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CHAPTER 5. IONS IN SOLUTION 5.1 Metal Ions in Solution…………………………………………………………...... 1 5.1.1 Hydration and Hydrolysis of Metal Ions…………………………………… 1 5.1.2 Ionization of Water and Hydration of the Proton…………………………... 4 5.1.3 Polymerization and Precipitation…………………………………………… 5 5.1.4 Structures of Polycations and Polyoxoanions………………………………. 7 5.2 The Concept of Equilibrium Constant…………………………………………. 10 5.2.1 The Solubility Product…………………………………………………….. 10 5.2.2 The Free Energy of Reaction and the Equilibrium Constant……………… 11 5.2.3 Solubility Calculations……………………………………………………..14 5.2.4 Solubility of Sparingly Soluble Salts……………………………………… 15 5.2.5 Lattice Energy, Hydration Energy, and Solubility………………………... 17 5.3 Acids and Bases…………………………………………………………………... 18 5.3.1 Acidic and Basic Solutions………………………………………………... 18 5.3.2 Strong Acids and Bases…………………………………………………… 19 5.3.3 Weak Monoprotic Acids and Bases……………………………………….. 23 5.4 Structural Aspects of Acid-Base Strength…………………………………….... 25 5.4.1 Gas Phase Acidity…………………………………………………………. 25 5.4.2 Hydration Effects………………………………………………………….. 28 5.4.3 Strengths of Hydroxyl-Group Acids………………………………………. 29 5.5 Graphical Representations of Ionic Equilibria………………………………… 30 5.5.1 Logarithmic Concentration Diagrams…………………………………….. 30 5.5.2 Distribution Diagrams…………………………………………………….. 34 5.6 The Partial Charge Model and the Reactions of Metal Cations……………….34 5.6.1 The Acidity of Hydrated Metal Cations…………………………………... 34 5.6.2 The Mean Electronegativity of an Aqueous Solution……………………... 35 5.6.3 Hydrolysis of Metal Cations………………………………………………. 37 5.6.4 Polymerization…………………………………………………………….. 41 5.6.5 Precipitation……………………………………………………………….. 44 5.1. Metal Ions in Solution 5.1.1 Hydration and Hydrolysis of Metal Ions In the aqueous processing of metals, we are concerned with two major questions: (i) What happens to metal ions in solution? and (ii) What happens to a solid placed in an aqueous environment? Let us for a moment focus our attention on the water molecules which constitute the solvent phase of the aqueous solution. Two hydrogen atoms and an oxygen atom come together to form a water molecule by sharing their outer electrons: oo oO o o o + H + H = o oH o oO o o H Each pair of shared electrons constitutes a covalent bond. (5.1) It can be seen from this simplified picture that in a water molecule, the oxygen atom is surrounded by 8 outer electrons, four of which are involved in covalent bonding and 4 of which are unshared. We can add to this picture, the fact that oxygen has a higher affinity than hydrogen for electrons. Thus in a water molecule, the electron cloud is denser around the oxygen nucleus than around the hydrogen nuclei. This effect is acknowledged by ascribing a dipolar structure to the water molecule: H+ (-) O H+ Thus like a magnet, the water molecule has a positive and a negative pole. Now let us consider a metal ion immersed in this sea of dipoles. Let us take the simplest case, i.e., the hypothetical situation of a metal ion Mz+ immersed in water with no other ions being present. Through its charge, this ion exerts some influence on the surrounding water molecules. The metal ion is positively charged and by analogy with the well known behavior of magnets, we would expect it to attract the negative pole of a water molecule. This is called an electrostatic interaction: H+ H Mz+ + O- Mz+ O H+ (5.2) H Depending on the nature of the metal ion, several more water molecules may be attracted towards it in a similar manner. Thus we say that metal ions are hydrated in aqueous solution. We would expect that this interaction will be most intense for the water molecules which are nearest to the central metal ion. These nearest neighbor water molecules constitute the first or inner hydration sphere of the hydrated ion. The hydration number is the number of such nearest neighbor water molecules, and is generally taken to be equal to 6. Thus in aqueous solution, we can represent the dissolved metals ions as M(H2O)6z+, e.g., Ni(H2O)62+, Al(H2O)63+, etc. In addition to the attractive Mz+-O- interaction noted above, we must recognize that a repulsive Mz+-H+ interaction also exists. In fact, we may go so far as to say that the hydration of a metal ion really involves two simultaneous processes: (a) attraction of the negative pole of the water molecule to the positively charged metal ion, and (b) repulsion of the positive pole of the water molecule by the positive charge on the metal ion. These two processes, in competition, can cause a splitting of the bound water molecule: H+ - M2+ + O H+ M2+ H+ - H+ M2+ O - O H+ H+ Mz+ (OH)- + H+ (5.3) The term hydrolysis describes processes such as Equation 5.3 in which the O-H bonds of water are broken. The resulting OH--containing product is termed a hydroxo metal complex. It is conventional practice to express the formation of a hydroxo complex as indicated in Equation 5.4. Mz+ + H2O = MOH(z-1)+ + H+ However, in view of our previous treatment of hydration, we can also write: (5.4) M(H2O)6z+ + H2O = M(H2O)5(OH)+ + H3O+ (5.5) The hydrolysis process may not necessarily stop with the splitting of one water molecule; it may involve the other water molecules in the inner hydration sphere. Thus we speak of successive or stepwise hydrolysis: M(H2O)62+ = M(H2O)5(OH)+ + H+ M(H2O)5(OH)+ = M(H2O)4(OH)2o + H+ M(H2O)4(OH)2o = M(H2O)3(OH)3- + H+ M(H2O)3(OH)3- = M(H2O)2(OH)42- + H+ etc. (5.6) 5.1.2 Ionization of Water and Hydration of the Proton A similar electrostatic process involving only water molecules, leads to the ionization of water and the hydration of the proton. The ionization of water may be viewed in terms of the transfer of a proton from a water molecule to a second water molecule, yielding a hydrated hydrogen ion and a hydroxyl ion: H O+H H - +H O - H O +H - +H O - +H +H H2O + H2O = H3O+ + OH- O O +H +H +H (5.7) The species H3O+ is called the oxonium ion and it may be further hydrated to give the trihydrated oxonium ion, H3O(H2O)3+: H H O H H O O H H H H O H In the above structure the dashed lines are used to emphasize the fact that the O-H bonds between the surrounding water molecules and the oxonium protons are weaker than those within the oxonium ion. The weaker bonds represent hydrogen bonds. It is common practice to express the ionization of water without explicitly indicating the hydration of the proton: H2O = H+ + OH- (5.8) However there are situations where it is necessary to invoke the hydrated nature of the proton. 5.1.3 Polymerization and Precipitation The hydrolysis products encountered above may react further with each other to give polymeric species: M(H2O)5(OH)2+ + M(H2O)5(OH)2+ = [(H2O)4M-(OH)2-M(H2O)4]4+ + 2H2O (5.9) For example, Fe(H2O)5OH2+ can undergo the following dimerization reaction: Fe(H2O)5OH2+ + Fe(H2O)5OH2+ = OH Fe(H2O)4]4+ + 2H2O [(H2O)4 Fe OH (5.10) In other words, the two OH groups form bridges between the two nuclei, i.e., the two Fe3+ ions. These polynuclear species can in turn become hydrolyzed: OH OH Fe(H2O)4]4+ = [(OH)(H2O)3Fe [(H2O)4Fe OH Fe(H2O)3(OH)]2+ + 2H+ (5.11) OH The presence of this new hydrolyzed species can then lead to more polymerization: OH OH Fe(H2O)3(OH)]2+ + [(OH)(H2O)3Fe [(OH)(H2O)3Fe OH OH OH = [(OH) (H2O)3Fe Fe(H2O)3(OH)]2+ OH Fe(H2O)2 OH OH Fe(H2O)3(OH)]4+ + 2H2O (5.12) (H2O)2Fe OH OH Hydrolysis-polymerization reactions can proceed until finally the resulting polymers become too large to remain soluble, i.e., they achieve colloidal dimensions. When this stage is reached, we say we have precipitated a solid. In this hypothetical system consisting of only one type of metal ion in water (i.e., in the absence of anions or other metals ions), each polymerization reaction involves the elimination of water and therefore ultimately we would expect metal hydroxides to be formed. EXAMPLE 5.1 Hydrolysis reactions For each of the polynuclear hydroxo species below, write down the corresponding chemical equation that describes its formation via interaction of Mz+ and H2O. (a) Be6(OH)84+ (b) Zr4(OH)88+ Solution (a) 6Be2+ + 8H2O = Be6(OH)84+ + 8H+ (c) Mg4(OH)44+ (d) Co2OH3+ (b) 4Zr4+ + 8H2O = Zr4(OH)88+ = 8H+ (c) 4Mg2+ + 4H2O = Mg4(OH)44+ + 4H+ (d) 2Co2+ + H2O = Co2OH3+ + H+ 5.1.4 Structures of Polycations and Polyoxoanions The species of interest here are those in which metal ions are linked by hydroxyl (M-OH-M) and/or oxo (M-O-M) bridges. In the case of complexes based on M(II), M(III), and M(IV) atoms, the hydroxyl bridge is used almost exclusively. Table 5.1 presents a summary of the structural information on these species. (see Baes and Messmer, p. 420). It can be seen that symmetrical structures are preferred. In these structures, up to six cations are organized into groups of two, three, four, or six and the coordination number of the hydroxyl ion may be 2 or 3. The structure of the square-planar M4(OH)8(H2O)16 complex is illustrated in Figure 5.1a (B&M, p. 157). Adjacent metal cations are linked by a double bridge of hydroxyls. Each metal ion is eight-coordinate - through the oxygens of four hydroxyls and four water molecules. The M6(OH)84+ and M6(OH)126+ structures are illustrated respectively in Figures 