Field experiments in a fractured clay till: 1. Hydraulic conductivity and fracture aperture
- 1 April 1993
- journal article
- Published by American Geophysical Union (AGU) in Water Resources Research
- Vol. 29 (4), 1149-1162
- https://doi.org/10.1029/92wr02592
Abstract
No abstract availableKeywords
This publication has 27 references indexed in Scilit:
- Groundwater Flow and Solute Transport in Fractured Lacustrine Clay Near Mexico CityWater Resources Research, 1991
- The Depth of Fractures and Active Ground‐Water Flow in a Clayey Till Plain in Southwestern OntarioGroundwater, 1991
- Remote Data Collection and Control for Hydrogeologic MonitoringGround Water Monitoring & Remediation, 1990
- Fracture effects in the shallow groundwater zone in weathered Sarnia-area clayCanadian Geotechnical Journal, 1989
- Fracture permeability and groundwater flow in clayey till near Saskatoon, SaskatchewanCanadian Geotechnical Journal, 1986
- Origin and Distribution of Sulfate in a Fractured Till in Southern Alberta, CanadaWater Resources Research, 1986
- Migration of Chlorophenolic Compounds at the Chemical Waste Disposal Site at Alkali Lake, Oregon —1. Site Description and Ground‐Water FlowGroundwater, 1984
- Origin, age and movement of pore water in argillaceous Quaternary deposits at four sites in southwestern OntarioJournal of Hydrology, 1981
- The Chalk groundwater tritium anomaly — A possible explanationJournal of Hydrology, 1975
- The Fracture Porosity of Glacial TillCanadian Journal of Earth Sciences, 1975