Chem 1721 Brief Notes: Chapters 16 and 17 Chapter 16: Acid-Base Equilibria; Chapter 17: Solubility and Complex-Ion Equilibria still largely focussed on acid/base chemistry; shift focus to solutions that contain both an acid and a base Common Ion Effect and Buffer Solutions Titrations, pH Curves and Indicators Solubility Equilibria Common Ion Solutions solutions that contain a conjugate acid/base pair presence of an ion common to the equilibrium from a secondary source in sol’ns of acids & bases, the presence of a common ion results in a ΔpH (increase for acids, decrease for bases) this is called the common ion effect (will see this again at the end of the chapter with solubility equilibria) What we want to know: What happens to a solution of an acid or base if a salt containing its conjugate is added? How is the dissociation equilibrium affected? Does the pH change? % dissociation? ex. calculate the pH of 0.25 M HC2H3O2 (aq) AND 0.25 M HC2H3O2 (aq) + 0.15 M NaC2H3O2 (aq) HC2H3O2 is a weak acid (Ka = 1.8 x 10 5); C2H3O2 is the conjugate base ⎯ note: initial [ ] HC2H3O2 0.25 M equil [ ] (0.25 – x) M initial [ ] HC2H3O2 0.25 M equil [ ] (0.25 – x) M ⎯ + H2O ↔ C 2 H3 O2 0M H3O+ 0M + ⎯ xM + H2O ↔ C 2 H3 O2 0.15 M xM H3O+ 0M + ⎯ (0.15 + x) M xM the big difference between these 2 calculations is that the initial [C2H3O2 ] in the common ion solution IS NOT 0 M ⎯ some numbers: 0.25 M HC2H3O2 [H3O+] = 0.0021 M pH = 2.68 % diss = 0.84% 0.25 M HC2H3O2 + 0.15 M NaC2H3O2 [H3O+] = 3.0 x 10 5 M pH = 4.52 % diss = 0.012% ⎯ demonstration of LeChatelier’s principle; presence of common ion C2H3O2 causes equilibrium to shift to left; lower [H3O+]; less acidic; higher pH ⎯ ex. calculate the pH of 0.66 M NH3 (aq) AND 0.66 M NH3 + 0.55 M NH4Cl (aq) NH3 is a weak base (Kb = 1.8 x 10 5); NH4+ is the conjugate acid ⎯ note: initial [ ] NH3 0.66 M equil [ ] (0.66 – x) M initial [ ] NH3 0.66 M equil [ ] (0.66 – x) M + ↔ H2O NH4+ 0M + OH 0M ⎯ xM + H2O ↔ NH4+ 0.55 M (0.55 + x) M xM + OH 0M ⎯ xM the big difference between these 2 calculations is that the initial [NH4+] in the common ion solution IS NOT 0 M some numbers: 0.66 M NH3 [OH ] = 0.0034 M pH = 11.53 % diss = 0.52% 0.66 M NH3 + 0.55 M NH4Cl [OH ] = 2.2 x 10 5 M pH = 9.34 % diss = 0.0033% ⎯ ⎯ ⎯ demonstration of LeChatelier’s principle; presence of common ion NH4+ causes equilibrium to shift to left; lower [OH ]; less basic; lower pH ⎯ Buffer Solutions solutions that contain both an acid and a base; usually a conjugate acid/base pair common ion solutions the job of a buffer solution is to maintain an approximately constant pH when small amounts of strong acid (H+) or strong base (OH ) are added ⎯ pH of a buffer solution is dependent on: Ka of the acid component, relative [acid] and [base] dependence given by Henderson-Hasselbalch equation: [A-] [base] pH = pKa + log pH = pKa + log OR [acid] [HA] buffer solutions resist a change in pH when H+ or OH are added H+ or OH consumed in a neutralization reaction; strong acid or base replaced by weak acid or base (HA or A ) ⎯ ⎯ ⎯ added H+ reacts with the base component of the buffer, A : H+ + A HA added OH reacts with the acid component of the buffer, HA: OH + HA A + H2O ⎯ ⎯ ⎯ ⎯ result of neutralization rxn: ⎯ [H+] or [OH ] = 0 after reaction [HA] and [A ] change (increase or decrease depending on reactant or product) but [A ]/[HA] remains relatively constant ⎯ ⎯ ⎯ some calculations ex. A buffer sol’n composed of 0.25 M HNO2 (pKa = 3.40) and 0.35 M KNO2 has a pH of 3.54. Calculate the change in pH that occurs when 0.010 mol of strong acid or 0.050 mol strong base are added to 1.00 L of the buffer solution. consider the addition of strong acid first: strong acid (H+) will react with the base component of this buffer, NO2 ⎯ neutralization reaction: note: initial mol H+ 0.010 mol Δ mol - 0.010 mol - 0.010 mol + 0.010 mol final mol 0 mol 0.34 mol 0.26 mol + NO2 0.35 mol ⎯ HNO2 0.25 mol the neutralization reaction happens FIRST; it goes very fast and effectively to completion after reaction: H+ completely consumed (limiting reactant); [NO2 ] = 0.34 mol/1.00 L = 0.34 M; ⎯ note: [HNO2] = 0.26 mol/1.00 L = 0.26 M after the added strong acid is consumed, the acid ionization equilibrium of HNO2 is re-established solve for pH using and equilibrium table OR using the Henderson-Hasselbalch equation equilibrium table: initial [ ] HNO2 (aq) 0.26 M equil [ ] (0.26 ⎯ x) M + H2O (l) ---- ↔ ---- NO2 (aq) 0.34 M + ⎯ H3O+ (aq) 0 (0.34 + x) M xM Ka = 4.0 x 10 4; solve for x ⎯ x = [H3O+] = 3.06 x 10 4 ⎯ Henderson-Hasselbalch equation: pH = pKa + log([NO2 ]/[HNO2]); pH = 3.40 + log (.34/.26) using either approach: ΔpH = 0.02 ⎯ pH = 3.52 consider the addition of strong base: strong base (OH ) will react with the acid component of this buffer, HNO ⎯ neutralization reaction: initial mol Δ mol - 0.050 mol - 0.050 mol + 0.050 mol final mol 0 mol 0.20 mol 0.40 mol ⎯ note: + OH 0.050 mol HNO2 0.25 mol NO2 0.35 mol + ⎯ H2O the neutralization reaction happens FIRST; it goes very fast and effectively to completion after reaction: OH completely consumed (limiting reactant); ⎯ [HNO2] = 0.20 mol/1.00 L = 0.20 M; note: [NO2 ] = 0.40 mol/1.00 L = 0.40 M ⎯ after the added strong base is consumed, the acid ionization equilibrium of HNO2 is re-established solve for pH using and equilibrium table OR using the Henderson-Hasselbalch equation equilibrium table: initial [ ] HNO2 (aq) 0.20 M equil [ ] (0.20 ⎯ x) M + H2O (l) ------- ↔ NO2 (aq) 0.40 M ⎯ (0.40 + x) M + H3O+ (aq) 0 xM Ka = 4.0 x 10 4; solve for x ⎯ x = [H3O+] = 2.0 x 10 4 ⎯ Henderson-Hasselbalch equation: pH = pKa + log([NO2 ]/[HNO2]); pH = 3.40 + log (.40/.20) using either approach: ΔpH = 0.30 ⎯ pH = 3.70 buffer capacity and buffer failure: buffer capacity refers to how much H+ or OH can be added before a buffer fails; buffer capacity can also be interpreted in terms of how large or small the ΔpH is upon addition of H+ or OH a buffer fails when ΔpH > 1 pH unit ⎯ ⎯ consider 2 HF + NaF buffer solutions 0.25 M HF + 0.50 M NaF 0.050 M HF + 0.100 M NaF pH = 3.76 pH = 3.76 [F ]/[HF] = 2 [F ]/[HF] = 2 after the addition of some strong acid (specifically 0.0020 mol to 0.100 L of solution) pH = 3.71 pH = 3.51 [F ]/[HF] = 1.78 [F ]/[HF] = 1.14 ⎯ ⎯ ⎯ ⎯ ⇑⇑⇑ this buffer is said to have a better buffer capacity – smaller ΔpH when H+ is added buffers are most efficient when [base]/[acid] ≈ 1 the acid component of the