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Chapter 16 Solubility and Complex Ion Equilibria Chapter 16 Table of Contents 16.1 16.2 16.3 Solubility Equilibria and the Solubility Product Precipitation and Qualitative Analysis Equilibria Involving Complex Ions Copyright © Cengage Learning. All rights reserved 2 Section 16.1 Solubility Equilibria and the Solubility Product Ca 5 (PO4 )3OH Ca 5 (PO 4 )3 OH In the forward direction: the acidic water(containing CO2) dissolves the underground limestone(CaCO3) , forming a cavern. In the backward direction: the water drips from the ceiling of the cave, and CO2 is lost to the air, causing solid CaCO3 to form, producing stalactites(鐘乳石) and stalagmites(石筍) 在石灰岩裏面,含有二氧化碳的水,滲入石灰岩隙縫中,會溶解其中 的碳酸鈣。這溶解了碳酸鈣的水,從洞頂上滴下來時,由於水分蒸發 、二氧化碳逸出,使被溶解的鈣質又變成固體(稱為固化)。由上而下 逐漸增長而成的,稱為「鐘乳石」。 Copyright © Cengage Learning. All rights reserved Return to TOC 3 Section 16.1 Solubility Equilibria and the Solubility Product 藍湖洞(巴西) 巴西馬托格羅索地區藍湖洞。洞內的鐘乳石,石筍密密麻 麻排列,令人讚嘆不已。地質學家普遍認為是由於洞中藍湖的 存在,為鐘乳石的形成提供了必要的碳酸鹽等組成。 Return to TOC Copyright © Cengage Learning. All rights reserved 4 Section 16.1 Solubility Equilibria and the Solubility Product • Tooth decay: when food lodges between the teeth, acids form that dissolve tooth enamel ( hydroxyapatite, Ca5(PO4)3OH ). Ca 5 (PO4 )3OH( s) Ca 5 (PO4 )3 (aq) OH Adding F- to drinking water, Since F- replaces the OH- in Ca5(PO4)3OH to produce Ca5(PO4)3F, and CaF, both of which are less soluble in acids than the original enamel. Ca 5 (PO4 )3F( s) CaF Ca 5 (PO4 )3 (aq) F Ca 2+ + 2F- Ksp Ksp Return to TOC Copyright © Cengage Learning. All rights reserved 5 Section 16.1 Solubility Equilibria and the Solubility Product Solubility Equilibria • Solubility product (Ksp) – equilibrium constant; has only one value for a given solid at a given temperature. • Solubility – an equilibrium position. Bi2S3(s) 2Bi3+(aq) + 3S2–(aq) 2 2 K sp = Bi S 3+ 3 Return to TOC Copyright © Cengage Learning. All rights reserved 6 Section 16.1 Solubility Equilibria and the Solubility Product Ksp Values at 25 °C for Common Ionic Solids Return to TOC Section 16.1 Solubility Equilibria and the Solubility Product • The solubility product is an equilibrium constant and has only one value for given solid at a given temperature. • Solubility is an equilibrium position Return to TOC Copyright © Cengage Learning. All rights reserved 8 Section 16.1 Solubility Equilibria and the Solubility Product Concept Check In comparing several salts at a given temperature, does a higher Ksp value always mean a higher solubility? Explain. If yes, explain and verify. If no, provide a counter-example. No The salts must contain the same number of ions to relate Ksp values to solubility directly, For example, for a binary salt, Ksp = s2 (s = solubility); for a ternary salt, Ksp = s3.