5.1b and 5.1c. (See Baes & Mesmer, p.378) In addition to the species listed in Table 5.1, Al(III) forms the complex Al13O4(OH)247+. This species (Figure 5.1d; see Baes and Mesmer, p.118) consists of a central AlO45- tetrahedron surrounded by twelve AlO6 octahedra; the octahedra are linked by shared edges. In the case of the M(V) and M(VI) atoms, O2- bridges are prominent. The elements which form these polyoxoanions come predominantly from the left-side of the d-block: V(V), Nb(V), Ta(V), Cr(VI), Mo(VI), and W(VI). Table 5.2 shows that the polymerization ranges from dimers to 19-mers. The typical structure consists of MO6 octahedra linked at the corners or edges, as illustrated in Figure 5.2 (Huheey). Table 5.1 Polynuclear hydroxo complexes (Baes and Mesmer, p. 420) Species Probable structure = Mz+, o = OH- Cation (source) M2OH3+ M4(OH)88+ Be2+, Mn2+, Co2+, Ni2+, Zn2+, Cd2+, Hg2+, Pb2+ Cu2+, Sn2+, UO22+, NpO22+, PuO22+, VO2+, Al3+ Sc3+, Ln3+, Ti3+, Cr3+ Th4+ Be2+, Hg2+ Sn2+, Pb2+ Al3+, Cr3+, Fe3+, In3+ UO22+, NpO22+, PuO22+ Sc3+, Y3+, Ln3+ Mg2+, Co2+, Ni2+, Cd2+ Pb2+ Zr4+, Th4+ M6(OH)84+ Be2+, Pb2+ M6(OH)126+ Bi3+ M2(OH2(2z-2)+ M3(OH)33+ M3(OH)4(3z-4)+ M3(OH)5(3z-5)+ M4(OH)44+ M4 square with eight OHions, one centered over and under each edge. M6 octahedron with eight OH- ions centered on faces. M6 octahedron with 12 OHions centered along edges. Table 5.2 Polyoxoanions M2 V2O74- V(V) M3 M4 V3O93- V4O124- M6 Nb6O198- Ta(V) Ta6O198- M12 M19 Cr2O72Mo7O246- Mo(VI) W(VI) M10 V10O286- Nb(V) Cr(VI) M7 W6O192- Mo19O594W12O4110- See B&M under the various metal ions, Huheey, pp.755-764, SAL, pp.164-165) (a) (b) (c) (d) Figure 5.1 Structures of polycations: (a) M4(OH)8(H2O)168+ , (b) M6(OH)84+ (c) M6(OH)126+ , (d) the Al13O4(OH)247+ polycation. Figure 5.2 Evolution of the structures of polyoxoanions. (Huheey, p. 757) 5.2 5.2.1 The Concept of Equilibrium Constant The Solubility Product We learned from our hypothetical metal ion-water system above that successive polymerization-hydrolysis reactions can result in the precipitation of a solid. When a solid, let us say a metal hydroxide, M(OH)2(s), is placed in an aqueous solution, it will dissolve according to a reaction such as: M(OH)2(s) = M2+ + 2OH- (5.13) Actually, in view of the hydration of metal ions, it is more appropriate to write M(OH)2 (s) + 6H2O = M(H2O)62+ + 2OH- (5.14) We would also expect further reactions to occur in the aqueous solution, e.g., hydrolysis, and polymerization. As more and more solid dissolves, these aqueous phase interactions also increase in extent until finally, the reverse process, i.e., precipitation, starts. Thus, in effect, the dissolution process can be considered, ideally, in terms of a reversible reaction in which the forward reaction will be dissolution and the reverse reaction, precipitation. The criterion which is used to determine which of these two reactions predominates under a given set of conditions, are called the solubility product. The concentration solubility product for the metal hydroxide reaction (Equation 5.13) is defined as: Kso = [M2+] [OH-]2 (5.15) where Kso is the solubility product constant and the square brackets represent concentration. The solid M(OH)2 will precipitate out of solution when the product [M2+] [OH-]2 exceeds the value of Kso. Alternatively, it is sometimes more convenient to write the dissolution reaction in terms of the hydrogen ion: M(OH)2(s) + 2H+ = M2+ + 2H2O (5.16) In this case, the solubility equilibrium is described by *Kso = [M2+]/[H+]2 (5.17) 5.2.2 The Free Energy of Reaction and the Equilibrium Constant Consider a general reaction, aA + bB = cC + dD (5.18) For any arbitrary conditions (i.e., for a system not necessarily at equilibrium), the free energy is given by G = Go + RTln Q (5.19) where Go is the standard Gibbs free energy of the reaction and Q is the reaction quotient and is given by Q = {C}c{D}d/{A}a{B}b (5.20) where the symbol { } denotes activity. At equilibrium, G = 0, and the equilibrium value of Q (i.e., Qeq) is termed the equilibrium constant, K: b K = {C} ceq {D} deq /{A} aeq {B}eq (5.21) Go = -RT 1n Qeq = -RT 1n K (5.22) It follows therefore that Application of Equation 5.22 to Equation 5.19 gives: G = RT (1n Q - 1n K) When (5.23) G = 0, equilibrium has been attained and ln Qeq = 1n K G < 0, G > 0, reactants form products simultaneously and ln Q < ln K conversion of reactants to products is impossible; however the reverse reaction is spontaneous and 1n Q > 1n K The standard Gibbs free energy of reaction is a function of the standard free energies of formation (Gof) of the reactants and products associated with the reaction. That is, for the general reaction described by Equation 5.18, the standard Gibbs free energy (Go) is given by: o o o o Go = cGf (C) + dGf (D) - aGf (A) - bGf (B) (5.24) o where Gf (C) is the standard free energy of formation of species C, etc. In infinitely dilute solutions, the activity of a dissolved species equals its concentration, i.e., {C} = [C], etc., and therefore under these conditions, Q = [C]c [D]d/[A]a[B]b (5.25) In more concentrated solutions, however, enhanced ionic interactions lead to nonidealities and the ionic activity generally deviates significantly from the concentration. Under these circumstances the concentration and activity can be related through an activity coefficient (), defined for species A as: {A} = A [A] (5.26) The activity coefficient of a given species is a function of the total ionic concentration in the electrolyte. Nonideality effects are treated in greater detail in Chapter 6. For the rest of this chapter it is assumed that the aqueous solutions are infinitely dilute so that concentration and activity equilibrium constants are numerically the same. The quantities Kso and K *so defined above (see Equations 5.15 and 5.17) are equilibrium constants. Referring to Equation 5.13 and recalling Equations 5.18 and 5.20, we can write: 2 /{M(OH) (s)} = {M2+} {OH-} 2 Kso = {Mz+}eq{OH-} eq 2 eq eq eq 2 = [M2+]eq[OH-] eq (5.27a) (5.27b) In equation 5.27a use is made of the fact that the activity of a pure substance is unity, i.e., {M(OH)2(s)} = 1; Equation 5.27b results from Equation 5.27a, upon applying the assumption of infinitely dilute solution. The ionization of water, Equation 5.8 is also characterized by an equilibrium constant, termed the ionization constant, Kw: Kw = {H+}eq{OH-}eq/{H2O}eq = {H+}eq{OH-}eq (5.28a) = [H+]eq[OH-]eq (infinitely dilute condition) = 10-14 at 25°C (5.28b) In Equation 5.28a, the activity of water is indicated as unity since for an infinitely dilute solution the solvent water may be considered to be a pure substance. EXAMPLE 5.2 Calculation of equilibrium constants from free energy data Based on the G of data (Wagman et al, The NBS Tables of Chemical Thermodynamic Properties, 1982) provided below, determine the free energies of reaction and the equilibrium constants for the following reactions: (a) 1/2O2 + H2 = H2O (b) H+ + OH- = H2O (c) CuO + 2H+ = Cu2+ + H2O (d) Cu2+ + H2 = Cu + 2H+ Solution First we must recall Equation 5.22: o o logK = -Gr /2.303 RT = -Gr /(2.303) (8.3143 Jmol-1K-1) (298.15K) = -G or /5.709, with G or in kJ mol-1 Note that this expression is valid only for 25°C, i.e., T = 298.15 K (a) o G or = G of (H 2 O) - 1/2 G of (O 2 ) - Gf (H2) = (-237.129)-1/2(0) - (0) = -237.129 kJ mol-1 logK = -G or /2.303 RT = -(-237.129)/5.709 = 41.54 (b) o G or = G of (H 2 O) - G of (H ) -Gf (OH-) = (-237.129) - (0) - (-157.244) = - 79.89 kJ mol-1 logK = - G or /2.303 RT = -(-79.89)/5.709 = 14.0 (c) o G or = G of (Cu 2 ) + G of (H 2 O) - G of (CuO ) - 2Gf (H+) = (65.49) + (-237.129) - (-129.7) - 2 (0.) = - 41.94 kJ mol-1 o logK = -Gr /2.303 RT = - (-41.94)/5.709 = 7.35 (d) G or = G of (Cu ) + 2G of (H ) - G of (Cu 2 ) - G of (H 2 ) = (0) + 2(0.) - (65.49) - (0.) = - 65.49 kJ mol-1 o logK = -Gr /2.303 RT = - (-65.49)/5.709 = 11.47 5.2.3 Solubility Calculations The equilibrium constant represents an important parameter which allows us to make theoretical predictions and assess the likelihood of reactions. Suppose we wish to find the equilibrium constant for the dissolution-precipitation reaction described by Equation 5.16. This can be done by combining Equation 5.13 with Equation 5.8: (-2)x Eq. 5.8: M(OH)2(s) = M2+ + 2OH- Kso 2H+ + 2OH- = 2H2O 1/Kw (5.30) M(OH)2(s) + 2H+ = M2+ + 2H2O *Kso (5.16) (5.29) 2 The equilibrium constant for Equation 5.16 is given by: 2 *Kso = [M2+]eq/[H+]eq2 = [M2+]eq[OH-]2eq/[OH-]eq2[H+]eq2 = Kso/Kw (5.31) In general, for a hydroxide M(OH)z(s), the following relation holds, z *Kso = Kso/Kw (5.32) Let us consider Equation 5.16 again. Using the definition of the reaction quotient for infinitely dilute solution, i.e., Equation 5.25, it follows that, Q = {M2+}/{H+}2 = [M2+]/[H+]2 (5.33) The equilibrium condition is then given by logQeq = log*Kso (5.34) Therefore, from Equations 5.33 and 5.34, log[M2+]eq = -2pHeq + log*Kso (5.35) where pH is defined as: pH = - log {H+} = - log [H+] (infinite dilution condition) 5.2.4 (5.36a) (5.36b) Solubility of Sparingly Soluble Salts Consider the salt MyAz consisting of cations Mz+ and anions Ay-. When this salt is present in a saturated solution of its ions, a chemical equilibrium exists: