Soil macropores: Control on infiltration, hillslope and surface hydrology on a reclaimed surface-mined watershed
Conference
·
· Geological Society of America, Abstracts with Programs; (United States)
OSTI ID:6109872
- Middle Tennessee State Univ., Murfreesboro, TN (United States). Dept. of Geography and Geology
- Pennsylvania State Univ., University Park, PA (United States). Dept. of Geosciences
The hydrologic response of a surface-mined watershed in central Pennsylvania is controlled by rapid macropore flow within the unsaturated man-made topsoil. Newly reclaimed surface-mined watersheds in central Pennsylvania exhibit low steady-state infiltration rates (1--2 cm/hr) and produce runoff dominated by infiltration-excess overland flow. However, within four years after reclamation, infiltration rates on some mine surfaces approach premined rates (8 cm/hr). As infiltration rate increases, the volume of infiltrated water increases, but the total porosity of minesoil matrix remains constant. There is little change in the surface discharge volume, indicating that infiltrated water continues to contribute to the basin surface discharge by the processes of throughflow and return flow. Throughflow in the topsoil horizon occurs in rapid response to rainfall input, producing large volumes of water with throughflow rates closely related to rainfall rates and with throughflow peaks following rainfall peaks by only minutes. Increased return flow alters the shape of the surface runoff hydrograph by slightly lagging behind infiltration excess overland flow. These changes in the shape of the surface runoff hydrograph reduce the potential for severe gully erosion on the reclaimed site. In addition, throughflow water remains predominantly in the topsoil horizon, and therefore has limited contact with potentially acid-producing backfill. Better understanding of macropore flow processes in reclaimed minesoils will help investigators evaluate past strategies and develop new reclamation techniques that will minimize the short-term surface erosional effects of mining and reclamation, while optimizing the long-term effluent and groundwater quality.
- OSTI ID:
- 6109872
- Report Number(s):
- CONF-921058--
- Conference Information:
- Journal Name: Geological Society of America, Abstracts with Programs; (United States) Journal Volume: 24:7
- Country of Publication:
- United States
- Language:
- English
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Related Subjects
01 COAL, LIGNITE, AND PEAT
010900* -- Coal
Lignite
& Peat-- Environmental Aspects
DEVELOPED COUNTRIES
GROUND WATER
HYDRAULIC CONDUCTIVITY
HYDROGEN COMPOUNDS
HYDROLOGY
LAND RECLAMATION
MECHANICS
MINING
NORTH AMERICA
OXYGEN COMPOUNDS
PENNSYLVANIA
POROSITY
SOIL MECHANICS
SURFACE MINING
USA
WATER
WATER INFLUX
WATERSHEDS
010900* -- Coal
Lignite
& Peat-- Environmental Aspects
DEVELOPED COUNTRIES
GROUND WATER
HYDRAULIC CONDUCTIVITY
HYDROGEN COMPOUNDS
HYDROLOGY
LAND RECLAMATION
MECHANICS
MINING
NORTH AMERICA
OXYGEN COMPOUNDS
PENNSYLVANIA
POROSITY
SOIL MECHANICS
SURFACE MINING
USA
WATER
WATER INFLUX
WATERSHEDS