Common-ion effect Knowledge-Based Study

Chemistry · Chemical Equilibrium · Chemistry · Solubility Equilibria

Chemistry topic explanations on Common-ion effect.

Study notes

  1. In aqueous solution chemistry, the common-ion effect refers to the suppression of the ionization or dissolution of a compound when an additional soluble substance containing a shared ion is introduced into the mixture.

    When applied to sparingly soluble salts, this phenomenon is directly governed by Le Chatelier's principle. Consider the dynamic dissolution equilibrium of a generic sparingly soluble ionic solid, MpXq(s)\text{M}_p\text{X}_q(s):

    MpXq(s)⇌p Mn+(aq)+q Xm−(aq)\text{M}_p\text{X}_q(s) \rightleftharpoons p\,\text{M}^{n+}(aq) + q\,\text{X}^{m-}(aq)

    The corresponding solubility product constant expression is:

    Ksp=[Mn+]p[Xm−]qK_{\text{sp}} = [\text{M}^{n+}]^p [\text{X}^{m-}]^q

    Because KspK_{\text{sp}} depends solely on temperature, the product of the ionic concentrations (raised to their stoichiometric powers) in a saturated solution remains constant. If a strong electrolyte providing either Mn+\text{M}^{n+} or Xm−\text{X}^{m-} is added, the system shifts toward the reactants (the solid phase) to reduce the concentration of the added ion, resulting in decreased molar solubility.

    Understanding the common-ion effect qualitatively requires tracking which ion is introduced and identifying the direction in which the solubility equilibrium shifts.

    Example: Silver Chloride

    Silver chloride (AgCl\text{AgCl}) is a sparingly soluble salt that dissolves according to the equilibrium:

    AgCl(s)⇌Ag+(aq)+Cl−(aq)\text{AgCl}(s) \rightleftharpoons \text{Ag}^+(aq) + \text{Cl}^-(aq)

    • In pure water: Dissolution yields equimolar amounts of silver ions and chloride ions, such that [Ag+]=[Cl−]=s[\text{Ag}^+] = [\text{Cl}^-] = s, where ss is the molar solubility.
    • In a solution containing NaCl\text{NaCl}: Sodium chloride completely dissociates into Na+(aq)\text{Na}^+(aq) and Cl−(aq)\text{Cl}^-(aq). The extra Cl−\text{Cl}^- acts as a common ion.
    • Equilibrium response: The presence of additional Cl−\text{Cl}^- increases the reaction quotient QQ above KspK_{\text{sp}}. To restore equilibrium, Ag+\text{Ag}^+ combines with excess Cl−\text{Cl}^- to precipitate as solid AgCl\text{AgCl}, driving the equilibrium to the left.

    Consequently, the concentration of free Ag+\text{Ag}^+ in solution decreases, and the molar solubility of AgCl\text{AgCl} is noticeably lower in a solution containing a chloride source than in pure water.

    To determine the molar solubility quantitatively in the presence of a common ion, an equilibrium table (ICE approach) is constructed, taking the initial concentration of the common ion into account.

    Worked Example

    Calculate the molar solubility of calcium fluoride, CaF2\text{CaF}_2 (Ksp=3.9×10−11K_{\text{sp}} = 3.9 \times 10^{-11}), in a 0.10 M solution of sodium fluoride (NaF\text{NaF}).

    First, write the dissolution equilibrium:

    CaF2(s)⇌Ca2+(aq)+2 F−(aq)\text{CaF}_2(s) \rightleftharpoons \text{Ca}^{2+}(aq) + 2\,\text{F}^-(aq)

    Sodium fluoride dissociates completely:

    NaF(aq)→Na+(aq)+F−(aq)\text{NaF}(aq) \rightarrow \text{Na}^+(aq) + \text{F}^-(aq)

    Therefore, the initial fluoride concentration from the strong electrolyte is [F−]0=0.10 M[\text{F}^-]_0 = 0.10\text{ M}.

    • Initial: [Ca2+]=0[\text{Ca}^{2+}] = 0, [F−]=0.10 M[\text{F}^-] = 0.10\text{ M}
    • Change: [Ca2+]=+s′[\text{Ca}^{2+}] = +s', [F−]=+2s′[\text{F}^-] = +2s'
    • Equilibrium: [Ca2+]=s′[\text{Ca}^{2+}] = s', [F−]=0.10+2s′[\text{F}^-] = 0.10 + 2s'

    Substitute these values into the solubility product expression:

    Ksp=[Ca2+][F−]2=(s′)(0.10+2s′)2=3.9×10−11K_{\text{sp}} = [\text{Ca}^{2+}][\text{F}^-]^2 = (s')(0.10 + 2s')^2 = 3.9 \times 10^{-11}

    Because KspK_{\text{sp}} is very small, we make the approximation that 2s′≪0.102s' \ll 0.10, which simplifies the expression:

    (s′)(0.10)2≈3.9×10−11(s')(0.10)^2 \approx 3.9 \times 10^{-11}

    s′(0.010)=3.9×10−11  ⟹  s′=3.9×10−9 Ms'(0.010) = 3.9 \times 10^{-11} \implies s' = 3.9 \times 10^{-9}\text{ M}

    For comparison, in pure water, the solubility of CaF2\text{CaF}_2 is given by 4s3=3.9×10−114s^3 = 3.9 \times 10^{-11}, yielding s≈2.1×10−4 Ms \approx 2.1 \times 10^{-4}\text{ M}. The presence of 0.10 M F−\text{F}^- reduces the solubility by several orders of magnitude.

    The common-ion effect plays a crucial role in analytical chemistry, wastewater remediation, and chemical synthesis.

    Selective Precipitation

    When a solution contains multiple metal cations, adding a common counterion gradually allows chemists to precipitate one ion while leaving others in solution. Precipitation occurs when the ion product quotient QQ exceeds KspK_{\text{sp}}:

    • The compound with the smaller concentration threshold for precipitation precipitates first.
    • By carefully controlling the common-ion concentration (such as hydroxide, sulfate, or sulfide ions), distinct separation of cations can be achieved.

    Gravimetric Analysis

    In gravimetric determinations, an analyte is precipitated as an insoluble compound. To minimize losses caused by incomplete precipitation, an excess of the precipitating agent (a source of the common ion) is added. This shifts the solubility equilibrium toward the solid phase, ensuring that nearly all target ions leave the solution phase and are captured quantitatively on the filter.