NG011
Properties of Fracture Networks and the Flow of Fluids through Discrete Fracture Networks
Properties of Fracture Networks and the Flow of Fluids through Discrete Fracture Networks
Session ID#: 162745
Session Description:
The flow of fluids through bedrock takes place primarily through the network of fractures over a broad range of scales. The spatial and temporal properties and patterns of individual fractures and fracture networks are nonlinear and typically scale invariant. This session welcomes abstracts from those conducting research on fracture initiation and growth and the ability of discrete fracture networks to conduct fluid flow over scales ranging from nanometers to the regional scale. We also welcome abstracts from those collecting data on the properties of rock fractures and fluid flow dynamics in the field, in the laboratory, and through numerical modeling.
Index Terms:
1829 Groundwater hydrology [HYDROLOGY]
4430 Complex systems [NONLINEAR GEOPHYSICS]
4460 Pattern formation [NONLINEAR GEOPHYSICS]
8010 Fractures and faults [STRUCTURAL GEOLOGY]
Primary Convener: Christopher Cramer Barton, Wright State University, Environmental Sciences and Chemistry, Dayton, United States
Conveners: Thomas Doe, Golder Associates Inc., Redmond, IL, United States and Lawrence M Cathles, Cornell Univ, Ithaca, NY, United States
See more of: Nonlinear Geophysics
