fluid_mechanics
478 Chapter 9 ■ Flow over Immersed Bodies 1 τ τ ~ w w √x x With the velocity profile known, it is an easy matter to determine the wall shear stress, t w m 10u0y2 y0 , where the velocity gradient is evaluated at the plate. The value of 0u0y at y 0 can be obtained from the Blasius solution to give t w 0.332U 3 2 B rm x (9.18) As indicated by Eq. 9.18 and illustrated in the figure in the margin, the shear stress decreases with increasing x because of the increasing thickness of the boundary layer—the velocity gradient at the wall decreases with increasing x. Also, t varies as U 32 w , not as U as it does for fully developed laminar pipe flow. These variations are discussed in Section 9.2.3. 9.2.3 Momentum Integral Boundary Layer Equation for a Flat Plate One of the important aspects of boundary layer theory is the determination of the drag caused by shear forces on a body. As was discussed in the previous section, such results can be obtained from the governing differential equations for laminar boundary layer flow. Since these solutions are extremely difficult to obtain, it is of interest to have an alternative approximate method. The momentum integral method described in this section provides such an alternative. We consider the uniform flow past a flat plate and the fixed control volume as shown in Fig. 9.11. In agreement with advanced theory and experiment, we assume that the pressure is constant throughout the flow field. The flow entering the control volume at the leading edge of the plate [section 112] is uniform, while the velocity of the flow exiting the control volume [section 122] varies from the upstream velocity at the edge of the boundary layer to zero velocity on the plate. The fluid adjacent to the plate makes up the lower portion of the control surface. The upper surface coincides with the streamline just outside the edge of the boundary layer at section 122. It need not 1in fact, does not2 coincide with the edge of the boundary layer except at section 122. If we apply the x component of the momentum equation 1Eq. 5.222 to the steady flow of fluid within this control volume we obtain where for a plate of width b a F x r 112 uV nˆ dA r 122 uV nˆ dA a F x d plate t w dA b plate t w dx (9.19) and d is the drag that the plate exerts on the fluid. Note that the net force caused by the uniform pressure distribution does not contribute to this flow. Since the plate is solid and the upper surface of the control volume is a streamline, there is no flow through these areas. Thus, d r 112 U1U2 dA r 122 u 2 dA The drag on a flat plate depends on the velocity profile within the boundary layer. or d d rU 2 bh rb u 2 dy 0 (9.20) y U Control surface U Streamline h Boundary layer edge δ(x) u x (1) τ w (x) (2) F I G U R E 9.11 Control volume used in the derivation of the momentum integral equation for boundary layer flow.
9.2 Boundary Layer Characteristics 479 Although the height h is not known, it is known that for conservation of mass the flowrate through section 112 must equal that through section 122, or Drag on a flat plate is related to momentum deficit within the boundary layer. which can be written as d Uh u dy d rU 2 bh rb Uu dy (9.21) Thus, by combining Eqs. 9.20 and 9.21 we obtain the drag in terms of the deficit of momentum flux across the outlet of the control volume as 0 0 y d d rb u1U u2 dy 0 (9.22) δ y δ U – u u(U – u) u The idea of a momentum deficit is illustrated in the figure in the margin. If the flow were inviscid, the drag would be zero, since we would have u K U and the right-hand side of Eq. 9.22 would be zero. 1This is consistent with the fact that t w 0 if m 0.2 Equation 9.22 points out the important fact that boundary layer flow on a flat plate is governed by a balance between shear drag 1the left-hand side of Eq. 9.222 and a decrease in the momentum of the fluid 1the right-hand side of Eq. 9.222. As x increases, d increases and the drag increases. The thickening of the boundary layer is necessary to overcome the drag of the viscous shear stress on the plate. This is contrary to horizontal fully developed pipe flow in which the momentum of the fluid remains constant and the shear force is overcome by the pressure gradient along the pipe. The development of Eq. 9.22 and its use was first put forth in 1921 by T. von Kármán 11881–19632, a Hungarian/German aerodynamicist. By comparing Eqs. 9.22 and 9.4 we see that the drag can be written in terms of the momentum thickness, , as d rbU 2 (9.23) Note that this equation is valid for laminar or turbulent flows. The shear stress distribution can be obtained from Eq. 9.23 by differentiating both sides with respect to x to obtain dd dx rbU 2 d dx (9.24) The increase in drag per length of the plate, dddx, occurs at the expense of an increase of the momentum boundary layer thickness, which represents a decrease in the momentum of the fluid. Since dd t w b dx 1see Eq. 9.192 it follows that dd dx bt w (9.25) Hence, by combining Eqs. 9.24 and 9.25 we obtain the momentum integral equation for the boundary layer flow on a flat plate t w rU 2 d dx (9.26) The usefulness of this relationship lies in the ability to obtain approximate boundary layer results easily by using rather crude assumptions. For example, if we knew the detailed velocity profile in the boundary layer 1i.e., the Blasius solution discussed in the previous section2, we could evaluate either the right-hand side of Eq. 9.23 to obtain the drag, or the right-hand side of Eq. 9.26 to obtain the shear stress. Fortunately, even a rather crude guess at the velocity profile will allow us to obtain reasonable drag and shear stress results from Eq. 9.26. This method is illustrated in Example 9.4.
