Survey
* Your assessment is very important for improving the work of artificial intelligence, which forms the content of this project
* Your assessment is very important for improving the work of artificial intelligence, which forms the content of this project
Thermodynamics and kinetics • • • • • • Heats of reaction Thermodynamic laws Electrochemistry Kinetics Acid-Base Equilibrium calculations 1-1 Heats of Reaction • 1 cal = 4.184 j • Heat Capacity (Cp) Heat required to raise one gram of substance 1 °C Al; Cp = 0.895 j/gK What is the heat needed to 40 g Al 10 K (0.895 j/gK)(40g)(10K)= 358 j • Exothermic Reaction produces heat (at 25 °C) C(s) + O2(g) <--> CO2(g) + 393.76 kj 1-2 Heats of Reaction • Endothermic Reaction requires energy (at 25 °C) 2 HgO + 181.70 kj <--> 2 Hg + O2 Enthalpy (∆H) • Energy of a system (heat content) ∆H = ∆Hproducts - ∆Hreactants Exothermic reactions have negative ∆H Negative ∆H tend to be spontaneous 1-3 Enthalpy (∆H) • Bond energies Can be used to estimate ∆H N2 + 3 H2 <--> 2 NH3 6(351.5)-945.6-3(436.0) = -144.6 kj/2 mole =-72.3 kj/mole (actual -46.1 kj/mol) • Aqueous Ions (use ∆H values) ∆Hproducts-∆Hreactants 2 H+ + CO32- <--> CO2 + H2O -393.5 + (-285.8)-(-677.1+2(0)) = -2.2 kj/mol CO2(g) H2O(l) CO32- H+ 1-4 Bond Energies (kJ/mol) at 298 K Single Bonds HH HC HN HO HF HS HCl HBr HI CC CN CO CF CS CCl CBr 436.0 418.4 351.5 464.4 564.8 338.9 431.8 368.2 297.1 343.1 267.8 347.3 426.8 255.2 330.5 276.1 Single Bonds CI NN NF NCl OO OF OSi OCl OS FF PCl SS ClCl ClI BrBr II 217.6 133.9 234.3 154.8 138.1 188.3 443.5 209.2 518.8 158.2 326.4 205.0 242.7 209.2 192.5 150.6 CC CN CO NN Double Bond 610.9 615.0 740.6 418.4 Triple Bond 836.8 891.2 1071.1 945.6 Bond in O2 498.7 1-5 Heat Capacities Elements (Jg-1K-1) Compounds (Jmol-1K-1-) Li 3.582 B 1.026 C 0.709 N 1.042 O 0.920 Al 0.900 Cr 0.449 Cu 0.385 Zr 0.278 Hf 0.140 W 0.130 Au 0.128 Hg 0.140 Pb 0.129 Th U 0.120 Pu 0.130 H2 O2 N2 CO CO2 CH4 C2H6 NH3 H2O(g) HBr SnO2 Al2O3 Fe2O3 0.113 Np 0.120 Am 0.110 28.87 29.50 29.04 29.16 37.49 35.98 53.18 36.11 24.77 27.53 56.61 79.33 104.35 1-6 Pure Substance Standard ∆H (kJ/mol) Ag(g) Ag+(g) AgCl(c,cerargyrite) AgNO3(c) Al3+(g) Al(OH)3 BaCO3(c,witherite) BaC2O4(c) BaCrO4(c) BaF2(c) BaSO4(c) BeO(c) Bi2S3(c) Br2(g) Br(g) Br-(g) C(c,diamond) C(g) CO(g) CO2(g) 284.55 1021.73 -127.068 -124.39 5483.17 -1276 -1216.3 -1368.6 -1446 -1207.1 -1473.2 -609.6 -143.1 30.907 111.88 -219.07 1.895 716.682 -110.525 -393.509 COCl2(g,phosgene) -218.8 CH4(g,methane) -74.81 C2H2(g,ethyne) 226.73 C2H2(g,ethene) 52.25 C2H6(g,ethane) -84.68 CH3OCH3(g) -184.05 CH3OH(g,methanol) -200.66 CH3OH(l,methanol) -238.66 C2H5OH(g,ethanol) -235.1 C2H5OH(l,ethanol) -277.69 CH3COOH(l,acetic acid) -484.51 (CH3)2O(g) -184.05 CH3CHO(l) -192.3 CH3Cl(g) -80.83 CHCl3(g) -103.14 CCl4(l) -135.44 CaO(c) -635.09 Ca(OH)2(c) -986.09 CaCO3(c, calcite) -1206.92 CaCO3(c, aragonite) -1207.13 1-7 Pure Substance Standard ∆H (kJ/mol) CaC2O4(c) CaF2(c) Ca3(PO4)2(c) CaSO4(c,anhydrite) Cd(g) Cd2+(g) Cd(OH)2(c) CdS(c) Cl(g) Cl-(g) ClO2(g) Cu(g) Cu2O(c,cuprite) CuO(c,tenorite) Cu(OH)2(c) Cu2S(c,chalcocite) CuS(c,covellite) F(g) F-(g) -1360.6 -1219.6 -4109.9 -1434.1 2623.54 112.01 -560.7 -161.9 121.679 -233.13 102.5 338.32 -168.6 -157.3 -449.8 -79.5 -53.1 