MyAz(s) = yMz+ + zAy- (5.37) The equilibrium constant, i.e., solubility product, is given by Kso = [Mz+]y [Ay-]z (5.38) where it is understood that the respective activities are equilibrium values. According to Equation 5.37, dissolution of one mole of salt yields y moles of cations and z moles of anions. Let C represent the solubility of the salt M yAz in pure water, e.g., the moles of salt which dissolve to give one liter of saturated solution. Then a mass balance on the dissolved species gives, [Mz+] = yC [Ay-] = zC (5.39) (5.40) Therefore, Equation 5.38 becomes Kso = [yC]y [zC]z (5.41) EXAMPLE 5.3 Solubility of sparingly soluble salts a) Determine the solubility product of barium sulfate, BaSO 4, at 25°C given that the solubility of this salt is 1.05 x 10-5 mol/liter. b) Calculate the solubility of calcium fluoride, CaF2, using the fact that the solubility product of this salt is 4.0 x 10-11. c) On the basis of the results obtained in part (a), determine the solubility of BaSO 4 in 1.0 x 10-4 molar BaCl2 solution. Solution 2(a) BaSO4(s) = Ba2+ + SO4 Dissolution of one mole of salt yields one mole of Ba2+ and one mole of SO 24 . Let C be the solubility of the salt. Then it follows that: 2[Ba2+] = [SO4 ] = C = 1.05 x 10-5 mol/L Thus 2Kso = [Ba2+] [SO4 ] = (1.05 x 10-5)2 = 1.10 x 10-10 (b) CaF2(s) = Ca2+ + 2FDissolution of one mol of salt yields one mole of Ca2+ and two moles of F-. Thus if C is the solubility of the salt, then, [Ca2+] = C and [F-] = 2C Thus Kso = [Ca2+][F-]2 = (C) (2C)2 = 4C3 Therefore C = (Kso/4)1/3 = (4.0 x10-11/4)1/3 = 2.15 x 10-4 mol/L (c) Let the solubility be C mol/L. Now the solution also contains 1.0 x 10 -4 mol/L BaCl2. Thus [Ba2+] = (C + 1.0 x 10-4) mol/L 2Kso = 1.10 x 10-10 = [Ba2+] [SO4 ] = (C + 1.0 x 10-4) (C) That is, C2 + 1.0 x 10-4 C - 1.10 x 10-10 = 0 Applying the quadratic formula, C = -1.0x10-4 + (1.0x10-4)2 - 4(1)(-1.0x10-10) 2(1) = (-1.0 x 10-4 + 1.02 x 10-4)/2 = 1.0 x 10-6 mol/L 5.2.5 Lattice Energy, Hydration Energy, and Solubility Some insight into the energetics of the dissolution of ionic solids may be gained by considering the thermodynamic cycle presented in Figure 5.3. The free energy change associated with the disintegration of the solid MyAz(s) into isolated gaseous ions is represented by GLo. The hydration of the gaseous ions when they are introduced into the aqueous phase results in the free energy change Gho. The free energy of solution of the solid is depicted as Gso. It follows from Figure 5.3 that Gso = GLo + Gho (5.42) yMz+ (g) + zAy- (g) Gh GL My Az (s) Gs yMz+ (aq) + zAy- (aq) Figure 5.3 Thermodynamic cycle illustrating the contributions to the standard free energy of solution. Recalling the Kapustinskii equation (Equation 4.8), etc., we can write GLo as: GLo = K (y + z)(z+y-)/(r+ + r-) - 31.1 (y + z) kJ mol-1 (5.43) K = 1.079 x 105 kJ mol-1 pm (see Johnson, p.48). Also an ionic model of ion hydration (see Chapter 6) results in the following equation for the free energy of hydration: Gho = -[B z2/(r + k)] + 7.9 kJ mol-1 (5.44) where B = 6.8583 x 104 kJ mol-1 pm, r is the ionic crystal radius, k has a value of 80 pm for cations and 17 for anions. (See SAL, pp.133-135; Huheey, pp.310-314; Johnson, pp.116-) 5.3 5.3.1 Acids and Bases Acidic and Basic Solutions As indicated in Equation 5.28b the ionization constant of water has a value of 1014 at room temperature. Thus, in an equilibrium aqueous system containing only pure water, [H+] = [OH-] = Kw 1/2 = 10-7 (5.45) pH = 7 (5.46) or Pure water is considered to be neutral and the solution is said to be an acidic solution when [H+] > [OH-] or pH < 7 (5.47) On the other hand, the solution is considered a basic solution when [H+] < [OH-] or pH > 7 (5.48) Shifts in pH from the neutral value are obtained by introducing acids and bases into the aqueous system. According to the Bronsted acid-base concept, an acid is a proton donor while a base is a proton acceptor. That is, the ionization of an acid (HA) may be written as: HA = H+ + A- (5.49) In contrast, the ionization of a base (B) may be represented as: B + H+ = BH+ (5.50) EXAMPLE 5.4 The neutral pH of hydrothermal solutions The ionization constant of water varies with temperature. Determine the pH of neutral solution at elevated temperatures given the following data: T(°C) Kw 100 -12.26 200 -11.27 300 -11.39 Solution For neutral pH, [H+] = [OH-] = Kw1/2 (Eq. 5.45). Therefore, the corresponding pH is given by pH = -(1/2) log Kw. Accordingly, neutral pH has the following values: 6.13 (100 oC), 5.64 (200 oC), 5.70 (300 oC). 5.3.2 Strong Acids and Bases A strong acid is one which dissociates completely to give protons and the corresponding anions. Similarly a strong base is completely protonated to give the corresponding ionic form. In contrast, weak acids and bases are only partially dissociated. Table 5.3 presents a collection of several strong acids and bases. Table 5.3 Ionization of Strong Acids and Bases Name of Acid or Base Chemical Formula Ionization Reaction Nitric acid HNO3 HNO3 = H+ + NO3- Nitrate Sulfuric acid H2SO4 Hydrochloric acid Hydrobromic acid Hydroiodic acid Perchloric acid HCl HBr HI HClO4 Lithium hydroxide Sodium hydroxide Potassium hydroxide Rubidium hydroxide Cesium hydroxide LiOH NaOH KOH RbOH CsOH H2SO4 = H+ + HSO4HCl = H+ + ClHBr = H+ + BrHI = H+ + IHClO4 = H+ + ClO4LiOH = Li+ + OHNaOH = Na+ + OHKOH = K+ + OHRbOH = Rb+ + OHCsOH = Cs+ + OH- Anion____ pKa___ Bisulfate -2 Chloride Bromide Iodide Perchlorate -7 -9 -11 -10 Hydroxyl Hydroxyl Hydroxyl Hydroxyl Hydroxyl The pH of solutions of strong acids and bases can be calculated by combining the ionization equilibrium of water with appropriate mass balances. Consider a solution containing C mol/L of the strong acid HA. We wish to determine the pH of this solution. In view of the ionization of water, the following condition must be satisfied: [H+][OH-] = Kw (5.51) Let [H+]' represent the concentration of protons released into the solution by the ionization of water. Then, since each proton produced from a water molecule also leads to the release of a hydroxide ion, [H+]' = [OH-] (5.52) Also, let [H+]" represent the concentration of protons associated with the dissociation of HA. Then, since HA is a strong acid, there is complete dissociation, and therefore [H+]" = [A-] = C (5.53) Thus, a mass balance on hydrogen ions may be written as: [H+] = [H+]' + [H+ ]" = [OH-] + C (5.54a) (5.54b) Combination of Equations 5.51 and 5.54b, with elimination of [OH-], gives [H+] as a quadratic equation: [H+]2 - C[H+] - Kw = 0 (5.55) Since [H+] has to be a positive number, the solution of Equation 5.55 is [H+] = [C + (C2 + 4 Kw)1/2]/2 (5.56) It can be seen from this expression that [H+] ~ C for C >> 2Kw1/2 (5.57a) ~ Kw1/2 for C << 2Kw1/2 (5.57b) Thus, the proton concentration of a highly concentrated solution of a strong acid corresponds to the analytical concentration of the acid. In contrast, the proton concentration in a very dilute solution of a strong acid is the same as that of pure water. EXAMPLE 5.5 Concentration dependence of the pH of a strong acid Determine the pH of a strong acid solution with the following concentrations (mol/L): (a) 10 -4, (b) 10-7, (c) 10-10. Solution We recall that Kw = 10-14. Therefore, Kw1/2 = 10-7. (a) C = 10-4 mol/L >> 2 Kw1/2. Thus, it follows from Equation 5.57 that [H+] = C = 10-4. Therefore, pH = 4. (b) Here C = 10-7 mol/L = Kw1/2. Therefore, we must use the complete expression, Equation 5.56. We find [H+] = 1.62 x 10-7 mol/L. Therefore, pH = 6.8 (c) C = 10-10 mol/L << 2 Kw1/2. Accordingly, invoking Equation 5.58, pH = -log(Kw1/2) = 7.00 A similar approach may be taken for the determination of the pH of a strong base. As + - already noted above, the dissociation of a water molecule releases one H ion and one OH . Thus, if [OH-]' represents the concentration of hydroxide ions released into solution via the dissociation of water, then it follows that: - + [OH ]' = [H ] (5.58a) Consider a base M(OH)z, which dissociates as: M(OH)z = Mz+ + zOH- (5.58b) For a strong base M(OH)z, there is complete ionization. Let the solution contain C mol/L - of the base. Let [OH ]" represent the concentration of hydroxide ions present in solution as a result of the dissociation of the base. Then, since the dissociation of a mole of M(OH)z produces a mole of M z+ - plus z moles of OH , [OH-]" = z[Mz+] = zC (5.58c) It follows, therefore, that the total hydroxide concentration is given by [OH-] = [OH-]' + [OH-]" = [H+] + zC (5.58d) + - Recalling the ionization equilibrium of water, we can use the fact that [H ] = Kw/[OH ]. Thus, Equation 5.58d can be rewritten as: [OH-] = (Kw/[OH-]) + zC (5.58e) That is, -2 - [OH ] - zC[OH ] - Kw = 0 (5.58f) [OH-] = [zC + (z2C2 + 4Kw)1/2]/2 (5.58g) Therefore, The relevant limiting conditions are: - [OH ] ≈ zC, [H+] = Kw/zC for zC >> 2Kw1/2 + ≈Kw1/2, [H ] = Kw1/2 for zC << 2K w1/2 (5.58h) (5.58i) _________________________________________________________________________ EXAMPLE 5.6 Concentration dependence of the pH of a strong base Repeat Ex.5.5 for the solution of a strong base MOH. 5.3.3 Weak Monoprotic Acids and Bases As indicated above in Section 5.3.2, weak acids and bases are not completely dissociated. Table 5.4 