Page 302 - Rock Mechanics For Underground Mining
P. 302

ENERGY, MINE STABILITY, MINE SEISMICITY AND ROCKBURSTS


                                          In the description of the plane P wave, the differential equation of motion (equation
                                        10.34) can be recast in the form

                                                                      2
                                                                           2 2
                                                                 2
                                                               ∂ u x /∂x = C ∂ u x /∂t 2             (10.38)
                                                                           p
                                        for which the general solution is of the type given in equation 10.36. The wave
                                        equation, written in its most general form, may be expressed as
                                                                                      2
                                                                                        2
                                                      2
                                                                     2
                                                                              2
                                                                         2
                                                           2
                                                                2
                                                     ∂  /∂x + ∂  /∂y + ∂  /∂z = (1/C )∂  /∂t 2       (10.39)
                                        where the nature of the variable   is determined by the fundamental particle motion
                                        associated with passage of the wave. ForaPwave, the parameter is the volumetric
                                        strain, or dilatation,  .
                                          In spherical polar co-ordinates, the governing equation for a spherically divergent
                                        P wave is shown by Kolsky (1963) to take the form
                                                                                 2
                                                        2
                                                                         2
                                                                2
                                                                                   2


                                                       ∂ (ru r )/∂r − 2ru r /r = 1/C ∂ (ru r )/∂t 2  (10.40)
                                                                                 p
                                        where r is the spherical co-ordinate radius. The general solution of equation 10.40
                                        can be readily verified to be of the form
                                                                                2

                                                        u r = (1/r) f (r − C p t) − (1/r ) f (r − C p t)  (10.41)
                                        where f is some arbitrary function, and f its first derivative with respect to the

                                        argument (r − C p t). The form of equation 10.41 indicates that remote from the wave
                                                             2
                                        source (when 1/r   1/r ), the term in f predominates, and the spherical wave

                                        solution is approximated by

                                                                u r = (1/r) f (r − C p t)            (10.42)
                                          As discussed for the bar wave, for an elastic medium the wave function is invariant
                                        with respect to the local co-ordinate of the propagating wave, in this case (r − C p t).
                                        Equation 10.42 therefore implies that for the spherically divergent wave
                                                                      u r ∝ 1/r                      (10.43)
                                        For a long cylindrical source, the wave equation takes the form

                                                           2
                                                 2
                                                                                2
                                                                                   2





                                                ∂ r 1/2  u r /∂r −  3   r 1/2 u r /r 2    = 1/C ∂ r 1/2 u r /∂t 2  (10.44)
                                                                                p
                                                              4
                                        There appears to be no completely general solution to this equation. For the case
                                        where r is large, equation 10.44 is approximated by
                                                                     2
                                                          2
                                                                            2
                                                                               2





                                                         ∂ r 1/2 u r /∂r = 1/C ∂ r 1/2 u r /∂t 2
                                                                            p
                                        which, by comparison with the one-dimensional wave equation 10.38 and its solution,
                                        equation 10.36, has the solution
                                                                 r  1/2 u r = f (r − C p t)          (10.45)
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