Example Calculate the solubility of A g C l \mathrm{AgCl} AgCl in 0.10 M 0.10\mathrm{ M} 0.10 M N a C l \mathrm{NaCl} NaCl .
K_`\{sp}` = [\mathrm{Ag}^+][\mathrm{Cl}^-] = s \times 0.10 S = 1.8 × 10 − 10 0.10 = 1.8 × 10 − 9 m o l / L S = \frac{1.8 \times 10^{-10}}{0.10} = 1.8 \times 10^{-9}\mathrm{ mol/L} S = 0.10 1.8 × 1 0 − 10 = 1.8 × 1 0 − 9 mol/L Compared to pure water (1.3 × 10 − 5 m o l / L 1.3 \times 10^{-5}\mathrm{ mol/L} 1.3 × 1 0 − 5 mol/L ), the solubility decreased by a factor Of about 7000 7000 7000 .
A precipitate forms when the ion product exceeds K s p K_{sp} K s p :
Q = [ M y + ] x [ A x − ] y Q = [\mathrm{M}^{y+}]^x[\mathrm{A}^{x-}]^y Q = [ M y + ] x [ A x − ] y Condition Result Q < K s p Q \lt K_{sp} Q < K s p No precipitate (unsaturated) Q = K s p Q = K_{sp} Q = K s p Saturated, at equilibrium Q > K s p Q \gt K_{sp} Q > K s p Precipitate forms
K s p K_{sp} K s p expressions do not include the concentration of the solid.Solids and pure liquids are excluded from equilibrium expressions. The common ion effect does not change K s p K_{sp} K s p itself — it shifts the equilibrium position. Problem 1 Calculate the p H \mathrm{pH} pH of a buffer prepared by mixing 100 m L 100\mathrm{ mL} 100 mL of 0.20 M 0.20\mathrm{ M} 0.20 M C H 3 C O O H \mathrm{CH}_3\mathrm{COOH} CH 3 COOH with 50 m L 50\mathrm{ mL} 50 mL of 0.20 M 0.20\mathrm{ M} 0.20 M N a O H \mathrm{NaOH} NaOH . (p K a = 4.76 \mathrm{p}K_a = 4.76 p K a = 4.76 )
Solution:
Moles of C H 3 C O O H = 0.100 × 0.20 = 0.020 m o l \mathrm{CH}_3\mathrm{COOH} = 0.100 \times 0.20 = 0.020\mathrm{ mol} CH 3 COOH = 0.100 × 0.20 = 0.020 mol
Moles of N a O H = 0.050 × 0.20 = 0.010 m o l \mathrm{NaOH} = 0.050 \times 0.20 = 0.010\mathrm{ mol} NaOH = 0.050 × 0.20 = 0.010 mol
N a O H \mathrm{NaOH} NaOH neutralises half the acid:
N ( C H 3 C O O H ) r e m a i n i n g = 0.020 − 0.010 = 0.010 m o l N(\mathrm{CH}_3\mathrm{COOH})_{\mathrm{remaining}} = 0.020 - 0.010 = 0.010\mathrm{ mol} N ( CH 3 COOH ) remaining = 0.020 − 0.010 = 0.010 mol N ( C H 3 C O O − ) f o r m e d = 0.010 m o l N(\mathrm{CH}_3\mathrm{COO}^-)_{\mathrm{formed}} = 0.010\mathrm{ mol} N ( CH 3 COO − ) formed = 0.010 mol Total volume = 150 m L = 0.150 L = 150\mathrm{ mL} = 0.150\mathrm{ L} = 150 mL = 0.150 L :
[ C H 3 C O O H ] = 0.010 0.150 = 0.0667 M [\mathrm{CH}_3\mathrm{COOH}] = \frac{0.010}{0.150} = 0.0667\mathrm{ M} [ CH 3 COOH ] = 0.150 0.010 = 0.0667 M [ C H 3 C O O − ] = 0.010 0.150 = 0.0667 M [\mathrm{CH}_3\mathrm{COO}^-] = \frac{0.010}{0.150} = 0.0667\mathrm{ M} [ CH 3 COO − ] = 0.150 0.010 = 0.0667 M p H = 4.76 + log 0.0667 0.0667 = 4.76 + 0 = 4.76 \mathrm{pH} = 4.76 + \log\frac{0.0667}{0.0667} = 4.76 + 0 = 4.76 pH = 4.76 + log 0.0667 0.0667 = 4.76 + 0 = 4.76 Problem 2 Will a precipitate form when 50.0 m L 50.0\mathrm{ mL} 50.0 mL of 1.0 × 10 − 4 M 1.0 \times 10^{-4}\mathrm{ M} 1.0 × 1 0 − 4 M A g N O 3 \mathrm{AgNO}_3 AgNO 3 Is mixed with 50.0 m L 50.0\mathrm{ mL} 50.0 mL of 1.0 × 10 − 4 M 1.0 \times 10^{-4}\mathrm{ M} 1.0 × 1 0 − 4 M N a C l \mathrm{NaCl} NaCl ? (K s p ( A g C l ) = 1.8 × 10 − 10 K_{sp}(\mathrm{AgCl}) = 1.8 \times 10^{-10} K s p ( AgCl ) = 1.8 × 1 0 − 10 )
Solution:
Total volume = 100 m L = 100\mathrm{ mL} = 100 mL . Diluted concentrations:
[ A g + ] = 0.050 × 1.0 × 10 − 4 0.100 = 5.0 × 10 − 5 M [\mathrm{Ag}^+] = \frac{0.050 \times 1.0 \times 10^{-4}}{0.100} = 5.0 \times 10^{-5}\mathrm{ M} [ Ag + ] = 0.100 0.050 × 1.0 × 1 0 − 4 = 5.0 × 1 0 − 5 M [ C l − ] = 0.050 × 1.0 × 10 − 4 0.100 = 5.0 × 10 − 5 M [\mathrm{Cl}^-] = \frac{0.050 \times 1.0 \times 10^{-4}}{0.100} = 5.0 \times 10^{-5}\mathrm{ M} [ Cl − ] = 0.100 0.050 × 1.0 × 1 0 − 4 = 5.0 × 1 0 − 5 M Q = ( 5.0 × 10 − 5 ) 2 = 2.5 × 10 − 9 Q = (5.0 \times 10^{-5})^2 = 2.5 \times 10^{-9} Q = ( 5.0 × 1 0 − 5 ) 2 = 2.5 × 1 0 − 9 Since Q = 2.5 × 10 − 9 > K s p = 1.8 × 10 − 10 Q = 2.5 \times 10^{-9} \gt K_{sp} = 1.8 \times 10^{-10} Q = 2.5 × 1 0 − 9 > K s p = 1.8 × 1 0 − 10 A precipitate of A g C l \mathrm{AgCl} AgCl Will form.
