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SPHERICAL CAVITY IN A HYDROSTATIC STRESS FIELD


                                        This implies that, for the cylindrically divergent wave

                                                                     u r ∝ 1/r 1/2                   (10.46)


                                        10.4  Spherical cavity in a hydrostatic stress field

                                        The purpose in this section is to examine the relative magnitudes of the static and
                                        dynamic stresses associated with creating an excavation, to illustrate methods of
                                        evaluating released and excess energy, and to correlate the dynamic stresses with
                                        excess energy magnitude. The reason for choosing a spherical opening for study
                                        is that the problem is analytically tractable. A two-dimensional problem, such as a
                                        cylindrical excavation, cannot be treated productively due to the lack of a closed form
                                        solution for the response to a step increase in pressure to the internal surface of the
                                        hole. The problem of the spherical opening has been considered by Hopkins (1960),
                                        Timoshenko and Goodier (1970), and Bray (1979), on whose work the following
                                        discussion is based.
                                          Figure 10.10 shows a diametral section of a spherical opening, of radius a,ina
                                        medium subject to a hydrostatic far-field stress, of magnitude p. Relative to spherical
                                        polar (r, 
,  ) co-ordinate axes, total stresses after excavation and excavation-induced
                                        displacement are given, according to Poulos and Davis (1974), by

                                                                          3
                                                                             3
                                                                rr = p[1 − (a /r )]
                                                                                3
                                                                                   3
                                                                

 =      = p[1 + (a /2r )]          (10.47)
                                                                r
 =   r  =   
  = 0
                                                                       3
                                                              u r =−pa /4Gr 2                        (10.48)
                                                              u 
 = u   = 0

              Figure  10.10  Diametral  section
              through a sphere in a medium subject
              to hydrostatic stress.
























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