O3 is produced in the troposphere through the photochemical oxidation of NO2. The photolytically formed O3 reacts with NO to regenerate NO2 through the following reaction: O3(g) + NO(g) → NO2(g) + O2(g) Calculate the equilibrium constant (K) of the reaction at 100 °C and 1 atm.

Chemistry for Engineering Students
3rd Edition
ISBN:9781285199023
Author:Lawrence S. Brown, Tom Holme
Publisher:Lawrence S. Brown, Tom Holme
Chapter11: Chemical Kinetics
Section: Chapter Questions
Problem 11.86PAE
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O3 is produced in the troposphere through the photochemical oxidation of NO2. The photolytically formed O3 reacts with NO to regenerate NO2
through the following reaction:
O3(g) + NO(g) → NO2(g) + O2(g)

Calculate the equilibrium constant (K) of the reaction at 100 °C and 1 atm.

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