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Ozone in the lower atmosphere can react with nitrogen monoxide (shown below). This is one of the steps in the formation of photochemical smog. O(g)

Ozone in the lower atmosphere can react with nitrogen monoxide (shown below). This is one of the steps in the formation of photochemical smog. O(g) + NO(g) O(g) + NO(g) The rate law for this reaction is rate = k[O][NO] If [O] and [NO] were to remain essentially constant at [NO] = 5.70 10 M and [O] = 2.20 10 M (because of continuous production from separate sources), and k = 3.10 10 Ms, calculate the mass in grams of NO(g) that would be produced per hour per liter of air.

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