Zobrazeno 1 - 10
of 18
pro vyhledávání: '"George S. Roadcap"'
Modeling a Large‐Scale Historic Aquifer Test: Insight into the Hydrogeology of a Regional Fault Zone
Publikováno v:
Groundwater. 58:453-463
Faults can act as flow barriers or conduits to groundwater flow by introducing heterogeneity in permeability. We examine the hydrogeology of the Sandwich Fault Zone, a 137 km long zone of high-angle faults in northern Illinois, using a large-scale hi
Publikováno v:
Hydrological Processes. 33:271-282
Deep basin aquifers are increasingly used in water‐stressed areas, though their potential for sustainable development is inhibited by overlying aquitards and limited recharge rates. Long open interval wells (LOIWs)—wells uncased through multiple
Publikováno v:
Ground water. 56(1)
Investigating changes in an aquifer system often involves comparison of observed heads from different synoptic measurements, generally with potentiometric surfaces developed by hand or a statistical approach. Alternatively, head-specified MODFLOW mod
Publikováno v:
Geological Society of America Abstracts with Programs.
Autor:
George S. Roadcap
Publikováno v:
Geological Society of America Abstracts with Programs.
Publikováno v:
Geological Society of America Abstracts with Programs.
Autor:
George S. Roadcap, Daniel B. Abrams
Publikováno v:
Geological Society of America Abstracts with Programs.
Publikováno v:
Ground Water. 43:806-816
Extremely alkaline ground water has been found underneath many shuttered steel mills and slag dumps and has been an impediment to the cleanup and economic redevelopment of these sites because little is known about the geochemistry. A large number of
Publikováno v:
Ground Water. 43:500-510
A total of 176 wells in sand-and-gravel glacial aquifers in central Illinois were sampled for arsenic (As) and other chemical parameters. The results were combined with archived and published data from several hundred well samples to determine potent
Publikováno v:
Ground Water. 41:57-65
Deposition from at least three episodes of glaciation left a complex glacial-drift aquifer system in central Illinois. The deepest and largest of these aquifers, the Sankoty-Mahomet Aquifer, occupies the lower part of a buried bedrock valley and supp