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330                                                  11  Air Dispersion



                                                                     Concentration
                       z                                               profile
            Wind
            speed u                                 Time-averaged plume
                                                    centerline

                                 Plume
                                 rise, Δh          Instantaneous
                                                   plume



                                             Effective
                                 Stack       plume
                Stack            height,     center line,
                                 h           H


                      x=0                                                   x

            Fig. 11.7 Schematic representation of Gaussian plume dispersion



            11.3.1 General Gaussian Dispersion Model


            Consider a cubic control volume DxDyDz along the center of the plume (z ¼ H).
            Due to the complex nature of air dispersion by turbulent mixing, we may
            approximate the flux of air pollutant being mixed across any surface by
                                               oC
                                        j ¼ D                           ð11:24Þ
                                               on
                                                     2
                                                                            3
            where j ¼ flux of mass flow per unit area (kg/s·m ), C = concentration (kg/m ),
            n = distance in the direction considered (normally x, y, or z) (m), D = turbulent
                                2
            dispersion coefficient (m /s).
              The dimension of D is the same as that for molecular diffusivity or thermal
            diffusivity. However, this does not mean that air dispersion is a result of thermal
            diffusion or molecular diffusion. Therefore, the turbulent dispersion coefficient, D,
            is also referred to as the eddy diffusivity. And, they are not necessarily the same for
            x, y and z directions.
              Then the net mass flow rate along x direction is described as the difference
            through surfaces x and x þ Dx
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