Solubility Equilibrium In saturated solutions dynamic equilibrium exists between undissolved solids...

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Solubility Equilibrium • In saturated solutions dynamic equilibrium exists between undissolved solids and ionic species in solutions • Solids continue to dissolve and ion-pairs continue to form solids. • The rate of dissolution process is equal to the rate of precipitation.

Transcript of Solubility Equilibrium In saturated solutions dynamic equilibrium exists between undissolved solids...

Page 1: Solubility Equilibrium In saturated solutions dynamic equilibrium exists between undissolved solids and ionic species in solutions Solids continue to dissolve.

Solubility Equilibrium

• In saturated solutions dynamic equilibrium exists between undissolved solids and ionic species in solutions

• Solids continue to dissolve and ion-pairs continue to form solids.

• The rate of dissolution process is equal to the rate of precipitation.

Page 2: Solubility Equilibrium In saturated solutions dynamic equilibrium exists between undissolved solids and ionic species in solutions Solids continue to dissolve.

Solubility Product Constant

• General expression:

• MmXn(s) ⇄ mMn+(aq) + nXm-(aq)

• Solubility product, Ksp = [Mn+]m[Xm-]n

Page 3: Solubility Equilibrium In saturated solutions dynamic equilibrium exists between undissolved solids and ionic species in solutions Solids continue to dissolve.

Solubility and Solubility Products

Examples:

• AgCl(s) ⇌ Ag+(aq) + Cl-(aq)

• Ksp = [Ag+][Cl-] = 1.6 x 10-10

• If s is the solubility of AgCl, then:

• [Ag+] = s and [Cl-] = s• Ksp = (s)(s) = s2 = 1.6 x 10-10

• s = 1.3 x 10-5 mol/L

Page 4: Solubility Equilibrium In saturated solutions dynamic equilibrium exists between undissolved solids and ionic species in solutions Solids continue to dissolve.

Solubility and Solubility Products

• Ag2CrO4(s) ⇌ 2Ag+(aq) + CrO42-(aq)

• Ksp = [Ag+]2[CrO42-] = 9.0 x 10-12

• If s is the solubility of Ag2CrO4, then:

• [Ag+] = 2s and [CrO42-] = s

• Ksp = (2s)2(s) = 4s3 = 9.0 x 10-12

• s = 1.3 x 10-4 mol/L

Page 5: Solubility Equilibrium In saturated solutions dynamic equilibrium exists between undissolved solids and ionic species in solutions Solids continue to dissolve.

Solubility and Solubility Products

• More Examples:

• Ca(IO3)2(s) ⇌ Ca2+(aq) + 2 IO3-(aq)

• Ksp = [Ca2+][IO3-]2 = 7.1 x 10-7

• If the solubility of Ca(IO3)2(s) is s mol/L, then:

• Ksp = 4s3 = 7.1 x 10-7

• s = 5.6 x 10-3 mol/L

Page 6: Solubility Equilibrium In saturated solutions dynamic equilibrium exists between undissolved solids and ionic species in solutions Solids continue to dissolve.

Solubility and Solubility Products

• Mg(OH)2(s) ⇌ Mg2+(aq) + 2 OH-(aq)

• Ksp = [Mg2+][OH-]2 = 8.9 x 10-12

• If the solubility of Mg(OH)2 is s mol/L, then:

• [Mg2+] = s mol/L and [OH-] = 2s mol/L,

• Ksp = (s)(2s)2 = 4s3 = 8.9 x 10-12

• s = 1.3 x 10-4 mol/L

Page 7: Solubility Equilibrium In saturated solutions dynamic equilibrium exists between undissolved solids and ionic species in solutions Solids continue to dissolve.

Solubility and Solubility Products

• More Examples:

• Ag3PO4(s) ⇌ 3Ag+(aq) + PO43-(aq)

• Ksp = [Ag+]3[PO43-] = 1.8 x 10-18

• If the solubility of Ag3PO4 is s mol/L, then:

• Ksp = (3s)3(s) = 27s4 = 1.8 x 10-18

• s = 1.6 x 10-5 mol/L

Page 8: Solubility Equilibrium In saturated solutions dynamic equilibrium exists between undissolved solids and ionic species in solutions Solids continue to dissolve.

