Page 18 - Essentials of applied mathematics for scientists and engineers
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book   Mobk070    March 22, 2007  11:7








                     8  ESSENTIALS OF APPLIED MATHEMATICS FOR SCIENTISTS AND ENGINEERS
                       at x +  x is

                                         V (x +  x)/H = tan α(x +  x) = ∂y/∂x(x +  x).              (1.17)

                       The vertical force V is then given by H∂y/∂x.The net vertical force is the difference between
                       the vertical forces at x and x +  x, and must be equal to the mass times the acceleration of
                                                                                   2
                                                                                        2
                       that portion of the string. The mass is ρ x and the acceleration is ∂ y/∂t .Thus
                                                 2
                                                     2
                                           ρ x∂ /∂t = H[∂y/∂x(x +  x) − ∂y/∂x(x)]                   (1.18)
                       Expanding ∂y/∂x(x +  x)inaTaylor series about  x = 0 and neglecting terms of order
                           2
                       ( x) and smaller, we find that

                                                          ρy tt = Hy xx                             (1.19)
                       which is the wave equation. Usually it is presented as

                                                                 2
                                                           y tt = a y xx                            (1.20)
                              2
                       where a = H/ρ is a wave speed term.
                            Had we included the weight of the string there would have been an extra term on the
                       right-hand side of this equation, the acceleration of gravity (downward). Had we included a
                       damping force proportional to the velocity of the string, another negative term would result:

                                                      ρy tt = Hy xx − by t − g                      (1.21)


                       1.4.1  Boundary Conditions
                       The partial differential equation is linear and if the gravity term is included it is nonhomo-
                       geneous. It is second order in both t and x, and requires two boundary conditions (initial
                       conditions) on t and two boundary conditions on x. The two conditions on t are normally
                       specifying the initial velocity and acceleration. The conditions on x are normally specifying the
                       conditions at the ends of the string, i.e., at x = 0and x = L.


                       1.5    VIBRATING MEMBRANE
                       The partial differential equation describing the motion of a vibrating membrane is simply an
                       extension of the right-hand side of the equation of the vibrating string to two dimensions.
                       Thus,
                                                                         2
                                                     ρy tt + by t =−g +∇ y                          (1.22)

                                                                        2
                       In this equation, ρ is the density per unit area and ∇ y is the Laplacian operator in either
                       rectangular or cylindrical coordinates.
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