Natural Stratosphere
Chapman Mechanism
R1 O2 + hv -> 2O J1 to be calculated R2 O + O2 + m -> O3 + m k2 = 6.0e-34/((temp/300)**2.3) R3a O3 + hv -> O(1D) + O2 J3a to be calculated R3b O3 + hv -> O(3P) + O2 J3b to be calculated R4 O + O3 -> 2O2 k4 = 8.0e-12*exp(-2060./temp)O(1D) Chemistry [Don't forget R3a]
R5 N2O + hv -> O(1D) + N2 J5 to be calculated R6 O(1D) + m -> O(3P) + m k6 = 2.1e-11*exp(+100/temp) R7a O(1D) + H2O -> 2OH k7a = 2.2e-10 R7b O(1D) + N2O -> 2NO k7b = 6.7e-11HxOy Chemistry
R8 OH + O3 -> HO2 + O2 k8 = 1.6e-12*exp(-940/temp)
R9 HO2 + O3 -> OH + 2O2 k9 = 1.1e-14*exp(-500/temp)
R10 OH + O -> HO2 k10 = 2.2e-11*exp(+120/temp)
R11 HO2 + O -> OH + O2 k11 = 3.0e-11*exp(+200/temp)
R12 HO + HO2 -> H2O + O2 k12 = 4.8e-11*exp(+250/temp)
R13a HO2 + HO2 -> H2O2 + O2 k13a = (2.3e-13*exp(+600/temp) +
nm*1.7e-33*exp(+1000/temp))
[NOTE: k13a is a 2-body + an effective 3-body rate coefficient]R13b OH + OH + m -> H2O2 + m k13b = 6.9e-31/((temp/300)**0.8) R14 H2O2 + hv -> 2OH J14 to be calculated R15 H2O2 + OH -> H2O + HO2 k15 = 2.9e-12*exp(-160/temp)NOy Chemistry
R16 NO + O3 -> NO2 + O2 k16 = 2.0e-12*exp(-1400/temp)
R17 NO2 + hv -> NO + O J17 to be calculated
R18 NO2 + O -> NO + O2 k18 = 6.5e-12*exp(+120/temp)
R19 OH + NO2 + m -> HNO3 + m k19 = 2.6e-30/((temp/300)**3.2)
[high pressure 2-body limit k19 = 2.4e-11/((temp/300)**1.3)]
R20 HNO3 + hv -> OH + NO2 J20 to be calculated
R21 OH + HNO3 -> H2O + k21 = 7.2e-15*exp(785/temp)
NO2 + O
[NOTE - in the troposphere k21 is more complex]
Additional NOy Reactions for Class InformationR22 NO2 + O3 -> NO3 + O2 k22 = 1.2e-13*exp(-2450./temp) R23a NO3 + hv -> NO + O2 J23a to be calculated R23b NO3 + hv -> NO2 + O J23b to be calculated R24a NO3 + NO2 + m -> N2O5 + m k24a = 2.2e-30/((temp/300)**3.9) [high pressure 2-body limit k24a = 1.5e-12/(temp/300)**0.7)] R24b N2O5 -> NO2 + NO3 K24b = k24a/(2.7e-27*exp(11,000./temp)) R25 N2O5 + hv -> NO2 + NO3 J25 to be calculated R26 N2O5 + aerosol -> removal k26 to be determinedAnother Potential NOy Reservoir
R27a NO2 + HO2 + m -> HO2NO2 + m k27a = 1.8e-31/((temp/300)**3.2) [high pressure 2-body limit k27a = 4.7e-12/((temp/300)**1.4)] R27b HO2NO2 -> HO2 + NO2 k27b = k27a/(2.1e-27*exp(10,900/temp) R28 HO2NO2 + hv -> HO2 + NO2 J28 to be calc., though some ? about products R29 HO2NO2 + OH -> products k29 = 1.3e-12*exp(+380/temp)Tropospheric Chemical Reactions [NOTE: All reactions that require O2 treat the O2 implicitly (O2). The O2 is NOT considered one of the reactants AND the rate coefficients are 2-body, except for J37 and J38 which are photodissociation rate coefficient.
R21 OH + HNO3 -> H2O + [The more complex form for the troposphere]
NO2 + O k21 = 7.2e-15*exp(785/temp) +
(1.9e-33*exp(725/temp)*nm(z))/
(1.0 + (1.9e-33*exp(725/temp)*nm(z)/
(4.1e-16*exp(1440/temp))))
R30 NO + HO2 -> NO2 + OH k30 = 3.7e-12*exp(250/temp)
R31 HNO3 or H2O2 -> deposition k31 = 1e-5 (z = 0.0)
= 2e-6 (z = 5.0)
= 6e-7 (z = 10.0)
= 0.0 (z > 10.0)
R32 OH + CO (O2)-> CO2 + HO2 k32 = 1.5e-13*(1 + (0.6*nm(iz)/nm(1)))
R33 OH + CH4 (O2)-> H2O + CH3O2 K33 = 2.65e-12*exp(-1800/temp)
R34 CH3O2 + NO (O2)-> H2CO + HO2
+ NO2 K34 = 4.2e-12*exp(180/temp)
R35 CH3O2 + HO2 -> CH3OOH + O2 K35 = 3.8e-13*exp(800/temp)
R36 H2CO + OH (O2)-> H2O + HO2
+ CO K36 = 1.0e-11
R37a H2CO + hv (O2)-> CO + 2HO2 J37a = pch2oa(iz) in Photocalc
R37b H2CO + hv -> CO + H2 J37b = pch2ob(iz) in Photocalc
R38 CH3OOH + hv (O2)-> H2CO +
HO2 + OH J38 = pch3ooh(iz) in Photocalc
R39 CH3OOH + OH -> H2O + CH3O2 K39 = 3.8e-12*exp(200/temp)