TY - GEN
T1 - Evaluation of fluid flow path in a single fracture undergoing normal stress and shear offset
AU - Nemoto, K.
AU - Oka, H.
AU - Watanabe, N.
AU - Hirano, N.
AU - Tsuchiya, N.
PY - 2006/5/15
Y1 - 2006/5/15
N2 - We report on an evidence of anisotropy in flow path in a single fracture on the basis of measurements of a contact area in a fracture with shear offset of up to 5 mm undergoing normal stress of up to 90 MPa. An area of contact in a fracture undergoing normal stress is measured by using a pressure-sensitive sheet inserted between fracture surfaces. This method allows simple measurements of contact area in the stressed conditions. Our results show that contact area increases with an increase in normal stress, on the contrary, contact area decreases with an increase in the offset. These dependencies in a contact area suggests that an open area, i.e., aperture area, which is illustrated as an area except for contact area in a fracture, can change associated with normal stress even under the condition of 100 MPa. In addition, we observed that contact area distributes in the direction perpendicular to the direction of offset, which indicates an anisotropy in aperture distribution that become possible flow path in a fracture. Results of numerical simulation of fluid flow in a fracture support the anisotropy in aperture distribution and consequent anisotropy in fluid flow in a fracture. The anisotropy in aperture distribution suggests an anisotropy in fracture permeability since tortuousity in a flow path could be affected by the aperture distribution.
AB - We report on an evidence of anisotropy in flow path in a single fracture on the basis of measurements of a contact area in a fracture with shear offset of up to 5 mm undergoing normal stress of up to 90 MPa. An area of contact in a fracture undergoing normal stress is measured by using a pressure-sensitive sheet inserted between fracture surfaces. This method allows simple measurements of contact area in the stressed conditions. Our results show that contact area increases with an increase in normal stress, on the contrary, contact area decreases with an increase in the offset. These dependencies in a contact area suggests that an open area, i.e., aperture area, which is illustrated as an area except for contact area in a fracture, can change associated with normal stress even under the condition of 100 MPa. In addition, we observed that contact area distributes in the direction perpendicular to the direction of offset, which indicates an anisotropy in aperture distribution that become possible flow path in a fracture. Results of numerical simulation of fluid flow in a fracture support the anisotropy in aperture distribution and consequent anisotropy in fluid flow in a fracture. The anisotropy in aperture distribution suggests an anisotropy in fracture permeability since tortuousity in a flow path could be affected by the aperture distribution.
KW - Fluid flow
KW - Fracture permesbility
KW - Laboratory experiment
KW - Shear offset
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U2 - 10.1063/1.2207095
DO - 10.1063/1.2207095
M3 - Conference contribution
AN - SCOPUS:33845597034
SN - 0735403279
SN - 9780735403277
T3 - AIP Conference Proceedings
SP - 156
EP - 161
BT - WATER DYNAMICS
T2 - WATER DYANMICS: 3rd International Workshop on Water Dynamics
Y2 - 16 November 2005 through 17 November 2005
ER -