Over the past fifty years, anecdotal and hydrogeologic evidence have accumulated suggesting that groundwater from the Prairie du Chien-Jordan aquifer flows under significant pressure beneath the Cannon River floodplain in Carleton College\u27s Cowling Arboretum. This study documents the contribution of this high-pressure groundwater to wetlands in the Cowling Arboretum by measuring specific conductance and temperature values across these wetlands. These results were then compared to baseline water quality report data, and data collected from the Cannon River Wilderness Area\u27s Prairie du Chien spring. Sampling from three wetlands on the Cannon River floodplain revealed wetlandspecific trends in specific conductance and temperature t...
The University Archives has determined that this item is of continuing value to OSU's history
Understanding surface water-groundwater interaction processes and quantification of hydrological flu...
Assessing the Periodic Groundwater Flow Conditions of a Perched Aquifer System in the Daniel Boone N...
Interactions between surface and ground water in wetland areas can provide a number of functions wit...
Wetlands are critical components of functioning at the interface between terrestrial and aquatic eco...
Wetlands are a vital component of the landscape, a keystone ecosystem, that are prone to degradation...
Natural ephemeral wetlands in the ridgetops of the Daniel Boone National Forest serve as reservoirs ...
The Northeast Creek/ Fresh Meadow watershed is home to Acadia National Park\u27s (ANP) largest wetla...
Historically, drier types of wetlands have been difficult to characterize and are not well researche...
Rainfall, runoff, overbank flow and groundwater, all contribute water to wetlands. Each transport el...
Historically, drier types of wetlands have been difficult to characterize and are not well researche...
Presented at The Oregon Water Conference, May 24-25, 2011, Corvallis, OR.Many freshwater ecosystems ...
The Cowles Bog National Natural Landmark and the wetlands between the dunes near the south shore of ...
Includes bibliographical references (pages [120]-123)Delineating the controls of wetland hydrology f...
Depressional wetlands are common in South Dakota cropland and the Prairie Pothole Region of central ...
The University Archives has determined that this item is of continuing value to OSU's history
Understanding surface water-groundwater interaction processes and quantification of hydrological flu...
Assessing the Periodic Groundwater Flow Conditions of a Perched Aquifer System in the Daniel Boone N...
Interactions between surface and ground water in wetland areas can provide a number of functions wit...
Wetlands are critical components of functioning at the interface between terrestrial and aquatic eco...
Wetlands are a vital component of the landscape, a keystone ecosystem, that are prone to degradation...
Natural ephemeral wetlands in the ridgetops of the Daniel Boone National Forest serve as reservoirs ...
The Northeast Creek/ Fresh Meadow watershed is home to Acadia National Park\u27s (ANP) largest wetla...
Historically, drier types of wetlands have been difficult to characterize and are not well researche...
Rainfall, runoff, overbank flow and groundwater, all contribute water to wetlands. Each transport el...
Historically, drier types of wetlands have been difficult to characterize and are not well researche...
Presented at The Oregon Water Conference, May 24-25, 2011, Corvallis, OR.Many freshwater ecosystems ...
The Cowles Bog National Natural Landmark and the wetlands between the dunes near the south shore of ...
Includes bibliographical references (pages [120]-123)Delineating the controls of wetland hydrology f...
Depressional wetlands are common in South Dakota cropland and the Prairie Pothole Region of central ...
The University Archives has determined that this item is of continuing value to OSU's history
Understanding surface water-groundwater interaction processes and quantification of hydrological flu...
Assessing the Periodic Groundwater Flow Conditions of a Perched Aquifer System in the Daniel Boone N...