Problem 3 Calculate the p H \mathrm{pH} pH of 0.050 M 0.050\mathrm{ M} 0.050 M N H 3 \mathrm{NH}_3 NH 3 (K b = 1.8 × 10 − 5 K_b = 1.8 \times 10^{-5} K b = 1.8 × 1 0 − 5 ).
Solution:
N H 3 + H 2 O ⇌ N H 4 + + O H − \mathrm{NH}_3 + \mathrm{H}_2\mathrm{O} \rightleftharpoons \mathrm{NH}_4^+ + \mathrm{OH}^- NH 3 + H 2 O ⇌ NH 4 + + OH − K b = [ N H 4 + ] [ O H − ] [ N H 3 ] = x 2 0.050 − x K_b = \frac{[\mathrm{NH}_4^+][\mathrm{OH}^-]}{[\mathrm{NH}_3]} = \frac{x^2}{0.050 - x} K b = [ NH 3 ] [ NH 4 + ] [ OH − ] = 0.050 − x x 2 Approximation: x = 1.8 × 10 − 5 × 0.050 = 9.0 × 10 − 7 = 9.5 × 10 − 4 x = \sqrt{1.8 \times 10^{-5} \times 0.050} = \sqrt{9.0 \times 10^{-7}} = 9.5 \times 10^{-4} x = 1.8 × 1 0 − 5 × 0.050 = 9.0 × 1 0 − 7 = 9.5 × 1 0 − 4
Check: 9.5 × 10 − 4 / 0.050 = 1.9 % < 5 % 9.5 \times 10^{-4} / 0.050 = 1.9\% \lt 5\% 9.5 × 1 0 − 4 /0.050 = 1.9% < 5% . Valid.
p O H = − log ( 9.5 × 10 − 4 ) = 3.02 \mathrm{pOH} = -\log(9.5 \times 10^{-4}) = 3.02 pOH = − log ( 9.5 × 1 0 − 4 ) = 3.02 p H = 14.00 − 3.02 = 10.98 \mathrm{pH} = 14.00 - 3.02 = 10.98 pH = 14.00 − 3.02 = 10.98 Problem 4 Explain why adding N H 4 C l \mathrm{NH}_4\mathrm{Cl} NH 4 Cl to an N H 3 \mathrm{NH}_3 NH 3 solution decreases the p H \mathrm{pH} pH .
Solution:
N H 4 C l \mathrm{NH}_4\mathrm{Cl} NH 4 Cl dissociates completely to give N H 4 + \mathrm{NH}_4^+ NH 4 + The conjugate acid of N H 3 \mathrm{NH}_3 NH 3 . This is the common ion effect :
N H 3 + H 2 O ⇌ N H 4 + + O H − \mathrm{NH}_3 + \mathrm{H}_2\mathrm{O} \rightleftharpoons \mathrm{NH}_4^+ + \mathrm{OH}^- NH 3 + H 2 O ⇌ NH 4 + + OH − Adding N H 4 + \mathrm{NH}_4^+ NH 4 + shifts the equilibrium to the left (Le Chatelier’s principle), decreasing [ O H − ] [\mathrm{OH}^-] [ OH − ] and therefore increasing [ H + ] [\mathrm{H}^+] [ H + ] Which lowers the p H \mathrm{pH} pH .
Worked Example: pH of a very dilute strong acid
Calculate the p H \mathrm{pH} pH of 1.0 × 10 − 8 M 1.0 \times 10^{-8}\mathrm{ M} 1.0 × 1 0 − 8 M H C l \mathrm{HCl} HCl at 25 ° C 25\degree\mathrm{C} 25° C .
