Large apertures can result from shear displacement
of discontinuities having appreciable roughness, from
outwash of filling materials (e.g. clay), from tensile opening,
and/or from solution. In most subsurface rock masses,
apertures are small, probably less than half a millimeter.
Aperture and its areal variation will have an
influence on the deformability, shear strength and
hydraulic conductivity of discontinuities
Large apertures can result from shear displacementof discontinuities having appreciable roughness, fromoutwash of filling materials (e.g. clay), from tensile opening,and/or from solution. In most subsurface rock masses,apertures are small, probably less than half a millimeter.Aperture and its areal variation will have aninfluence on the deformability, shear strength andhydraulic conductivity of discontinuities
การแปล กรุณารอสักครู่..