presents examples of weak monoprotic acids and bases, i.e., weak acids which dissociate to give only one proton per molecule, and weak bases which can only bind one proton. Acids carrying more than one ionizable proton (called polyprotic acids) and bases capable of binding more than one proton are considered in Chapter 7. Table 5.4 also includes equilibrium constants for the various dissociation reactions. In the case of the acids, the greater the numerical value of log K, the greater the tendency for the acid to ionize. Examination of the tabulated log K values therefore clearly indicates that the designation "weak" is a relative term. For example, it will be noticed that log K = 1.92 for methylsulfonic acid whereas the corresponding value for phenol is -9.98. Thus, the sulfonic acid is a much stronger acid than phenol. In the case of the amines, the greater the numerical value of log K, the greater the tendency towards protonation, i.e., the stronger the base. Therefore, here too, there is a range of basicities, with dimethylamine (log K = 10.77) giving the highest and aniline (log K = 4.60) giving the lowest. The pH of a solution of a weak acid or base may be determined by combining the equilibrium expressions for the ionization of water, and the acid or base with appropriate mass balances. Consider the weak acid HA which dissociates as HA = H+ + A- (5.59) The corresponding equilibrium constant is given by: K = [H+] [A-]/[HA] (5.60) A mass balance on the proton gives [H+] = [H+]' + [H+]" = [OH-] + [A-] (5.61) Table 5.4 Ionization of Weak Monoprotic Acids and Bases Name of Acid or Base Chemical Formula Ionization Reaction log K Methylsulfonic acid CH3SO3H CH3SO3H = H+ + CH3SO3 -1.92 Hydrogen sulfate ion HSO4 2HSO4 = H+ + SO4 -1.99 Hydrofluoric acid HF HF = H+ + F- -3.17 S || Diethyldithiocarbamic acid (C2H5)2C-SH (C2H5)2C(S)SH = H+ + (C2H5)2C(S)S- -3.42 Formic acid HCOOH HCOOH = H+ + COO- -3.75 Acetic acid CH3COOH CH3COOH = H+ + CH3COO- -4.76 Hydrogen hypochlorite HOCl HOCl = H+ + OCl- -7.53 Hydrogen hypobromite HOBr HOBr = H+ + OBr- -8.63 Hydrocyanic acid HCN HCN = H+ + CN- -9.21 Phenol (Hydroxybenzene) OH O- OH O O = H+ + -9.98 O Hydrogen hypoiodite HOI HOI = H+ + OI- -10.64 Dimethylamine (CH3)2N (CH3)2NH + H+ = (CH3)2NH4+ 10.77 Methyl amine CH3NH2 CH3NH2 + H+ = CH3NH3+ 10.64 Trimethylamine (CH3)3N (CH3)3N + H+ = (CH3)3NH+ Ammonia NH3 NH3 + H+ = NH4+ O Pyridine Aniline O N O - NH2 O 9.80 9.24 O + + N +H = NH 5.23 - NH2 + H+ = O - NH3+ 4.60 where [H+]' and [H+]" respectively represent the protons released by the dissociation of the water and acid molecules. If the acid is present in solution at an analytical concentration of C, then a mass balance on the anion becomes: C = [HA] + [A-] (5.62) where [HA] is the concentration of the residual unionized acid. Combination of Equations 5.60 and 5.62 gives: [A-] = C/(1 + [H+]/Ka) (5.63) [HA] = C([H+]/Ka)/(1 + [H+]/Ka) (5.64) Recalling the equilibrium relation for the ionization of water, [OH-] = Kw/[H+] (5.65) Substitution of Equations 5.63 and 5.65 respectively for [A-] and [OH-] in Equation 5.61 gives the following results: [H+] = Kw/[H+] + C/(1 + [H+]/Ka) (5.66a) C = (1 + ([H+]/Ka))([H+] - (Kw/[H+])) (5.66b) EXAMPLE 5.7 The pH of a weak acid solution Determine the pH of a 10-3 mol/L solution of (a) hydrogen sulfate ion (pK a = 1.99), (b) formic acid (pKa = 3.75), (c) hypochlorous acid (pKa = 7.53), (d) phenol (pKa = 9.98) Solution 5.4 Structural Aspects of Acid-Base Strength 5.4.1 Gas-Phase Acidity We saw above that the strength of a Bronsted acid, HA, is expressed by the acid ionization constant: HA(aq) + H2O = A-(aq) + H3O+(aq) Ka (5.67) We found that some acids are strong (Ka > 1, pKa < 0; Table 5.3), while others are weak (Ka <1, pKa > 0; Table 5.4). We now wish to address this question: what are the factors that govern acid strength ? A convenient starting point is to consider the feasibility of gas-phase proton transfer. It is helpful to define a quantity termed the proton-gain enthalpy, Hpo, which is the standard enthalpy of protonation for the following gas phase reaction: A- + H+ = HA Hpo (A-) (5.68) A related quantity is the proton affinity, Ap, defined as the negative of the proton-gain enthalpy (i.e., Ap = -Hpo). The proton affinity is high when proton attachment is highly favored, as reflected in a highly negative value of the proton-gain enthalpy. Proton affinity values for selected bases are presented in Table 5.5 (Shriver, p.152). We can use a thermodynamic cycle to discern the factors that contribute to the magnitude of the proton affinity. On the basis of the thermodynamic cycle presented in Figure 5.4, the proton-gain enthalpy can be expressed as: Hpo (A-) = Ae(A) - I(H) -B(HA) (5.69) where Ae(A) = the electron affinity of A, I(H) = ionization energy of H, and B(HA) = the H-A bond enthalpy. Alternatively, the proton afinity can be expressed as: Ap = -Hpo = B(HA) + I(H) - Ae(A) (5.70) Equations 5.69 and 5.70 can be used to rationalize trends observed when one goes across the period or down a group in the Periodic Table. Thus, on proceeding from left to right across a period, the electron affinity increases, and this is expected to lower the proton affinity. On the other hand, as one goes down a group, the bond dissociation enthalpy decreases, and this should decrease the proton affinity. Table 5.5 Proton affinities (Shriver, p.152) Conjugate acid Base F- HF Ap/kJ mol-1 Ap/kJ mol-1 1553 1150 HCl Cl - 1393 1090 HBr Br- 1353 1079 - HI I 1314 1068 CH4 CH3- 1741 1380 NH3 NH2- 1670 1351 PH3 PH2 - 1548 1283 H2O OH- 1634 1188 - CN 1476 1183 H2O 723 1130 NH3 865 1182 936 1160 HCN + H3O NH4+ + C6H5NH C6H5N o *Ap = -Hp is the gas-phase proton affinity: Ap the effective proton affinity for the base in water. Source: J. E. Bartmess and R. J. McIver, in Gas Phase Ion Chemistry, M. T. Bowers (ed.). Academic Press. New York (1978). A- (g) + H (g) -I (H) - eA e (A) A (g) + H (g) + e- -B (HA) - A (g) + H +(g) HA (g) Hop (A- ) Figure 5.4 Thermodynamic cycle illustrating the contributions to the proton affinity. EXAMPLE 5.8 Proton transfer to water in the gas phase On the basis of the gas-phase proton affinity values presented in Table 5.5, determine the feasibility of proton transfer from the various acids to water in the gas phase. Solution The proton transfer to water in the gas phase can be evaluated as shown below: HA(g) = A-(g) + H+(g) -Hpo (A-) H2O(g) + H+(g) = H3O+(g) Hpo (H2O) __________________________________________ HA(g) + H2O(g) = A-(g) + H3O+(g) (1) Ho = Hpo (H2O) - Hpo (A-) = Ap (A-) - Ap (H2O) (4) (2) (3) According to Equation 4, in order for proton transfer from an acid HA to water to be favorable in the gas phase (i.e., Ho < 0), we must have Ap(A-) < Ap (H2O). As can be seen from Table 5.5, none of the acids listed satisfies this condition. 5.4.2 Hydration Effects The conclusion obtained in Ex. 5.8 (which involves gas-phase proton transfer) appears to contradict our everyday experience with aqueous solutions: HCl, for example, is a strong acid that readily transfers protons to water molecules in aqueous solution. This apparent contradiction is resolved by recognizing the key role played by hydration in proton transfer in aqueous solution. To account for hydration effects, an effective proton affinity, Ap', is defined on the basis of the enthalpy change associated with the gas-phase transfer of a proton to a cluster of water molecules. Values of Ap' are also included in Table 5.5, and these can be used to treat proton transfers in aqueous solution: HA(aq) + H2O(aq) = A-(aq) + H3O+(aq) Ho = Ap'(A-) - Ap'(H2O) (5.71) When the Ap and Ap' values in Table 5.5 are compared, it can be seen that for all the bases above H2O, hydration decreases the proton affinity (Ap(A-) > Ap'(A-)). On the other hand, for H2O, NH3, and C5H5N, hydration increases the proton affinity (Ap < Ap'). The decrease in proton affinity means that hydration stabilizes A-. On the other hand, the increase in proton affinity means that hydration stabilizes A (e.g., H3O+, NH4+, and C5H5NH+). It is interesting to note that in these examples, the stabilized species are the charged conjugate species (e.g., Cl- vs. HCl, NH4+ vs. NH3). These trends illustrate the fact that the electrostatic interactions between water dipoles and ions will stabilize ions in solution relative to the gas phase. Thus for a series of bases, we expect proton affinity to increase with decrease in ionic size and with increase in ionic charge. Another factor which influences proton affinity is hydrogen bonding between aqueous species and water molecules. _________________________________________________________________________ EXAMPLE 5.9 Trends in the basicity of ammonia and substituted amines The ability of an ammonia molecule to accept a proton, i.e., its basicity, is related to the availability of the lone electron-pair on the nitrogen atom (H3N: ->H+). Using this fact and the ability of H2O to serve as a hydrogen-bond acceptor, as noted above, rationalize the following trends in the basicity of ammonia and amines. (a) How would one expect the basicity to change upon substituting one of the hydrogen atoms in ammonia with (i) an electron-withdrawing group, (ii) an