“…The average undrained shear strength of the soils in subzones B1 and B3 were only 2.3 and 2.5 kPa, respectively. The 1‐D consolidation and permeability tests are conducted by Sun et al
36 . and obtained nonlinear and time‐independent compressibility and permeability as,
where e is the void ratio, k is the coefficient of the permeability, σ ′ is the effective stress of soil mass, e L is the void ratio at the liquid limit state, and e L = G s w L , where G s is the specific gravity, and w L is liquid limit.…”