Electrochemistry Solutions of Electrolytes Dissociation of Water Dissociation of Water and the Acidity Constant Ph of Strong

Electrochemistry Solutions of Electrolytes Dissociation of Water Dissociation of Water and the Acidity Constant Ph of Strong

1/28 2/28 Electrochemistry co04 Solutions of electrolytes co04 Subject of electrochemistry: strong electrolyte: (almost) completely ionizes (dissociates) no uncharged molecules in the solution dissociation (solutions of electrolytes, melts of salts) H2SO4, KOH, Ca(OH)2, NaCl, BaSO4,... conductivity not necessarily to max. degree: 100 % partially 2 phenomena at interfaces s/l (electrolysis, galvanic cells) H2SO4 H+ + HSO4 2 H+ + SO4 → − → − weak electrolyte: contains neutral (not dissociated) molecules Conductors: organic acids and bases, NH3,H2O, . electrons (or holes) are moving: standard states: solvent (water): ; in dilute 1 • water = metals, graphite, graphene, semiconductors c st ions: [ ] ( = γc/c ) ions are moving (or jumping): dissociation constant = equilibrium constant of the dissociation reaction solutions of electrolytes , molten salts, ionic liquids + CH3 COOH CH3 COO− + H both electrons and ions are moving: → + NH3 + H2O NH4 + OH− plasma → + (COOH)2 HOOC-COO− + H → pH log = log10, p = log − γ + =1 c + c + H H H ? + ? + pH = log H+ = log = log = log[H ] = log{H } cst mol dm 3 − − − − − − 3/28 4/28 Dissociation of water co04 Dissociation of water and the acidity constant co04 Dissociation of water: Acidity constant (ionization constant) Ka is common in tables = equilibrium con- + stant of deprotonisation, often given as pKa H2O H + OH− → acids: dissociation constant of the acid Ionic product (autoionization constant) of water Kw: + H+ OH cH+ cOH . CH3 COOH CH3 COO + H Ka = Kd K − − H+ OH 1.00 10 14 25 C − w = st 2 [ ][ −] = − ( ◦ ) → H2O ≈ (c ) ≡ × bases: dissociation constant of the conjugated acid Equivalently (at 25 C): ◦ NH4+ NH3 + H+ (Ka) ( 1) pH + pOH = pKw = 14 more accurate 13.997 → × − H O H+ OH K 1 2 + − ( w) (+ ) → × depends on temperature: pK (100 C) = 12.29 w ◦ NH H O NH + OH K K /K heavy water: pK (25 C) = 14.87 3 + 2 4 + − d = w a w ◦ → (isotopic effect: D is more strongly bound) Example. Acidity constant of ammonium is pKa = 9.25 (at 25 C). Calculate× the ◦ − 10 78 . 1 dissociation constant of ammonium hydroxide (water solution of NH3). 5 5/28 6/28 pH of strong acids and bases co04 Dissociation of a weak acid I co04 Calculate pH of aqueous HCl of concentration 0.01 mol dm 3. Example. − + HA H + A− 100 % dissociation to the 1st degree: → Determine pH of a weak acid from known concentration. cH+ = cHC pH = log H+ log cH+ = 2 ⇒ − ≈ − (analytic) concentration: c0 Calculate pH of aqueous H SO of concentration 0.001 mol dm 3. acidity constant: Ka Example. 2 4 − It dissociates completely to the 1st degree, partially to the 2nd degree, but since Assumptions: here c K 1.3 10 2, we can assume also 100 % dissociation. 