Polyprotic acids Knowledge-Based Study

Chemistry · Acids & Bases · Chemistry · Acid–Base Equilibria

Chemistry topic explanations on Polyprotic acids.

Study notes

  1. What Are Polyprotic Acids?

    Acids are classified by the number of ionizable protons (hydrogen ions, H+\text{H}^+) they can donate per molecule in aqueous solution:

    • Monoprotic acids: Can donate only one proton per molecule (e.g., HCl\text{HCl}, HNO3\text{HNO}_3, CH3COOH\text{CH}_3\text{COOH}).
    • Diprotic acids: Can donate up to two protons per molecule through successive steps (e.g., H2SO4\text{H}_2\text{SO}_4, H2CO3\text{H}_2\text{CO}_3, H2C2O4\text{H}_2\text{C}_2\text{O}_4).
    • Triprotic acids: Can donate up to three protons per molecule (e.g., H3PO4\text{H}_3\text{PO}_4, H3AsO4\text{H}_3\text{AsO}_4, citric acid).

    Acids capable of donating more than one proton per molecule are collectively referred to as polyprotic acids. The loss of each proton occurs in a discrete, stepwise equilibrium rather than all at once.

    Successive Dissociation Equilibria

    Consider a general diprotic acid, H2A\text{H}_2\text{A}. Its ionization in water takes place in two sequential steps, each with its own acid dissociation constant:

    First ionization step:

    H2A(aq)+H2O(l)⇌H3O+(aq)+HA−(aq)Ka1=[H3O+][HA−][H2A]\text{H}_2\text{A}(aq) + \text{H}_2\text{O}(l) \rightleftharpoons \text{H}_3\text{O}^+(aq) + \text{HA}^-(aq) \quad K_{\text{a1}} = \frac{[\text{H}_3\text{O}^+][\text{HA}^-]}{[\text{H}_2\text{A}]}

    Second ionization step:

    HA−(aq)+H2O(l)⇌H3O+(aq)+A2−(aq)Ka2=[H3O+][A2−][HA−]\text{HA}^-(aq) + \text{H}_2\text{O}(l) \rightleftharpoons \text{H}_3\text{O}^+(aq) + \text{A}^{2-}(aq) \quad K_{\text{a2}} = \frac{[\text{H}_3\text{O}^+][\text{A}^{2-}]}{[\text{HA}^-]}

    Why is Ka1K_{\text{a1}} Always Greater Than Ka2K_{\text{a2}}?

    For any polyprotic acid, the successive ionization constants decrease drastically:

    Ka1≫Ka2≫Ka3K_{\text{a1}} \gg K_{\text{a2}} \gg K_{\text{a3}}

    This occurs because the first proton is removed from a neutral molecule (H2A\text{H}_2\text{A}), whereas the second proton must be removed from a negatively charged anion (HA−\text{HA}^-). Electrostatic attraction makes it significantly more difficult to separate a positively charged proton (H+\text{H}^+) from a negatively charged species, resulting in a substantially smaller equilibrium constant for subsequent steps (often by a factor of 10410^4 to 10610^6).

    Equilibrium Calculations for Weak Polyprotic Acids

    Because Ka1K_{\text{a1}} is typically several orders of magnitude greater than Ka2K_{\text{a2}}, the hydronium ion concentration in a solution of a typical weak diprotic acid is governed almost entirely by the first ionization step.

    Key Approximations

    • Hydronium concentration and pH: We can calculate [H3O+][\text{H}_3\text{O}^+] by treating the solution as if it contains only the monoprotic weak acid H2A\text{H}_2\text{A} with constant Ka1K_{\text{a1}}. The contribution of [H3O+][\text{H}_3\text{O}^+] from the second dissociation step is negligible in comparison.
    • Intermediate species concentration: From the stoichiometry of the first step, [HA−]≈[H3O+][\text{HA}^-] \approx [\text{H}_3\text{O}^+].
    • Divalent conjugate base concentration: By substituting [HA−]≈[H3O+][\text{HA}^-] \approx [\text{H}_3\text{O}^+] into the expression for Ka2K_{\text{a2}}:
    Ka2=[H3O+][A2−][HA−]≈[H3O+][A2−][H3O+]=[A2−]K_{\text{a2}} = \frac{[\text{H}_3\text{O}^+][\text{A}^{2-}]}{[\text{HA}^-]} \approx \frac{[\text{H}_3\text{O}^+][\text{A}^{2-}]}{[\text{H}_3\text{O}^+]} = [\text{A}^{2-}]

    Therefore, for an unbuffered aqueous solution of a weak diprotic acid where Ka1≫Ka2K_{\text{a1}} \gg K_{\text{a2}}, the concentration of the fully deprotonated anion [A2−][\text{A}^{2-}] is approximately equal to Ka2K_{\text{a2}}.

    Sulfuric Acid (H2SO4\text{H}_2\text{SO}_4)

    Sulfuric acid is unique because it is a strong acid in its first dissociation and a weak acid in its second dissociation:

    • H2SO4(aq)+H2O(l)→H3O+(aq)+HSO4−(aq)\text{H}_2\text{SO}_4(aq) + \text{H}_2\text{O}(l) \rightarrow \text{H}_3\text{O}^+(aq) + \text{HSO}_4^-(aq) (complete ionization, Ka1→∞K_{\text{a1}} \to \infty)
    • HSO4−(aq)+H2O(l)⇌H3O+(aq)+SO42−(aq)\text{HSO}_4^-(aq) + \text{H}_2\text{O}(l) \rightleftharpoons \text{H}_3\text{O}^+(aq) + \text{SO}_4^{2-}(aq) (Ka2=1.2×10−2K_{\text{a2}} = 1.2 \times 10^{-2})

    For moderately concentrated H2SO4\text{H}_2\text{SO}_4 solutions (greater than 0.1 M0.1\text{ M}), [H3O+][\text{H}_3\text{O}^+] is predominantly determined by the first step. However, at lower concentrations, the second dissociation contributes significantly to total [H3O+][\text{H}_3\text{O}^+] and must be solved using an equilibrium expression.

    Amphiprotic Salts

    Intermediate ions such as hydrogen carbonate (HCO3−\text{HCO}_3^-) or dihydrogen phosphate (H2PO4−\text{H}_2\text{PO}_4^-) are amphiprotic—they can act either as an acid (donating a proton) or as a base (accepting a proton). For an amphiprotic intermediate HA−\text{HA}^-, the approximate pH of its salt solution is independent of initial concentration (provided the solution is reasonably concentrated) and is given by:

    pH≈pKa1+pKa22\text{pH} \approx \frac{\text{p}K_{\text{a1}} + \text{p}K_{\text{a2}}}{2}