buffer solution should have pKa close to the desired pH (pKa = desired pH + 1) ex. Consider these acids: acid, HA pKa base, A H2PO4 NH4+ HF HC7H5O2 7.21 9.25 3.14 4.19 HPO42 NH3 F C7H5O2 ⎯ ex. ⎯ ⎯ ⎯ ⎯ pH range of best buffering; pH = pKa + 1 6.21 – 8.21 8.25 – 10.25 2.14 – 4.14 3.19 – 5.19 Calculate the pH of a buffer prepared by mixing 1.04 M NaF and 0.86 M HF. (for HF pKa = 3.14) answer: pH = 3.22 ex. Calculate the [NaC7H5O2] required to prepare a buffer of pH 4.10 with 0.249 M HC7H5O2 (pKa = 4.19). answer: [C7H5O2 ] = 0.202 M ⎯ Titrations see Titration Calculation Strategies handout on Chem 173 web page: http://www2.onu.edu/~sbates/chem173/handouts.html an analytical technique; volulmetric analysis determination of composition i.e. molar concentration, mass %, etc. reaction between a titrant (known composition) and analyte (unknown composition) one reactant added to the other until the reaction is just complete stoichiometrically correct mole ratio of reactants no limiting reactant, no excess reactant reactants completely consumed, only products present this is the stoichiometric point (or end point) of the titration ex. for the reaction 3 A + 2 B C + 2 D2 at the stoichiometric point the mol ratio of A:B is 3:2 A and B completely consumed; only C and D2 present titrations require an indicator – some indication (usually visual) of when you have reached the stoichiometric point color change specific pH change different types of titrations acid/base oxidation/reduction (i.e. your Solubility of Ca(IO3)2 lab) complexiometric (i.e. determination of Ni concentration in a plating bath) strong acid + strong base titrations HCl (aq) + NaOH (aq) NaCl (aq) + H2O (l) Cl and Na+ are spectator ions net ionic equation: H+ + OH H2O ⎯ ⎯ ex. consider the titration of 40.0 mL of 0.110 M HCl titrated with 0.095 M NaOH mol H+ = (0,0400 L)(0.110 mol/L) = 0.00440 mol H+ 1:1 stoichiometry, so at stoichiometric point mol H+ = mol OH = 0.00440 mol volume NaOH required to reach stoichiometric point? vol NaOH = (0.00440 mol)÷(0.095 mol/L) = 0.0463 L ⎯ before the stoichiometric point: after the addition of 10.00 mL NaOH (aq) mol OH = (0.0100 L)(0.095 mol/L) = 9.5 x 10 4 mol OH added ⎯ ⎯ ⎯ mol before: H+ 0.00440 mol Δ mol: - 0.00095 mol - 0.00095 mol mol after: 0.0035 mol 0 + OH 0.00095 mol ⎯ after neutralization reaction H+ remains in excess (OH is limiting reactant) [H+] = 0.0035 mol/(0.0400 + 0.0100)L = 0.070 M pH = 1.15 ⎯ H2O AT the stoichiometric point: after the addition of 46.30 mL NaOH (aq) (see calculation above) mol OH = (0.04630 L)(0.095 mol/L) = 0.00440 mol OH added ⎯ ⎯ mol before: H+ 0.00440 mol Δ mol: - 0.00440 mol - 0.00440 mol mol after: 0 0 + OH 0.00440 mol ⎯ H2O after neutralization reaction [H+] and [OH ] = 0, only H2O present in pure water at 25°C, [H+] = 1.0 x 10 7 M pH = 7.00 ⎯ ⎯ beyond the stoichiometric point: after the addition of 60.00 mL NaOH (aq) mol OH = (0.0600 L)(0.095 mol/L) = 0.0057 mol OH added ⎯ ⎯ mol before: H+ 0.00440 mol Δ mol: - 0.00440 mol mol after: 0 + OH 0.0057 mol ⎯ H2O - 0.00440 mol 0.0013 mol + after neutralization reaction OH remains in excess (H is limiting reactant) [OH ] = 0.0013 mol/(0.0400 + 0.0600)L = 0.13 M pOH = 1.89 pH = 12.11 ⎯ ⎯ pH curves for acid/base titrations (see Titrations handout) strong acid + strong base: H+ + OH H2O start at low pH (excess H+) stoichometric point at pH = 7 end at high pH (excess OH ) ⎯ ⎯ ex. weak acid + strong base: HA + OH A + H2O start at acidic, but slightly higher pH (excess HA, but weak acid) stoichiometric point at pH > 7; HA and OH consumed but A (a weak base) in solution end at high pH (excess OH ) ⎯ ⎯ ⎯ ⎯ ⎯ before the stoichometric point – a buffer solution exists (HA and A present) ⎯ special point in a weak/strong titration: at the half-way point (i.e. half way to the stoichometric point): pH = pKa + OH 0.025 mol mol before: HA 0.050 mol Δ mol: - 0.025 mol - 0.025 mol + 0.025 mol mol after: 0.025 mol 0 0.025 mol ⎯ A 0 ⎯ + H2O mol HA = mol A ∴ [HA] = [A ] pH = pKa + log([A ]/[HA]) pH = pKa + log(1); pH = pKa ⎯ ⎯ ⎯ Consider specifically the titration of 30.0 mL of 0.125 M HC2H3O2 (aq) with 0.100 M NaOH (aq) note: see Titrations handout for details of calculations, reaction tables, pH calculations, and pH curve pH after the addition of 20.0 mL NaOH (aq) pH = 4.80 pH at the half-way point pH = 4.74 pH at the stoichiometric point pH = 8.75 pH after the addition of 60.0 mL NaOH (aq) pH = 12.40 ex. weak base + strong acid: H+ + B BH+ start at basic pH (excess B, but weak base) stoichiometric point at pH < 7; H+ and B consumed but BH+ (a weak acid) in solution end at low pH (excess H+) before the stoichometric point – a buffer solution exists (B and BH+ present) special point in a weak/strong titration: see discsusion above too at the half-way point (i.e. half way to the stoichometric point): pH = pKa; here pKa of BH+ ( or 14 ⎯ pKb) Consider specifically the titration of 20.0 mL of 1.20 M CH3NH2 (aq) with 0.75 M HNO3 (aq) note: see Titrations handout for details of calculations, reaction tables, pH calculations, and pH curve pH at the half-way point pH = 10.57 pH after the addition of 20.0 mL HNO3 (aq) pH = 10.35 pH at the stoichiometric point pH = 5.46 pH after the addition of 60.0 mL HNO3 (aq) pH = 1.00 miscellaneous acid + base and titration calculations ex. What volume of 0.368 M Sr(OH)2 is required to reach the stoichiometric point in the titration of 75.0 mL of 0.44 M HBr (aq)? HBr (aq) + Sr(OH)2 (aq) SrBr2 (aq) + 2 H2O (l) at stoichiometric point: mol Sr(OH)2 = 1/2 mol HBr logical pathway: vol HBr ⇒ mol HBr ⇒ mol Sr(OH)2 ⇒ vol Sr(OH)2 ex. Determine the molar concentration of HNO3 (aq) if 33.3 mL of 1.04 M LiOH (aq) is required to reach the stoichiometric point in the titration of 25.5 mL of the acid. HNO3 (aq) + LiOH (aq) LiNO3 (aq) + H2O (l) at stoichiometric point: mol HNO3 = mol LiOH logical pathway: vol LiOH ⇒ mol LiOH ⇒ mol HNO3; [HNO3] = mol HNO3 ÷ 0.02525 L ex. 25.00 mL of 0.750 M HCl (aq) and 45.00 mL of 0.840 M KOH (aq) are mixed. Is the resulting solution acidic, basic, or neutral? What is the pH? HCl + mol before: Δ mol: mol after: identify limiting reactant and excess reactant determine concentration of the excess reactant pH = ???? KOH KCl + H2O Acid Base Indicators used to visually indicate the stoichiometric point of a titration with a color change important to choose an indicator with a color change that