Lessons · Equilibrium & acid–base

The pH of a weak base: ammonia

ICE ledger machine-checked — every dissolved row is initial + ν·x, one extent xKb data-sourced (openstax-chemistry-2e)3 modeling assumptions (disclosed)

Dissolve enough ammonia to make the solution 0.100M0.100\,\text{M}. Ammonia is a weak base: it has no OH\mathrm{OH^-} of its own — instead it pulls a proton off a water molecule, NH3+H2ONH4++OH\mathrm{NH_3} + \mathrm{H_2O} \rightleftharpoons \mathrm{NH_4^+} + \mathrm{OH^-}, and only a small fraction reacts, so the equilibrium sits far to the left. What is the pH? It is the ICE table once more — the same species ledger, initial → change → equilibrium — but with two new twists. First, water is the pure solvent: its activity is 1, so it never enters the equilibrium expression Kb=[NH4+][OH]/[NH3]K_b = [\mathrm{NH_4^+}][\mathrm{OH^-}]/[\mathrm{NH_3}] — exactly as a pure solid drops out of a KspK_{sp}. Second, the extent gives [OH][\mathrm{OH^-}], not [H+][\mathrm{H^+}]; the bridge to pH is the ion-product of water, [H+][OH]=Kw=1.0×1014[\mathrm{H^+}][\mathrm{OH^-}] = K_w = 1.0\times10^{-14}, which is why pH+pOH=14.00\mathrm{pH} + \mathrm{pOH} = 14.00.

NH3(aq)+H2O(l)NH4+(aq)+OH(aq)\mathrm{NH_{3}}\,\text{(aq)} + \mathrm{H_{2}O}\,\text{(l)} \rightleftharpoons \mathrm{NH_{4}}^{+}\,\text{(aq)} + \mathrm{OH}^{-}\,\text{(aq)}
Kb=[NH4+][OH][NH3]K_b = \dfrac{[\mathrm{NH_{4}}^{+}][\mathrm{OH}^{-}]}{[\mathrm{NH_{3}}]}=1.8×10⁻⁵at 25 °C
SpeciesInitial (M)Change (M)Equilibrium (M)
NH3\mathrm{NH_{3}} (aq)0.100−x0.0987
H2O\mathrm{H_{2}O} (l)pure liquid · excluded from Q
NH4+\mathrm{NH_{4}}^{+} (aq)0+x0.00133
OH\mathrm{OH}^{-} (aq)0+x0.00133

machine-checkedThe Change row is ν·x — the very same extent ledger ci = ci,0 + νi·xas any reaction. Water is the pure solvent (activity 1), so it never enters the equilibrium expression.

Mass actionx = 0.00133 M = [OH⁻], the extent where Q = Kb.

Kb=[NH4+][OH][NH3]K_b = \dfrac{[\mathrm{NH_{4}}^{+}][\mathrm{OH}^{-}]}{[\mathrm{NH_{3}}]}=(0.00133)(0.00133) / (0.0987)=1.8×10⁻⁵= Kb

Put the committed equilibrium concentrations back in and the quotient reproduces Kb to within 3.3×10⁻¹² — the solver found the extent, and an independent check re-solves it and agrees.

[OH]0.00133 M1.33% of the base ionized
pOH2.88= −log10[OH]
pH11.12= 14.00 − pOH

Kw bridgeThe extent gives [OH] = 0.00133 M, not [H+]. Water ties them together:[H+][OH] = Kw = 1×10⁻¹⁴, so[H+] = Kw/[OH] = 0.0000000000075 M andpH + pOH = 11.12 + 2.88 = 14.00.

VerificationProven at build time — not asserted.
  • Every equilibrium concentration = initial + ν·x [ICE identity]
  • The extent x re-solved independently — numerically, to high precision — reproduces Q = Kb [mass-action root]
  • Water is excluded from Q; 0 < x < [NH₃]₀ — no concentration goes negative [extent physical]
  • [H⁺] = K_w/[OH⁻]; pH = −log₁₀[H⁺]; pH + pOH = pK_w [K_w bridge]
Common misconception: “The base is 0.100 M, so [OH-] = 0.100 M, pOH = -log(0.100) = 1.00, and pH = 14.00 - 1.00 = 13.00.

That would be true for a strong base like NaOH, which delivers its OH⁻ completely. But ammonia has no OH⁻ of its own — it must take one from water, and the ledger shows the extent is only x = 0.00133 M, just 1.33% ionized. So [OH] = 0.00133 M, pOH = 2.88, and through Kw the pH = 11.12 — not 13.00; the other 0.0987 M (98.67%) stays as intact NH₃. Notice the mirror: this base at 0.100 M lands as far above pH 7 as 0.100 M acetic acid (same K) lands below it.

Modeling assumptions — author-asserted, disclosed not discharged
  • model The solution has reached equilibrium, and this single ionization is the only reaction that matters (one dominant equilibrium).
  • model Activities are approximated by molar concentrations — the ideal-dilute-solution model, which is why KbK_b and KwK_w are written with concentrations.
  • model The OH\mathrm{OH^-} from water's own autoionization (107M10^{-7}\,\text{M}) is negligible beside the base's, so [OH]0=0[\mathrm{OH^-}]_0 = 0 in the table; Kw=1.0×1014K_w = 1.0\times10^{-14} is the 25 °C value.

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