78.99 -255.39 Fe3+(g) Fe2O3(c,hematite) H+(g) H2O(g) H2O(l) H2O2(g) H2O2(l) H2SO4(l) HF(g) HCl(g) HBr(g) HI(g) HCN(g) PbO(c,red) PbO2(c) Pb3O4(c) PbS(c,galena) PbSO4(c) ThO2(c) 5712.8 -824.2 1536.202 -241.818 -285.83 -136.31 -187.78 -813.989 -271.1 -92.307 -36.4 26.48 135.1 -218.99 -277.4 -718.4 -100.4 -919.94 -1226.4 Fe(g) 416.3 UO2(c) -1084.9 1-8 Solution Standard ∆H (kJ/mol) Ag+ AgCl2Ag(NH3)2+ Ag(S2O3)2Al3+ BrBrO3Ca2+ Cd2+ Cd(CN)42Cd(NH3)42+ Ce3+ Ce4+ CH3COOCH3COOH CNCNSClClO4CO2 105.579 -245.2 -111.29 -1285.7 -531 -121.55 -67.07 -542.83 -75.9 428 -450.2 -696.2 -537.2 -486.01 -485.76 150.6 76.44 -167.15 -129.33 -413.8 CO2 CO32H+ H2O2 II3IO3K+ NH3 NH4+ NO3Na+ OHO2 SO42Sn2+ Sr2+ Tl3+ U4+ UO22+ -413.8 -677.14 0 -191.17 -55.19 -51.5 -221.3 -252.38 -80.29 -132.51 -205 -240.12 -229.99 -11.7 -909.27 -8.8 -545.8 196.6 -591.2 -1019.6 1-9 ∆H determination from other data ∆HT2 Reactants at T2 ∆Hreactants=(SCp)(T2-298) Reactants at 298 K Products at T2 ∆Hproducts=(SCp)(298-T2) ∆H298 Products at 298 K SCp is the sum of the heat capacities 1-10 Entropy (∆S) • 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 1-11 Calculations Compound H2O 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? • 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 1-12 Thermodynamic Laws • 1st law of thermodynamics If the state of a system is changed by applying work or heat or both, then the change in the energy of the system must equal the energy applied. ∆E = q (heat absorbed) + w (work) Conservation of energy Energy can be transferred, but no direction is given 1-13 Thermodynamic Laws • 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 0K 1-14 Faraday Laws • In 1834 Faraday demonstrated that the quantities of chemicals which react at electrodes are directly proportional to the quantity of charge passed through the cell • 96487 C is the charge on 1 mole of electrons = 1F (faraday) 1-15 Faraday Laws • Cu(II) is electrolyzed by a current of 10A for 1 hr between Cu electrode anode: Cu <--> Cu2+ + 2e cathode: Cu2+ + 2e- <--> Cu Number of electrons (10A)(3600 sec)/(96487 C/mol) = 0.373 F 0.373 mole e- (1 mole Cu/2 mole e-) = 0.186 mole Cu 1-16 Half-cell potentials • Standard potential Defined as °=0.00V H2(atm) <--> 2 H+ (1.000M) + 2e• 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 Fe3+ is reduced, Zn is oxidized 1-17 Half-Cell Potentials • Overall 2Fe3+ +Zn <--> 2Fe2+ + Zn2+ °=0.77+0.76=1.53 V • Half cell potential values are not multiplied Application of Gibbs • If work is done by a system ∆G = -°nF (n= e-) • Find ∆G for Zn/Cu cell at 1.0 M Cu2+ + Zn <--> Cu + Zn2+ °=1.10 V 2 moles of electrons (n=2) ∆G =-2(96487C/mole e-)(1.10V) ∆G = -212 kJ/mol 1-18 Reduction Potentials Electrode Couple Na+ + e- --> Na Mg2+ + 2e- --> Mg Al3+ + 3e- --> Al Zn2+ + 2e- --> Zn Fe2+ + 2e- --> Fe Cd2+ + 2e- --> Cd Tl+ + e- --> Tl Sn2+ + 2e- --> Sn Pb2+ + 2e- --> Pb 2H+ + 2e- --> H2(SHE) S4O62- + 2e- --> 2S2O32Sn4+ + 2e- --> Sn2+ SO42- + 4H+ + 2e- --> H2O + H2SO3(aq) Cu2+ + e- --> Cu+ S + 2H+ + 2e- --> H2S AgCl + e- --> Ag + ClSaturated Calomel (SCE) UO22+ + 4H+ + 2e- --> U4+ + 4H2O "E0, V" -2.7144 -2.3568 -1.676 -0.7621 -0.4089 -0.4022 -0.3358 -0.141 -0.1266 0 0.0238 0.1539 0.1576 0.1607 0.1739 0.2221 0.2412 0.2682 1-19 Reduction Potentials