electron-donating group. (b) Given pKb (MeNH2) = 3.36, pKb (NH3) = 4.74, pKb (NH2NH2) = 5.77, pKb (NH2OH) = 7.97, determine whether the groups -Me, -NH2, and -OH are electron-donating or electron-withdrawing. (c) On the basis of the finding in part (b), speculate about the trend in the gas-phase basicity of the following methylamines: MeNH2, Me2NH, Me3N. (d) Rationalize the following trends: pKb (NH3) = 4.74, pKb (MeNH2) = 3.36, pKb (Me2NH) = 3.29, pKb (Me3N) = 4.28 Solution (a) An electron-withdrawing group will decrease the availability of the lone-pair electron and this would be expected to decrease the proton affinity and therefore the basicity. On the other hand, an electron-donating group will amplify the availability of the lone-pair electron, which should register as an increase in basicity. (b) On the basis of part (a), since substitution of -NH2 or -OH results in a decrease in basicity (an increase in pKb), these groups must be electron-withdrawing. On the other hand, the presence of the -Me group increases the basicity (a decreaase in pK b) and therefore this group must be electron-donating. (c) Since the -Me group was found above to be electron-donating, one would expect the basicity to increase with successive substitution of this group, i.e., the trend NH 3 < MeNH2 < Me2NH < Me3N. (d) The trend expected from electron donation (part (c)) is satisfied with respect to the trend pK b (NH3) > pKb (MeNH2) > pKb (Me2NH). The trend pKb (Me2NH) < pKb (Me3N) is, however, unexpected. This reversal in basicity can be rationalized by considering the role of hydrogen bonding in the solvation of the ammonium ions. As already noted above, hydration enhances basicity. Thus, for the protonated amines, hydrogen bonding is mediated through the hydrogen atoms, and consequently, the extent of hydrogen bonding and hence increased basicity is expected to follow the order: MeNH2 > Me2NH > Me3N. This is the reverse of the trend based on electron donation. Hence, the basicity goes through a maximum with increasing substitution. ________________________________________________________________________________________ 5.4.3 Strengths of Hydroxyl -Group Acids Hydroxyl-group acids are characterized by the presence of hydroxyl groups which can deprotonate. These acids fall into three classes, i.e., aqua acids (e.g., M(OH2)nz+), hydroxoacids (e.g., M(OH)z), and oxoacids (e.g., H2SO4). In an aqua acid, the hydroxyl group comes from a water molecule attached to a metal ion. In the case of a hydroxoacid, the hydroxyl group is attached directly to the central atom and no oxo group is bonded directly to this atom. An oxoacid results when the central atom is bonded to both a hydroxo group and an oxo group. The progression: aqua acid hydroxoacid oxoacid, can be considered in terms of a consecutive deprotonation process: H2O-M-OH2 (aqua acid) = HO-M-OH (hydroxoacid) + 2H+ (5.72) HO-M-OH (hydroxoacid) = HO-M=O (oxoacid) + H+ (5.73) Which elements are most likely to form aquoacids? Typically in aquo acids, the central atom has a low oxidation number: atoms from the s-block, d-block, and leftside of the p-block. In some cases, trends in the acidities of aquo acids can be correlated with an electrostatic model. This is the case when the central atom of the aquo acids is derived from s-block elements. These are also the elements which have the greatest tendency to form ionic solids. Here the tendency to deprotonate is expected to increase with increase in charge and decrease in size. Such an electrostatic model is less useful for the d-band and pblock metals, where there is significant covalent bonding. Trends for oxoacids (see SAL, p.159) 5.5 Graphical Representations of Ionic Equilibria 5.5.1 Logarithmic Concentration Diagrams Recall Equation 5.16: M(OH)2(s) + 2H+ = M2+ + 2H2O (5.16) For a given pH, when [M2+] is less than the equilibrium value, it follows from Equations 5.33 and 5.34 that log Q < log K and Equation 5.16 proceeds from left to right, i.e., dissolution takes place. Under these conditions, it can be said that M2+ is more stable than M(OH)2(s). On the other hand, when [M2+] is greater than the equilibrium value, the reaction proceeds from right to left, i.e., precipitation occurs, and in this case M(OH)2(s) is more stable than M2+. Thus for the M2+ - M(OH)2(s) pair, M2+ is the stable species when log[M2+] < -2pH + log *Kso (5.74) while M(OH)2(s) is the stable species when log[M2+] > -2pH + log *Kso (5.75) We saw previously that the concentration of metal ion, [M2+]eq, which is in equilibrium with the metal hydroxide M(OH)2(s) is given by log[M2+]eq = -2pHeq + log*Kso (5.76) y = mx + c (5.77) This equation is of the form i.e., the equation of a straight line with a slope m = -2, and an intercept at log[M2+]eq = 0 given by pHeq = (1/2) log*Kso (5.78) Thus, assuming a negative slope, it can be seen that on a log[M2+] versus pH plot, M2+ will be stable to the left of this straight line (Equation 5.74) while M(OH)2(s) will be stable to the right (Equation 5.75). EXAMPLE 5.10 The solubility diagram for Fe(OH)3 in acidic solution The following reaction occurs in the Fe(OH)3(s)-H2O system: Fe(OH)3(s) + 3H+ = Fe3+ + 3H2O where log *Kso = 3.3. Prepare a log[M] vs pH diagram that describes the solubility of Fe(OH) 3(s). Solution Following Equation 5.35, 5.76, and 5.77, the solubility relation is given by log[Fe3+]eq = 3.3 -3pHeq (1) Furthermore, according to Equations 5.76 and 5.77, the straight line represented by Equation 1 can be drawn as shown in Figure E.5.10. Finally, recalling the inequalities given by Equations 2.74 and 2.75, Fe 3+ is stable to the left of this line, while Fe(OH)3(s) is stable to the right. 0 -1 -2 Fe(OH) 3 (s) 3+ log[Fe ] -3 Fe3+ -4 -5 -6 0 2 pH 4 6 Figure E.5.10 Solubility of Fe(OH)3(s), (neglecting hydrolysis). EXAMPLE 5.11 Selective precipitation and selective dissolution a) You have been asked to investigate the method of selective-precipitation as a means of separating metal ions from each other. A multicomponent solution containing Ag+, Zn2+, Ca2+ at 10-5 mol/liter each has been provided. The solution is initially acidic and you have a bottle of concentrated NaOH (caustic soda) at your disposal. As you add the caustic soda solution dropwise, (i) Which of the metals would you expect to precipitate first? (ii) What is the order in which the remaining metals would precipitate? (iii) What would be the concentration of the other metals when the last metal ion begins to precipitate? b) In another experiment similar to that described above, you presented your technician with a solution containing 1 mol/liter each of Mg2+, Cu2+, Ca2+, Fe3+. Unfortunately, you explained your technique hurriedly to the technician and you came back to find that instead of adding caustic soda dropwise, he added a large dose at once, thereby, precipitating all the ions from solution. You decide then to apply the technique of selective dissolution(leaching) to separate the metal ions in the precipitate from each other. In this method, you add sulfuric acid dropwise to an aqueous slurry of the precipitate. (i) Which of the metals will dissolve first? (ii) Which will dissolve last? Relevant thermodynamic data are provided below: Reaction Fe(OH)3(s) = Fe3+ + 3OHCu(OH)2(s) = Cu2+ + 2OHZn(OH)2(s) = Zn2+ + 2OHMg(OH)2(s) = Mg2+ + 2OHCa(OH)2(s) = Ca2+ + 2OHAg(OH) (s) = Ag+ + OH- logK(25°C) -38.7 -19.0 -16.0 -9.2 -5.43 -7.8 It was assumed in Ex. 5.10 that the solids were in equilibrium with only hydrated metal ions, i.e., we ignored the fact that metal ions may be hydrolyzed in aqueous solution. In fact, to fully describe the solubility of solids, we need to take into account the possibility that solids may be in equilibrium with hydrolyzed metal ions. Like the dissolutionprecipitation reactions discussed above, hydrolysis reactions are also characterized by equilibrium constants. These constants can be combined with solubility product constants to establish the solubility of an oxide or hydroxide over the entire acid to alkaline pH range. This more complicated situation is addressed in Chapter 7. Another kind of concentration diagram is that describing the dissociation of a weak acid or base. For the acid HA, the effect of pH on the concentration ([A]) of HA or A - can be depicted graphically in terms of a log [A] vs pH plot. Referring to Equations 5.63 and 5.64, the following limiting results may be obtained: Low pH (i.e., [H+] >> K): [A-] = CK/[H+] (5.78) log [A-] = log C + log K + pH (5.79) [HA] = C (5.80) log [HA] = log C (5.81) or Also, or High pH (i.e., [H+] << K): [A-] = C or (5.82) log [A-] = log [C] (5.83) [HA] = C[H+]/K (5.84) log [HA] = log C - logK - pH (5.85) Also, or Figure 5.5 presents a schematic illustration of the above log [A] vs. pH relationships. log[C] [HA] [A- ] log[A] pKa pH Figure 5.5 A schematic speciation diagram for the weak acid HA. 5.5.2 Distribution Diagrams Let us return to the acid HA. Again Let C be the analytical concentration of the acid in aqueous solution. Then we can define the following concentration fractions: A = [A-]/C HA = [HA]/C (5.86) (5.87) A plot of A vs. pH is termed the dissociation curve. On the other hand a plot of HA vs. pH is called the formation