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Thermomechanical behaviour of single energy piles  279


                   6.7 Thermally and mechanically induced vertical displacement
                   variations

                   The application of thermal loads along energy piles involves at best a linear distribu-
                   tion of the vertical displacement with depth and at worst a notably nonlinear distribu-
                   tion of the vertical displacement (becoming more pronounced with increasing pile
                   compressibility and slenderness) (Rotta Loria et al., 2018). This consideration is appli-
                   cable to the analysis of both rigid and deformable piles whether they have a predomi-
                   nantly floating or end-bearing character. In general, heating thermal loads cause
                   energy pile head heaves while cooling thermal loads cause energy pile head settle-
                   ments. The reason for this is due to the fact that thermal loads applied to energy piles
                   generally involve two pile portions that displace in opposite directions from the so-
                   called null point of the vertical displacement (located at a depth, z NP;w )(Laloui et al.,
                   2003a). The location of the null point depends on the end-restraint conditions
                   (Mimouni and Laloui, 2014; Rotta Loria et al., 2015; Sutman et al., 2018). For an
                   infinitely rigid base, the null point is located at the toe of energy piles. For an infinitely
                   rigid slab, the null point is located at the pile head. In practice the null point is located
                   somewhere along the length of the energy pile and always closer to the region of the
                   system characterised by the higher restraint.
                      An example of the head heave of an energy pile free to move vertically at its head
                   under the application of a heating passive cooling cycle is shown in Fig. 6.7 with ref-
                   erence to the results presented by Laloui et al. (2003a). An average temperature varia-

                   tion along an energy pile free to move vertically at its head of ΔT 5 22 Ccan
                   cause a vertical head displacement of approximately w h 524 mm. Higher head displa-
                   cements can be expected for energy piles resting on stiff soil strata compared to energy
                   piles floating in soft ground (the significant value of head displacement discussed with
                   reference to the considered case is to be associated with the former situations). This
                   phenomenon can be associated with the lower location of the null point in the former
                   case compared to the latter for the same applied temperature variation. Higher energy
                   pile displacements can be expected for longer piles. The reason for this is because,
                   although the thermally induced deformation is independent of the pile length, the ther-
                   mally induced displacement of energy piles is proportional to their length.
                      In contrast to the previous behaviour, the application of mechanical loads at the
                   head of energy piles involves an approximately constant distribution of the vertical dis-
                   placement with depth as well as a comparable distribution of shear stress (Rotta Loria
                   et al., 2018). This consideration is particularly applicable to the analysis of rigid piles
                   with a predominantly frictional character but is also acceptable for most piles.
                   Compressive mechanical loads applied at the head of piles involve energy pile head
                   settlements, while tensile mechanical loads involve energy pile head heaves. In particu-
                   lar, unless dealing with the phenomenon of negative skin friction, the action of
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