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Hydraulic simulation in fractured media is a complex modeling, since it deals with formations that have anisotropic characteristics. Volcanic and metamorphic rocks are examples of materials that make up fractured formations, which commonly have two distinct regions, in terms of fluid movement.. The fractures (or joints), that are planes along which stress has caused partial loss of cohesion in the rock, representing a plane of weakness (discontinuity) in the rock (SINGHAL and GUPTHA, 2010). These planes are quite permeable, facilitating flow occurrence. Meanwhile, the rocky matrix, formed by the cohesive material, presents low or no permeability, hindering the passage of fluids.

Hydraulic simulation in fractured media using 1D equivalent pipes - FratCond tool module II