curve. These plots may also be designated as distribution diagrams; a vertical line drawn through a given pH directly indicates the relative amounts of the acid-derived species A- and HA. For example in the case of the HA vs. pH curve, the region below the curve gives HA whereas that above the curve corresponds to A. EXAMPLE 5.12 Distribution diagrams for weak bases Using the logK data provided in Table 5.4, prepare distribution diagrams for the following: (a) weak bases: ammonia, aniline, and dimethylamine. (b) weak acids: formic acid, hydrogen hypochlorite, hydrogen sulfate ion, and phenol. Solution 5.6 The Partial Charge Model and the Reactions of Metal Cations 5.6.1 The Acidity of Hydrated Metal Cations In Section 2.4.3, the concept of electronegativity equalization was presented. According to this concept, the shared electrons in a stable molecule are distributed among the constituent atoms in such a manner that the electronegativity (i) of each bonded atom attains the same magnitude as the mean electronegativity of the complex (). As discussed in Section 2.4.3, this electronegativity equalization results in the acquisition of partial charges by the constituent atoms. For a complex with total charge z, the partial charges on the constituent atoms satisfy the condition: z = pi i (5.89) i where pi is the number of moles of atom i in one mole of the complex. The partial charge distribution in a molecule provides a powerful predictive tool for the aqueous chemistry of metal cations. EXAMPLE 5.13 Partial charge distribution in hydrated metal cations z+ 2+ 3+ Determine the mean electronegativity () of the following M(OH)6 species: (a) Mg , (b) Al , (c) 5+ 6+ Ti , (d) V , (e) W . For each hydrated species, determine the partial charges on the constituent atoms. 4+ Solution (a) 2+ Mg(OH2)6 : From Table 2.9 (Allred-Rochow), oMg = 1.23, H = 2.20, oO = 3.50. Also, for o the hydrated M(II) cation, z=2. Thus, using Equation 2.12h, = [1.11 + 17.80 + 11.23 + 2.72]/[(0.90) + (8.09) + (3.21)] = 32.86/12.2 = 2.69 Then, from Equation 2.12g, H = ( - H )/1.36(H ) = (0.49)/2.02 = 0.24 o o 1/2 = (2.69-2.20)/1.36(2.20) 1/2 O = (-O )/1.36(O ) = (2.69 - 3.50)/1.36 (3.50) = -0.81/2.544 = -0.32 o o 1/2 Mg = ( - Mg )/1.36(Mg ) = (1.46)/(1.51) = 0.97 o o 1/2 1/2 = (2.69 - 1.23)/1.36 (1.23) 1/2 ___________________________________________ It can be seen from Ex 5.13 that as the oxidation state of the metal cation increases from +2(Mg) to +6(W), the partial charge on the metal cation (M) decreases dramatically. This trend reflects the ability of the metal cation to draw electrons from the water molecules through the M 2 bonds. Additionally, the results of Ex 5.13 indicate that the partial charge on the proton (H) increases with increase in the charge on the metal cation. In fact, in W(OH2)66+, the partial charge on H(H= 0.60) is higher than that on W(W = 0.31). It will be recalled from Ex 2.13 that for the free water molecule, the partial charge on the proton is H=0.2. This means that the O-H bond is weaker when a water molecule is in the hydration sphere of a metal cation than when the water molecule is free. Another way of expressing this fact is to say that a water molecule in the hydration sphere of a metal ion is a stronger acid than a free water molecule in the bulk aqueous phase. 5.6.2 The Mean Electronegativity of an Aqueous Solution The chemical potential (i) of a species i is given by i = io + RTlnCi (5.90a) where io is the standard chemical potential, Ci is the concentration of the species, R is the universal gas constant, and T is the absolute temperature. Thus, for the proton in aqueous solution, + + + (H ) = io (H ) + RTln[H ] + = io (H ) - 2.3RT pH (5.90b) (5.90c) The electronegativity may be viewed as an electronic chemical potential. Therefore, assuming a proportionality between and (i.e., i = ki, where k is the proportionality constant), we can write: + + k(H ) = kio (H ) - 2.3RTk pH (5.91a) or + o + (H ) = (H ) - 2.3RTkpH (5.91b) It follows from Equation 5.91b that when pH = 0, + o + (H ) = (H ) (5.92) In strongly acidic solutions, the proton is bihydrated and therefore, the species [H2O-HOH2]+ (i.e., H5O2+) can be chosen as the reference state for the hydrated proton. That is, at pH 0, + o + + (H ) = (H ) = (H5O2 ) = 2.732 (5.93) Using Equation 5.93 in Equation 5.91b gives + + (H ) = (H5O2 ) - 2.3k RT pH = 2.732 - 2.3k RT pH (5.94) Now, in water, the proton is highly delocalized and therefore, invoking the principle of electronegativity equalization, we expect the electronegativity of the hydrated proton to equal the mean electronegativity of the aqueous solution (w). Thus, + (H ) = w (5.95) At pH 7, the aqueous solution has no excess of hydrated proton or hydroxide ions. Therefore, it is convenient to assume that at pH, + (H ) = w = (H2O) = 2.491 (5.96) Combining Equations 5.94 and 5.96 gives: 2.3kRT = [2.732 - (H+)]/pH = [2.732 - (H2O)]/(7) = [2.732 - 2.491]/7 = 0.035 (5.97) Thus, Equation 5.94 becomes: (H+) = w = 2.732 - 0.035pH 5.6.3a Hydrolysis of Metal Cations (5.98) According to the Partial Charge Model (PCM), complex formation can be rationalized in terms of electronegativity equalization. Let us consider the hydrolysis of a metal cation. As discussed in Section 5.1, this refers to the reaction with water molecules that leads to deprotonation and the formation of hydroxo or oxo metal complexes: M(OH2)n z+ + hH2O = M(OH)h(OH2)n-h (z-h)+ + + hH3O (5.99) (z-h)+ The complex on the right-hand-side of Equation 5.99 can be expressed as MOnH2n-h . z+ Then, it can be seen that the complex is: (a) an aquo-ion, M(OH2)n , when h=0, (b) an (2n-z)- oxo-ion, MOn , when h = 2n, (c) an oxo-hydroxo complex, MOx(OH)n-x when 0<h<2n and h>n, (d) a hydroxo-aquo complex, M(OH)h(OH2)n-h 0<h<2n and h<n, and (e) a hydroxo-complex, M(OH)n (n+x-z)- , (z-h)+ , when (n-z)- , when 0<h<2n and h=n. EXAMPLE 5.14a Hydrolysis of Cr(VI) and Cr(III) metal ions The following hydrolysis products of Cr(VI) are known: corresponding Cr(III) complexes are: 3+ Cr(OH 2)6 , o - 2- CrO 2(OH)2 , CrO3(OH) , CrO4 . 2+ Cr(OH)(OH2)5 , The + o Cr(OH)2(OH2)4 , Cr(OH)3(OH2)3 , - Cr(OH)4 . For each complex, determine the value of h and state whether it is an aquo-ion, oxo-ion, etc. 5.6.3b Acid Ionization of Hydrated Metal Ions Interaction between the partial positive charges on the metal ion and the protons of the bound H2O and OH- can lead to the deprotonation of a hydrated metal ion: M(OH 2 ) 2n hH 2 O M(OH) h (OH 2 ) (zn hh) hH 3 O (5.99) When OH is negative, the attractive OH--H+ interaction will discourage deprotonation. However, deprotonation will continue so long as OH is positive, i.e., proton transfer ceases when OH=0. EXAMPLE 5.14b Deprotonation of hydrated metal ions a) Show that the maximum extent of deprotonation is achieved when: h = (z-nH - M)/(1-H) b) Show that the mean electronegativity () of the stable complex is given by: (1) = OH = 2.71 c) (2) Show from Equation 1 and 2 that: h = 1.45z – 0.45n – 1.07(2.71 - M )/( M )1/2 d) With the aid of Equation 3, speculate on the nature of the cationic species that are expected to exist at very low pH in a dilute aqueous solution. (3) 5.6.3c Basic Ionization of Oxo Metal Ions z) Consider the anionic oxo species MO (2m . The negative charges carried by the m oxygen atoms can lead to attractive interaction with the protons from the solvent water molecules: z) z q) MO (2m + qH2O = MOmH (2m + qOHm q (5.99b) The protonation will proceed so long as H < 0. The limit is reached when H = 0. EXAMPLE 5.14c Ionization of oxo metal ions a) With the aid of the partial charge model show that the stable protonated oxo species is given by: q = 2m – z + mO + M b) Show that the mean electronegativity of the stable species is given by: (1) = 2.1 c) (2) On the basis of Equations 1 and 2, show that q = 1.45m – z + 0.74(2.1 - M )/( M )1/2 (3) d) With the aid of Equation 3, speculate on the nature of the anionic species that are expected to exist at high pH in a dilute aqueous solution. (z-h)+ Based on Equation 5.89, it can be shown that for the species M(OH)h (OH2)n-h , the hydrolysis parameter, h, is given by: h = (z - M - nO - 2nH)/(1 - H) (5.100) A relevant question then is this: How far can the deprotonation process proceed? That is, what is the limiting value of the hydrolysis parameter, h, in the complex (z-h)+ M(OH)h(OH2)n-h ? In order to address this question, we invoke the principle of electronegativity equalization. That is, the proton exchange between the complex and the aqueous solution will proceed up to the point where the mean electronegativity of the complex () becomes equal to the mean electronegativity of the aqueous solution (w). Thus, = w (5.101) We recall the expression for the partial charge: o o 1/2 i = ( - i )/1.36 (i ) (5.102) An expression for w was derived above (Equation 5.98). Thus, o o 1/2 iw - i )/1.36 (i ) o (5.103) o 1/2 i = (2.732 - 0.035 pH - i )/1.36 (i ) o (5.104) o Using H = 2.10 and O = 3.50 in Equation 5.104 leads to: H = 0.321 - 0.0178 pH (5.105) O = -0.302 - 0.138 pH (5.106) Also, from Equation 5.104, the partial charge on the metal is given by: o o 1/2 M = (2.732 - 0.035 pH - M )/1.36(M ) = 2.01 (Mo)1/2 – 0.0257(Mo)-1/2 pH – 0.735(Mo)1/2 (5.107) It