“…As shown in Figure 1, z represents the downward vertical coordinate, and
represents the timeādependent loading subjected to the clay with a thickness of L . Moreover, to consider the effects of nonāisothermal distribution condition on the consolidation process,
49 it is assumed that the temperature T in clay is linearly distributed with depth and rapidly reaches a stable state,
46,47,50,51 where
and
represent the temperature at the top and bottom boundary, respectively.…”