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Thermodynamics and kinetics • • • • • Thermodynamic laws Half-cell reactions Kinetics Acid-Base Equilibrium calculations Speciation calculation from complexation constants • Provide review of concepts for applications to radiochemistry 2-1 Thermodynamic terms • Heat Capacity (Cp) Heat required to raise one gram of substance 1 °C Enthalpy (∆H) • Energy of a system (heat content) Internal energy, volume, pressure Accounts for energy transferred to environment by expansion or heating • ∆H = ∆Hproducts - ∆Hreactants • Exothermic reactions, negative ∆H Negative ∆H tend to be spontaneous ∆Hproducts-∆Hreactants 2 H+ + CO32- <--> CO2 + H2O -393.5 + (-285.8)-(-677.1+2(0)) = -2.2 kj/mol 2-2 Thermodynamic terms • Endothermic Reaction requires energy (at 25 °C) 2 HgO + 181.70 kj <--> 2 Hg + O2 Enthalpy (∆H) • Energy of a system (heat content) Internal energy, volume, pressure Accounts for energy transferred to environment by expansion or heating • ∆H = ∆Hproducts - ∆Hreactants • Exothermic reactions, negative ∆H Negative ∆H tend to be spontaneous 2-3 Entropy (∆S) and Gibbs Free Energy (∆G) • • • Randomness of a system increase in ∆S tends to be spontaneous Enthalpy and Entropy can be used for evaluating the free energy of a system Gibbs Free Energy ∆G = ∆H -T∆S ∆G=-RTlnK K is equilibrium constant Activity at unity Compound H2 O OH-(aq) H+(aq) ∆G° (kJ/mol) at 298.15 K -237.129 -157.244 0 H2OH++OH What is the constant for the reaction? Products-reactants • At 298.15 K ∆G(rxn) = 0 + -157.244 - (-273.129) = 79.9 kJ/mol lnK= (79.9E3/(-8.314*298.15))=-32.2; K=1E-14, Kw = [H+][OH-] 2-4 Thermodynamic Laws • 1st law of thermodynamics Energy is conserved in a system Can be changed or transferred Heat and work are energy transfer ∆E = q (heat absorbed) + w (work) • 2nd law of thermodynamics Reactions tend towards equilibrium Increase in entropy of a system Spontaneous reaction for -∆G ∆G = 0, system at equilibrium • 3rd law of thermodynamics Entropies of pure crystalline solids are zero at 0 K Defines absolute zero 2-5 Half-cell potentials • Cell reaction for Zn and Fe3+/2+ at 1.0 M Write as reduction potentials Fe3+ + e- <--> Fe2+ °=0.77 V Zn2+ + 2e- <-->Zn °=-0.76 V • Reduction potential for Fe3+ is larger Fe3+ is reduced, Zn is oxidized in reaction • Overall balanced equation 2Fe3+ +Zn <--> 2Fe2+ + Zn2+ °=0.77+0.76=1.53 V • Use standard reduction potential Application of Gibbs Free Energy • If work is done by a system ∆G = -°nF (n= e-) • Find ∆G for Zn/Cu cell at 1.0 M 2.30RT [C]c [D]d log Cu2+ + Zn <--> Cu + Zn2+ °=1.10 V nF [A]a [B]b 2 moles of electrons (n=2) ∆G =-2(96487C/mole e-)(1.10V) ∆G = -212 kJ/mol 2-6 Kinetics and Equilibrium • Kinetics and equilibrium important concepts in examining and describing chemistry Identify factors which determine rates of reactions Temperature, pressure, reactants, mixing Describe how to control reactions Explain why reactions fail to go to completion Identify conditions which prevail at equilibrium • General factors effecting kinetics Nature of reactants Effective concentrations Temperature Presence of catalysts Number of steps 2-7 Rate Law • Concentration of reactant or product per unit time • Effect of initial concentration on rate can be examined rate = k[A]x[B]y rate order = x + y knowledge of order can help control reaction rate must be experimentally determined Rate=k[A]n; A=conc. at time t, Ao=initial conc., X=product conc. Order rate equation k 0 [A0]-[A]=kt, [X]=kt mole/L sec 1 2 3 ln[A0]-ln[A]=kt, ln[A0]-ln([Ao]-[X])=kt 1 1 kt [A] [Ao ] 1 1 kt [A]2 [Ao ]2 2 1 1 kt [Ao ] [X] [Ao ] 1 1 kt 2 2 2 ([Ao ] [X]) [Ao ] 1/sec L/mole sec L2/mole2-82 sec Acid-Base Equilibria • Brønsted Theory of Acids and Bases Acid Substance which donates a proton Base Accepts proton from another substance NH3 + HCl <--> NH4+ + ClH2O + HCl <--> H3O+ + ClNH3 + H2O <--> NH4+ + OH• Remainder of acid is base • Complete