Anisotropic features of geometry and permeability in fractured rock masses
Zhang, Xing and Sanderson, David J. (1995) Anisotropic features of geometry and permeability in fractured rock masses. Engineering Geology, 40, (1-2), 65-75. (doi:10.1016/0013-7952(95)00040-2).
Full text not available from this repository.
A geometric anisotropy factor (A f) of two-dimensional, natural fracture systems has been defined according to fracture spacing and orientation in a given direction. Geometric anisotropy of fracture systems has a major effect on the percolation threshold (the critical fracture density) of fracture systems below which the overall permeability is zero.
A two-dimensional distinct element code (UDEC) has been used to calculate directional flow-rates of fracture systems. Simulated and natural fracture patterns, sampled on outcrops in the Lake District (England), have been tested to examine the relation between geometric anisotropy and permeability anisotropy, which is demonstrated to have a power-law form. Also, the differential anisotropy factor (A f) results in different universal exponents which govern the relation between fracture density and flow rates.
|Subjects:||T Technology > TA Engineering (General). Civil engineering (General)
Q Science > QE Geology
|Divisions:||University Structure - Pre August 2011 > School of Civil Engineering and the Environment
|Date Deposited:||11 Mar 2010|
|Last Modified:||25 Apr 2013 20:56|
|Contributors:||Zhang, Xing (Author)
Sanderson, David J. (Author)
|RDF:||RDF+N-Triples, RDF+N3, RDF+XML, Browse.|
Actions (login required)