“…For a discontinuum approach, the parameter for hydraulic conductivity in Darcy's equation (Equation 2.11) is replaced by parameters describing the equivalent parallel plate aperture, e, and the number of joints intersecting the test section (Equations 2.12 and 2.13), as discussed earlier in this chapter. Finite element models have also been developed to simulate and analyze flow in jointed media (for example, Ebeling, Pace, and Morrison 1997). Bennett and Anderson (1982) state that most references to rock mass analysis emphasize the homogeneous, isotropic case of hydraulic property distribution and treat anisotropy as a special condition.…”