reaction is proton exchange between sets • Extent of exchange based on strength • Water can act as solvent and reactant 2-9 Dissociation Constants • Equilibrium expression for the behavior of acid [A ][H3O ] HA + H2O <--> A- + H3O+ K Water concentration is constant [HA][H2O] [A ][H3O ] Ka K[H2 O] [HA] pKa=-logKa • Can also be measured for base Constants are characteristic of the particular acid or base Acid Acetic Carbonic Phosphoric Oxalic Formula HC2H3O2 H2CO3 HCO3H3PO4 H2PO4HPO42H 2 C 2 O4 HC2O4- Ka 1.8E-5 3.5E-7 5E-11 7.5E-3 6.2E-8 4.8E-13 5.9E-2 6.4E-5 2-10 Buffer Solutions • Buffers can be made over a large pH range • Can be useful in controlling reactions and separations Buffer range Effective range of buffer Determined by pKa of acid or pKb of base HA + H2O <--> A- + H3O[A ][H3O ] Ka [HA] Write as pH [H3O ] Ka [HA] [A ] [HA] pH pKa log [A ] • The best buffer is when [HA]=[A-] largest buffer range for the conditions pH = pKa - log1 • For a buffer the range is determined by [HA]/[A-] [HA]/[A-] from 0.1 to 10 Buffer pH range = pKa ± 1 Higher buffer concentration increase durability 2-11 Hydrolysis Constants • Reaction of water with metal ion Common reaction Environmentally important Strength dependent upon metal ion oxidation state • 2 H2O <--> H3O+ + OH Water concentration remains constant, so for water: Kw = [H3O+][OH-]= 1E-14 at 25°C • Metal ions can form hydroxide complexes with water • Mz+ + H2O <--> MOHz-1+ + H+ • Constants are listed for many metal ion with different hydroxide amounts Database at: http://www.escholarship.org/uc/item/9427347g 2-12 Equilibrium Le Châtelier’s Principle • At equilibrium, no further change as long as external conditions are constant • Change in external conditions can change equilibrium A stressed system at equilibrium will shift to reduce stress concentration, pressure, temperature • N2 + 3 H2 <--> 2 NH3 + 22 kcal What is the shift due to Increased temperature? Increased N2? Reduction of reactor vessel volume? 2-13 Equilibrium Constants • For a reaction aA + bB <--> cC + dD • At equilibrium the ratio of the product to reactants is a constant The constant can change with conditions By convention, constants are expressed as products over reactants [C]c [D]d K [A]a [B]b • Conditions under which the constant is measured should be listed Temperature, ionic strength 2-14 Activities • Strictly speaking, activities, not concentrations should be used C[C]c D [D]d K A [A]a B[B]b • At low concentration, activities are assumed to be 1 • The constant can be evaluated at a number of ionic strengths and the overall activities fit to equations • Debye-Hückel (Physik Z., 24, 185 (1923)) 0.5085Z 2a log A 1 0.3281R A ZA = charge of species A µ = molal ionic strength RA = hydrated ionic radius in Å (from 3 to 11) First estimation of activity 2-15 Activities • Debye-Hückel term can be written as: 0.5107 D 1 1.5 • Specific ion interaction theory Uses and extends Debye-Hückel long range Debye-Hückel Short range ion interaction term 2 log Z D ij i ij = specific ion interaction term log ß() logß(0) Z2i D ij • Pitzer Binary (3) and Ternary (2) interaction parameters 2-16 6.6 Experimental Data Cm-Humate shows change in stability constant with ionic strength Ion Specific Interaction Theory used 6.5 logß 6.4 6.3 6.2 6.1 K+ 6.0 0.0 0.5 1.0 1.5 2.0 2.5 sqrt Im Ca2+ Al3+ Fe(CN)642-17 3.0 Constants • Constants can be listed by different names Equilibrium constants (K) Reactions involving bond breaking * 2 HY <--> H2 + 2Y Stability constants (ß), Formation constants (K) Metal-ligand complexation * Pu4+ + CO32- <--> PuCO32+ * Ligand is written in deprotonated form Conditional Constants An experimental condition is written into equation * Pu4+ + H2CO3 <--> PuCO32+ +2H+ Constant can vary with concentration, pH Must look at equation! 