Solubility and Solubility Products

• Cr(OH)3(s) ⇌ Cr3+(aq) + 3 OH-(aq)

• Ksp = [Cr3+][OH-]3 = 6.7 x 10-31

• If the solubility is s mol/L, then:• Ksp = [Cr3+][OH-]3 = (s)(3s)3 = 27s4 = 6.7 x 10-31

• s = 1.3 x 10-8 mol/L

Page 9: Solubility Equilibrium In saturated solutions dynamic equilibrium exists between undissolved solids and ionic species in solutions Solids continue to dissolve.

Solubility and Solubility Products

• More Examples:

• Ca3(PO4)2(s) ⇌ 3Ca2+(aq) + 2PO43-(aq)

• Ksp = [Ca2+]3[PO43-]2 = 1.3 x 10-32

• If the solubility is s mol/L, then:

• [Ca2+] = 3s, and [PO43-] = 2s

• Ksp = (3s)3(2s)2 = 108s5 = 1.3 x 10-32

• s = 1.6 x 10-7 mol/L

Page 10: Solubility Equilibrium In saturated solutions dynamic equilibrium exists between undissolved solids and ionic species in solutions Solids continue to dissolve.

Factors that affect solubility

• Temperature– Solubility generally increases with temperature;

• Common ion effect– Common ions reduce solubility

• Salt effect– This slightly increases solubility

• pH of solution– pH affects the solubility of ionic compounds in which the

anions are conjugate bases of weak acids;

• Formation of complex ion– The formation of complex ion increases solubility

Page 11: Solubility Equilibrium In saturated solutions dynamic equilibrium exists between undissolved solids and ionic species in solutions Solids continue to dissolve.

Common Ion Effect

• Consider the following solubility equilibrium:

• AgCl(s) ⇌ Ag+(aq) + Cl-(aq); Ksp = 1.6 x 10-10;

• The solubility of AgCl is 1.3 x 10-5 mol/L at 25oC.• If NaCl is added, equilibrium shifts left due to

increase in [Cl-] and some AgCl will precipitate out.• For example, if [Cl-] = 1.0 x 10-2 M, • Solubility of AgCl = (1.6 x 10-10)/(1.0 x 10-2) • = 1.6 x 10-8 mol/L

Page 12: Solubility Equilibrium In saturated solutions dynamic equilibrium exists between undissolved solids and ionic species in solutions Solids continue to dissolve.

Effect of pH on Solubility

• Consider the following equilibrium:

Ag3PO4(s) ⇌ 3Ag+(aq) + PO43-(aq);

• If HNO3 is added, the following reaction occurs:

H3O+(aq) + PO43-(aq) ⇌ HPO4

2-(aq) + H2O• This reaction reduces PO4

3- in solution, causing more solid Ag3PO4 to dissolve.

• In general, the solubility of compounds such as Ag3PO4, which anions are conjugate bases of weak acids, increases as the pH is lowered by adding nitric acid.

Page 13: Solubility Equilibrium In saturated solutions dynamic equilibrium exists between undissolved solids and ionic species in solutions Solids continue to dissolve.

Effect of pH on Solubility

• Consider the following equilibrium:

Mg(OH)2(s) ⇌ Mg2+(aq) + 2 OH-(aq);

• Increasing the pH means increasing [OH-] and equilibrium will shift to the left, causing some of Mg(OH)2 to precipitate out.

• If the pH is lowered, [OH-] decreases and equilibrium shifts to the right, causing solid Mg(OH)2 to dissolve.

• The solubility of compounds of the type M(OH)n decreases as pH is increased, and increases as pH is decreased.

Page 14: Solubility Equilibrium In saturated solutions dynamic equilibrium exists between undissolved solids and ionic species in solutions Solids continue to dissolve.

