13/14 Acid–Base and Solubility Equilibria

A progressive guide to acid–base theories, pH and equilibrium calculations, buffers, titrations, and precipitation through solubility equilibria at \(25\,^{\circ}\mathrm{C}\).

13/14 Acid–Base and Solubility Equilibria

Acid–base and solubility chemistry are applications of chemical equilibrium. A forward process and its reverse process continue simultaneously; at equilibrium, they occur at equal rates. Equilibrium calculations connect molecular reactions to measurable quantities such as concentration, pH\mathrm{pH}, titrant volume, and precipitate formation.

Unless otherwise stated, aqueous solutions are assumed to be at 25 ∘C25\,^{\circ}\mathrm{C}, where

Kw=[H3O+][OH−]=1.0×10−14.K_w=[\mathrm{H_3O^+}][\mathrm{OH^-}]=1.0\times10^{-14}.

A useful strategy is to identify the reacting species, write the appropriate equilibrium or stoichiometric relationship, solve using the controlling approximation, and then check whether the result is chemically reasonable.

Takeaway: Equilibrium does not mean that reactions stop; it means that opposing reaction rates are equal.

Three Theories of Acids and Bases

Acid–base definitions become broader as the theory changes.

  • An produces H3O+\mathrm{H_3O^+} in water, while an Arrhenius base produces OH−\mathrm{OH^-}. For example, HCl\mathrm{HCl} reacts with water to form H3O+\mathrm{H_3O^+}, and NaOH\mathrm{NaOH} dissociates to form OH−\mathrm{OH^-}.

  • A donates a proton, and a Brønsted–Lowry base accepts a proton. In NH3+H2O⇌NH4++OH−\mathrm{NH_3+H_2O\rightleftharpoons NH_4^++OH^-}, ammonia accepts a proton and is the base, while water donates a proton and is the acid.

  • A accepts an electron pair, and a Lewis base donates an electron pair. In BF3+NH3→F3B←NH3\mathrm{BF_3+NH_3\rightarrow F_3B\leftarrow NH_3}, BF3\mathrm{BF_3} is the and NH3\mathrm{NH_3} is the Lewis base.

A conjugate acid–base pair differs by one proton. For the general reaction

HA+B⇌A−+HB+,\mathrm{HA+B\rightleftharpoons A^-+HB^+},

HA/A−\mathrm{HA/A^-} and B/HB+\mathrm{B/HB^+} are conjugate pairs. Water is amphiprotic because it can either donate or accept a proton.

Takeaway: Use Arrhenius definitions for ion production in water, Brønsted–Lowry definitions for proton transfer, and Lewis definitions for electron-pair transfer.

Water, pH, and pOH

Water undergoes slight self-ionization:

2H2O(l)⇌H3O+(aq)+OH−(aq).\mathrm{2H_2O(l)\rightleftharpoons H_3O^+(aq)+OH^-(aq)}.

The acidity and basicity scales are defined by

pH=−log⁡[H3O+],pOH=−log⁡[OH−].\mathrm{pH=-\log[H_3O^+]},\qquad \mathrm{pOH=-\log[OH^-]}.

At 25 ∘C25\,^{\circ}\mathrm{C},

pH+pOH=14.00.\mathrm{pH+pOH=14.00}.

A solution is acidic when [H3O+]>[OH−]\mathrm{[H_3O^+]>[OH^-]}, neutral when the concentrations are equal, and basic when [H3O+]<[OH−]\mathrm{[H_3O^+]<[OH^-]}. The neutral value pH=7.00\mathrm{pH=7.00} applies specifically at 25 ∘C25\,^{\circ}\mathrm{C}.

To convert concentration to pH, use the negative logarithm. For [H3O+]=2.5×10−3 M\mathrm{[H_3O^+]=2.5\times10^{-3}\,M},

pH=−log⁡(2.5×10−3)=2.60.\mathrm{pH=-\log(2.5\times10^{-3})=2.60}.

