Page 193 - Analysis and Design of Energy Geostructures
P. 193

166   Analysis and Design of Energy Geostructures






























                Figure 4.14 An example of axisymmetric problem.
                formulations referring to axisymmetric conditions are very useful to analyse problems
                involving, for example, single energy piles (cf. Fig. 4.14).
                   In situations where an axisymmetric formulation can be used, by symmetry the two
                components of the displacement in any plane section along the axis of symmetry completely
                define the state of strain and hence the state of stress (Zienkiewicz and Taylor, 2005). In par-
                ticular, considering a cylindrical coordinate system, any displacement along the radial direc-
                tion causes a strain in the circumferential direction that will be associated to a stress different
                from zero. The need of considering four strain and stress components in axisymmetric pro-
                blems instead of the three involved in plane strain and plane stress problems represents one
                crucial difference between the considered alternative formulations of the thermoelastic prob-
                lem. One additional difference is that, while the axisymmetric formulation of the thermoe-
                lastic problem leads to an equivalent yet simpler analysis of the associated three-dimensional
                problem, plane strain and plane stress formulations of the thermoelastic problem lead to an
                approximate (simplified) analysis of the associated three-dimensional problem.
                   The 10 quantities σ rr ; σ zz ; σ θθ ; σ rz ; ε rr ; ε zz ; ε θθ ; ε rz ; u; w satisfy in either case the
                following 10 equations:
                1. Two equilibrium equations (for the case of no body forces)
                                           8
                                                           σ θθ
                                           >  @σ rr  1  @σ rz  2  5 0
                                           >
                                           >
                                           <
                                              @r     @z     r
                                                                                      ð4:64Þ
                                                  1      1
                                           >  @σ rz  @σ zz  σ rz
                                           >                   5 0
                                           >
                                           :
                                              @r     @z      r
   188   189   190   191   192   193   194   195   196   197   198