(not include coefficient of soluble salt) Return to TOC Copyright © Cengage Learning. All rights reserved 9 Section 16.1 Solubility Equilibria and the Solubility Product Exercise Calculate the solubility of silver chloride in water. Ksp = 1.6 × 10–10 (AgCl Ag++Cl- ) x x Ksp x 2 x 1.6 1010 1.3×10-5 M Calculate the solubility of silver phosphate in water. Ksp = 1.8 × 10–18 (Ag3PO4 3Ag++PO4- ) 3x 1.6×10-5 x 3 4 18 Ksp (3 x ) ( x ) 27 x 1.8 10 M x 1.6 105 Return to TOC Copyright © Cengage Learning. All rights reserved 10 Section 16.1 Solubility Equilibria and the Solubility Product Concept Check How does the solubility of silver chloride in water compare to that of silver chloride in an acidic solution (made by adding nitric acid to the solution)? Explain. The solubilities are the same. The solubilities are the same. Since HCl is a strong acid, it is completely dissociated in water. There are no common ions between AgCl and HNO3. Copyright © Cengage Learning. All rights reserved Return to TOC 11 Section 16.1 Solubility Equilibria and the Solubility Product Concept Check How does the solubility of silver phosphate in water compare to that of silver phosphate in an acidic solution (made by adding nitric acid to the solution)? Explain. The silver phosphate is more soluble in an acidic solution. This is because the phosphate ion is a relatively good base and will react with the proton from the acid (essentially to completion). The phosphate ion does not react nearly as well with water. Return to TOC Copyright © Cengage Learning. All rights reserved 12 Section 16.1 Solubility Equilibria and the Solubility Product Concept Check How does the Ksp of silver phosphate in water compare to that of silver phosphate in an acidic solution (made by adding nitric acid to the solution)? Explain. The Ksp values are the same. The Ksp values are the same (assuming the temperature is constant). Return to TOC Copyright © Cengage Learning. All rights reserved 13 Section 16.1 Solubility Equilibria and the Solubility Product Exercise Calculate the solubility of AgCl in: Ksp = 1.6 × 10–10 a) 100.0 mL of 4.00 x 10-3 M calcium chloride. (8 103 x)( x) 1.6 1010 8 103 x 1.6 1010 2.0×10-8 M b) 100.0 mL of 4.00 x 10-3 M calcium nitrate. 1.3×10-5 M ( x)( x) 1.6 1010 x 1.3 105 Return to TOC Copyright © Cengage Learning. All rights reserved 14 Section 16.2 Atomic Masses Precipitation and Qualitative Analysis Precipitation (Mixing Two Solutions of Ions) MX(s) M + + X- Q= M + X - 0 0 + Ksp= M X • Q > Ksp; precipitation occurs and will continue until the concentrations are reduced to the point that they satisfy Ksp. • Q < Ksp; no precipitation occurs. Return to TOC Copyright © Cengage Learning. All rights reserved 15 Section 16.2 Atomic Masses Precipitation and Qualitative Analysis 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. Return to TOC Copyright © Cengage Learning. All rights reserved 16 Section 16.2 Atomic Masses Precipitation and Qualitative Analysis Separation of Cu2+ and Hg2+ from Ni2+ and Mn2+ using H2S + - H 2S H + HS HS- H + + S2- CuS(Ksp=8.5 10-45 ) HgS(Ksp=1.6 10-54 ) MnS(Ksp=2.3 10-13 ) NiS(Ksp=3 10-21 ) • 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. Return to TOC Copyright © Cengage Learning. All rights reserved 17 Section 16.2 Atomic Masses Precipitation and Qualitative Analysis Separation of Cu2+ and Hg2+ from Ni2+ and Mn2+ using H2S Return to TOC Copyright © Cengage Learning. All rights reserved 18 Section 16.2 Atomic Masses Precipitation and Qualitative Analysis Qualitative Analysis • Group 1- insoluble chloride (Ag+,Pb2+,Hg22+) • Group 2- Sulfides insoluble in acidic solution ( Hg2+, Cd2+, Bi3+, Cu2+, Sn4+) • Group 3- Sulfides insoluble in basic solution ( Co2+, Zn2+, Mn2+, Ni2+, Fe2+) and Cr(OH)3, Al(OH)3) • Group 4- Insoluble carbonates ( Group 2A cations form insoluble carbonates by the addition of CO32-. For example, Ba2+, Ca2+ and Mg2+) • Group 5- Alkali metal and ammonium ions (Group 1A cations and NH4+,identified by the characteristic colors they produce by flame test) Return to TOC Copyright © Cengage Learning. All rights reserved 19 Section 16.2 Atomic Masses Precipitation and Qualitative Analysis Separating the Common Cations by Selective Precipitation Return to TOC Copyright © Cengage Learning. All rights reserved 20 Section 16.2 Precipitation Atomic Masses and Qualitative Analysis Flame Test Potassium Sodium Ken O'Donoghue Return to TOC Section 16.2 Atomic Masses Precipitation and Qualitative Analysis CdS Cr(OH)3 Al(OH)3 Ni(OH)2 Return to TOC Section 16.3 The Mole Involving Complex Ions Equilibria Complex Ion Equilibria • Charged species consisting of a metal ion surrounded by ligands. Ligand: Lewis base(molecule or ion having a lone pair that can donated to an empty orbital on the metal ion to form covalence bond) • Formation (stability) constant. Equilibrium constant for each step of the formation of a complex ion by the addition of an individual ligand to a metal ion or complex ion in aqueous solution. Return to TOC 23 Section 16.3 The Mole Involving Complex Ions Equilibria Aqueous Ammonia Added to Silver Chloride Silver Chloride Dissolves to Form Ag(NH3)2+ (aq) and Cl- (aq) Return to TOC Section 16.3 The Mole Involving Complex Ions Equilibria Complex Ion Equilibria Be2+(aq) + F–(aq) BeF+(aq) K1 = 7.9 x 104 BeF+(aq) + F–(aq) BeF2(aq) K2 = 5.8 x 103 BeF2(aq) + F–(aq) BeF3– (aq) K3 = 6.1 x 102 BeF3– (aq) + F–(aq) BeF42– (aq) K4 = 2.7 x 101 Return to TOC Copyright © Cengage Learning. All rights reserved 25 Section 16.3 The Mole Involving Complex Ions Equilibria Example 16.8(page761) Ag + + S2O32Ag(S2O3 )- + (S2O3 )2- Ag(S2O3 )Ag(S2O3 )23- Return to TOC Copyright © Cengage Learning. All rights reserved 26 Section 16.3 The Mole Involving Complex Ions Equilibria 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. Return to TOC Copyright © Cengage Learning. All rights reserved 27 Section 16.3 The Mole Involving Complex Ions Equilibria Concept Check 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+ AgNH3+ + NH3 Ag(NH3)2+ 0.48 M(page 762) K = 2.1 x 103 K = 8.2 x 103 Calculate the concentration of NH3 in the final equilibrium mixture. 9.0 M Return to TOC Copyright © Cengage Learning. All rights reserved 28 Section 16.3 The Mole Involving Complex Ions Equilibria Ag + (aq) + Cl- (aq) AgCl(s) Ag + + NH3 K = 2.1 103 AgNH3+ Ag(NH3 ) + + NH3 Ksp = 1.6 10-10 Ag(NH3 ) 2+ K = 8.2 103 Ag total dissolved Ag + Ag(NH3 )+ Ag(NH3 )2+ AgCl(s) + 2NH3 10-2x Ag(NH3 )2+ + Clx K = Ksp K1 K 2 2.8 103 x x2 x 3 K=2.8 10 2.8 10 x 0.48M 2 (10-2x) 10 2 x 3 Return to TOC Copyright © Cengage Learning. All rights reserved 29 Section 16.3 The Mole Involving Complex Ions Equilibria Figure 16.3: Separation of Group 1 Ions PbCl2 heat Pb2+ + 2Cl- Hg 2Cl2 (s)+2NH3 (aq) HgNH 2Cl( s)+ Hg(l )+NH 4 + (aq)+Cl2H+ (aq)+Ag(NH3 )2+ (aq) +Cl- (aq) 2NH4 +(aq)+AgCl(s) Return to TOC