Hg2Cl2 + 2e- --> 2Cl- + 2Hg Bi3+ + 3e- --> Bi Cu2+ + 2e- --> Cu Fe(CN)63- + e- --> Fe(CN)64Cu+ + e- --> Cu I2 + 2e- --> 2II3- + 2e- --> 3IH3AsO4(aq) + 2H+ + 2e- -->H3AsO3(aq) + H2O 2HgCl2 + 4H+ + 2e- -->Hg2Cl2 + 2ClHg2SO4 + 2e- --> 2Hg + SO42I2(aq) + 2e- --> 2IO2 + 2H+ + 2e- --> H2O2(l) O2 + 2H+ + 2e- --> H2O2(aq) Fe3+ + e- --> Fe2+ Hg22+ + 2e- --> Hg Ag+ + e- --> Ag Hg2+ + 2e- --> Hg 2Hg2+ + 2e- --> Hg22+ NO3- + 3H+ + 2e- -->HNO2(aq) + H2O 0.268 0.286 0.3394 0.3557 0.518 0.5345 0.5354 0.5748 0.6011 0.6152 0.6195 0.6237 0.6945 0.769 0.7955 0.7991 0.8519 0.9083 0.9275 1-20 Reduction Potentials VO2+ + 2H+ + e- --> VO2+ + H2O HNO2(aq) + H+ + e- --> NO + H2O Br2(l) + 2e- --> 2BrBr2(aq) + 2e- --> 2Br2IO3- + 12H+ + 10e- -->6H2O + I2 O2 + 4H+ + 4e- --> 2H2O MnO2 + 4H+ + 2e- -->Mn2+ + 2H2O Cl2 + 2e- --> 2ClMnO4- + 8H+ + 5e- -->4H2O + Mn2+ 1.0004 1.0362 1.0775 1.0978 1.2093 1.2288 1.1406 1.3601 1.5119 2BrO3- + 12H+ + 10e- -->6H2O + Br2 1.5131 1-21 Nernst Equation • Compensated for non unit activity (not 1 M) • Relationship between cell potential and activities • aA + bB +ne- <--> cC + dD 2.30RT [C]c [D]d log nF [A]a [B]b • At 298K 2.3RT/F = 0.0592 • What is potential of an electrode of Zn(s) and 0.01 M Zn2+ • Zn2+ +2e- <--> Zn °= -0.763 V • activity of metal is 1 0.0592 1 0.763 log 0.822V 2 0.01 1-22 Kinetics and Equilibrium • Kinetics and equilibrium are 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 1-23 Kinetics • Rate of reaction Can depend upon conditions Paper reacts slowly with oxygen, but increases with temperature • Free energy does not dictate kinetics 16 H+ + 2 MnO4- + 5 Sn2+ <--> 5 Sn4+ + 2 Mn2+ + 8 H2O °= 1.39 V, ∆G = -1390 kcal/mol 8 H+ + MnO4- + 5 Fe2+ <--> 5 Fe3+ + Mn2+ + 4 H2O °= 0.78 V, ∆G = -376 kcal/mol The reaction with Fe is much faster 1-24 Kinetics • Rate can depend upon reaction path C6H12O6(s) + 6 O2(g) <--> 6 CO2(g) + 6 H2O(l) ∆G = -791 kcal/mol Glucose can be stored indefinitely at room temperature, but is quickly metabolized in a cell • Thermodynamics is only concerned with difference between initial and final state • Kinetics account for reaction rates and describe the conditions and mechanisms of reactions 1-25 Kinetics • Kinetics are very difficult to describe from first principles structure, elements, behavior • General factors effecting kinetics Nature of reactants Effective concentrations Temperature Presence of catalysts Number of steps 1-26 Nature of Reactants • Ions react rapidly Ag+ + Cl- <--> AgCl(s) Very fast • Reactions which involve bond breaking are slower NH4+ + OCN- <-->OC(NH2)2 • Redox reactions in solutions are slow Transfer of electrons are faster than those of atomic transfer • Reactions between covalently bonded molecules are slow 2 HI(g) <--> H2(g) + I2(g) 1-27 Nature of Reactants • Structure P4 Same formula P P P P P White Phosphorus P P P P P Red PhosphorusP Concentration Reaction can occur when molecules contact P 1-28 Concentration • Surface area larger surface area increases reaction • Mixing increases interaction • Need to minimized precipitation or colloid formation Rate Law • Concentration of reactant or product per unit time • Effect of initial concentration on rate can be examined 1-29 Rate Law • • • • rate = k[A]x[B]y rate order = x + y