occurs very close to the stoichiometric pt of the titration; minimizes experimental error pH of indicator color change should be close to pH of stoichiometric point acid/base indicators are typically large organic weak acids; can exist as acid (HIn) OR conjugate base (In ) acid form (HIn) and base form (In ) are 2 different colors ⎯ ⎯ HIn (a q) + H2O (l) ↔ In (aq) + H3O+ (aq) color 1 color 2 ⎯ Ka OR KIn = [In-][H3O+] KIn [HIn] [H3O+] color is dependent on pH and [In ]/[HIn] consider 2 extremes: = [In-] [HIn] ⎯ very low pH; acidic solution [H3O+] is high; common ion pushes equilibrium to left [HIn] is large, [In ] is small ⎯ ∴color of solution is the color of HIn very high pH; basic solution [OH ] is high; reaction occurs between OH and H3O+ pushing equilibrium to right: OH + H3O+ 2 H2O [In ] is large, [HIn] is small ⎯ ⎯ ⎯ ⎯ ∴ color of solution is the color of In ⎯ in the middle, range of colors depends of pH and [In ]/[H3O+] ⎯ pH of visible color change? for the human eye to detect the color change 1 part in 10 of the indicator must be converted to the other form ex. bromothymol blue; KIn = 1.0 x 10 7; HIn is yellow; In is blue ⎯ ⎯ If a few drops of bromothymol blue indicator is added to a solution of HCl (aq), what color is the solution initially? If this HCl (aq) is then titrated with NaOH (aq), at what pH will the color change be visible? HCl (aq) is an acidic solution ∴ the indicator is in its HIn form; the solution is yellow for the color change to be visible, 1 part in 10 must change from HIn In OR [In ]/[HIn] = 1/10 ⎯ ⎯ pH = ? Can solve this 2 ways: [In-][H3O+] KIn = [HIn] OR [H3O+] = KIn pH = pKIn + log [HIn] [In-] [In-] [HIn] answer: pH = 6.00 note: this same indicator in a basic solution would start blue (indicator in In form); the color change would occur at [In ]/[HIn] of 10/1; pH = 8.00 ⎯ ⎯ the general rule is: an indicator will change color at pH = pKIn + 1; for a titration choose an indicator with a pKIn value close (+ 1) to the pH of the stoichiometric point of the titration, Solubility Equilibria equilibrium established between an ionic solid and its ions in solution: (s) ↔ (aq); a saturated solution is one in which solid and ions exist in dynamic equilibrium heterogeneous equilibrium equlibrium constant, Ksp, solubility product constant ex. write the chemical equation for the solubility equilibrium and Ksp expression for: magnesium fluoride: MgF2 (s) ↔ Mg2+ (aq) + 2 F (aq); ⎯ Ksp = [Mg2+][F ]2 ⎯ calcium phosphate: Ca3(PO4)2 (s) ↔ 3 Ca2+ (aq) + 2 PO43 (aq); ⎯ Ksp = [Ca2+]3[PO43 ]2 ⎯ Calculating Ksp for Saturated Solutions consider 2 different ways to prepare a saturated solution of calcium fluoride: 1. solid CaF2 added to water and let stand; over time the solution will become saturated CaF2 (s) ↔ Ca2+ (aq) + 2 F (aq) measure experimentally [Ca2+] and [F ]; calculate Ksp ⎯ ⎯ so . . . if [Ca2+] = 3.3 x 10 4 M and [F ] = 6.7 x 10 4 M ⎯ ⎯ ⎯ Ksp = [Ca2+][F ]2 = (3.3 x 10 4)(6.7 x 10 4)2 = 1.5 x 10 10 ⎯ 2. ⎯ ⎯ note: here [F ] = 2•[Ca2+] ⎯ ⎯ mix 2 solutions together – one with Ca2+ (aq) and the other with F (aq); CaF2 (s) will precipitate from solution, but some Ca2+ and F will remain in solution and equilibrium will be established ⎯ ⎯ CaF2 (s) ↔ Ca2+ (aq) + 2 F (aq) measure experimentally [Ca2+] and [F ]; calculate Ksp ⎯ ⎯ so . . . if [Ca2+] = 1.5 x 10 4 M and [F ] = 1.0 x 10 3 M ⎯ ⎯ ⎯ Ksp = [Ca2+][F ]2 = (1.5 x 10 4)(1.0 x 10 3)2 = 1.5 x 10 10 ⎯ ⎯ ⎯ note: here [F ] ≠ 2•[Ca2+] ⎯ ⎯ and knowing Ksp you can calculate the concentration of an ion in an saturated solution Calculate [Ca2+] in a saturated solution of CaF2 with [F ] = 0.010 M. ⎯ answer: [Ca2+] = 1.5 x 10 6 M ⎯ Quantifying Solubility in mol/L and g/L solubility is defined in terms of mol of solid that will dissolve per L of solution (molar solubility), OR g of solid dissolved per L of solution use an equilibrium table to determine solubility if you know Ksp, OR to determine Ksp if you know solubility some examples ex. Calculate the solubility of MgF2 in mol/L and g/L. For MgF2, Ksp = 7.4 x 10 11. let x = mol of MgF2 (s) that will dissolve per L of sol’n; i.e. x = molar solubility of MgF2 ⎯ ↔ Mg2+ (aq) 0 initial [ ] MgF2 (s) ---- + 2 F (aq) 0 Δ[] ---- +x + 2x equil [ ] ----- xM 2x M ⎯ Ksp = [Mg2+][F ]2; 7.4 x 10 11 = (x)(2x)2 = 4x3 ⎯ ⎯ x = molar solubility = 2.6 x 10 4 mol/L; i.e. 2.6 x 10 4 mol MgF2 will dissolve per L of solution at 25°C ⎯ ⎯ g/L solubility? use molar mass of MgF2 (62.31 g/mol) to convert from mol/L to g/L 0.016 g MgF2/L ex. A saturated solution of silver chromate is found to have [Ag+] = 1.3 x 10 4 M. Calculate Ksp for Ag2CrO4. ⎯ initial [ ] Ag2CrO4 (s) ---- Δ[] ---- equil [ ] 2 Ag+ (aq) 0 ↔ ---- + 2 2⎯ 2 CrO42 (aq) 0 + ⎯ + 2x +x 2x M xM 3 Ksp = [Ag ] [CrO4 ] = (2x) (x) = 4x [Ag+] = 2x = 1.3 x 10 4 M ∴ x = 6.5 x 10 5 ⎯ ⎯ Ksp = 4(6.5 x 10 5)3 = 1.1 x 10 ⎯ ⎯ 12 Relative Solubilities of Ionic Compounds Which is more soluble: PbCl2 (Ksp = 1.6 x 10 5) OR PbF2 (Ksp = 4 x 10 8)? ⎯ ⎯ Which is more soluble: PbCl2 OR CaSO4 (Ksp = 6.1 x 10 5) ⎯ When can you compare Ksp’s directly to determine relative solubility? When comparing 2 compounds that produce the same number of ions in solution, Ksp values can be compared directly to determine relative solubility larger Ksp equilibrium position farther to right higher [ion] in solution greater solubility i.e. PbCl2 vs PbF2 PbCl2 (s) ↔ Pb2+ (aq) + 2 Cl (aq); Ksp = [Pb2+][Cl ]2 = 4x3 ⎯ ⎯ PbF2 (s) ↔ Pb2+ (aq) + 2 F (aq); Ksp = [Pb2+][F ]2 = 4x3; ⎯ answer: PbCl2 is more soluble ⎯ When comparing 2 compounds that do not produce the same number of ions in solution, Ksp values can NOT be compared directly; you must calculate x (molar solubility) to determine which compound is more soluble i.e. PbCl2 vs. CaSO4 PbCl2 (s) ↔ Pb2+ (aq) + 2 Cl (aq); Ksp = [Pb2+][Cl ]2 = 4x3 ⎯ ⎯ CaSO4 (s) ↔ Ca2+ (aq) + SO42 (aq); Ksp = [Ca2+][SO42 ] = x2 ⎯ answer: PbCl2 is more soluble ⎯ Factors the Affect Solubility 1. The Common Ion Effect same idea as with acids and bases; the presence of an ion common to the solubility equilibrium will cause the equilibrium position to shift and affect solubility for ionic compounds, the presence of a common ion results in decreased solubility ex. Calculate the solubility of MgF2 in 0.10 M NaF (aq). Above we calculated the solubility of MgF2 in water at 25°C: 2.6 x 10 4 mol/L, 0.016 g/L. ⎯ ↔ Mg2+ (aq) 0 initial [ ] MgF2 (s) ---- + 2 F (aq) 0.10 M Δ[] ---- +x + 2x