follows from Equations 5.100, 5.105, 5.106 that: h = [z - M - n(-0.302 - 0.0138 pH) -2n(0.321 - 0.0178 pH)]/[1 - (0.321 - 0.0178 pH)] = [z - M + 0.302n + 0.0138n pH - 0.642n + 0.0356n pH]/[0.679 + 0.0178 pH] h = [z - M - 0.34n + 0.0494n pH]/[0.679 + 0.0178 pH] (5.108) EXAMPLE 5.15 Hydrolysis of Si(IV) (a) Given that for Si(IV), Si = 1.74 and n = 4, show that application of the partial charge model gives the pH dependence of the hydrolysis parameter (h) as: o h = (2.088 + 0.217 pH)/(0.679 + 0.018 pH) (b) Using the above expression determine the hydrolyzed Si(IV) complexes that can form in the pH range of 0-14. Solution (a) According to Equation 5.108, h = [z - M - 0.34n + 0.0494n pH]/[0.679 + 0.0178 pH] (5.108) From Equation 5.107, Si = (2.732 - 0.035 pH - Si )/1.36 (Si ) 1/2 Si = (2.732 - 0.035 pH - 1.74)/1.36(1.74) = (0.992 - 0.035 pH)/1.794 = 0.553 - 0.0195 pH o o 1/2 (1) For Si(IV), z=4 and n=4. Therefore, inserting these values and Si from Equation 1 into Equation 5.108 gives: h = [4 - 0.553 + 0.0195 pH - 0.34(4) + 0.0494(4) pH]/[0.679 + 0.0178 pH] = (2.088 + 0.217 pH)/(0.679 + 0.0178 pH) (b) (2) When pH = 0, Equation 2 gives: h = 2.088/0.679 = 3.1 Correspondingly, for pH = 14, h = [2.088 + 0.217(14)]/[0.679 + 0.0178(14)] = 5.126/0.928 = 5.52 Thus, taking h as the nearest whole number, we find that in the pH = 0-14 range, h varies from 3 at pH=0 to 6 at pH = 14. Therefore, summarizing, h 3 4 5 6 (4-h)+ M(OH)h(OH2)4-h + Si(OH)3(OH2) o Si(OH)4 Si(OH)5(OH2)-1 (i.e., SiO(OH)3 ) 22Si(OH)6(OH2)-2 (i.e., SiO2(OH)2 ) 5.6.4 Polymerization Polymerization via Olation. In the framework of the partial charge model, olation may be visualized as a two-step process. First, the negative end of the M-OH group interacts with the positive end of a hydrated metal cation, giving an intermediate complex. Next, a water molecule is expelled from the intermediate complex: M OH M OH2 M OH M OH2 (5.109) M OH M H2 O It must be noted that the removal of a water molecule is necessary because hydrated metal cations typically have the highest coordination number available to the M z+ ion. In order for polymerization to occur, a negative partial charge must exist on the OH group in the MOH unit (i.e., OH < 0). Additionally, the positive partial charge on M (in the MOH unit) must be sufficiently large. The available experimental data suggest M ≥ + 0.3. Figure 5.6 presents typical examples of the different types of hydroxo bridges that are found in polynuclear hydroxo metal complexes. Figure 5.6. Types of hydroxo bridges in polynuclear complexes. EXAMPLE 5.16 Polymerization limit of hydroxo complexes For each of the following dimeric complexes: (1) determine the partial charge (OH) on the OH group of the monomer, (2) speculate on the feasibility of dimer formation, and (3) speculate on the feasibility of further polymerization beyond the dimer. OH (a) [(H2O)4 Cr Cr (OH2)4] 4+ Ni (OH2)4] 4+ OH OH (b) [(H2O)4 Ni OH Solution (a) For the monomer, [Cr(OH)(OH2)] , the partial charge on the hydroxyl group is OH = -0.02. Also, M = 1.56. Thus, the two criteria for polymerization (i.e., OH<0, M ≥ + 0.3) are met. Therefore, dimerization is feasible. For the dimer, OH = +0.01. Therefore, polymerization is not possible. (b) For the monomer, [Ni(OH)(OH2)5] , OH = -0.12. Accordingly dimerization is expected. For the dimer, OH = -0.10. Therefore further polymerization is feasible. In fact, condensation of two dimers 4+ gives the tetramer [Ni4(OH)4(OH2)12] whose structure is depicted in Table 5.1. For the tetramer, OH = +0.6 and therefore further polymerization beyond this is not possible. 2+ + Polymerization via Oxolation. When metal complexes no longer have water molecules as ligands, the olation pathway for polymerization is no longer available. In this case, polymerization must proceed via oxolation. The metal ions that undergo oxolation tend to be high-valent (z>4+) which form oxo-hydroxo anions, [MOx(OH)m-x] (m+x-z)- . Two different pathways are available for oxolation, depending on whether or not the coordination of the metal ion in the starting complex is the highest attainable. If coordination is not saturated, then oxolation can lead to expansion of the coordination: O M + O M In this case, there is no need to eliminate hydroxyl groups or water molecules. If the metal coordination is fully saturated in the starting complex, then oxolation requires the elimination of hydroxyl groups or water molecules: - + M OH + M OH M O M OH H M OH- + M+ OH M O M OH H OH H... OH M O M M O M M O M It can be seen from the above steps that the first step involves OH( )M( interaction. Thus, a useful guide in ascertaining the feasibility of additional polymerization is to consider the sign of the partial charge on the OH group. EXAMPLE 5.17 Polarization of Cr(VI) complexes Determine the extent to which the following Cr complexes can undergo polymerization: o (a) [CrO2(OH)2] , (b) [CrO3(OH)] . Solution (a) The first stage of polymerization is dimer formation: 2[CrO2(OH)2] [(HO)O2Cr-O-CrO2(OH)] + H2O o o The partial charge on the OH groups in the dimer is determined as OH = +0.04. The positive partial charge indicates polymerization beyond the dimer is not feasible. (b) The relevant dimerization reaction is: - 2- 2[CrO3(OH)] = [Cr2O7] + H2O In this case, after forming the dimer, no more hydroxyl groups are available for further polymerization. Thus, polymerization ceases after the dimer forms. ________________________________________________________________________________________ 5.6.5a Precipitation Formation of a solid metal hydroxide/oxide phase may be viewed in terms of infinite polymerization of neutral complexes (h=z) via the hydroxo groups. Complete olation results in a metal hydroxide while complete oxolation gives a metal oxide. Formation of an oxo bridge from an ol bridge involves the transfer of a proton from one hydroxo group to a neighboring hydroxo group: H OH H... OH H M O M M OMMOM It can be seen that this process produces a water molecule. The nature of the partial charge on this water molecule provides a guide as to the relative importance of ol and oxo groups in the solid product: (a) (H2O) < 0. The metal cation M() is attracted to the water molecule (). Therefore, the water molecule is retained and a reversal of the proton transfer occurs. In this case, oxolation is not favored. (b) (H2O)>0. The cation M() repels the water molecule. Elimination of the water molecule is therefore feasible and oxolation is favored. EXAMPLE 5.18 Olation vs. oxolation in metal metal (hydr)oxide precipitation Starting with the following neutral soluble species, speculate on the likelihood that precipitation will result in a hydroxide or oxide solid product: o o Mn(OH)2(OH2)4 , Y(OH)3(OH2)3 , o o Fe(OH)3(OH2)3 , Zr(OH)4(OH2)4 Solution Neutral Complex (H2O) Predicted Solid Phase Observed Solid Phase o Mn(OH)2(OH2)4 -0.02 Mn(OH)2 o Y(OH)3(OH2)3 -0.05 Y(OH)3 o Fe(OH)3(OH2)3 +0.03 Fe2O3 ________________________________________________________________________________________ 5.6.5b Precipitation (cont’d) Precipitation occurs in aqueous solution when the pH reaches the corresponding point of zero charge. At this pH, the charge on the metal species is zero or nearly zero and, therefore, electrostatic repulsion is too weak to stop their collision. Following collision, condensed species form through olation or oxolation. In either case, OH groups are involved. From the acid side, cationic species M(OH)h(OH2) (zn hh) acquire additional OHgroups and decrease in charge, as the pH is raised. On the other hand, starting from a basic z q) pH, anionic species MOnH (2n can be condensed by lowering the pH. At the point of q zero charge where precipitation occurs, q = 2n-z. Consider the neutral species (MOnH2n-z) at the point of zero charge. The condition for the condensation of these species is that OH < 0. Therefore, the limit for condensation is reached when OH = 0. At this limit the partial charge model gives: M + nO + (2n-z)H = 0 (5.112) Also, it follows from the condition OH = 0 that = OH = 2.71 (5.113) EXAMPLE 5.19 The mean electronegativity of the neutral species (MOnH2n-z). Consider the neutral species (MOnH2n-z). For the limiting condition OH = 0, determine: a) the mean electronegativity OH b) the electronegativity of the bonded O and H in OH c) the mean electronegativity of the neutral species (MOnH2n-z) d) the partial charges O and H Solution a) Using Equation 2.12h, and recognizing that, for the condition OH = 0 the charge (z) on OH is zero, gives: OH = (OH)1/2 = [(3.50)(2.10)]1/2 = 2.71 b) Recalling the principle of electronegativity equalization, when two atoms combine to give a stable molecule (in this case OH), the two partially charged atoms acquire the same electronegativity. It follows, therefore, that: O = H = OH = 2.71 c) Again, according to the principle of electronegativity equalization, for the stable neutral molecule (MOnH2n-z), the partially charged atoms acquire the same electronegativity. Therefore, in view of part (b), and the fact that O, H, and M are atoms in the same stable molecule, i.e., (MOnH2n-z), complex = O = H = M = 2.71 d) Recalling Equation 2.12g, i = ( - i )/1.36( i )1/2 (2.12g) Therefore, for i = O = 