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Thermohydromechanical behaviour of soils and soil structure interfaces  249


                   Table 5.3 Values of normal stiffness K int for different soils.
                                                                          Stiffness, K int [kPa/mm]
                   Reference           Soil              Shear modulus,       Radius, R [m]
                                                         G 0 [MPa]
                                                                        0.5    0.8   1     1.2
                   Lo Presti (1989)    Cemented sand     300            1200   750   600   500
                   Ghionna et al. (1983)  Lightly cemented  280         1120   700   560   467
                                         sand
                   Ghionna et al. (1983)  Sand gravel    125            500    313   250   208
                   Lo Presti (1989)    Gravel            100            400    250   200   167
                   Lo Presti (1989)    Fine-grained soil  50            200    125   100   83
                   Source: Data from Di Donna, A., 2014. Thermomechanical aspects of energy piles. In: Laboratory of Soil Mechanics.
                   Swiss Federal Institute of Technology in Lausanne (EPFL), Lausanne.



                   normal to the interface. Using the cylindrical cavity expansion theory, the value of K
                   can be deduced from the equilibrium equation, as suggested by (Wernick, 1978)

                                                           G 0
                                                    K int 5 2                             ð5:8Þ
                                                           R
                   where G 0 is the shear modulus of the soil at small strains and R is the radius of the
                   cavity (e.g. a pile). Theoretically, the value of K int can vary from 0 (CNL) to infinite
                   (‘constant normal height’, CNH). Reasonable values of K int range between 100 and
                   1200 kPa/mm, being lower for clays, and are reported in Table 5.3 (Di Donna, 2014).
                      Fig. 5.35 compares the stress paths in the Mohr plane of dense sand concrete and
                   loose sand concrete interfaces subjected to monotonic mechanical loading under iso-
                   thermal CNS and CNL conditions by Fioravante et al. (1999). The interface angle of
                   shear strength is identified by δ. In the case of dense soil (cf. Fig. 5.35A), the interface
                   initially contracts and then dilates, so that in CNS conditions the normal effective
                   stress decreases at the beginning and increases later, providing at the end a higher shear
                   strength with respect the one observed under CNL conditions. In the case of loose
                   sand (cf. Fig. 5.35B), the effect is almost negligible in terms of shear strength as the
                   volumetric deformation is limited. However, in CNS conditions, the normal load
                   decreases slightly due to the slight observed contraction. While the shear strength of a
                   specific material under CNS conditions depends on the related volumetric behaviour,
                   the interface angle of shear strength is unique for a given soil structure interface (Di
                   Donna et al., 2015).
                      Further results allowing to expand on the role of CNS and CNL conditions on
                   the response of soil structure interfaces are reported in Fig. 5.36 with reference to the
                   results presented by Di Donna et al. (2015) for sand concrete interfaces subjected to
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