Solution At this concentration, the contribution from water autoionization ([ H + ] = 10 − 7 M [\mathrm{H}^+] = 10^{-7}\mathrm{ M} [ H + ] = 1 0 − 7 M ) is Significant and cannot be ignored. Let x = [ O H − ] x = [\mathrm{OH}^-] x = [ OH − ] from water autoionization:
[ H + ] t o t a l = 1.0 × 10 − 8 + x [\mathrm{H}^+]_{\mathrm{total}} = 1.0 \times 10^{-8} + x [ H + ] total = 1.0 × 1 0 − 8 + x
K w = [ H + ] [ O H − ] = ( 1.0 × 10 − 8 + x ) ( x ) = 1.0 × 10 − 14 K_w = [\mathrm{H}^+][\mathrm{OH}^-] = (1.0 \times 10^{-8} + x)(x) = 1.0 \times 10^{-14} K w = [ H + ] [ OH − ] = ( 1.0 × 1 0 − 8 + x ) ( x ) = 1.0 × 1 0 − 14
x 2 + 1.0 × 10 − 8 x − 1.0 × 10 − 14 = 0 x^2 + 1.0 \times 10^{-8}x - 1.0 \times 10^{-14} = 0 x 2 + 1.0 × 1 0 − 8 x − 1.0 × 1 0 − 14 = 0
Using the quadratic formula:
x = − 1.0 × 10 − 8 + ( 1.0 × 10 − 8 ) 2 + 4 ( 1.0 × 10 − 14 ) 2 = − 1.0 × 10 − 8 + 2.00 × 10 − 7 2 = 9.5 × 10 − 8 x = \frac{-1.0 \times 10^{-8} + \sqrt{(1.0 \times 10^{-8})^2 + 4(1.0 \times 10^{-14})}}{2} = \frac{-1.0 \times 10^{-8} + 2.00 \times 10^{-7}}{2} = 9.5 \times 10^{-8} x = 2 − 1.0 × 1 0 − 8 + ( 1.0 × 1 0 − 8 ) 2 + 4 ( 1.0 × 1 0 − 14 ) = 2 − 1.0 × 1 0 − 8 + 2.00 × 1 0 − 7 = 9.5 × 1 0 − 8
[ H + ] t o t a l = 1.0 × 10 − 8 + 9.5 × 10 − 8 = 1.05 × 10 − 7 M [\mathrm{H}^+]_{\mathrm{total}} = 1.0 \times 10^{-8} + 9.5 \times 10^{-8} = 1.05 \times 10^{-7}\mathrm{ M} [ H + ] total = 1.0 × 1 0 − 8 + 9.5 × 1 0 − 8 = 1.05 × 1 0 − 7 M
p H = − log ( 1.05 × 10 − 7 ) = 6.98 \mathrm{pH} = -\log(1.05 \times 10^{-7}) = 6.98 pH = − log ( 1.05 × 1 0 − 7 ) = 6.98
The p H \mathrm{pH} pH is close to 7 but slightly acidic, as expected for a very dilute strong acid. Ignoring Water autoionization would give the incorrect result p H = 8.00 \mathrm{pH} = 8.00 pH = 8.00 (a basic p H \mathrm{pH} pH from Adding acid), which violates chemical intuition.
Worked Example: pH at the equivalence point of a weak acid—strong base titration
Calculate the p H \mathrm{pH} pH at the equivalence point when 25.0 m L 25.0\mathrm{ mL} 25.0 mL of 0.100 M 0.100\mathrm{ M} 0.100 M C H 3 C O O H \mathrm{CH}_3\mathrm{COOH} CH 3 COOH (K a = 1.8 × 10 − 5 K_a = 1.8 \times 10^{-5} K a = 1.8 × 1 0 − 5 ) is titrated with 0.100 M 0.100\mathrm{ M} 0.100 M N a O H \mathrm{NaOH} NaOH .