Then pOH=14.00−2.60=11.40\mathrm{pOH=14.00-2.60=11.40}. Conversely, if pH=9.20\mathrm{pH=9.20},

[H3O+]=10−9.20=6.3×10−10 M.\mathrm{[H_3O^+]=10^{-9.20}=6.3\times10^{-10}\,M}.

Because pH is logarithmic, its decimal places indicate the significant figures reported for the ion concentration.

Takeaway: Use KwK_w to connect hydronium and hydroxide concentrations, and use pH+pOH=14.00\mathrm{pH+pOH=14.00} at 25 ∘C25\,^{\circ}\mathrm{C}.

Strong and Weak Acids and Bases

The distinction between strong and weak electrolytes determines whether an equilibrium calculation is needed.

A strong acid or base ionizes essentially completely. For a monoprotic strong acid such as HCl\mathrm{HCl},

[H3O+]≈CHCl.\mathrm{[H_3O^+]\approx C_{HCl}}.

For Ba(OH)2\mathrm{Ba(OH)_2}, each formula unit supplies two hydroxide ions:

[OH−]≈2CBa(OH)2.\mathrm{[OH^-]\approx 2C_{Ba(OH)_2}}.

A weak acid or base ionizes only partially. For a weak acid,

HA+H2O⇌H3O++A−,\mathrm{HA+H_2O\rightleftharpoons H_3O^++A^-},
Ka=[H3O+][A−][HA].K_a=\frac{[\mathrm{H_3O^+}][\mathrm{A^-}]}{[\mathrm{HA}]}.

For a weak base,

B+H2O⇌BH++OH−,\mathrm{B+H_2O\rightleftharpoons BH^++OH^-},
Kb=[BH+][OH−][B].K_b=\frac{[\mathrm{BH^+}][\mathrm{OH^-}]}{[\mathrm{B}]}.

A larger KaK_a indicates a stronger acid, while a larger KbK_b indicates a stronger base. For conjugate pairs at 25 ∘C25\,^{\circ}\mathrm{C},

KaKb=Kw,pKa+pKb=14.00.K_aK_b=K_w,\qquad \mathrm{p}K_a+\mathrm{p}K_b=14.00.

For a weak acid with initial concentration CC, an ICE table gives

Ka=x2C−x,K_a=\frac{x^2}{C-x},

where xx is the equilibrium hydronium concentration produced by ionization. If xx is less than about 5%5\% of CC, use

x≈KaC.x\approx\sqrt{K_aC}.

For 0.100 M0.100\,\mathrm{M} acetic acid with Ka=1.8×10−5K_a=1.8\times10^{-5}, this gives [H3O+]=1.34×10−3 M\mathrm{[H_3O^+]=1.34\times10^{-3}\,M} and pH=2.87\mathrm{pH=2.87}. The percent ionization is 1.34%1.34\%, so the approximation is reasonable.

Takeaway: Strong species are treated primarily by stoichiometry; weak species require an equilibrium expression and a check of any approximation.

Salt

Ions from weak acids and weak bases can react with water. This process is called .

The acetate ion, which is the conjugate base of acetic acid, reacts according to

CH3CO2−+H2O⇌CH3CO2H+OH−.\mathrm{CH_3CO_2^-+H_2O\rightleftharpoons CH_3CO_2H+OH^-}.

Because hydroxide is produced, sodium acetate gives a basic solution. The ammonium ion, which is the conjugate acid of ammonia, reacts according to

NH4++H2O⇌NH3+H3O+.\mathrm{NH_4^++H_2O\rightleftharpoons NH_3+H_3O^+}.

Because hydronium is produced, ammonium chloride gives an acidic solution. A salt such as NaCl\mathrm{NaCl}, formed from a strong acid and a strong base, generally gives a nearly neutral solution because its ions are very weak acid–base reactants.

