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STABILITY OF UNSATURATED SOIL SLOPES 127






















            Figure 4.13 Effect of permeability anisotropy on initial groundwater table.
              For the case of higher anisotropic ratio, k /k =4, the main groundwater table
                                                x
                                                  y
            rises  substantially  at  all  three  sections  considered.  The  substantial  increase  in
            pore water pressures at Sections A-A and B-B is somewhat unexpected. This could
            be due to some small numerical errors occurred at the air-water interface on the
            sloping surface.
              Figure 4.15 shows the influence of various anisotropic permeability ratios (k /
                                                                           x
            k ) on the stability of the cut slope. As expected, the large increase in pore water
             y
            pressure  in  the  vicinity  of  the  cut  slope  has  significant  implications  on  its
            stability. At the initial steady state, the factor of safety of the cut slope decreases
            as  the  anisotropic  permeability  ratio  (k /k )  increases.  The  factor  of  safety
                                              x
                                                y
            decreases further when the slope is subjected to a daily rainfall of 267 mm/day
            and  the  cut  slope  fails  if  k /k =4.  For  the  range  of  heterogeneous  anisotropic
                                     y
                                  x
            flows  analysed,  the  factor  of  safety  of  the  slope  is  very  sensitive  to  the
            anisotropic permeability ratio. The higher the degree of hydraulic anisotropy, the
            lower the factor of safety becomes.
                                       Conclusions
            A series of finite element parametric analyses has been conducted to investigate
            the  influence  of  various  rainfall  events  and  initial  ground  and  boundary
            conditions on transient seepage and hence slope stability in unsaturated soils. A
            typical steep unsaturated cut slope on a hillside in Hong Kong has been used to
            illustrate key results from the parametric studies.
              Infiltration  due  to  rain-water  causes  a  reduction  of  matrix  suction  and  an
            increase in moisture content and water permeability in the unsaturated zones. A
            perched  water  table  is  developed  above  the  main  water  table.  This  offers  a
            theoretical explanation and illustration of some slope failures in Hong Kong. For
            an  initially  low  main  water  table  in  the  ground,  infiltration  will  not  result  in  a
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