Appropriate Domain Size for Groundwater Flow Modeling with a Discrete Fracture Network Model

When a discrete fracture network (DFN) is constructed from statistical conceptualization, uncertainty in simulating the hydraulic characteristics of a fracture network can arise due to the domain size. In this study, the appropriate domain size, where less significant uncertainty in the stochastic DFN model is expected, was suggested for the Korea Atomic Energy Research Institute Underground Research Tunnel (KURT) site. The stochastic DFN model for the site was established, and the appropriate domain size was determined with the density of the percolating cluster and the percolation probability using the stochastically generated DFNs for various domain sizes. The applicability of the appropriate domain size to our study site was evaluated by comparing the statistical properties of stochastically generated fractures of varying domain sizes and estimating the uncertainty in the equivalent permeability of the generated DFNs. Our results show that the uncertainty of the stochastic DFN model is acceptable when the modeling domain is larger than the determined appropriate domain size, and the appropriate domain size concept is applicable to our study site.

[1]  Yong Huang,et al.  Simulation of groundwater flow in fractured rocks using a coupled model based on the method of domain decomposition , 2014, Environmental Earth Sciences.

[2]  S. Ji,et al.  Derivative‐Assisted Classification of Fractured Zones Crossing a Deep Borehole , 2014, Ground water.

[3]  D. Stauffer,et al.  Self similarity and correlations in percolation , 1983 .

[4]  Young-Jin Park,et al.  Influence of Fracture Connectivity and Characterization Level on the Uncertainty of the Equivalent Permeability in Statistically Conceptualized Fracture Networks , 2011 .

[5]  J. Bear,et al.  1 – Modeling Flow and Contaminant Transport in Fractured Rocks , 1993 .

[6]  Peter Jackson,et al.  A methodology to constrain the parameters of a hydrogeological discrete fracture network model for sparsely fractured crystalline rock, exemplified by data from the proposed high-level nuclear waste repository site at Forsmark, Sweden , 2014, Hydrogeology Journal.

[7]  Jean-Raynald de Dreuzy,et al.  Hydraulic properties of two‐dimensional random fracture networks following a power law length distribution: 1. Effective connectivity , 2001 .

[8]  J. Thovert,et al.  Macroscopic permeability of three-dimensional fracture networks with power-law size distribution. , 2004, Physical review. E, Statistical, nonlinear, and soft matter physics.

[9]  A hybrid modeling approach to evaluate the groundwater flow system at the low- and intermediate-level radioactive waste disposal site in Gyeong-Ju, Korea , 2012, Hydrogeology Journal.

[10]  J. Thovert,et al.  Effective permeability of fractured porous media with power-law distribution of fracture sizes. , 2007, Physical review. E, Statistical, nonlinear, and soft matter physics.

[11]  Vladimir Cvetkovic,et al.  Inference of field‐scale fracture transmissivities in crystalline rock using flow log measurements , 2010 .

[12]  Jan-Olof Selroos,et al.  Comparison of alternative modelling approaches for groundwater flow in fractured rock , 2002 .