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DERIVATION     OF   THE   WAVE    EQUATION
                                                                            WAVE    MOTION     ON   AN   INTERVAL WAVE
                                        CHAPTER 16                          MOTION     IN AN    INFINITE MEDIUM


                                        The Wave


                                        Equation























                            16.1        Derivation of the Wave Equation

                                        Vibrations in a membrane or steel plate, or oscillations along a guitar string, are all modeled
                                        by the wave equation and appropriate initial and boundary conditions. We will begin with a
                                        derivation of the one-dimensional wave equation.
                                           Suppose an elastic string has its ends fastened by two pegs. The string is displaced, released
                                        and allowed to vibrate in a plane.
                                           Place the string along the x - axis from 0 to L and assume that it vibrates in the x, y - plane.
                                        We want a function y(x,t) such that, at time t, the graph of y(x,t) is the shape of the string at
                                        that time. We call y(x,t) the position function for the string.
                                           To take a simple case, neglect damping forces such as the weight of the string and assume
                                        that the tension T(x,t) acts tangent to the string, and that individual particles of the string move
                                        only vertically. Also assume that the mass ρ per unit length is constant. Consider a segment of
                                        string between x and x +  x. By Newton’s second law of motion, the net force on this segment
                                        due to the tension is equal to the acceleration of the center of mass of this segment, multiplied
                                        by its mass. This is a vector equation. Its vertical component (Figure 16.1) gives us
                                                                                               2
                                                                                              ∂ y
                                                      T (x +  x,t)sin(θ +  θ) − T (x,t)sin(θ) = ρ x  (x,t),
                                                                                              ∂t  2
                                        where x is the center of mass of this segment and T (x,t) =  T(x,t)  . Then

                                                                                              2
                                                       T (x +  x,t)sin(θ +  θ) − T (x,t)sin(θ)  ∂ y
                                                                                          = ρ   (x,t).
                                                                        x                    ∂t  2
                                        Now v(x,t) = T (x,t)sin(θ) is the vertical component of the tension, so this equation becomes

                                                                                      2
                                                               v(x +  x,t) − v(x,t)  ∂ y
                                                                                  = ρ   (x,t).
                                                                        x            ∂t  2
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                                   October 14, 2010  15:23  THM/NEIL   Page-565        27410_16_ch16_p563-610
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