The following reaction mechanism is a simplified mechanism for the destruction of ozone during the Austral Spring resulting in an "ozone" hole over Antarctica. Determine the rate law for the formation of oxygen predicted by this mechanism. (Assume the steady-state approximation is valid for any reaction intermediates.) k₁ (CIO)2 CIO + CIO + M (CIO)2 + sunlightk₂ ClOO + Cl ClOO + M 2x (Cl +03 net: 2 03 k3 → Cl + O₂ k4 → 30₂ Clo + 0₂) CIO (this reaction occurs twice in the mechanism)

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The following reaction mechanism is a simplified mechanism for the destruction
of ozone during the Austral Spring resulting in an "ozone" hole over Antarctica.
Determine the rate law for the formation of oxygen predicted by this mechanism. (Assume
the steady-state approximation is valid for any reaction intermediates.)
k₁ (CIO)2
CIO + CIO + M
(CIO)2 + sunlight
k3
ClOO + M
2x (Cl + 03
net: 2 03
k4
2 Cloo + Cl
Cl + O₂
CIO + O2)
3 0₂
(this reaction occurs twice in the mechanism)
Transcribed Image Text:The following reaction mechanism is a simplified mechanism for the destruction of ozone during the Austral Spring resulting in an "ozone" hole over Antarctica. Determine the rate law for the formation of oxygen predicted by this mechanism. (Assume the steady-state approximation is valid for any reaction intermediates.) k₁ (CIO)2 CIO + CIO + M (CIO)2 + sunlight k3 ClOO + M 2x (Cl + 03 net: 2 03 k4 2 Cloo + Cl Cl + O₂ CIO + O2) 3 0₂ (this reaction occurs twice in the mechanism)
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