Formation of Complex Ions on Solubility

• Many transition metals ions have strong affinity for ligands to form complex ions.

• Ligands are molecules, such as H2O, NH3 and CO, or anions, such as F-, CN- and S2O3

2-.

• Complex ions are soluble – thus, the formation of complex ions increases solubility of slightly soluble ionic compounds.

Page 15: Solubility Equilibrium In saturated solutions dynamic equilibrium exists between undissolved solids and ionic species in solutions Solids continue to dissolve.

Effect of complex ion formation on solubility

• Consider the following equilibria:• AgCl(s) ⇌ Ag+(aq) + Cl-(aq); Ksp = 1.6 x 10-10

• Ag+(aq) + 2NH3(aq) ⇌ Ag(NH3)2+

(aq) ; Kf = 1.7 x 107

• Combining the two equations yields:• AgCl(s) + 2NH3(aq) ⇌ Ag(NH3)2

+(aq) + Cl-(aq);

• Knet = Ksp x Kf = (1.6 x 10-10) x (1.7 x 107) = 2.7 x 10-3

• Knet > Ksp implies that AgCl is more soluble in aqueous NH3 than in water.

Page 16: Solubility Equilibrium In saturated solutions dynamic equilibrium exists between undissolved solids and ionic species in solutions Solids continue to dissolve.

Solubility Exercise #1

• Calculate the solubility of AgCl in water and in 1.0 M NH3 solution at 25oC.

• Solutions: Solubility in water = (Ksp)

= (1.6 x 10-10) = 1.3 x 10-5 mol/L

Page 17: Solubility Equilibrium In saturated solutions dynamic equilibrium exists between undissolved solids and ionic species in solutions Solids continue to dissolve.

Solubility Exercise #1

• Solubility of AgCl in 1.0 NH3:

• AgCl(s) + 2NH3(aq) ⇌ Ag(NH3)2+(aq) + Cl-(aq)

• [Initial], M - 1.0 0.0 0.0

• [Change] - -2S +S +S

• [Equilm.] - (1 – 2S) S S

3-2

2

23

-23

net 10x 2.7 )2 - (1

]NH[

]Cl][)[Ag(NH

S

SK

Page 18: Solubility Equilibrium In saturated solutions dynamic equilibrium exists between undissolved solids and ionic species in solutions Solids continue to dissolve.

Solubility Exercise #1

• Solubility of AgCl in 1.0 NH3 (continued):

• S = 0.052 – 0.104S; • S = 0.052/1.104 = 0.047 mol/L

• AgCl is much more soluble in NH3 solution than in water.

0.052 10x 2.7 )2 - (1

3- S

S

Page 19: Solubility Equilibrium In saturated solutions dynamic equilibrium exists between undissolved solids and ionic species in solutions Solids continue to dissolve.

Predicting Formation of Precipitate

• Qsp = Ksp saturated solution, but no precipitate

• Qsp > Ksp saturated solution, with precipitate

• Qsp < Ksp unsaturated solution,

• Qsp is ion product expressed in the same way as Ksp for a particular system.

Page 20: Solubility Equilibrium In saturated solutions dynamic equilibrium exists between undissolved solids and ionic species in solutions Solids continue to dissolve.

Predicting Precipitation

• Consider the following case:20.0 mL of 0.025 M Pb(NO3)2 is added to 30.0 mL of 0.10 M NaCl. Predict if precipitate of PbCl2 will form.

(Ksp for PbCl2 = 1.6 x 10-5)

Page 21: Solubility Equilibrium In saturated solutions dynamic equilibrium exists between undissolved solids and ionic species in solutions Solids continue to dissolve.

Predicting Precipitation

• Calculation:• [Pb2+] = (20.0 mL x 0.025 M)/(50.0 mL) = 0.010 M• [Cl-] = (30.0 mL x 0.10 M)/(50.0 mL) = 0.060 M

• Qsp = [Pb2+][Cl-]2 = (0.010 M)(0.060 M)2

• = 3.6 x 10-5

• Qsp > Ksp precipitate of PbCl2 will form.