2 = − × cOH cH+ − cH+ = 2cH2SO4 pH = log H+ log(2cH+ ) = 2.7 ⇒ − ≈ − γ 1 (approximation of infinite dilution) more accurate 2.75 (partial dissociation + Debye–Hückel) = compound 0 eq. Example. Calculate pH of aqueous NaOH of concentration 0.01 mol dm 3 at 25 C. − ◦ H+ A 2 3 14 12 3 HA c0 c0 [ ][ −] cOH = 0.01 mol dm , cH+ = 10 /0.01 = 10 mol dm , pH = 12 Balance: − Equation: = = Ka − − − − − A 0 HA c − [ ] 0 Calculate pH of 0.001 M aqueous Ca(OH) at 25 C. + − Example. 2 ◦ H 0 3 cOH = 0.002 mol dm , pOH = 2.7, pH = 14 2.7 = 11.3 2 − − st − Correctly st = Ka. We will neglect c (concentrations should be inserted in (c0 )c mol dm 3). − − 7/28 8/28 Dissociation of a weak acid II co04 Weak acid in a buffer co04 H+ A 2 [ ][ −] + Equation: = = Ka HA H + A− [HA] c0 → − Solution: How much of deprotonated form can we find in a solution of given pH? 10 2 compound 0 eq. Ka Ka c0 Ka A K cH+ = = + Kac0 Kac0 HA c0 c0 [ −] a v 2 − 2 ≈ u − = + -- Æ A 0 [HA] [H ] [CH3COOH] [CH3COO ] Summary of approximations: t − + -3 H cH+ cH+ maintained by buffer dm the acid is stronger than water (K K ) ← a w 5 c0Ka CH COOH concentration c0 is high enough (c0 Ka), then most of the acid is not ionized = cA = 3 − c + K c/mmol -3 H + a 10 mmol dm c0 is not too high so that we can use the infinite dilution approximations (γ = 1) Degree of dissociation: pKa = 4.76 Alternate form: 1 1 α = pH = (pKa + pcA) c + /Ka 1 0 2 H + 2 3 4 5 6 7 8 Degree of dissociation: We have assumed the infinite dilution ap- pH proximations 1 Ka α for pH=pK α = 2 a ≈ vc0 u t 9/28 10/28 C Calculate pH of rainwater at 25 ◦ and 1 bar. co04 pH of a weak base co04 3 1 Example. Calculate pH of aqueous solution of ethylamine of concentration c0 = Henry constant of dissolution of CO2: Kh = 0.033 mol dm bar − − 0.01 mol dm 3 at 25 C. The acidity constant of ethylammonium is K 1.6 10 11. − ◦ a = − Acidity constant of CO2: pKa1 = 6.37. This is total for reactions × C H NH H O C H NH + OH 2 5 2 + 2 2 5 3 + − CO H O H CO H+ HCO → 2 + 2 2 3 + 3− K 1 10 14 → → w − Dissociation constant of ethylamine: Kd = = × = 0.000 625 CO in the air (2019/2 Mauna Loa): y 411 ppm (18th century: y 280 ppm) K 1.6 10 11 2 = = a − 2 + × CO3 can be neglected (pKa2 = 10.32) Assumptions: [H ] [OH ], γ = 1. And in the same way as for weak acids: − − OH can be neglected − compound 0 eq. 2 3 1 C H NH + OH c K y p 0.033 mol dm bar 0.000411 1 bar C2H5NH2 c0 c0 [ 2 5 3 ][ −] CO2 = h CO2 = − − Balance: Equil.: K 5 3 × × − = = d = 1.36 10 mol dm C2H5NH3+ 0 [C2H5NH2] c0 − − − × OH 0 ? − Balance: c + c (Not cCO cCO c + because CO is given by equilib- H = HCO3− 2 = 2.0 H 2 rium, not initial concentration.) − 2 Kd Kd c0 Kd Equation: = [OH ] = + Kdc0 Kdc0 [H+][HCO3 ] − v 2 2 − K log 1.36 10 5 u − ≈ = a1 − Æ [CO2] − × or: t . 1 + 1 1 pH = (pKa + pKw pc0) [H ] = Ka1[CO2], pH = 2(pKa1 + p[CO2]) = 2(6.37 + 4.87) = 5.62 2 − = 22 . 