knowledge of order can help control reaction rate must be experimentally determined Injection Flow meter mixing detector 1-30 Rates Rate=k[A]n; A=conc. at time t, Ao=initial conc., X=product conc. Order rate equation 0 [A0]-[A]=kt, [X]=kt 1 ln[A0]-ln[A]=kt, ln[A0]-ln([Ao]-[X])=kt k mole/L sec 1/sec 2 L/mole sec 3 1 1 kt [A] [Ao ] 1 1 kt [Ao ] [X] [Ao ] 1 1 kt 1 1 kt 2 2 2 2 2 2 [A] [Ao ] ([Ao ] [X]) [Ao ] L2/mole2 sec 1-31 Rate Law • Half-life A =Aoe-t = ln2/t1/2 If a rate half life is known, fraction reacted or remaining can be calculated (CH3)2N2(g) <--> N2(g) + C2H6(g) Time Pressure (torr) 0 36.2 30 46.5 ln 2(30 min) t1/2 62.1 min 25.9 ln( ) 36.2 1-32 Rate Law • Temperature Reactions tend to double for every 10 °C • Catalysts Accelerate reaction but are not used Pt surface Thermodynamically drive, catalysts drive kinetics If not thermodynamically favored, catalysts will not drive reaction • Autocatalytic reactions form products which act as catalysts • Catalytic amount is moles of catalysts needed to cause reaction 1-33 Complexation Kinetics Uranium and cobalt with pyridine based ligands N HOOC N COOH N N N HOOC N N N COOH N COOH HOOC N N COOH N COOH COOH 111Py12 111Py14 222Py14 Examine complexation by UV-Visible spectroscopy 1-34 Complexation of U with 111Py12 0.60 Absorbance 0.50 Time (minutes) 1148 3956 0.40 8538 14153 21593 32767 34185 0.30 0.20 0.10 0.00 250 300 350 400 Wavelength (nm) 450 1-35 Absorbance Kinetics Absorbance sum from 250 nm to 325 nm for 111Py12 and uranium at pH 4 14.0 12.0 10.0 8.0 6.0 4.0 2.0 0.0 0 5000 10000 15000 20000 25000 30000 35000 Time (minutes) 1-36 Kinetic Data Evaluation Evaluation of change in absorbance 2 Abst 1 2 Abso 1 2 Abseq (1 e kt ) 1 Evaluation of absorbance and kinetic data for 111Py12 and 111Py14 with uranium at pH 4. The concentration of ligand and uranium is 50x10-6 mol/L. Ligand Abso ∆Abseq 111Py12 111Py14 7.86±0.82 5.66±1.28 4.82±1.70 7.06±5.76 k (min-1) 95% Equilibrium Time (min) 4.65±0.47x10-5 6.44±0.65x104 4.24±0.80x10-5 7.07±1.33x104 1-37 Acid-Base Equilibria Water can act as solvent and reactant • 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 1-38 Acid Strengths • Strong acids tend towards completion HCl + H2O <--> H3O+ + Cl Strong acids tend to have weak conjugate bases • Weak acid forms only slightly ionized species CH3COOH + H2O <--> CH3COO- + H3O+ Stronger conjugate base • Relative strengths of acids can be compared Can be rated relative to water • Some salts can have acid-base properties NH4Cl 1-39 Relative Strengths of Acids and Bases Acid Strength Conjugate Acid Conjugate Base HClO4 H2SO4 HCl H3 O+ H2SO3 HF HC2H3O2 HSO3H2S NH4+ HCO3 H2 O HSOH H2 ClO4SO42ClH2 O HSO3FC2H3O2SO32HSNH3 CO32OHS2O2H- Base Strength 1-40 Dissociation Constants • Equilibrium expression for the behavior of acid HA + H2O <--> A- + H3O+ [A ][H3O ] K Water concentration is constant [HA][H2O] [A ][H3O ] Ka K[H2 O] pKa=-logKa [HA] • Can also be measured for base Constants are characteristic of the particular acid or base [HB ][OH ] Kb [B] 1-41 Dissociation Constants for Acids at 25°C Acid Formula Acetic Hydrocyanic Carbonic HC2H3O2 HCN H2CO3 HCO3HNO2 H2 S HSH3PO4 H2PO4 HPO4 2H 2 C 2 O4 HC2O4- Nitrous Hydrosulfuric Phosphoric Oxalic Ka 1.8E-5 7.2E-10 3.5E-7 5E-11 