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Table D.2

Heterogeneous reactions involving chemistry species studied in the ID photochemistry model.

Key Heterogeneous Reaction Uptake Coefficient (γ) Citations
hCl1 6H2O+hv+DustMg(ClO4)2Cl+4O+DustMg(ClO4)6H2O$\eqalign{ & 6{{\rm{H}}_2}{\rm{O}} + {\rm{h}}v + {\rm{Dus}}{{\rm{t}}_{{\rm{Mg}}{{\left( {{\rm{Cl}}{{\rm{O}}_4}} \right)}_2}}} \cr & {\rm{Cl}} + 4{\rm{O}} + {\rm{Dus}}{{\rm{t}}_{{\rm{Mg}}\left( {{\rm{Cl}}{{\rm{O}}_4}} \right) \cdot 6{{\rm{H}}_2}{\rm{O}}}} \cr} $ 6.20×10−2 × MIN(RH,1.0) × jClO This study, motivated by Zhang et al. (2021)
Huynh & McNeill (2021) and Huynh & McNeill (2020)
hCl2 HCl+ Dust CaCO3 Products ${\rm{HCl}} + {\rm{ Dust}}{{\rm{ }}_{{\rm{CaC}}{{\rm{O}}_3}}}{\rm{ Products }}$ MPMa(0.02, 2.03E3, 12.30E3) fit to the MPM
((Berland et al. 1997))
hCl3 HCl + Ice → Products MPM(0.09, 8.33E8, 30.50E3) × (1 − θLang) Hynes et al. (2001)
hCl4 Cl2 + DustNaCl → Products lE-5 Burkholder et al. (2019) upper limits
hCl5 CIO + Ice → Products lE-4 Burkholder et al. (2019) upper limits

a MPM denotes the MPM function, where MPM(A,ADes /AR,ΔE)=A×(1+ADesAR×exp(ΔE/RT))1${\mathop{\rm MPM}\nolimits} \left( {{\rm{A}},{{\rm{A}}_{{\rm{Des }}}}/{{\rm{A}}_R},\Delta E} \right) = {\rm{A}} \times {\left( {1 + {{{A_{Des}}} \over {{A_R}}} \times \exp ( - \Delta {\rm{E}}/{\rm{RT}})} \right)^{ - 1}}$. ADes (s−1) denotes the pre-exponential factor of the adsorbed molecule; AR (s−1) denotes the pre-exponential factor of the adsorbed molecules ionisation; Δ E (J mol−1) denotes the difference in activation energies of the Arrhenius equations controlling the absorption of molecule onto the solid and the ionisation of the adsorbed molecule at the solid surface; R (J mol−1 K−1) is the universal gas constant; T is the atmospheric temperature.

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