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Title: Strata-movement concepts and the hydrogeological impact of underground coal mining. [Effects of subsidence on permeability of rock above longwall]

Journal Article · · Ground Water; (United States)

A review of mining-engineering concepts and studies in mine hydrology suggests a conceptual model linking the strata deformation, hydraulic property changes, and ground-water impacts due to underground coal mining. The pressure-arch deformation pattern about a small opening creates a local zone of increased permeabilities and dewatering in the seam and immediate roof, but should not hydraulically affect shallower aquifiers. Networks of supported headings, rooms, and pillars intensely drain lower aquifiers but only slightly affect higher strata except in areas of naturally high permeability. Longwall mining causes extensive, high-reaching, well-defined zones of stress, fracturing, and hydraulic impact, the maximum permeability increases being in the tensile zones immediately above the panel and at the sides of the subsidence trough. In shallow aquifiers, permeabilities and ground-water velocities increase, and hydraulic gradients decline independently of mine drainage. A study of a deep coal mine in the Appalachian Plateau, Pennsylvania indicated: probable hydraulic connections between the mine and shallow aquifiers in a principle valley area; no obvious response of water levels in shallow aquifiers to undermining by supported headings; and rapid, considerable declines in such water levels in response to nearby longwall mining. These results are consistent with the conceptual model.

Research Organization:
Dept. of Geology, Northern Illinois Univ., DeKalb, IL 60115
OSTI ID:
5376020
Journal Information:
Ground Water; (United States), Vol. 24:4
Country of Publication:
United States
Language:
English