Solution At the equivalence point, all of the weak acid has been converted to its conjugate base:
n ( C H 3 C O O H ) = 0.0250 × 0.100 = 0.00250 m o l n(\mathrm{CH}_3\mathrm{COOH}) = 0.0250 \times 0.100 = 0.00250\mathrm{ mol} n ( CH 3 COOH ) = 0.0250 × 0.100 = 0.00250 mol
V ( N a O H ) = 0.00250 0.100 = 25.0 m L V(\mathrm{NaOH}) = \frac{0.00250}{0.100} = 25.0\mathrm{ mL} V ( NaOH ) = 0.100 0.00250 = 25.0 mL
V t o t a l = 50.0 m L = 0.0500 L V_{\mathrm{total}} = 50.0\mathrm{ mL} = 0.0500\mathrm{ L} V total = 50.0 mL = 0.0500 L
[ C H 3 C O O − ] = 0.00250 0.0500 = 0.0500 M [\mathrm{CH}_3\mathrm{COO}^-] = \frac{0.00250}{0.0500} = 0.0500\mathrm{ M} [ CH 3 COO − ] = 0.0500 0.00250 = 0.0500 M
The conjugate base hydrolyses water:
C H 3 C O O − + H 2 O ⇌ C H 3 C O O H + O H − \mathrm{CH}_3\mathrm{COO}^- + \mathrm{H}_2\mathrm{O} \rightleftharpoons \mathrm{CH}_3\mathrm{COOH} + \mathrm{OH}^- CH 3 COO − + H 2 O ⇌ CH 3 COOH + OH −
K b = K w K a = 1.0 × 10 − 14 1.8 × 10 − 5 = 5.56 × 10 − 10 K_b = \frac{K_w}{K_a} = \frac{1.0 \times 10^{-14}}{1.8 \times 10^{-5}} = 5.56 \times 10^{-10} K b = K a K w = 1.8 × 1 0 − 5 1.0 × 1 0 − 14 = 5.56 × 1 0 − 10
[ O H − ] = K b × [ C H 3 C O O − ] = 5.56 × 10 − 10 × 0.0500 = 5.27 × 10 − 6 M [\mathrm{OH}^-] = \sqrt{K_b \times [\mathrm{CH}_3\mathrm{COO}^-]} = \sqrt{5.56 \times 10^{-10} \times 0.0500} = 5.27 \times 10^{-6}\mathrm{ M} [ OH − ] = K b × [ CH 3 COO − ] = 5.56 × 1 0 − 10 × 0.0500 = 5.27 × 1 0 − 6 M
p O H = − log ( 5.27 × 10 − 6 ) = 5.28 \mathrm{pOH} = -\log(5.27 \times 10^{-6}) = 5.28 pOH = − log ( 5.27 × 1 0 − 6 ) = 5.28
p H = 14.00 − 5.28 = 8.72 \mathrm{pH} = 14.00 - 5.28 = 8.72 pH = 14.00 − 5.28 = 8.72
The equivalence point is basic because the conjugate base of a weak acid is itself a weak base. Phenolphthalein (transition range 8.3—10.0) is a suitable indicator. Bromothymol blue (6.0—7.6) would change colour Before reaching the equivalence point and would give a systematically low titre reading.
Worked Example: Selective precipitation using K s p K_{sp} K s p
A solution contains 0.020 M 0.020\mathrm{ M} 0.020 M C l − \mathrm{Cl}^- Cl − and 0.020 M 0.020\mathrm{ M} 0.020 M C r O 4 2 − \mathrm{CrO}_4^{2-} CrO 4 2 − . Solid A g N O 3 \mathrm{AgNO}_3 AgNO 3 is added gradually. K s p ( A g C l ) = 1.8 × 10 − 10 K_{sp}(\mathrm{AgCl}) = 1.8 \times 10^{-10} K s p ( AgCl ) = 1.8 × 1 0 − 10 K s p ( A g 2 C r O 4 ) = 1.1 × 10 − 12 K_{sp}(\mathrm{Ag}_2\mathrm{CrO}_4) = 1.1 \times 10^{-12} K s p ( Ag 2 CrO 4 ) = 1.1 × 1 0 − 12 . Determine which salt precipitates first, the [ A g + ] [\mathrm{Ag}^+] [ Ag + ] at which precipitation begins, and the [ A g + ] [\mathrm{Ag}^+] [ Ag + ] at which the second salt begins To precipitate.
Solution Step 1: Calculate the threshold [ A g + ] [\mathrm{Ag}^+] [ Ag + ] for each salt.
For A g C l \mathrm{AgCl} AgCl :
[ A g + ] = K s p [ C l − ] = 1.8 × 10 − 10 0.020 = 9.0 × 10 − 9 M [\mathrm{Ag}^+] = \frac{K_{sp}}{[\mathrm{Cl}^-]} = \frac{1.8 \times 10^{-10}}{0.020} = 9.0 \times 10^{-9}\mathrm{ M} [ Ag + ] = [ Cl − ] K s p = 0.020 1.8 × 1 0 − 10 = 9.0 × 1 0 − 9 M
For A g 2 C r O 4 \mathrm{Ag}_2\mathrm{CrO}_4 Ag 2 CrO 4 :
[ A g + ] = K s p [ C r O 4 2 − ] = 1.1 × 10 − 12 0.020 = 7.4 × 10 − 6 M [\mathrm{Ag}^+] = \sqrt{\frac{K_{sp}}{[\mathrm{CrO}_4^{2-}]}} = \sqrt{\frac{1.1 \times 10^{-12}}{0.020}} = 7.4 \times 10^{-6}\mathrm{ M} [ Ag + ] = [ CrO 4 2 − ] K s p = 0.020 1.1 × 1 0 − 12 = 7.4 × 1 0 − 6 M
Step 2: Identify which precipitates first.
A g C l \mathrm{AgCl} AgCl precipitates first since it requires a lower [ A g + ] [\mathrm{Ag}^+] [ Ag + ] (9.0 × 10 − 9 M 9.0 \times 10^{-9}\mathrm{ M} 9.0 × 1 0 − 9 M Vs 7.4 × 10 − 6 M 7.4 \times 10^{-6}\mathrm{ M} 7.4 × 1 0 − 6 M ).
Step 3: Calculate [ C l − ] [\mathrm{Cl}^-] [ Cl − ] remaining when A g 2 C r O 4 \mathrm{Ag}_2\mathrm{CrO}_4 Ag 2 CrO 4 begins to precipitate.
