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404    CHAPTER 12  Vector Integral Calculus

                                    so

                                                   ∇· FdV =      3dV
                                                M             M
                                                           = 3[volume of the cone of height 1, radius 1]

                                                               1
                                                           = 3    π = π.
                                                               3
                         EXAMPLE 12.25

                                 Let   be the piecewise smooth surface of the cube having vertices
                                                         (0,0,0),(1,0,0),(0,1,0),(0,0,1)

                                                        (1,1,0),(0,1,1),(1,0,1),(1,1,1).

                                                    2
                                                2
                                                         2
                                 Let F(x, y, z) = x i + y j + z k. We want to compute the flux of F across  . This flux is

                                    F · ndσ. We can certainly evaluate this integral, but this will be tedious because   has

                                 six smooth faces. It is easier to use the triple integral of the divergence theorem. Compute
                                                              ∇· F = 2x + 2y + 2z.
                                 Then

                                                   flux =     F · ndσ


                                                       =      ∇· FdV =     (2x + 2y + 2z)dV
                                                           M             M
                                                              1
                                                           1
                                                                 1
                                                       =          (2x + 2y + 2z)dz dy dx
                                                          0  0  0
                                                           1
                                                              1
                                                       =       (2x + 2y + 1)dy dx
                                                          0  0
                                                            1
                                                            (2x + 2)dx = 3.
                                                       =
                                                          0
                                 12.8.1  Archimedes’s Principle
                                 Archimedes’s principle is that the buoyant force a fluid exerts on a solid object immersed in it,
                                 is equal to the weight of the fluid displaced. An aircraft carrier floats in the ocean if it displaces
                                 a volume of seawater whose weight at least equals that of the carrier. We will use the divergence
                                 theorem to derive this principle.
                                    Imagine a solid object M bounded by a piecewise smooth surface  .Let ρ be the constant
                                 density of the fluid. Draw a coordinate system as in Figure 12.22 with M below the surface.
                                 Using the fact that pressure equals depth multiplied by density, the pressure ρ(x, y, z) at a point
                                 on   is p(x, y, z) =−ρz, the negative sign because z is negative in the downward direction and
                                 we want pressure to be positive. Now consider a piece   j of  . The force of the pressure on
                                   j is approximately −ρz multiplied by the area A j of   j .If n is the unit outer normal to   j ,
                                 then the force caused by the pressure on   j is approximately ρznA j . The vertical component of
                                 this force is the magnitude of the buoyant force acting upward on   j . This vertical component is




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                                   October 14, 2010  14:53  THM/NEIL   Page-404        27410_12_ch12_p367-424
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