Causes of Historical Changes in Groundwater Recharge Rates in Southeastern Wisconsin
BACKGROUND/NEED Recharge is the process by which rain, snowmelt and surface waters infiltrate to and replenish groundwater. As such, it is the ultimate source of all of our groundwater reso...
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Using “PREDICT” to reduce herbicide usage and improve groundwater quality
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Stratigraphic controls on the mobilization and transport of naturally- occurring arsenic in groundwater: Implication for wellhead protection
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Stratigraphy, sedimentaology and porosity distribution of the Silurian rocks of Door County, Wisconsin
Final report was submitted as a journal article: Harris, M. T., Kuglitsch, J. J., Watkins, R., Hegrenes, D. P., and Waldhuetter, K. R., 1998, Early Silurian stratigraphic sequences of eas...
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Characterization of the role of evapotranspiration on groundwater movement and solute chemistry in groundwater-fed wetlands
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Mineral Phase Sorption of Selected Agrichemicals to Wisconsin Soils
Final report was submitted as a journal article: Grundl, T., & Small, G. (1993). Mineral contributions to atrazine and alachlor sorption in soil mixtures of variable organic carbon an...
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