Abstract:
The paper provides a survey of approaches to groundwater flow modeling in fractured
porous media, discussing their merits and shortcomings. The DFM (Discrete Fracture
and Matrix) model implemented in the GeRa software is described, emphasizing its capacity to explicitly consider the geometry of fractures and the water exchange between
fractures and the porous matrix. The use of multipoint flux approximation on the fracture
within the finite volume method based on the O-scheme is proposed. The implemented
numerical scheme is applied to solve a practical problem of estimating water inflow to
underground research laboratory in a fractured rock massif.