For a conjugate base and conjugate acid,

Kb=KwKa,Ka=KwKb.K_b=\frac{K_w}{K_a},\qquad K_a=\frac{K_w}{K_b}.

Takeaway: Determine whether a salt solution is acidic or basic by asking whether either ion is the conjugate partner of a weak acid or weak base.

Buffers and pH Control

A buffer contains appreciable amounts of a weak acid and its conjugate base, or a weak base and its conjugate acid. It resists large pH changes because added strong acid or base is consumed by one of the buffer components.

For an acidic buffer, added acid reacts mainly with the conjugate base:

A−+H3O+→HA+H2O.\mathrm{A^-+H_3O^+\rightarrow HA+H_2O}.

Added base reacts mainly with the weak acid:

HA+OH−→A−+H2O.\mathrm{HA+OH^-\rightarrow A^-+H_2O}.

The is

pH=pKa+log⁡([A−][HA]).\mathrm{pH=p}K_a+\log\left(\frac{[\mathrm{A^-}]}{[\mathrm{HA}]}\right).

When both components occupy the same solution, mole ratios can replace concentration ratios. Buffer effectiveness is greatest when [A−]=[HA]\mathrm{[A^-]=[HA]}, because then pH=pKa\mathrm{pH=p}K_a. To design a buffer, choose a weak acid with a pKa\mathrm{p}K_a near the desired pH and then adjust the conjugate-base-to-acid ratio.

For a buffer containing 0.200.20 mol of acetic acid and 0.300.30 mol of acetate with pKa=4.76\mathrm{p}K_a=4.76,

pH=4.76+log⁡(0.300.20)=4.94.\mathrm{pH=4.76+\log\left(\frac{0.30}{0.20}\right)=4.94}.

If 0.0100.010 mol of strong acid is added, the acetate amount becomes 0.2900.290 mol and the acid amount becomes 0.2100.210 mol. The new pH is approximately 4.904.90, illustrating the buffer’s resistance to a large change.

Takeaway: A buffer changes the ratio of conjugate partners rather than allowing the added strong reagent to change the pH dramatically.

Acid–Base Titrations

A titration determines an unknown concentration by reacting an analyte with a solution of known concentration, called the titrant. The occurs when the reactants have combined in stoichiometrically equivalent amounts. The endpoint is the observed indicator or instrumental signal and should be close to the .

For a 1:1 reaction such as

HA+OH−→A−+H2O,\mathrm{HA+OH^-\rightarrow A^-+H_2O},
nHA=nOH−andMacidVacid=MbaseVbase.n_{\mathrm{HA}}=n_{\mathrm{OH^-}}\quad\text{and}\quad M_{\mathrm{acid}}V_{\mathrm{acid}}=M_{\mathrm{base}}V_{\mathrm{base}}.

For a strong-acid–strong-base titration, calculate pH from the initial strong reagent before titrant is added, use excess moles divided by total volume before or after equivalence, and expect approximately pH=7.00\mathrm{pH=7.00} at equivalence at 25 ∘C25\,^{\circ}\mathrm{C}.

For example, titrating 25.00 mL25.00\,\mathrm{mL} of 0.100 M0.100\,\mathrm{M} HCl\mathrm{HCl} with 30.00 mL30.00\,\mathrm{mL} of 0.100 M0.100\,\mathrm{M} NaOH\mathrm{NaOH} leaves 0.000500 mol0.000500\,\mathrm{mol} of excess hydroxide in 0.05500 L0.05500\,\mathrm{L}. Thus [OH−]=9.09×10−3 M\mathrm{[OH^-]=9.09\times10^{-3}\,M}, pOH=2.04\mathrm{pOH=2.04}, and pH=11.96\mathrm{pH=11.96}.

