Field experiments in a fractured clay till: 1. Hydraulic conductivity and fracture aperture

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Field Experiments in a Fractured Clay Till 2. Solute and Colloid Transport

A field tracer experiment was conducted in a lateral flow field in the weathered and highly fractured upper 6 m of a 40-m-thick clay-rich till plain in southwestern Ontario. In the upper 3 m where fractures are closely spaced (<0.13 m) the advancing front (C/Co = 0.01) of the nonreactive solute tracers, bromide and O, migrated at rates of 0.01 to 0.07 m/d, over distances of 4 and 6 m and under ...

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Most of the Earth's crust contains fluids, and fractures are common throughout the upper part. They exist at a wide range of scales from micro-fractures within grains to major faults and shear zones that traverse the crust. In this paper, the stress-dependent permeability in fractured rock masses have been investigated considering the effects of nonlinear normal deformation and shear dilation o...

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ژورنال

عنوان ژورنال: Water Resources Research

سال: 1993

ISSN: 0043-1397

DOI: 10.1029/92wr02592