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Variation of permeability tensor ellipsoid in homogeneous anisotropic soils
Permeability tests were conducted on anisotropic sandstone; cylindrical cores were taken at various directions with respect to fixed coordinate system, and permeability values were determined in constant-head permeameter; values obtained when plotted on polar coordinate paper result in two-dimensional permeability ellipse; necessary graphical constructions for determining direction of velocity or direction of hydraulic gradient from corresponding tensor ellipses are also given.
Variation of permeability tensor ellipsoid in homogeneous anisotropic soils
Permeability tests were conducted on anisotropic sandstone; cylindrical cores were taken at various directions with respect to fixed coordinate system, and permeability values were determined in constant-head permeameter; values obtained when plotted on polar coordinate paper result in two-dimensional permeability ellipse; necessary graphical constructions for determining direction of velocity or direction of hydraulic gradient from corresponding tensor ellipses are also given.
Variation of permeability tensor ellipsoid in homogeneous anisotropic soils
Am Geophysical Union. Water Resources Research
Liakopoulos, A.C. (author)
1965
7 pages
Article (Journal)
English
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