Wisconsin's Role in Great Lakes Restoration - American Water ...
Wisconsin's Role in Great Lakes Restoration - American Water ...
Wisconsin's Role in Great Lakes Restoration - American Water ...
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15. Prelim<strong>in</strong>ary Hydrogeologic Characterization M<strong>in</strong>k River Estuary – <strong>Water</strong> Chemistry<br />
and Flow<br />
Maureen A. Muldoon, Department of Geology, University of Wiscons<strong>in</strong> Oshkosh, Oshkosh,<br />
WI, muldoon@uwosh.edu<br />
Jack Borski, Department of Geology, University of Wiscons<strong>in</strong> Oshkosh, Oshkosh, WI,<br />
borskj88@uwosh.edu<br />
Kenneth R. Bradbury, Wiscons<strong>in</strong> Geological and Natural History Survey, Madison, WI,<br />
krbradbu@wisc.edu<br />
The M<strong>in</strong>k River Estuary, located <strong>in</strong> northeastern Door County, is one of the most prist<strong>in</strong>e<br />
freshwater estuaries <strong>in</strong> the country. Groundwater quantity and quality are critical to the health<br />
of the estuary, but to date there has been little <strong>in</strong>vestigation of groundwater <strong>in</strong>puts to the<br />
system. The objectives of this project are to 1) establish a groundwater monitor<strong>in</strong>g network<br />
around the estuary, 2) gather prelim<strong>in</strong>ary <strong>in</strong>formation on the groundwater system, and 3)<br />
evaluate mix<strong>in</strong>g between the M<strong>in</strong>k River and Lake Michigan.<br />
Dur<strong>in</strong>g the summer of 2010 a survey of surface-water chemistry revealed a dist<strong>in</strong>ct mix<strong>in</strong>g<br />
pattern between groundwater discharg<strong>in</strong>g <strong>in</strong> discrete spr<strong>in</strong>g complexes and Lake Michigan<br />
waters. Stream discharge measurements and <strong>in</strong>-stream m<strong>in</strong>i-piezometers yielded mixed<br />
results concern<strong>in</strong>g groundwater/surface-water <strong>in</strong>teractions. In the northwest arm of the M<strong>in</strong>k<br />
River, both stream discharge and m<strong>in</strong>i-piezometer data collected <strong>in</strong> May suggest that<br />
groundwater discharges from discrete spr<strong>in</strong>gs near the edges of the marsh but that the M<strong>in</strong>k<br />
River does not ga<strong>in</strong> flow along significant reaches. In contrast, m<strong>in</strong>i-piezometers <strong>in</strong>stalled <strong>in</strong><br />
the northeast arm <strong>in</strong> August 2010 showed consistently upward hydraulic gradients. Heatpulse<br />
flow logs from three bedrock monitor<strong>in</strong>g wells <strong>in</strong>dicate upward flow from fractures near<br />
the base of the wells (~90 ft. depth) to fractures near the bedrock surface (~depth 20 - 40 ft.).<br />
We are collect<strong>in</strong>g cont<strong>in</strong>uous water-level measurements from both bedrock wells and still<strong>in</strong>g<br />
wells <strong>in</strong> the estuary. Quarterly samples of both surface and groundwater were collected <strong>in</strong><br />
November and February.<br />
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