| Main Title |
IJC Menomonee River Watershed Study: Ground Hydrology. Volume 7. |
| Author |
Anderson, M. P. ;
Eisen, C. C. ;
Hoffer, R. N. ;
Konrad, John G. ;
Chesters, Gordon ;
|
| CORP Author |
Wisconsin Univ.-Madison. Water Resources Center.;Environmental Protection Agency, Chicago, IL. Great Lakes National Program Office. |
| Year Published |
1979 |
| Report Number |
EPA-R-005142; EPA-905/4-79-029-G; |
| Stock Number |
PB81-203069 |
| Additional Subjects |
Ground water ;
Water pollution ;
Menomonee River ;
Aquifers ;
Glacial deposits ;
Dolomite(Rock) ;
Sewage disposal ;
Waste water ;
Water flow ;
Solid waste disposal ;
Correlation techniques ;
Gravel ;
Wisconsin ;
Sandstones ;
NTISEPAELA
|
| Internet Access |
|
| Holdings |
| Library |
Call Number |
Additional Info |
Location |
Last
Modified |
Checkout
Status |
| EJBM |
PB81-203069 |
Most EPA libraries have a fiche copy filed under the call number shown. Check with individual libraries about paper copy. |
Headquarters Library/Washington,DC |
06/23/1988 |
| NTIS |
PB81-203069 |
Some EPA libraries have a fiche copy filed under the call number shown. |
|
07/26/2022 |
|
| Collation |
166p |
| Abstract |
The research was a comprehensive study of the quantity and quality of groundwater discharged into the Menomonee River System, southeastern Wisconsin. The Menomonee River Watershed comprises three aquifer systems: the deep artesian sandstone, the Niagara dolomite and the glacial aquifers. Groundwater discharge into the river system is supplied mainly by the shallow glacial aquifer, with only a minor component of discharge supplied by the dolomite aquifer. During the 1 year study, groundwater was found to account for 45 to 65% of the non-event flow in the Menomonee River. Discharges from sewage treatment plants and of industrial waste waters supplied the remainder of the non-event flow. |
