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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Session 1A – Biological and Chemical Contam<strong>in</strong>ants<br />
Salon C<br />
Moderator: John Panuska, University of Wiscons<strong>in</strong>-Extension<br />
2:15 Modern Statistical Methods for Predict<strong>in</strong>g Bacterial Exceedances <strong>in</strong><br />
Beach <strong>Water</strong>. Wesley Brooks**<br />
2:35 Effects of Starvation on the Transport of Escherichia Coli K12 <strong>in</strong><br />
Saturated Porous Media are Dependent on pH and Ionic Strength.<br />
Lucia Feriancikova**<br />
2:55 Geochemical Indicators of Sanitary Sewer Effluent Transport <strong>in</strong>to Deep<br />
<strong>Water</strong> Supply Wells <strong>in</strong> Madison, Wiscons<strong>in</strong>. Christopher A. Gellasch**<br />
3:15 The Importance of Quantify<strong>in</strong>g Gas Generation and Migration <strong>in</strong><br />
Contam<strong>in</strong>ated Sediments. Nathaniel R. Keller<br />
Session 1B – Advances <strong>in</strong> Hydrologic Technology and Resources<br />
Salon D<br />
Moderator: Joe Dorava, Vierbicher Associates<br />
2:15 Us<strong>in</strong>g Onl<strong>in</strong>e Video To Tell People about Wiscons<strong>in</strong>’s <strong>Water</strong> Resources.<br />
John Karl<br />
2:35 F<strong>in</strong>d<strong>in</strong>g the Source: F<strong>in</strong>gerpr<strong>in</strong>t<strong>in</strong>g of Suspended Sediment <strong>in</strong> Lower Fox<br />
River Wiscons<strong>in</strong> Tributaries. Paul D. Baumgart<br />
2:55 Us<strong>in</strong>g Heated Distributed Temperature Sens<strong>in</strong>g to Monitor Soil <strong>Water</strong>.<br />
Arlen M. Striegl**<br />
3:15 Evaluation of Turf- Grass and Prairie- Vegetated Ra<strong>in</strong> Gardens <strong>in</strong> a Clay<br />
Soil. William R. Selbig<br />
3:35 – 3:55 p.m. Break<br />
3:55 – 5:35 p.m. Concurrent Sessions 2A and 2B<br />
3