§9.3 The rate equation of reaction with simple order H2 + I2 = 2 HI r k[H 2 ]1[I 2 ]1 H2 + Cl2 = 2 HCl r k[H 2 ]1[Cl2 ]0.5 H2 + Br2 = 2 HBr [H 2 ][Br2 ]0.5 rk [HBr] 1 k ' [Br2 ] Overall reactions Reaction with definite order Reaction without definite order Reaction with simple order It was found that reactions with same reaction order are usually of same kinetic characteristics, therefore, reactions are usually classified on the basis of reaction order. Reaction with simple order: The reaction whose rate only depends on the concentration of reactants, and both the partial order and the reaction order is zero or plus integer is called reaction with simple order. r = kcn n kinds 0 zeroth-order reaction 1 first-order reaction 2 second-order reaction 3 third-order reaction Comparison between reactions with different reaction orders order First Second Third Zeroth Differential rate equation Integrated rate equation Linearity Half-life Unit of k 3.1 First-order reaction: Reaction: A P at t = 0 c0 at t = t c Differential rate equation: dc k1c dt can be rearranged into: dc k1dt c Which can be integrated directly c0 ln k1t c c c0 exp(k1t ) c c0 exp(k1t ) 1.0 C / mol dm-3 c~t curve of firstorder reaction 0.8 0.6 0.4 0.2 0.0 0 1000 2000 3000 4000 5000 t/s Half-life c0 c 2 c0 ln k1t c ln 2 0.6932 t1 k1 k1 2 Only when t , can c 0, which suggests that, the first-order reaction can not complete. ln(C/mol dm-3) 0 lnc ~ t curve of the first-order reaction -1 -2 -3 -4 -5 0 1000 2000 3000 4000 5000 t/s ln c ln c0 k1t The slope of the lnc ~ t curve is the k1 Characteristics of the first-order reaction 1) Unit of k is s-1 2) lnc is in linear proportion to t 3) can not complete 4) Half-life does not depend on c0 Example: 1) Decay of isotopes 226 88 Ra 226 86 Rn 42 He 2) Decomposition 1 N 2 O5 N 2 O 4 O 2 2 3) Isomerization Example: The half-life of the first-order decay of radioactive 14C is about 5720 years. The natural abundance of 14C isotope is 1.1 10-13 mol% in living matter. Willard F. Libby 1960 Noble Prize Radiochemical analysis of an object obtained in an archeological excavation USA shows that the 1908/12/17 ~1980/09/08 10-14 mol%. Application of 14C for age determinations (radiocarbon dating) 14C isotope content is 0.89 3.2 Second-order reaction 2A P; A + B P A + B P a b cA= ax cB =bx Differential rate equation: dx k 2 (a x)(b x) dt dCA k 2 CA C B dt dx k2 dt (a x)(b x) x 0 x 0 t dx k2 dt (a x)(b x) 0 x t dx dx k 2 dt 0 (a b)(b x) (a b)( a x) 0 ln( b x) ln b ln( a x) ln a k 2t ( a b) ( a b) ( a b) ( a b) 1 b( a x ) ln k 2t (a b) a(b x) When a = b dc k2 c 2 dt dc 2 k2 dt C0 c C 1 1 k2t c c0 C / mol dm-3 1.0 0.8 0.6 0.4 0.2 0.0 0 1000 2000 3000 t/s 4000 5000 c~t curve of second-order reaction When c 0, t , which suggests that, the pure secondorder reaction can not complete, either. Half-life t1/ 2 1 k2 c0 1/C/ mol dm-3 1/c ~ t curve of second-order reaction 50 40 30 20 10 0 0 1000 2000 3000 4000 5000 t/s For pure second-order reaction 1 dc 2 k2 c 2 dt 1 1 2k2t c c0 t1/ 2 1 2k2 c0 Characteristics of second-order reaction 1) Unit of k is mol-1dm3s-1 2) 1/c is in linear proportion to t 3) can not complete 4) Half-life 1 t1 c0 2 Increasing the initial concentration of the reactant will shorten the reaction time. Example: 1) dimerization 2) decomposition 2HI = H2 + I2 3) recombination 2CH3 = C2 H6 4) esterification CH 3 COOH+C 2 H 5 OH → CH 3 COOC2 H 5 +H 2 O 5) hydrolysis C12H22O11 + H2O C6H12O6 + C6H12O6 C12H22O11 + H2O C6H12O6 + C6H12O6 In 1850, experiment done by Wilhelmy suggested that the rate equation of the reaction is: r k[C12 H22O11 ] r k[C12 H 22O11 ][H 2O]v Because the amount of water keeps nearly unchanged during the reaction, [H2O] keeps nearly constant, and the rate equation can be then simplified as r k '[C12 H 22O11 ] Pseudo first-order reaction r k[C12 H 22O11 ][H 2O]6 [H 3O ] 3.3 third-order reaction 3A P A + B + C P 2A + B P 3A P 1 1 1 2 2 3k3t 2 c c0 1 dc k3 c 3 3 dt 1 1 2 6k3t 2 c c0 1 t1 2 2 k c 3 0 2 For A + B + C P with same initial concentration Differential rate equation dc k3 c 3 dt Integrated rate equation 1 1 2 2k3t 2 c c0 1 1 1 2 2 k3t 2 c c0 3 t1 2 2 k c 3 0 2 Only five third-order gaseous reactions have been observed. 2NO + X2 N2O + X2O; X = H, D 2NO + O2 2NO2; 2NO + X2 2NOX; X = Br, Cl Are these true third order reactions ? r = k [C6H5CHO]2[CN-] r = k [C2H4O][H+][Br-] 3.4 Zeroth-order reaction A P Differential rate equation c t c0 0 dc k0 dt c0 c k0t dc k0 dt t1/ 2 c0 2k0 When c = 0, the reaction completes, the reaction time is: c0 t k0 The zero-order reaction can complete. C / mol dm-3 1.0 0.8 0.6 0.4 0.2 0.0 0 1000 2000 3000 4000 5000 t/s c ~ t curve for zero-order reaction Characteristics of zeroth-order reaction 1) Unit of k is mol dm-3s-1 2) c is in linear proportion to t 3) can complete 4) When c increases, reaction time will be prolonged. C0 t k0 Examples: Decomposition over catalysts: 1) 2N2O 2N2 + O2 over Pt wire 2) 2NH3 N2 + 3H2 over W wire Photochemical reaction: r=kI I: intensity of radiation 5.5 for nth-order reaction r kc n 1 1 1 { n1 } k n t n 1 n 1 (a x) a t1/ 2 2n 1 1 A n 1 n 1 (n 1)kc0 c0 For n 1