When [ A g + ] = 7.4 × 10 − 6 M [\mathrm{Ag}^+] = 7.4 \times 10^{-6}\mathrm{ M} [ Ag + ] = 7.4 × 1 0 − 6 M :
[ C l − ] r e m a i n i n g = K s p [ A g + ] = 1.8 × 10 − 10 7.4 × 10 − 6 = 2.4 × 10 − 5 M [\mathrm{Cl}^-]_{\mathrm{remaining}} = \frac{K_{sp}}{[\mathrm{Ag}^+]} = \frac{1.8 \times 10^{-10}}{7.4 \times 10^{-6}} = 2.4 \times 10^{-5}\mathrm{ M} [ Cl − ] remaining = [ Ag + ] K s p = 7.4 × 1 0 − 6 1.8 × 1 0 − 10 = 2.4 × 1 0 − 5 M
Fraction of C l − \mathrm{Cl}^- Cl − precipitated: 0.020 − 2.4 × 10 − 5 0.020 × 100 % = 99.9 % \dfrac{0.020 - 2.4 \times 10^{-5}}{0.020} \times 100\% = 99.9\% 0.020 0.020 − 2.4 × 1 0 − 5 × 100% = 99.9%
This analysis underpins Mohr’s method for argentometric determination of chloride: the red colour of A g 2 C r O 4 \mathrm{Ag}_2\mathrm{CrO}_4 Ag 2 CrO 4 appears only after virtually all C l − \mathrm{Cl}^- Cl − has been removed.
Worked Example: Buffer preparation from a weak base
Prepare an N H 3 \mathrm{NH}_3 NH 3 /N H 4 C l \mathrm{NH}_4\mathrm{Cl} NH 4 Cl buffer with p H = 9.50 \mathrm{pH} = 9.50 pH = 9.50 . Given K b ( N H 3 ) = 1.8 × 10 − 5 K_b(\mathrm{NH}_3) = 1.8 \times 10^{-5} K b ( NH 3 ) = 1.8 × 1 0 − 5 . Calculate the mass of N H 4 C l \mathrm{NH}_4\mathrm{Cl} NH 4 Cl (M = 53.49 g / m o l M = 53.49\mathrm{ g/mol} M = 53.49 g/mol ) that must be dissolved in 500 m L 500\mathrm{ mL} 500 mL of 0.200 M 0.200\mathrm{ M} 0.200 M N H 3 \mathrm{NH}_3 NH 3 .
Solution Step 1: Find the p K a \mathrm{p}K_a p K a of the conjugate acid N H 4 + \mathrm{NH}_4^+ NH 4 + .
p K b = − log ( 1.8 × 10 − 5 ) = 4.74 \mathrm{p}K_b = -\log(1.8 \times 10^{-5}) = 4.74 p K b = − log ( 1.8 × 1 0 − 5 ) = 4.74
p K a = 14.00 − 4.74 = 9.26 \mathrm{p}K_a = 14.00 - 4.74 = 9.26 p K a = 14.00 − 4.74 = 9.26
Step 2: Apply the Henderson-Hasselbalch equation.
9.50 = 9.26 + log [ N H 3 ] [ N H 4 + ] 9.50 = 9.26 + \log\frac{[\mathrm{NH}_3]}{[\mathrm{NH}_4^+]} 9.50 = 9.26 + log [ NH 4 + ] [ NH 3 ]
log [ N H 3 ] [ N H 4 + ] = 0.24 \log\frac{[\mathrm{NH}_3]}{[\mathrm{NH}_4^+]} = 0.24 log [ NH 4 + ] [ NH 3 ] = 0.24
[ N H 3 ] [ N H 4 + ] = 10 0.24 = 1.74 \frac{[\mathrm{NH}_3]}{[\mathrm{NH}_4^+]} = 10^{0.24} = 1.74 [ NH 4 + ] [ NH 3 ] = 1 0 0.24 = 1.74
Step 3: Solve for the required [ N H 4 + ] [\mathrm{NH}_4^+] [ NH 4 + ] .
[ N H 4 + ] = 0.200 1.74 = 0.115 M [\mathrm{NH}_4^+] = \frac{0.200}{1.74} = 0.115\mathrm{ M} [ NH 4 + ] = 1.74 0.200 = 0.115 M
Step 4: Calculate the mass of N H 4 C l \mathrm{NH}_4\mathrm{Cl} NH 4 Cl .
n ( N H 4 C l ) = 0.115 × 0.500 = 0.0575 m o l n(\mathrm{NH}_4\mathrm{Cl}) = 0.115 \times 0.500 = 0.0575\mathrm{ mol} n ( NH 4 Cl ) = 0.115 × 0.500 = 0.0575 mol
m ( N H 4 C l ) = 0.0575 × 53.49 = 3.08 g m(\mathrm{NH}_4\mathrm{Cl}) = 0.0575 \times 53.49 = 3.08\mathrm{ g} m ( NH 4 Cl ) = 0.0575 × 53.49 = 3.08 g
Worked Example: Titration curve analysis for a polyprotic acid
25.0 m L 25.0\mathrm{ mL} 25.0 mL of 0.100 M 0.100\mathrm{ M} 0.100 M H 3 P O 4 \mathrm{H}_3\mathrm{PO}_4 H 3 PO 4 (K a 1 = 7.5 × 10 − 3 K_{a1} = 7.5 \times 10^{-3} K a 1 = 7.5 × 1 0 − 3 K a 2 = 6.2 × 10 − 8 K_{a2} = 6.2 \times 10^{-8} K a 2 = 6.2 × 1 0 − 8 , K a 3 = 4.8 × 10 − 13 K_{a3} = 4.8 \times 10^{-13} K a 3 = 4.8 × 1 0 − 13 ) is titrated with 0.100 M 0.100\mathrm{ M} 0.100 M N a O H \mathrm{NaOH} NaOH . Calculate the p H \mathrm{pH} pH at the first and second equivalence points and identify Suitable indicators.