4.5E-4 1E-7 1E-14 7.5E-3 6.2E-8 4.8E-13 5.9E-2 6.4E-5 1-42 Dissociation Constants for Bases at 25°C Base Ammonia Pyridine Methylamine Formula NH3 C5H5N CH3NH2 Kb 1.8E-5 2.3E-9 4.4E-4 Protonation of amine group 1-43 Calculations • 1 L of 0.1 M acetic acid has pH = 2.87 What is the pKa for acetic acid CH3COOH + H2O <--> CH3COO- + H3O+ [CH3COO-] = [H3O+] =10-2.87 pKa=4.73 10 (2*2.87) 5 Ka 1.84x10 0.1 10 2.87 1-44 Calculations • What is pH of 0.1 M NH3 Kb=1.8E-5 NH3 + H2O <-->NH4+ + OH[NH4+] = [OH -] = x [NH3] = 0.1 - x x2 + 1.8E-5x -1.8E-6 = 0 x2 1.8x10 5 0.1 x • [OH-] = 1.33E-3 M, pOH = 2.87, pH ≈ 14-pOH ≈11.12 1.8E 5 (1.8E 5)2 4 * 1.8E 6 x 2 1-45 Acid-Base Reactions For Water 2 H2O <--> H3O+ + OHWater concentration remains constant, so for water: Kw = [H3O+][OH-]= 1E-14 at 25°C 1-46 Common ion effect • Same products from different acids (hydronium ion) 0.2 M CH3COOH in 0.1 M HCl What is the free acetic acid concentration HCl is totally dissociated x=[CH3COO-], [CH3COOH]=0.2-x, [H3O+] = 0.1 + x • Ka = 1.8E-5 • Small Ka, x is much smaller than 0.1 x=3.6E-5 M 0.1x Ka 0.2 1-47 Hydrolysis Constants • Reaction of water with metal ion Common reaction Environmentally important Dependent upon metal ion oxidation state • Mz+ + H2O <--> MOHz-1+ + H+ • Constants are listed for many metal ion with different hydroxide amounts 1-48 Buffers • Weak acid or weak base with conjugate salt • Acetate as example Acetic acid, CH3COONa CH3COOH + H2O <--> CH3COO- + H3O+ large quantity If acid is addedhuge quantity large quantity small quantity hydronium reacts with acetate ion, forming undissociated acetic acid If base is added Hydroxide reacts with hydronium, acetic acid dissociates to removed hydronium ion 1-49 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- Write as pH [A ][H3O ] Ka [HA] Ka [HA] [H3O ] [A ] 1-50 Buffer Solutions [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 1-51 Buffers • What is a good buffer system for maintaining a solution at pH 4? Want 0.1 M total in 1L total volume • For acetic acid, pKa=4.75 [CH 3COOH] 4.00 4.75 log [CH 3COO ] We have 0.1 M each Volume CH3COO- =1/6.62 L = 0.15 L Acid =1-0.15 =0.85 L [CH 3COOH] log 0.75 [CH 3 COO ] [CH 3COOH] 5.62 [CH 3COO ] 1-52 Buffers • You have a buffer with 0.1 M acetic acid and 0.1 M sodium acetate in 1L. 0.01 moles of NaOH(s) is added. What is the pH? NaOH reacts with 0.01 moles of proton from the acid. • At equilibrium, we have 0.11 M sodium acetate and 0.09 M acetic acid • [H3O+]=1.5E-5, pH =4.8 ][0.11] [H O (pKa=4.75)K 1.8E 5 3 a [0.09] 1-53 Equilibrium • Reactions proceed in the forward and reverse direction simultaneously N2 + 3 H2 <--> 2 NH3 Initially contains nitrogen and hydrogen Forward rate decreases as concentration (pressure) decreases Ammonia production increase reverse rate Eventually, forward rate is equal to reverse rate No net change in concentration Reaction still occurring 1-54 Equilibrium • Some reactions have a negligible reverse rate Proceeds in forward direction Reaction is said to go to completion 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 1-55 Equilibrium • N2 + 3 H2 <--> 2 NH3 + 22 kcal What is the shift due to Increased temperature? Increased N2? Reduction of reactor vessel volume? 