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   394   Ch a p t e r w e l v e

              simplicity. It also has some theoretical basis in that the initial stresses at
              t  = 0 has significant influence on the subsequent viscous and plastic deformation and
              the stress analysis can be performed using elasticity theory through the elastic-viscoelas-
              tic correspondence principle. In this chapter, an anistropic elasticity analysis of a pave-
              ment under wheel load will be presented. Although AC may demonstrate general an-
              isotropy, only cross anisotropy or orthotropy is considered for the purpose of simplifica-
              tion, and due to the experimental evidence. For the orthotropic case, AC is considered to
              have significant differences only in vertical and horizontal directions due to the aniso-
              tropic compaction, aggregate orientation, restraint conditions, and gravity direction. In
              orthotropic elasticity, there are only five material constants. However, the general aniso-
              tropic elasticity has 21 material constants and is not realistic for modeling and character-
              ization. The five material constants of the orthotropic elasticity are E v , E h , n vh , n hh , and G vh .
              Where E v  and E h  are elastic modulus in vertical and horizontal directions respectively; n vh
              and n hh are Poisson’s ratios for vertical-horizontal and horizontal-horizontal responses,
              respectively; and G vh  is the shear modulus along the vertical plane. Hooke’s Law for the
              orthotropic case can be expressed as follows:

                                   Δε =  1  Δσ − ν  1  Δσ − ν  1  Δσ            (12-1a)
                                     x  E    x  hh  E  y  vh  E  z
                                         h         h         v
                                        1         1         1
                                   Δε =   Δσ − ν    Δσ − ν    Δσ                (12-1b)
                                     y  E   y   hh  E  x  vh  E  z
                                         h         h         v
                                        1         1         1
                                   Δε =   Δσ − ν    Δσ − ν    Δσ                (12-1c)
                                     z  E   y   vh  E  x  vh  E  y
                                         v         h        v
                                                  1
                                            Δγ  =   Δτ                          (12-1d)
                                              yz  G    yz
                                                   vh
                                            Δγ  =  1  Δτ                         (12-1e)
                                              zx  G    zx
                                                   vh
                                                (1  + ν )
                                          Δγ  =     hh  Δτ                       (12-1f)
                                            xy    E     xy
                                                   h
                 Where Δe x , Δe y , Δe z  are normal strain increments and Δs x , Δs y , Δs z  are normal stress
              increments; Δg yz , Δg zx  and Δg xy  are shear strain increments; and Δt yz , Δt zx  and Δt xy  are the
              corresponding shear stress increments. It should be noted that in the above formula-
              tions, the properties in tension and compression are considered the same.


        12.3  Boussinesq’s Solution for Orthotropic Materials
              For a full-depth AC pavement of isotropic materials, if the distributed tire load could be
              approximated as a point load, the stress field could be approximated by the Boussin-
              esq’s solution, a half-space subjected to a concentrated load P as illustrated in Figure
              12.1. The corresponding Boussinesq’s solution for orthotropic material was obtained by
              Wolf (1935). The analytical expressions for two of the four stress components, s θ  and t yz ,
              are presented in Equations 12-2a and 12-2b. The solution is based on the cylindrical
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