Solution First equivalence point (25.0 m L 25.0\mathrm{ mL} 25.0 mL N a O H \mathrm{NaOH} NaOH added):
All H 3 P O 4 \mathrm{H}_3\mathrm{PO}_4 H 3 PO 4 is converted to H 2 P O 4 − \mathrm{H}_2\mathrm{PO}_4^- H 2 PO 4 − (an amphoteric species).
[ H 2 P O 4 − ] = 0.00250 0.0500 = 0.0500 M [\mathrm{H}_2\mathrm{PO}_4^-] = \frac{0.00250}{0.0500} = 0.0500\mathrm{ M} [ H 2 PO 4 − ] = 0.0500 0.00250 = 0.0500 M
For an amphoteric species, the p H \mathrm{pH} pH is approximately the average of the two relevant p K a \mathrm{p}K_a p K a values:
p H ≈ p K a 1 + p K a 2 2 = 2.12 + 7.21 2 = 4.67 \mathrm{pH} \approx \frac{\mathrm{p}K_{a1} + \mathrm{p}K_{a2}}{2} = \frac{2.12 + 7.21}{2} = 4.67 pH ≈ 2 p K a 1 + p K a 2 = 2 2.12 + 7.21 = 4.67
A suitable indicator: bromocresol green (3.8—5.4) or methyl red (4.4—6.2).
Second equivalence point (50.0 m L 50.0\mathrm{ mL} 50.0 mL N a O H \mathrm{NaOH} NaOH added):
All H 2 P O 4 − \mathrm{H}_2\mathrm{PO}_4^- H 2 PO 4 − is converted to H P O 4 2 − \mathrm{HPO}_4^{2-} HPO 4 2 − (also amphoteric).
[ H P O 4 2 − ] = 0.00250 0.0750 = 0.0333 M [\mathrm{HPO}_4^{2-}] = \frac{0.00250}{0.0750} = 0.0333\mathrm{ M} [ HPO 4 2 − ] = 0.0750 0.00250 = 0.0333 M
p H ≈ p K a 2 + p K a 3 2 = 7.21 + 12.32 2 = 9.76 \mathrm{pH} \approx \frac{\mathrm{p}K_{a2} + \mathrm{p}K_{a3}}{2} = \frac{7.21 + 12.32}{2} = 9.76 pH ≈ 2 p K a 2 + p K a 3 = 2 7.21 + 12.32 = 9.76
A suitable indicator: phenolphthalein (8.3—10.0).
Third equivalence point: Not achievable in aqueous solution because K a 3 K_{a3} K a 3 is too small (4.8 × 10 − 13 4.8 \times 10^{-13} 4.8 × 1 0 − 13 ) for complete neutralisation of the third proton.
Assuming complete dissociation for all diprotic acids : H 2 S O 4 \mathrm{H}_2\mathrm{SO}_4 H 2 SO 4 has a complete first dissociation but a partial second (K a 2 = 1.2 × 10 − 2 K_{a2} = 1.2 \times 10^{-2} K a 2 = 1.2 × 1 0 − 2 ), so [ H + ] ≠ 2 [ a c i d ] [\mathrm{H}^+] \neq 2[\mathrm{acid}] [ H + ] = 2 [ acid ] . For H 2 C O 3 \mathrm{H}_2\mathrm{CO}_3 H 2 CO 3 Both dissociation steps are weak. Always check the magnitude of each K a K_a K a before making simplifying assumptions.
Using p O H = 14 − p H \mathrm{pOH} = 14 - \mathrm{pH} pOH = 14 − pH without specifying temperature : K w = 1.0 × 10 − 14 K_w = 1.0 \times 10^{-14} K w = 1.0 × 1 0 − 14 only at 25 ° C 25\degree\mathrm{C} 25° C . At 37 ° C 37\degree\mathrm{C} 37° C , K w ≈ 2.4 × 10 − 14 K_w \approx 2.4 \times 10^{-14} K w ≈ 2.4 × 1 0 − 14 So p H + p O H = 13.62 \mathrm{pH} + \mathrm{pOH} = 13.62 pH + pOH = 13.62 . Always state the temperature assumption explicitly.
Applying Henderson-Hasselbalch to strong acid—base mixtures : The equation requires a weak acid and its conjugate base. For a strong acid titrated with a strong base, calculate the excess [ H + ] [\mathrm{H}^+] [ H + ] or [ O H − ] [\mathrm{OH}^-] [ OH − ] directly from stoichiometry.
Forgetting dilution when mixing buffer components : When two solutions are combined to make a buffer, the total volume changes. Convert all quantities to moles first, then recalculate concentrations in the combined volume before applying the Henderson-Hasselbalch equation.
