Page 72 - Air pollution and greenhouse gases from basic concepts to engineering applications for air emission control
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46                                            2  Basic Properties of Gases

              Assuming constant fluid density for the incompressible fluid, Eq. (2.72) becomes
                                     1   2
                                  P þ qv þ qgz ¼ constant                ð2:73Þ
                                     2
                                                 2
            where P represents the static pressure and qv =2 the velocity pressure. The con-
                                   1
                                      2
            sequent total pressure is P þ qv . This equation is applicable to most air emission
                                   2
            related to analysis.
              When z 1 ¼ z 2 , the pressure difference between two points along a streamline is
            related to the speeds at these points
                                            1    2   2
                                   P 1   P 2 ¼ q v   v 1                 ð2:74Þ
                                                 2
                                            2
              This simple equation finds important applications in air emission analysis such
            as the estimation of the resistance to airflow (pressure drop) in an air cleaning
            device. It is also the principle behind the design of a Pitot tube, which will be
            introduced later in Chap. 15.




            2.2.3 Boundary Layer and Drag

            When a gas flows around outside of a body, it produces a force on the body that
            tends to drag the body in the direction of the gas flow. There are two mechanisms
            behind this drag effect, one is the skin friction drag and another is form drag. To
            illustrate the skin drag, let us consider a flat surface with a sharp leading edge
            attacked by a uniform fluid flow (Fig. 2.3).
              Denote the uniform free stream speed as u 1 and set the coordinate origin at the
            leading edge with x ¼ 0 and y ¼ 0 on the solid surface. The fluid is slowed down
            with a layer that is close to the solid surface, which is called boundary layer. The



                            y     Undisturbed external
                                  flow
                                                                   Boundary
                                                                   layer
                                                  Subboundary layer
                                          u(x,y)
                          (0,0)                                      x
                                  Laminar
                                  boundary       Turbulent boundary layer
                                  layer
                                             Transition zone
            Fig. 2.3 Boundary layer concept
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