2-18 Realistic Case • Consider uranium in an aquifer Species to consider include free metal ion: UO22+ hydroxides: (UO2)x(OH)y carbonates: UO2CO3 humates: UO2HA(II), UO2OHHA(I) Need to get stability constants for all species UO22+ + CO32- <--> UO2CO3 Know or find conditions Total uranium, total carbonate, pH, total humic concentration 2-19 Stability constants for selected uranium species at 0.1 M ionic strength Species logß UO2 OH+ 8.5 UO2(OH)2 17.3 UO2(OH)322.6 Other species may need to be UO2(OH)4223.1 considered. If total uranium (UO2)2OH3+ 11.0 concentration is low enough, (UO2)2(OH)2+ 22.0 binary or tertiary species can be excluded. UO2CO3 8.87 UO2(CO3)2216.07 UO2(CO3)3421.60 UO2HA(II) 6.16 UO2(OH)HA(I) 14.7±0.5 2-20 Equations • Write concentrations in terms of species [UO2]tot= UO2free+U-carb+U-hydroxide+U-humate [CO32-]free=f(pH) [OH-] = f(pH) [HA]tot = UO2HA + UO2OHHA+ HAfree • Write the species in terms of metal, ligands, and constants [(UO2)xAaBb] = 10-(xpUO2+apA+bpB-log(UO2)xAaBb) pX = -log[X]free [(UO2)2(OH)22+]=10-(2pUO2+2pOH-22.0) • Set up equations and solve for known terms 2-21 U speciation with different CO2 partial pressure 0% CO2 1.0 UO 2(OH) 1.0 3 UO 2 UO 2OHHA(I) UO 2(OH) Mole Fraction of U(VI) Species 0.8 UO 2HA(II) 2 0.6 0.4 0.2 0.0 2.0 4.0 6.0 8.0 UO 22+ 0.8 UO 2HA(II) UO 2OHHA(I) UO 2(CO 3) 34- 0.6 0.4 UO 2(CO 3) 22- 0.2 0.0 10.0 2.0 pH 4.0 6.0 8.0 10.0 pH 1.0 Mole Fraction of U(VI) Species Mole Fraction of U(VI) Species 2+ 1% CO2 0.8 UO 22+ UO 2HA(II) UO 2OHHA(I) UO 2(CO 3) 34- 0.6 10% CO2 0.4 UO 2(CO 3) 22- 0.2 0.0 2.0 4.0 6.0 pH 8.0 10.0 2-22 Comparison of measured and calculated uranyl organic colloid 1.0 0.8 10% 1% total [U(VI)] [U-colloid] 100% 0.6 0.4 0% 0.035% 0.2 0.0 2.0 4.0 6.0 pH 8.0 10.0 2-23 Excel spreadsheets CHESS Program 2-24 Energy terms Rlnß • Constants can be used to evaluate energetic of reaction From Nernst equation ∆G=-RTlnK ∆G=∆H-T∆S -RTlnK = ∆H-T∆S RlnK= - ∆H/T + ∆S * Plot RlnK vs 1/T Temperature effect on Np-Humate stability T emp (°C) 56 48 40 32 24 16 76 74 72 70 ²H = -22.2 ± 2.8 kJ/mol ²G 298=-21.7 kJ/mol ²S=1.2±1.4 J/molK 68 66 64 0.003 0.0031 0.0032 0.0033 0.0034 1/T (K) 2-25 0.0035 Solubility Products • Equilibrium involving a solid phase AgCl(s) <--> Ag+ + Cl[Cl ][Ag ] K [AgCl] AgCl concentration is constant Solid activity and concentration is treated as constant By convention, reaction goes from solid to ionic phase in solution Can use Ksp for calculating concentrations in solution Ksp K[AgCl] [Cl ][Ag ] 2-26 Solubility calculations • Ksp of UO2 = 10-52. What is the expected U4+ concentration at pH 6. Generalize equation for any pH Solubility reaction: UO2 + 2 H2OU(OH)4 U4+ + 4 OH Ksp= [U4+][OH-]4 [U4+]= Ksp /[OH-]4 pOH + pH =14 At pH 6, pOH = 8, [OH-]=10-8 [U4+]= 10-52 /[10-8]4= 10-52 /10-32 = 10-20 M For any pH [U4+]= 10-52 /[10-(14-pH)*4] Log [U4+]= -52+((14-pH)*4) 2-27 Limitations of Ksp • Solid phase formation limited by concentration below ≈1E-5/mL no visible precipitate forms colloids • formation of supersaturated solutions slow kinetics • Competitive reactions may lower free ion concentration • Large excess of ligand may form soluble species AgCl(s) + Cl- <--> AgCl2-(aq) Ksp really best for slightly soluble salts 2-28 Overview • Understand heats of reactions Enthalpy, entropy, Gibbs free energy Reaction data from constituents • Understand half-cell reactions Nernst Equation • Kinetics Influence of reaction conditions • Equilibrium and constants Use to develop a speciation spreadsheet 2-29 Questions • What is the difference between 1st and 2nd order kinetics? • What can impact reaction rates? • How can a compound act as a base and acid? Provide an example. • What does the dissociation constant of an acid provide? • Provide the speciation of acetic acid at pH 3.5, 4.5, and 5.5. • What are the species from carbonic acid at pH 4.0, 6.0, and 8.0? • Set up the equations to describe the speciation of uranyl, the uranyl monocarbonate, and the uranyl dicarbonate. 2-30 Pop Quiz • Show the relationship between Gibbs free energy, enthalpy, and entropy 2-31