
6.8 Reaction Quotient Q
The reaction quotient (Q) has the same formula as K but is evaluated at any (non-equilibrium) state:
\[Q_c = \frac{[C]^c[D]^d}{[A]^a[B]^b}\]| If… | Then… | Reaction shifts |
|---|---|---|
| Q < K | Too few products | FORWARD (→) until Q = K |
| Q = K | At equilibrium | No net change |
| Q > K | Too many products | REVERSE (←) until Q = K |
6.9 Homogeneous & Heterogeneous Equilibria
6.9.1 Homogeneous
All species in the same phase. Examples: 2NO(g) + O₂(g) ⇌ 2NO₂(g) (all gas); CH₃COOH(aq) + H₂O(l) ⇌ CH₃COO⁻(aq) + H₃O⁺(aq) (all aqueous, with water solvent).
6.9.2 Heterogeneous
Species in different phases. The activities of pure solids and pure liquids are taken as 1 (constant), so they don't appear in K:
CaCO₃(s) ⇌ CaO(s) + CO₂(g) → K_c = [CO₂], K_p = p_{CO₂}
H₂O(l) ⇌ H₂O(g) → K_p = p_{H₂O} (at given T, the saturated VP)
3Fe(s) + 4H₂O(g) ⇌ Fe₃O₄(s) + 4H₂(g) → K_p = p_{H₂}⁴ / p_{H₂O}⁴
🎯 Interactive: K_c ↔ K_p Converter
Pick a reaction (Δn_g auto-set) and a temperature. The calculator gives you both K_c and K_p.
K_p = K_c × (RT)^Δn_g = —
Using R = 0.0831 L·bar K⁻¹ mol⁻¹ and pressures in bar.
Setup: 1.00 mol N₂ and 3.00 mol H₂ are mixed in a 1.0-L vessel at 700 K. At equilibrium, 0.40 mol NH₃ is found. Calculate K_c.
| N₂(g) | 3H₂(g) | 2NH₃(g) | |
|---|---|---|---|
| I (mol/L) | 1.00 | 3.00 | 0 |
| C (mol/L) | −x | −3x | +2x |
| E (mol/L) | 1.00−x | 3.00−3x | 2x = 0.40 → x = 0.20 |
So [N₂] = 0.80 M, [H₂] = 2.40 M, [NH₃] = 0.40 M.
K_c = [NH₃]² / ([N₂][H₂]³) = (0.40)² / (0.80 × 2.40³) = 0.16 / (0.80 × 13.824) = 0.0145 mol⁻²·L²
Worked Example 6.3: Direction Using Q
For the reaction 2SO₂(g) + O₂(g) ⇌ 2SO₃(g), K_c = 280 at 1000 K. The mixture initially contains [SO₂] = 0.20 M, [O₂] = 0.50 M, [SO₃] = 0.10 M. In which direction will the reaction proceed?
Q (0.5) << K (280), so Q < K → reaction proceeds forward (→) producing more SO₃ until Q = K.
Worked Example 6.4: K_p from K_c
For the reaction N₂(g) + 3H₂(g) ⇌ 2NH₃(g), K_c = 0.50 mol⁻²·L² at 750 K. Calculate K_p. (Use R = 0.0831 L·bar K⁻¹ mol⁻¹)
K_p = K_c × (RT)^Δn = 0.50 × (0.0831 × 750)^(−2) = 0.50 × (62.325)⁻² = 0.50 × 1/3884.4 = 1.29 × 10⁻⁴ bar⁻²
K_p < K_c because Δn is negative (gas moles decrease).
Worked Example 6.5: Heterogeneous Equilibrium
For CaCO₃(s) ⇌ CaO(s) + CO₂(g), the equilibrium pressure of CO₂ at 1100 K is 1.42 bar. Write K_p and find its value.
K_p = p_{CO₂} = 1.42 bar.
This is why a closed lime kiln reaches a constant CO₂ pressure regardless of how much solid is loaded.
🎯 Competency-Based Questions
Q1. The equilibrium constant K depends on: L1 Remember
Q2. For 2NO(g) + O₂(g) ⇌ 2NO₂(g), Δn_g = ____ and K_p / K_c = ____. L2 Understand
Q3. For PCl₅(g) ⇌ PCl₃(g) + Cl₂(g), K_c = 1.8 × 10⁻³ at 250 °C. Initially: [PCl₅] = 0.5 M; [PCl₃] = [Cl₂] = 0. Will reaction proceed? L3 Apply
Q4. The K of N₂ + 3H₂ ⇌ 2NH₃ is K₁. What is K for ½N₂ + (3/2)H₂ ⇌ NH₃? L4 Analyse
Q5. HOT (Apply): 0.5 mol H₂ + 0.5 mol I₂ heated to 700 K in a 1-L flask. K_c = 49 for H₂ + I₂ ⇌ 2HI. Find equilibrium concentrations. L3 Apply
[H₂]_eq = 0.5 − x, [I₂]_eq = 0.5 − x, [HI]_eq = 2x.
K_c = (2x)² / ((0.5 − x)²) = 49
Take √: 2x / (0.5 − x) = 7 → 2x = 3.5 − 7x → 9x = 3.5 → x = 0.389 M
[H₂]_eq = [I₂]_eq = 0.111 M, [HI]_eq = 0.778 M. Verify: (0.778)² / (0.111)² = 0.605 / 0.0123 ≈ 49 ✓
🧠 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: The equilibrium constant K_c does not include the concentrations of pure solids or pure liquids.
R: The activity (effective concentration) of any pure solid or liquid is 1.
A: K_p = K_c when Δn_g = 0.
R: K_p = K_c (RT)^Δn_g.
A: If Q > K, the reaction proceeds in the forward direction.
R: When Q > K, [products] is too high relative to equilibrium.