0 α the real pH isÆ usually lower (HNO3,H2SO4) (18th cent.: pH = 5.70) 11.40; approx.: pH=11.34, 11/28 12/28 Simultaneous equilibria: very dilute solutions co04 Very dilute solutions co04 Dissociation of water has to be taken into account. CH3COOH, pKa = 4.76 + 8 HA H + A− (Ka) → + H2O H + OH− (Kw) → “exact” 7 “Explicit” balance “Implicit” balance 2 6 compound 0 eq. compound balance + Ka Ka [H ] = 2 + Kac0 2 HA c0 c0 A [A ] + [HA] = c0 s − − − pH 5 A 0 charge H+ A OH 0 − [ ] ([ −] + [ −]) = + − H 0 + y + Equations [H ] = Kac0 4 OH 0 y − (approximate formula) H+ A p [ ][ −] 3 = Ka Equations HA [ ] In a realistic region of concentrations the ( + y) H+ OH K [ ][ −] = w simplified formula is sufficient 2 = Ka -1- 0 1 2 3 4 5 6 7 8 9 10 c0 − 4 equations, 4 unknowns: p[C H COOH] ( + y)y = Kw 2 5 H+ , HA , A , OH [ ] [ ] [ −] [ −] 2 equations, 2 unknowns: , y [cd show; blend -g lysine]13/28 [cd ../maple; xmaple lysine.mws]14/28 Simultaneous equilibria: ion speciation co04 Lysine co04 Aminoacids, ionization degree according to pH. E.g., HIS, LYS: NH -(CH ) -CH(NH )-COOH, pK 2.15, pK 9.16, pK 10.67 2 2 2 4 2 a1 = a2 = a3 = AH3 + AH2+ + H+ (Ka1) → AH2+ AH + H+ (Ka2) 1 AH → A H+ K pKa1 pKa2 pKa3 − + ( a3) → 2 H+ easily detaches from AH3 +, hardly from AH Ka1 > Ka2 > Ka3 or pKa1 < pKa2 < pKa3. − ⇒ Lys Balance: 3 Lys − LysH+ + 2+ dm 2+ [A ] + [AH] + [AH2 ] + [AH3 ] = c0 LysH − 0.5 Equation: mmol / + + i [AH2 ][H ] c K 2 = a1 [AH3 +] [AH][H+] = Ka2 [AH2+] A H+ 0 [ −][ ] 0 1 2 3 4 5 6 7 8 9 10 11 12 13 14 = Ka3 [AH] pH 15/28 16/28 From real life co04 Salt of weak acid + strong base + co04 Titanium dental implants are treated (e.g.) in a phosphoric E.g., M=Na, A=CH3COO. acid solution. Calculate the needed concentration (in pure + MA M + A− (100 %) water) for pH = 3.42. Data: pK1 = 2.18, pK2 = 7.198, → A H O AH OH (hydrolysis) pK 12.319. − + 2 + − 3 = → 3 4 neglected) PO .8mo/ (H mmol/L 0.38 compound 0 eq. conditions − 2 3 4 4 ) PO +H PO .0mo/ (H mmol/L 0.40 M+ c0 c0 Kw A c c H+ A c0 − 0 0 [ ][ −] ( ) − Ka = − OH 0 HA − [ ] ≈ HA 0 H+ 0 Kw/ for [OH ] [H+] − Solution: 2 c0Kw Kw Kw c0Kw 1 = + pH 2(pKw + pKa pc0) v Ka 2Ka − 2Ka ≈ v Ka ⇒ ≈ − credit: Wikipedia u u t t Kw where the last approximation holds for c0 K & Kw, i.e., c0 Ka a p 17/28 18/28 Little soluble salts of strong electrolytes co04 Little soluble salts: more ions co04 Solubility product = equilibrium constant of dissociation. 9 Calcium oxalate: Ks(CaC2O4) = 3.9 10 . × − activities of salts (s) are salt = 1 a) how much dissolves in pure water? b) how much dissolves in blood? γ = 1 assumed for ions ( Ca2+ 2.4 mmol dm 3) [ ] = − Ba2+ SO 2 2+ 2 4 − 2+ 2 BaSO4 Ba + SO4 Ks = = [Ba ][SO4 ] 2+ 2 − − CaC2O4 Ca + C2O4 → BaSO4 − → 2 2 2+ 2+ 2 Ks = [Ca +][C2O4 ] Mg(OH)2 Mg + 2 OH− Ks = [Mg ][OH ] − → − 3+ 2 3 2 2 3 Solution: As2S3 2 As 3 S Ks As + S + − = [ ] [ −] 2 2+ 2 → 3+ 2 a) [C2O4 ] = [Ca ] = Ks but: S + H2O HS + OH ..

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