“…In the dual-permeability model, the fractured blocks interact with the matrix blocks according to the interface area between the two connecting blocks and their respective state variables. In the previous qualified version (Pruess et al, 1996), the complete fracture-matrix interface area was available by the setting isotropic parameter, ISOT=l, for each fracture-matrix connection. However, there is evidence that fracture-matrix interaction in the unsaturated zone at Yucca Mountah is limited due to fingering flow in fractures (Glass et al, 1996) and mineral coatings on the fracture surfaces, and in fact there may be only part of fracturematrix interface areas that contributes fracture-matrix inter flow.…”