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9.2 Boundary Layer Characteristics 479<br />
Although the height h is not known, it is known that for conservation of mass the flowrate<br />
through section 112 must equal that through section 122, or<br />
Drag on a flat plate<br />
is related to momentum<br />
deficit<br />
within the boundary<br />
layer.<br />
which can be written as<br />
d<br />
Uh u dy<br />
d<br />
rU 2 bh rb Uu dy<br />
(9.21)<br />
Thus, by combining Eqs. 9.20 and 9.21 we obtain the drag in terms of the deficit of momentum<br />
flux across the outlet of the control volume as<br />
0<br />
0<br />
y<br />
d<br />
d rb u1U u2 dy<br />
0<br />
(9.22)<br />
δ<br />
y<br />
δ<br />
U – u<br />
u(U – u)<br />
u<br />
The idea of a momentum deficit is illustrated in the figure in the margin. If the flow<br />
were inviscid, the drag would be zero, since we would have u K U and the right-hand side of<br />
Eq. 9.22 would be zero. 1This is consistent with the fact that t w 0 if m 0.2 Equation 9.22<br />
points out the important fact that boundary layer flow on a flat plate is governed by a balance<br />
between shear drag 1the left-hand side of Eq. 9.222 and a decrease in the momentum of the<br />
<strong>fluid</strong> 1the right-hand side of Eq. 9.222. As x increases, d increases and the drag increases. The<br />
thickening of the boundary layer is necessary to overcome the drag of the viscous shear stress<br />
on the plate. This is contrary to horizontal fully developed pipe flow in which the momentum<br />
of the <strong>fluid</strong> remains constant and the shear force is overcome by the pressure gradient along<br />
the pipe.<br />
The development of Eq. 9.22 and its use was first put forth in 1921 by T. von<br />
Kármán 11881–19632, a Hungarian/German aerodynamicist. By comparing Eqs. 9.22 and 9.4 we<br />
see that the drag can be written in terms of the momentum thickness, , as<br />
d rbU 2 <br />
(9.23)<br />
Note that this equation is valid for laminar or turbulent flows.<br />
The shear stress distribution can be obtained from Eq. 9.23 by differentiating both sides with<br />
respect to x to obtain<br />
dd<br />
dx<br />
rbU<br />
2<br />
d<br />
dx<br />
(9.24)<br />
The increase in drag per length of the plate, dddx, occurs at the expense of an increase of the<br />
momentum boundary layer thickness, which represents a decrease in the momentum of the <strong>fluid</strong>.<br />
Since dd t w b dx 1see Eq. 9.192 it follows that<br />
dd<br />
dx bt w<br />
(9.25)<br />
Hence, by combining Eqs. 9.24 and 9.25 we obtain the momentum integral equation for the boundary<br />
layer flow on a flat plate<br />
t w rU 2 d<br />
dx<br />
(9.26)<br />
The usefulness of this relationship lies in the ability to obtain approximate boundary layer<br />
results easily by using rather crude assumptions. For example, if we knew the detailed velocity<br />
profile in the boundary layer 1i.e., the Blasius solution discussed in the previous section2, we could<br />
evaluate either the right-hand side of Eq. 9.23 to obtain the drag, or the right-hand side of Eq. 9.26<br />
to obtain the shear stress. Fortunately, even a rather crude guess at the velocity profile will allow<br />
us to obtain reasonable drag and shear stress results from Eq. 9.26. This method is illustrated in<br />
Example 9.4.