Page 22: Solubility Equilibrium In saturated solutions dynamic equilibrium exists between undissolved solids and ionic species in solutions Solids continue to dissolve.

Practical Applications of Solubility Equilibria

• Qualitative Analyses– Isolation and identification of cations and/or anions in

unknown samples

• Synthesis of Ionic Solids of commercial interest

• Selective Precipitation based on Ksp

Page 23: Solubility Equilibrium In saturated solutions dynamic equilibrium exists between undissolved solids and ionic species in solutions Solids continue to dissolve.

Qualitative Analysis

• Separation and identification of cations, such as Ag+, Ba2+, Cr3+, Fe3+, Cu2+, etc. can be carried out based on their different solubility and their ability to form complex ions with specific reagents, such as HCl, H2SO4, NaOH, NH3, and others.

• Separation and identification of anions, such as Cl-, Br-, I-, SO4

2-, CO32-, PO4

3-, etc., can be accomplished using reagents such as AgNO3, Ba(NO3)2 under neutral or acidic conditions.

Page 24: Solubility Equilibrium In saturated solutions dynamic equilibrium exists between undissolved solids and ionic species in solutions Solids continue to dissolve.

Selective Precipitation (Mixtures of Metal Ions)

• Use a reagent whose anion forms a precipitate with only one or a few of the metal ions in the mixture.

• Example: Solution contains Ba2+ and Ag+ ions. Adding NaCl will form a precipitate with Ag+

(AgCl), while still leaving Ba2+ in solution.

Page 25: Solubility Equilibrium In saturated solutions dynamic equilibrium exists between undissolved solids and ionic species in solutions Solids continue to dissolve.

Separation of Cu2+ and Hg2+ from Ni2+ and Mn2+ using H2S

• At a low pH, [S2–] is relatively low and only the very insoluble HgS and CuS precipitate.

• When OH– is added to lower [H+], the value of [S2–] increases, and MnS and NiS precipitate.

Page 26: Solubility Equilibrium In saturated solutions dynamic equilibrium exists between undissolved solids and ionic species in solutions Solids continue to dissolve.

Separation of Cu2+ and Hg2+ from Ni2+ and Mn2+ using H2S

Page 27: Solubility Equilibrium In saturated solutions dynamic equilibrium exists between undissolved solids and ionic species in solutions Solids continue to dissolve.

Separating the Common Cations by Selective Precipitation

Page 28: Solubility Equilibrium In saturated solutions dynamic equilibrium exists between undissolved solids and ionic species in solutions Solids continue to dissolve.

Synthesis of Ionic Solids

• Chemicals such as AgCl, AgBr, and AgI that are important in photography are prepared by precipitation method.

• AgNO3(aq) + KBr(aq) AgBr(s) + KNO3(aq)

Page 29: Solubility Equilibrium In saturated solutions dynamic equilibrium exists between undissolved solids and ionic species in solutions Solids continue to dissolve.

Selective Precipitation

• Compounds with different solubility can be selectively precipitated by adjusting the concentration of the precipitating reagents.

• For example, AgCl has a much lower Ksp than PbCl2

• If Ag+ and Pb2+ are present in the same solution, the Ag+ ion can be selectively precipitated as AgCl, leaving Pb2+ in solution.

Page 30: Solubility Equilibrium In saturated solutions dynamic equilibrium exists between undissolved solids and ionic species in solutions Solids continue to dissolve.

Complex Ion Equilibria

• Complex ions are ions consisting central metal ions and ligands covalently bonded to the metal ions;

• Ligands can be neutral molecules such as H2O, CO, and NH3, or anions such as Cl-, F-, OH-, and CN-;

• For example, in the complex ion [Cu(NH3)4]2+, four NH3 molecules are covalently bonded to Cu2+.

Page 31: Solubility Equilibrium In saturated solutions dynamic equilibrium exists between undissolved solids and ionic species in solutions Solids continue to dissolve.

