Surface water and groundwater interactions in an extensively mined watershed, upper Schuylkill River, Pennsylvania, USA

Streams crossing underground coal mines may lose flow, whereas abandoned mine drainage (AMD) restores flow downstream. During 2005–2012, discharge from the Pine Knot Mine Tunnel, the largest AMD source in the upper Schuylkill River Basin, had near‐neutral pH and elevated concentrations of iron, mang...

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Veröffentlicht in:	Hydrological processes 2014-05, Vol.28 (10), p.3574-3601
Hauptverfasser:	Cravotta, Charles A., III, Goode, Daniel J, Bartles, Michael D, Risser, Dennis W, Galeone, Daniel G
Format:	Artikel
Sprache:	eng
Schlagworte:	Abandoned mines acid mine drainage acidity carbon dioxide coal drainage geochemical model Groundwater groundwater flow groundwater model hydrograph analysis ionic strength Iron manganese mathematical models mine hydrology oxidation rivers streams sulfates surface water Water quality water table watersheds
Online-Zugang:	Volltext
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