In Problem 14.37, NO 2 transport by diffusion in a stagnant atmosphere was considered for steady-state conditions.

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In Problem 14.37, NO2 transport by diffusion in a stagnant atmosphere was considered for steady-state conditions. However, the problem is actually time dependent, and a more realistic approach would account for transient effects. Consider the ground level emission of NO2 to begin in the early morning (at t = 0), when the NO2 concentration in the atmosphere is everywhere zero. Emission occurs throughout the day at a constant flux N''A,0, and the NO2 again experiences a first-order photochemical reaction in the atmosphere (NA = –k1CA).

(a) For a differential element in the atmosphere, derive a differential equation that could be used to determine the molar concentration CA(x, t). State appropriate initial and boundary conditions

(b) Obtain an expression for CA (x, t) under the special condition for which photochemical reactions may be neglected. For this condition what are the molar concentrations of NO2 at ground level and at 100-m elevation 3 h after the start of the emissions, if N''A,0 = 3 x 10-11k mol/s ∙ m2 and DAB = 0.15 x 10-4 m2/s?

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Fundamentals of Heat and Mass Transfer

ISBN: 978-0471457282

6th Edition

Authors: Incropera, Dewitt, Bergman, Lavine

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