TY - JOUR
T1 - Hydrogeology and groundwater availability in southwest Maclean and southeast Tazewell counties, part 1
T2 - aquifer characterization
AU - Herzog, B. L.
AU - Wilson, S. D.
AU - Larson, D. R.
AU - Smith, E. C.
AU - Larson, T. H.
AU - Greenslate, M. L.
PY - 1995
Y1 - 1995
N2 - The confluence of the buried Mahomet and Mackinaw Bedrock Valleys, underlying southwest McLean and southeast Tazewell Counties, contains part of one of the largest sand and gravel aquifers in Illinois - the Sankoty-Mahomet Sand aquifer. This groundwater resources study was undertaken to estimate the quantity of water the Sankoty-Mahomet Sand aquifer can safely yield and to determine potential locations from which a supply of 10-15 million gallons of groundwater per day could be developed. New data were generated from a surface geophysical survey, test drilling, mass measurements of water levels, aquifer tests, water quality samples, rain gauges, and stream measurements. These data show that, although the Sankoty-Mahomet Sand aquifer is more complex than previously thought, it is very prolific in this area. -from Authors
AB - The confluence of the buried Mahomet and Mackinaw Bedrock Valleys, underlying southwest McLean and southeast Tazewell Counties, contains part of one of the largest sand and gravel aquifers in Illinois - the Sankoty-Mahomet Sand aquifer. This groundwater resources study was undertaken to estimate the quantity of water the Sankoty-Mahomet Sand aquifer can safely yield and to determine potential locations from which a supply of 10-15 million gallons of groundwater per day could be developed. New data were generated from a surface geophysical survey, test drilling, mass measurements of water levels, aquifer tests, water quality samples, rain gauges, and stream measurements. These data show that, although the Sankoty-Mahomet Sand aquifer is more complex than previously thought, it is very prolific in this area. -from Authors
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M3 - Article
AN - SCOPUS:85041149236
SN - 1001-0742
JO - [No source information available]
JF - [No source information available]
ER -