equil [ ] ----- xM (.10 + 2x) M ⎯ Ksp = [Mg2+][F ]2; ⎯ 7.4 x 10 11 = (x)(.10 + 2x)2 ≈ (x)(0.10)2 ⎯ x = molar solubility = 7.4 x 10 9 mol/L OR 4.6 x 10 7 g MgF2/L at 25°C ⎯ ⎯ ex. Calculate the solubility of Pb(OH)2 in a solution with pH = 10.0. For Pb(OH)2 Ksp = 1.2 x 10 15 ⎯ in a solution with pH = 10.0, pOH = 4.0 and [OH ] = 10 4 M; this is a common ion solution ⎯ ↔ ⎯ Pb2+ (aq) 0 initial [ ] Pb(OH)2 (s) ---- + 2 OH (aq) 10 4 M Δ[] ---- +x + 2x equil [ ] ---- xM (10 4 + 2x) M ⎯ ⎯ ⎯ answer: solubility = 1.2 x 10 7 mol/L vs. 6.7 x 10 6 mol/L in a neutral sol’n ⎯ ⎯ 2. pH of the solution general rule: the solubility of an ionic compound that contains a basic anion will increase as the pH of the solution decreases also an application of Le Chatelier’s Principle consider calcium carbonate: CaCO3 (s) ↔ Ca2+ (aq) + CO32 (aq) ⎯ in an acidic solution [H3O+] is relatively high: H3O+ + CO32 HCO3 + H2O [CO32 ] decreases as the ion is removed from solution by reaction with H3O+ ⎯ ⎯ ⎯ equilibrium position shift to the right (to replenish CO32 ), and solubility increases ⎯ other common basic anions: OH , CN , PO43 , S2 , F , SO42 , C2H3O2 , NO2 ⎯ ⎯ ⎯ ⎯ ⎯ ⎯ ⎯ ⎯ note: the solubility of salts with neutral anions (Cl , Br , I , NO3 and ClO4 ) will NOT be affected by pH ⎯ 3. ⎯ ⎯ ⎯ ⎯ formation of complex ions the solubility of an ionic compound will increase dramatically if the solution contains a Lewis Base that can form a Lewis acid-base adduct with a metal cation again, Le Chatelier’s Principle in action: consider AgCl; insoluble in water and acid, but will dissolve in solutions containing NH3 (aq) AgCl (s) ↔ Ag+ (aq) + Cl (aq) in solutions containing NH3 (aq): Ag+ (aq) + 2 NH3 (aq) ↔ Ag(NH3)2+ (aq) ⎯ as Ag(NH3)2+ forms, [Ag+] decreases; equilibrium shifts to the right (to replenish Ag+); solubility increases the formation of Ag(NH3)2+ (aq) is an equilibrium; Kf = formation constant or stability constant consider a series of equations: step 1: AgCl (s) ↔ Ag+ (aq) + Cl (aq) ⎯ step 2: Ag+ (aq) + NH3 (aq) ↔ AgNH3+ (aq) step 3: AgNH3+ (aq) + NH3 (aq) ↔ Ag(NH3)2+ (aq) net: AgCl (s) + 2 NH3 (aq) ↔ Ag(NH3)2+ (aq) + Cl (aq) ⎯ Ion Product (Q) and Predictions about Precipitation: compare Q and Ksp if Q = Ksp the solution is at equilibrium; the solution is saturated – no more solid will dissolve and no precipitation will occur if Q < Ksp the solution is unsaturated – reaction will proceed in forward direction; more solid will dissolve, no precipitation will occur if Q > Ksp the solution is supersaturated – reaction will proceed in the reverse direction; precipitation will occur remember to calculate the [ion] in the solution that results from combining 2 volumes; i.e. [ion] = mol ion/total solution volume some examples ex. 250.0 mL of 0.0062 M AgNO3 (aq) mixed with 250.0 mL of 0.00014 M Na2CO3 (aq). Will a precipitate of Ag2CO3 (s) form? For Ag2CO3 Ksp = 8.1 x 10 12. Total solution volume after mixing = 500.0 mL. ⎯ answer: Q > Ksp ∴ Ag2CO3 precipitate will form ex. Calculate the minimum [CO32 ] required to precipitate Ag2CO3 from 5.8 x 10 4 M AgNO3. Precipitation occurs when Q > Ksp ⎯ ⎯ answer: [CO32 ] = 2.4 x 10 5 M ⎯ ⎯
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