Comparing K s p K_{sp} K s p values across different stoichiometries : K s p ( A g C l ) = 1.8 × 10 − 10 K_{sp}(\mathrm{AgCl}) = 1.8 \times 10^{-10} K s p ( AgCl ) = 1.8 × 1 0 − 10 and K s p ( A g 2 C r O 4 ) = 1.1 × 10 − 12 K_{sp}(\mathrm{Ag}_2\mathrm{CrO}_4) = 1.1 \times 10^{-12} K s p ( Ag 2 CrO 4 ) = 1.1 × 1 0 − 12 But A g 2 C r O 4 \mathrm{Ag}_2\mathrm{CrO}_4 Ag 2 CrO 4 is more soluble in water because its K s p K_{sp} K s p expression contains [ A g + ] 2 [\mathrm{Ag}^+]^2 [ Ag + ] 2 . Always calculate molar solubility from K s p K_{sp} K s p before comparing.
Ignoring water autoionization for dilute solutions : When the calculated [ H + ] [\mathrm{H}^+] [ H + ] from the acid or base alone is below 10 − 6 M 10^{-6}\mathrm{ M} 1 0 − 6 M The contribution from water (10 − 7 M 10^{-7}\mathrm{ M} 1 0 − 7 M ) is comparable and must be included via the full quadratic.
Confusing buffer capacity with buffer range : Buffer capacity (total moles of acid or base that can be absorbed) depends on the absolute concentrations of the buffer components, not their ratio. A 0.01 M 0.01\mathrm{ M} 0.01 M buffer at p H = p K a \mathrm{pH} = \mathrm{p}K_a pH = p K a has far less capacity than a 1.0 M 1.0\mathrm{ M} 1.0 M buffer at the same p H \mathrm{pH} pH .
Assuming the 5% rule is always valid : The approximation [ H A ] ≈ c 0 [\mathrm{HA}] \approx c_0 [ HA ] ≈ c 0 fails when K a K_a K a is large relative to c 0 c_0 c 0 . Always verify by computing x / c 0 × 100 % x/c_0 \times 100\% x / c 0 × 100% . If it exceeds 5%, solve the full quadratic.
Using the wrong p K a \mathrm{p}K_a p K a in Henderson-Hasselbalch : When working with a weak base (e.g., N H 3 \mathrm{NH}_3 NH 3 ), use the p K a \mathrm{p}K_a p K a of its conjugate acid (N H 4 + \mathrm{NH}_4^+ NH 4 + ), not the p K b \mathrm{p}K_b p K b of the base itself. The relationship is p K a + p K b = 14.00 \mathrm{p}K_a + \mathrm{p}K_b = 14.00 p K a + p K b = 14.00 .
Assuming the common ion effect changes K s p K_{sp} K s p : Adding a common ion shifts the equilibrium position (decreasing solubility), but K s p K_{sp} K s p itself is a thermodynamic constant that depends only on temperature.
Calculate the p H \mathrm{pH} pH of the solution formed when 15.0 m L 15.0\mathrm{ mL} 15.0 mL of 0.100 M 0.100\mathrm{ M} 0.100 M H 2 S O 4 \mathrm{H}_2\mathrm{SO}_4 H 2 SO 4 is added to 35.0 m L 35.0\mathrm{ mL} 35.0 mL of 0.100 M 0.100\mathrm{ M} 0.100 M N a O H \mathrm{NaOH} NaOH at 25 ° C 25\degree\mathrm{C} 25° C . (K a 2 K_{a2} K a 2 of H S O 4 − \mathrm{HSO}_4^- HSO 4 − = 1.2 × 10 − 2 1.2 \times 10^{-2} 1.2 × 1 0 − 2 .) State all assumptions and justify their validity. [Medium]
A buffer is prepared by dissolving 4.10 g 4.10\mathrm{ g} 4.10 g of sodium ethanoate (C H 3 C O O N a \mathrm{CH}_3\mathrm{COONa} CH 3 COONa , M = 82.03 g / m o l M = 82.03\mathrm{ g/mol} M = 82.03 g/mol ) in 250 m L 250\mathrm{ mL} 250 mL of 0.200 M 0.200\mathrm{ M} 0.200 M ethanoic acid (p K a = 4.76 \mathrm{p}K_a = 4.76 p K a = 4.76 ). (a) Calculate the buffer p H \mathrm{pH} pH . (b) Calculate the new p H \mathrm{pH} pH after adding 5.0 m L 5.0\mathrm{ mL} 5.0 mL of 0.100 M 0.100\mathrm{ M} 0.100 M H C l \mathrm{HCl} HCl . (c) Calculate the percentage change in p H \mathrm{pH} pH and comment on the effectiveness of the buffer. [Medium]
Will a precipitate form when 25.0 m L 25.0\mathrm{ mL} 25.0 mL of 2.0 × 10 − 4 M 2.0 \times 10^{-4}\mathrm{ M} 2.0 × 1 0 − 4 M P b ( N O 3 ) 2 \mathrm{Pb}(\mathrm{NO}_3)_2 Pb ( NO 3 ) 2 is mixed with 25.0 m L 25.0\mathrm{ mL} 25.0 mL of 1.0 × 10 − 3 M 1.0 \times 10^{-3}\mathrm{ M} 1.0 × 1 0 − 3 M N a I \mathrm{NaI} NaI ? K s p ( P b I 2 ) = 7.1 × 10 − 9 K_{sp}(\mathrm{PbI}_2) = 7.1 \times 10^{-9} K s p ( PbI 2 ) = 7.1 × 1 0 − 9 . If a precipitate forms, calculate [ P b 2 + ] [\mathrm{Pb}^{2+}] [ Pb 2 + ] and [ I − ] [\mathrm{I}^-] [ I − ] remaining at equilibrium. [Hard]