3.50, o = (2.71 – 3.50)/1.36(3.50)1/2 = -0.310 Similarly, for i = H = 2.10, H = (2.71 – 2.10)/1.36(2.10)1/2 = +0.310 Alternatively, we can argue that given that OH = 0 for the neutral species, it follows that H = -O = 0.310. e) We can express the neutral molecule (MOnH2n-z) as (M(OH)nHn-z). It follows, therefore, that M + nOH + (n-z)H = 0 But OH = 0. Thus, M = (z-n)H f) From Equation 2.12g, M = ( - M )/1.36( M )1/2 Thus, M + 1.36M( M )1/2 - = 0 Solution of this quadratic equation gives ( M )1/2 = {-1.36M + [(1.36M)2 + 4]}/2 Making the substitutions M = (z-n)H, H = 0.310, = 2.71 gives ( M )1/2 = 0.21(n-z) + [2.71 + 0.044(z-n)2]1/2 5.6.6 Alkoxide Reactions Three important reactions of metal alkoxides (M(OR)n) are hydrolysis (Equation 5.114a), condensation (Equation 5.114b), and chemical modifications (Equation 5.114c) M OR + HO H M OH + ROH (5.114a) M OR + HO M M O M + ROH (5.114b) M OR + HO R M O R + ROH (5.114c) All these reactions can be viewed in terms of the following three-step process: a) A nucleophilic addition of an OH group to the metal atom: + X O + M OR H X O M OR H (5.115) This step is feasible provided OH < 0 and M > 0. b) A transition state during which a proton from the entering ligand (XOH) attaches to an oxygen of a neighboring OR group: - XOMOR +H XO M O R H (5.116) The requirement here is that H > OR. c) Release of the protonated group (ROH): + + XO M O R H XO M + ROH (5.117) Removal of the ROH group requires that ROH > 0. Thus, consideration of the partial charge distribution leads to the following conditions: M > 0, H > OR, and ROH > 0 EXAMPLE 5.20 Correlation between M and the hydrolysis rate of silicon alkoxides The hydrolysis rate of silicon alkoxides (Si(OR) 4) were determined by Aelion and Akerman ( following results were obtained: R kx102 M-1s-1[H+]-1 Ethyl 5.1 Butyl 1.9 ). The Hexyl 0.83 Rationalize these results with the aid of the partial charge model. What will be the effect of an increasingly positive partial charge on Si? Solution As noted above, the first step in the alkoxide hydrolysis reaction involves the nucleophilic addition of the OH group to the metal ion (Equation 5.115). The requirement M > 0 suggests that increasing the positive partial charge on the metal atom should enhance the reaction rate. Si(OR)4 can be expressed as Si(OCnH2n+1)4 or SiC4nH8n+4O4. Using Equations 2.12h and 2.12g, the mean electronegativities and partial charges can be calculated, as summarized in Table E5.20. 1/ 2 1/ 2 [( Si ) 4n( C )1 / 2 (8n 4)( H )1 / 2 4( O )1 / 2 ] /[1 /( Si ) 4n /( C )1 / 2 (8n 4) /( H )1 / 2 4 /( O )1 / 2 ] i ( i ) / 1.36 ( i )1/ 2 TABLE E5.20 R Ethyl n 2 M OR ROH H kx102 M-1s-1[H+]-1 5.1 Butyl Hexyl 4 6 1.9 0.83 EXAMPLE 5.21 Comparison of the hydrolysis rates of titanium and silicon alkoxides Titanium alkoxides are known to hydrolyze more rapidly than the corresponding silicon precursors. Rationalize this observation with the aid of the partial charge model. Show that for the alkoxides M(OR) 4 this observation should be expected at least up to R = hexyl. Solution Based on Equations 2.12h and 2.12g, the mean electronegativities and the partial charges can be calculated, as summarized in Table E5.21. It can be seen that in all cases, the positive charge on titanium is approximately twice that on silicon. Thus, recalling Equation 5.115 above, we should expect the rate of hydrolysis of titanium alkoxides to be faster than that of the corresponding silicon compounds. TABLE E5.21 EXAMPLE 5.22 Alcohol vs. water elimination in the condensation of metal alkoxides In principle, the condensation of the hydrolyzed species M(OR) 3(OH) can occur via the elimination of a water molecule (Equation 5.114a) or an alcohol molecule (Equation 5.114b): M(OR)3OH + HO M(OR)3 M(OR)3OH + RO M(OR)2(OH) (RO)3M O M(OR)3 + H2O (RO)3M O M(OR)2OH + ROH (1) (2) Refer to the three-step process for alkoxide reactions. Consider the case where R = Pr = C 3H7. Show that for both Si and Ti, the conditions for steps 1 and 2 are satisfied (i.e., OH < 0, M > 0 (Step 1); H > 0 (Step 2). b) Determine whether the condensation reaction will favor alcohol or water elimination. a) Solution According to the three-step mechanism for alkoxide reactions, the first step is nucleophilic addition of an OH group to a metal atom: Step 1a: - + (RO)3M O + M (OR)3 H OH (RO)3M O M (OR)3 H OH Required: OH < 0, M > 0. Step 2a: (RO)3M O M (OR)3 H OH + Required: H > OH. (RO)3MO M (OR)3 OH2 Step 3a: (RO)3M O M(OR)3 Required: H2O > 0. OH2 (RO)3M O M(OR)3 + H2O The first step (Step 1b) of the alcohol elimination pathway involves nucleophilic OH addition. Step 1b: - + (RO)3M O + M (OR)2(OH) H OR (RO)3M O M (OR)2(OH) H OR Required: OH < 0, M > 0. Step 2b: (RO)3M O M (OR)2(OH) H OR + - (RO)3M O M (OR)2(OH) HOR Required: H > OR Step 3b: (RO)3M O M (OR)2(OH) HOR (RO)3M O M(OR)2(OH) + ROH Required: ROH > 0 Compound M OH H H O 2 ROH Si(OPr)3(OH) Ti(OPr)3(OH) Si2(OPr)6(OH)2 Ti2(OPr)6(OH)2 5.6.7 Metal Complexation A monodentate monovalent anion X- can form a complex with a hydrated metal ion via a ligand substitution (anation) reaction in which a water molecule is released: M(OH2) zn + X- = [M(X)(OH2)n-1](z-1) + H2O (5.118) Consider the complex [M(X)(OH2)n-1](z-1). In order for this complex to remain stable in aqueous solution, it must withstand: (a) the tendency towards ionic dissociation (Equation 5.119) caused by the high dielectric constant of the solvent water, and (b) the tendency towards hydrolytic dissociation (Equation 5.120): [M(OH)h(X)(OH2)n-h-1] (z h 1) + H2O = [M(OH)h(OH2)n-h] (zh) + X[M(OH)h(X)(OH2)n-h-1] (z h 1) (5.119) = [M(OH)h+1(HX)(OH2)n-h-2] (z h 1) (5.120) = [M(OH)h+1(OH2)n-h-2] (zh 1) + HX The stability of the M X bond, as related to Equations 5.119 and 5.120, can be assessed with the help of the partial charge model. In the case of the tendency towards ionic dissociation (Equation 5.119), the electronegativity of X- can be compared with that for H2O( = 2.49). If X- is more electronegative (i.e., X > H2O ) electron transfer from M to X occurs, the negative charge on X increases (X < -1), and the M X bond becomes more ionic. The result is enhanced ionization. On the other hand, if x < H2O , electrons will be withdrawn from X-, thereby decreasing the negative charge on X (X > -1). The result is a more covalent M X bond and a decreased tendency towards ionic dissociation. Considering the tendency towards hydrolytic dissociation (Equation 5.120), we focus on the intermediate species [M(OH)h+1(HX)(OH2)n-h-2](z-h-1). The condition HX < 0 discourages the release of HX and, therefore, the M X bond is stable. On the other hand, HX > 0 favors the release of HX and, therefore, hydrolytic dissociation. EXAMPLE 5.23 Complexation of Fe3+ by bidentate monovalent anions Determine whether the following monovalent anions can complex the hydrated ferric ion 3 Fe(OH2) 6 : ClO 4 , NO 3 , HSO 4 , H2PO 4 , and CH3COO-. Assume that these ions are bidentate ligands. Solution Since these anions are bidentate, they can displace two water molecules to give complexes of the type [Fe(X)(OH2)4]2+. The corresponding destabilization reactions can be written as: Ionic dissociation [Fe(X)(OH2)4]2+ + 2H2O = [Fe(OH2)6]3+ + X- Hydrolytic dissociation [Fe(OH)(HX)(OH2)3]2+ = [Fe(OH)(OH2)5]2+ + HX Table E5.23 presents tabulation of the following quantities: X (the mean electronegativity of anion X-), x (the partial charge of X in [Fe(X)(OH2)4]2+), and HX (the partial charge of HX in [Fe(OH)(HX)(OH2)4]2+. Consider an anion Xx-. Define the change in charge x as x = charge on bonded anion - charge on free anion = x – (-x) = x + x For a monovalent anion, x = 1 and therefore we get: x = 1 + x When x < -1, x < 0, and anion complexation is not feasible. On the other hand, when x > -1, x > 0, and anion complexation is feasible. Table E5.23 - Anion (X ) ClO 4 NO 3 HSO 4 HCO 3 CH3COO- X x x HX FURTHER READING 1. J. N. Butler, Ionic Equilibria: Reading, MA, 1964. A Mathematical Approach, Addison-Wesley, 2. W. Stumm and J. J. Morgan, Aquatic Chemistry, 2nd ed., Wiley, New York, 1981. 3. D. A. Johnson, Some Thermodynamic Aspects of Inorganic Chemistry, 2nd ed., Cambridge, New York, 1982. 4. A. F. Wells, Structural Inorganic Chemistry., 5th ed., Oxford, New York, 1984. 5. L. Pauling, The Nature of the Chemical Bond, 3rd. ed., Cornell University Press, Ithaca, New York, 1960. 6. J. E. Huheey, E.A. Keiter, and R. L. Keiter, Inorganic Chemistry. Principles of Structure and Reactivity, 4th ed., HarperColins 1993. 7. A. G. Sharpe, Inorganic Chemistry, 3rd. ed., Longman, London, 1992. 8. D. E. Shriver, P. W. Atkins, and C. H. Langford, Inorganic Chemistry, Freeman, New York, 1990. 9. B. Webster, Chemical Bonding Theory, Blackwell, Oxford, 1990. 10. F. A. Cotton and G. Wilkinson, Advanced Inorganic Chemistry, 5th ed., Wiley New York, 1988. 11. M. Henry, J. P. Jolivet, and J. Livage, "Aqueous Chemistry of Metal Cations: Hydrolysis, Condensation and Complexation", Structure and Bonding, 77, 153-206 (1992). 12. J. Livage, M. Henry, and C. Sanchez, "Sol-Gel Chemistry of Transition Metal Oxides", Prog. Solid Stage Chem., 18, 259-341 (1988). 13. J. P. Jolivet, Metal Oxide Chemistry and Synthesis. From Solution to Solid State, Wiley, New York, 2000.