Formation of Complex Ions

• In aqueous solutions, metal ions form complex ions with water molecules as ligands.

• If stronger ligands are present, ligand exchanges occur and equilibrium is established.

• For example:

Cu2+(aq) + 4NH3(aq) ⇌ [Cu(NH3)4]2+(aq)

134

32

243

f 10x 1.1 ]NH][Cu[

])[Cu(NH

K

Page 32: Solubility Equilibrium In saturated solutions dynamic equilibrium exists between undissolved solids and ionic species in solutions Solids continue to dissolve.

Stepwise Formation of Complex Ion

• At molecular level, ligand molecules or ions combine with metal ions in stepwise manner;

• Each step has its equilibrium and equilibrium constant;

• For example:

(1) Ag+(aq) + NH3(aq) ⇌ Ag(NH3)+(aq)

(2) Ag(NH3)+(aq) + NH3(aq) ⇌ Ag(NH3)2+(aq);

3

3

3f1 10x 2.1

]][NH[Ag

])[Ag(NH

K

3

33

232f 10x 8.2

]][NH)[Ag(NH

])[Ag(NH

K

Page 33: Solubility Equilibrium In saturated solutions dynamic equilibrium exists between undissolved solids and ionic species in solutions Solids continue to dissolve.

Stepwise Formation of Complex Ion

Individual equilibrium steps:

(1) Ag+(aq) + NH3(aq) ⇌ Ag(NH3)+(aq); Kf1 = 2.1 x 103

(2) Ag(NH3)+(aq) + NH3(aq) ⇌ Ag(NH3)2+(aq); Kf2 = 8.2 x 103

Combining (1) and (2) yields:

• Ag+(aq) + 2NH3(aq) ⇌ Ag(NH3)2+(aq);

7f2f12

3

23f 10x 1.7 x

]][NH[Ag

])[Ag(NH

KKK

Page 34: Solubility Equilibrium In saturated solutions dynamic equilibrium exists between undissolved solids and ionic species in solutions Solids continue to dissolve.

Stepwise complex ion formation for Cu(NH3)42+

Individual equilibrium steps:1. Cu2+(aq) + NH3(aq) ⇌ Cu(NH3)2+(aq); K1 = 1.9 x 104

2. Cu(NH3)2+(aq) + NH3(aq) ⇌ Cu(NH3)22+(aq); K2 = 3.9 x 103

3. Cu(NH3)22+(aq) + NH3(aq) ⇌ Cu(NH3)3

2+(aq); K3 = 1.0 x 103

4. Cu(NH3)32+(aq) + NH3(aq) ⇌ Cu(NH3)4

2+(aq); K4 = 1.5 x 102

Combining equilibrium:• Cu2+(aq) + 4NH3(aq) ⇌ Cu(NH3)4

2+(aq);

• Kf = K1 x K2 x K3 x K4 = 1.1 x 1013

]][NH[Cu

])[Cu(NH

43

2

243

f

K

Page 35: Solubility Equilibrium In saturated solutions dynamic equilibrium exists between undissolved solids and ionic species in solutions Solids continue to dissolve.

Complex Ions and Solubility

• Two strategies for dissolving a water–insoluble ionic solid. If the anion of the solid is a good base, the

solubility is greatly increased by acidifying the solution.

In cases where the anion is not sufficiently basic, the ionic solid often can be dissolved in a solution containing a ligand that forms stable complex ions with its cation.

Page 36: Solubility Equilibrium In saturated solutions dynamic equilibrium exists between undissolved solids and ionic species in solutions Solids continue to dissolve.

Concept Check

(a) Calculate the solubility of silver chloride in 10.0 M ammonia given the following information:

Ksp (AgCl) = 1.6 x 10–10

Ag+ + NH3 AgNH3+ K = 2.1 x 103

AgNH3+ + NH3 Ag(NH3)2

+ K = 8.2 x 103

(b) Calculate the concentration of NH3 in the final equilibrium mixture.

Answers: (a) 0.48 M; (b) 9.0 M