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Pseudokarst groundwater hydrologic characteristics of a mine spoil aquifer.
Mine Water and the Environ 1992 Jun; 11(2):37-52
Aquifer tests of surface coal mine spoil indicate two distinctly different groundwater hydrologic characteristics exist. Slug tests empirically indicate the presence of discrete conduits within the spoil. Groundwater flow within conduits is pseudokarst, and flow between conduits is porous media. Under transient or stress conditions, pseudokarst groundwater flow in the spoil becomes prominent; under steady-state conditions, porous media flow dominates. Tracer testing indicates the average linear velocity of groundwater through spoil is close to pure porous media and significantly lower than true karst flow.
OP; Journal Article
Issue of Publication
Mine Water and the Environment
Page last reviewed: April 12, 2019
Content source: National Institute for Occupational Safety and Health Education and Information Division