Smith's Elements of Soil Mechanics. Ian Smith

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      Unless kx is equal to kz the equation is not a true Laplacian and cannot therefore be solved by a flow net. To obtain a graphical solution, the equation must be written in the form (i.e. divide through by kz):

equation

      or

      (2.29)equation

      where

equation

      or

equation

      i.e.

      (2.30)equation

      (2.31)equation

      2.15.2 Calculation of seepage quantities in an anisotropic soil

      This is exactly as before:

      (2.32)equation

      and the only problem is what value to use for k.

      Let k be the effective permeability for the anisotropic condition. Then k is the operative permeability in Fig. 2.26a.

      Hence, in Fig. 2.26a:

equation Schematic illustration of transformed and natural ‘squares’. (a) Transformed. (b) Natural.

      (2.33)equation

       Solution:

      The flow net is shown in Fig. 2.27b. From it, we have Nf = 4.0 and Nd = 14.

equation Schematic illustration of seepage loss through dam (a) The problem. (b) Flow net.

      Determine the seepage loss through the dam.

       Solution:

      Transformed scale for x direction, images

      This means that, if the vertical scale is 1 : 500, then the horizontal scale is 0.63 : 500 or 1 : 794.

equation Schematic illustration of seepage loss through dam.

      A dam has the same details as in Example 2.8, except that there is no filter drain at the toe. Determine the seepage loss through the dam.

       Solution:

equation

      Hence Δa = 7.6 m

equation

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