“…There are several computational models for simulating the flow of fluids and the associated transport of dissolved chemicals through subsurface fractured systems, which is of great importance for understanding the behavior of natural subsurface fracture systems and a variety of industrial and civil engineering endeavors, including the environmental restoration of contaminated fractured media [1,2,3], aquifer storage and management [4], hydrocarbon extraction [5,6], longterm storage of spent civilian nuclear fuel [7,8], and CO 2 sequestration [9,10]. The computational models currently used today can be loosely grouped into three categories [11]: (1) continuum models -including stochastic continuum [2,12,13] and dual-porosity / dual-permeability models [14,15,16], (2) discrete fracture networks (DFN) models [17,18,19,20,21], and (3) discrete fracture matrix (DFM) models [22,23,24,25,26,27,28,29,30,31,32,33,34]. The distinguishing feature between the categories is the relative fidelity with which the rock matrix and embedded fractures are represented.…”