1-56 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 1-57 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 1-58 Activities • 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 1-59 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 ij = specific ion interaction term log i Z 2D ij log ß() logß(0) Z2i D ij 1-60 Activities • Pitzer Binary (3) and Ternary (2) interaction parameters K+ Ca2+ Al3+ Fe(CN)641-61 Cm-Humate at pH 6 6.6 Experimental Data shows change in stability constant with ionic strength 6.5 Ion Specific Interaction Theory used logß 6.4 6.3 6.2 6.1 6.0 0.0 0.5 1.0 1.5 I mIm sqrt 2.0 2.5 3.0 1-62 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 1-63 Constants Conditional Constants An experimental condition is written into equation * Pu4+ + H2CO3 <--> PuCO32+ +2H+ Constant can vary with concentration, pH Must look at equation! Often the equation is not explicitly written 1-64 Using Equilibrium Constants • Constants and balanced equation can be used to evaluate concentrations at equilibrium [H2 ][Y]2 2 HY <--> H2 + 2Y, K K=4E-15 [HY]2 If you have one mole of HY initially, what are the concentration of the species at equilibrium? Try to write species in terms of one unknown Start will species of lowest concentration [H2] =x, [Y]=2x, [HY]=1-2x Since K is small, x must be small, 1-2x ≈ 1 K=4x3, x =1E-5, 2x=2E-5 [x][2x]2 K [1 2x]2 1-65 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 1-66 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 UO2(OH)4223.1 Other species may need to be (UO2)2OH3+ 11.0 considered. If the total (UO2)2(OH)2+ 22.0 uranium concentration is low UO2CO3 8.87 enough, binary or tertiary UO2(CO3)2216.07 species can be excluded. 4UO2(CO3)3 21.60 UO2HA(II) 6.16 UO2(OH)HA(I) 14.7±0.5 1-67 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 1-68 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 1-69 Comparison of measured and calculated uranyl organic colliod 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 1-70 Energy terms • 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 1-71 Temperature effect on Np-Humate stability T emp (°C) 56 48 40 32 24 16 76 74 Rlnß 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 1/T (K) 0.0034 0.0035 1-72 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 Ksp K[AgCl] [Cl ][Ag ] 1-73 Solubility calculations • AgCl(s) at equilibrium with water at 25°C gives 1E-5 M silver ion in solution. What is the Ksp?? AgCl(s) <--> Ag+ + Cl-: [Ag+] = [Cl-] Ksp = 1E-52 = 1E-10 • What is the [Mg2+] from Mg(OH)2 at pH 10? Ksp = 1.2E-11= [Mg2+] [OH]2 [OH] = 10-(14-10) [Mg 2 1.2E 11 ] 1.2E 3 1E 8 1-74 Solubility Calculations • 50 mL of 0.02 M Ag+ added to 50 mL 0.1 M HCl, what is the silver ion concentration in solution?? So assume all Ag+ forms AgCl 0.001 moles Ag+, 0.005 moles Cl [Cl-] = 0.004 moles/0.1 L =0.04 M Ksp= 1E-10 [Ag+] =1E-10/0.04 =2.5E-9 M 1-75 Solubility Calculations • What is the maximum pH of a 0.1 M Mg2+ solution in which Mg(OH)2 will not precipitate?? Ksp = 1.2E-11= [Mg2+][OH-]2 [OH-]=(1.2E-11/0.1)0.5 =1.09E-5 pOH = 4.96 pH = 9.04 • How can this be used to separate metal ions? Separate Mg2+ from Fe2+, 0.1 M each metal ion. Want minimum 500:1 Mg2+:Fe2+ Ksp(Fe(OH)2)=1.6E-14 1-76 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 1-77