20.0 m L 20.0\mathrm{ mL} 20.0 mL of 0.150 M 0.150\mathrm{ M} 0.150 M N H 3 \mathrm{NH}_3 NH 3 (K b = 1.8 × 10 − 5 K_b = 1.8 \times 10^{-5} K b = 1.8 × 1 0 − 5 ) is titrated with 0.150 M 0.150\mathrm{ M} 0.150 M H C l \mathrm{HCl} HCl . Calculate the p H \mathrm{pH} pH at each of the following volumes of H C l \mathrm{HCl} HCl added: (a) 0.0 m L 0.0\mathrm{ mL} 0.0 mL (b) 10.0 m L 10.0\mathrm{ mL} 10.0 mL (c) 20.0 m L 20.0\mathrm{ mL} 20.0 mL (equivalence point), (d) 25.0 m L 25.0\mathrm{ mL} 25.0 mL . Sketch the approximate titration curve and label the buffer region. [Hard]
The solubility of C a F 2 \mathrm{CaF}_2 CaF 2 in pure water is 2.15 × 10 − 4 M 2.15 \times 10^{-4}\mathrm{ M} 2.15 × 1 0 − 4 M at 25 ° C 25\degree\mathrm{C} 25° C . (a) Calculate K s p K_{sp} K s p . (b) Calculate the solubility of C a F 2 \mathrm{CaF}_2 CaF 2 in 0.050 M 0.050\mathrm{ M} 0.050 M C a C l 2 \mathrm{CaCl}_2 CaCl 2 . (c) Determine the maximum concentration of N a F \mathrm{NaF} NaF that can coexist with 0.010 M 0.010\mathrm{ M} 0.010 M C a C l 2 \mathrm{CaCl}_2 CaCl 2 without precipitation. [Medium]
Explain why phenolphthalein is a suitable indicator for the titration of ethanoic acid with sodium hydroxide, but methyl orange is not. Support your answer with a quantitative calculation of the equivalence point p H \mathrm{pH} pH and reference to the transition ranges of both indicators. [Medium]
A student prepares a buffer by mixing 100 m L 100\mathrm{ mL} 100 mL of 0.200 M 0.200\mathrm{ M} 0.200 M C H 3 C O O H \mathrm{CH}_3\mathrm{COOH} CH 3 COOH with 100 m L 100\mathrm{ mL} 100 mL of 0.100 M 0.100\mathrm{ M} 0.100 M N a O H \mathrm{NaOH} NaOH . (a) Calculate the buffer p H \mathrm{pH} pH . (b) Determine the maximum volume of 0.100 M 0.100\mathrm{ M} 0.100 M H C l \mathrm{HCl} HCl that can be added before the p H \mathrm{pH} pH drops below 4.00 4.00 4.00 . (c) Comment on whether this buffer would be effective at p H = 4.00 \mathrm{pH} = 4.00 pH = 4.00 given the p K a \mathrm{p}K_a p K a of ethanoic acid. [Hard]
An environmental scientist measures the p H \mathrm{pH} pH of a lake at 4.50 4.50 4.50 . (a) Calculate [ H + ] [\mathrm{H}^+] [ H + ] and [ S O 4 2 − ] [\mathrm{SO}_4^{2-}] [ SO 4 2 − ] Assuming the acidity is entirely from dissolved H 2 S O 4 \mathrm{H}_2\mathrm{SO}_4 H 2 SO 4 with complete dissociation of both protons. (b) Determine whether C a S O 4 \mathrm{CaSO}_4 CaSO 4 would precipitate if [ C a 2 + ] = 1.5 × 10 − 3 M [\mathrm{Ca}^{2+}] = 1.5 \times 10^{-3}\mathrm{ M} [ Ca 2 + ] = 1.5 × 1 0 − 3 M . K s p ( C a S O 4 ) = 2.4 × 10 − 5 K_{sp}(\mathrm{CaSO}_4) = 2.4 \times 10^{-5} K s p ( CaSO 4 ) = 2.4 × 1 0 − 5 . (c) Calculate the minimum [ C a 2 + ] [\mathrm{Ca}^{2+}] [ Ca 2 + ] required to initiate precipitation of C a S O 4 \mathrm{CaSO}_4 CaSO 4 . [Medium]
flowchart TD
A[2_Acids And Bases Advanced] --> B[Key Concepts]
A --> C[Core Principles]
A --> D[Practical Applications]
B --> E[Fundamental definitions]
C --> F[Design patterns]
D --> G[Real-world usage] This topic covers the essential chemistry of acids and bases (advanced), including key reactions, underlying theories, and practical applications.
Key concepts include:
Brønsted-Lowry theory strong and weak acids/bases pH calculations titration curves and indicators hydrolysis of salts Mastery of these concepts requires both theoretical understanding and the ability to apply knowledge to unfamiliar contexts, particularly in calculation and practical questions.