Weak-acid–strong-base titrations contain a buffer region before equivalence. At the half-, equal amounts of weak acid and conjugate base are present, so pH=pKa\mathrm{pH=p}K_a. At equivalence, the conjugate base hydrolyzes and the pH is greater than 77. Weak-base–strong-acid titrations are analogous, but their half- satisfies pOH=pKb\mathrm{pOH=p}K_b and their is acidic.

Choose an indicator whose color-change interval overlaps the steep portion of the titration curve near equivalence.

Takeaway: Divide a titration into regions, identify the controlling reaction in each region, and use stoichiometry before equilibrium calculations whenever a strong reagent is in excess.

Solubility Equilibria and Precipitation

A sparingly soluble ionic solid establishes an equilibrium between the solid and its dissolved ions. For silver chloride,

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

The is

Ksp=[Ag+][Cl−].K_{sp}=[\mathrm{Ag^+}][\mathrm{Cl^-}].

For a general salt,

MpXq(s)⇌pMm+(aq)+qXn−(aq),\mathrm{M_pX_q(s)\rightleftharpoons pM^{m+}(aq)+qX^{n-}(aq)},
Ksp=[Mm+]p[Xn−]q.K_{sp}=[\mathrm{M^{m+}}]^p[\mathrm{X^{n-}}]^q.

The stoichiometric coefficients determine the exponents. For CaF2\mathrm{CaF_2}, if the molar solubility is ss, then [Ca2+]=s\mathrm{[Ca^{2+}]=s} and [F−]=2s\mathrm{[F^-]=2s}, so

Ksp=s(2s)2=4s3.K_{sp}=s(2s)^2=4s^3.

To predict precipitation after mixing solutions, calculate the ion product QspQ_{sp} from concentrations immediately after dilution:

  • If Qsp<KspQ_{sp}<K_{sp}, the solution is unsaturated and precipitation is not expected.

  • If Qsp=KspQ_{sp}=K_{sp}, the solution is saturated and at equilibrium.

  • If Qsp>KspQ_{sp}>K_{sp}, precipitation is thermodynamically favored.

For [Ag+]=[Cl−]=1.0×10−4 M\mathrm{[Ag^+]=[Cl^-]=1.0\times10^{-4}\,M}, Qsp=1.0×10−8Q_{sp}=1.0\times10^{-8}. With Ksp(AgCl)=1.6×10−10K_{sp}(\mathrm{AgCl})=1.6\times10^{-10}, Qsp>KspQ_{sp}>K_{sp}, so silver chloride precipitates.

Takeaway: Always use post-mixing concentrations and compare QspQ_{sp} directly with KspK_{sp}.

Factors Affecting Solubility and Measurement

Solubility can change when other chemical equilibria alter the concentration of a dissolved ion.

The decreases the solubility of a solid when an ion already present in its dissolution equilibrium is added. For silver chloride,

AgCl(s)⇌Ag++Cl−,\mathrm{AgCl(s)\rightleftharpoons Ag^++Cl^-},

adding excess Cl−\mathrm{Cl^-} shifts the equilibrium toward solid AgCl\mathrm{AgCl}.

Acid can increase the solubility of salts containing basic anions. Carbonate reacts with hydronium:

CO32−+H3O+⇌HCO3−+H2O.\mathrm{CO_3^{2-}+H_3O^+\rightleftharpoons HCO_3^-+H_2O}.

This removes carbonate from solution and shifts the dissolution of a carbonate such as calcium carbonate toward additional dissolution.

In selective precipitation, two ions are exposed to a common precipitating ion. The compound with the smaller effective solubility generally begins to precipitate first, allowing the ions to be separated if the conditions are suitable.

For reliable quantitative work, account for dilution after mixing, calibrate pH meters, read buret menisci at eye level, add titrant slowly near the endpoint, use replicate trials, and report appropriate significant figures and uncertainty.

Takeaway: Le Châtelier’s principle links acid effects and common-ion effects to changes in solubility, while careful measurement determines whether the predicted change can be observed quantitatively.