Influence of mechanical damage on fluid flow patterns investigated using CT scanning imaging and acoustic emissions techniques
- 29 August 2008
- journal article
- Published by American Geophysical Union (AGU) in Geophysical Research Letters
- Vol. 35 (16)
Abstract
In order to get some insight into the influence of mechanical deformation on fluid flow patterns, we performed series of X‐ray CT scanning runs during capillary imbibition experiments to image the water front displacement in Bentheim sandstone samples. A three steps procedure was followed: 1) intact rock samples were tested, 2) the samples were deformed in creep experiments under triaxial conditions with recording of acoustic emissions, 3) the deformed samples experienced a second capillary imbibition test with CT scanning imaging. Using image analysis tools, relevant flow parameters like the height, velocity and curvature of the water front were measured. Stress‐induced damage had a significant impact on the flow patterns. However contrasted results were obtained: localized damage evidenced by acoustic emissions clustering resulted in one experiment in local disturbance of the flow patterns, whereas in the second one a fracture detected by CT scan did not modify the local flow geometry.Keywords
This publication has 9 references indexed in Scilit:
- Permeability anisotropy and its relations with porous medium structureJournal of Geophysical Research, 2008
- Volumetric Digital Image Correlation Applied to X‐ray Microtomography Images from Triaxial Compression Tests on Argillaceous RockStrain, 2007
- Acoustic emission and velocities associated with the formation of compaction bands in sandstoneJournal of Geophysical Research: Solid Earth, 2006
- Imaging strain localization by X-ray computed tomography: discrete compaction bands in Diemelstadt sandstoneJournal of Structural Geology, 2006
- Influence of open and sealed fractures on fluid flow and water saturation in sandstone cores using Magnetic Resonance ImagingGeophysical Journal International, 2001
- Quantitative analysis of reservoir rocks by microfocus X-ray computerised tomographySedimentary Geology, 2000
- Characterization by computed X-ray tomography of the evolution of the pore structure of a dolomite rock during freeze-thaw cyclic testsPhysics and Chemistry of the Earth, Part A: Solid Earth and Geodesy, 1999
- The transition from brittle faulting to cataclastic flow: Permeability evolutionJournal of Geophysical Research, 1997
- Geometry of flow paths for fluid transport in rocksJournal of Geophysical Research, 1993