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<font face='Univers condensed',Helvetica,Arial size=+2>News Release

<font face='Univers condensed',Helvetica,Arial size=-1>U.S. Department of the Interior
<font face='Univers condensed',Helvetica,Arial size=-1>U.S. Geological Survey

<font face='Univers condensed',Helvetica,Arial size=-1>Address
Office of Communications
119 National Center
Reston, VA 20192
<font face='Univers condensed',Helvetica,Arial size=-1>Release
March 18, 2002
<font face='Univers condensed',Helvetica,Arial size=-1>Contact
Frank Manheim
<font face='Univers condensed',Helvetica,Arial size=-1>Phone
703-648-6150
<font face='Univers condensed',Helvetica,Arial size=-1>Fax


<font face='Univers condensed',Helvetica,Arial size=+2>Fresh Water Under the Sea?

By using electrical measurements, USGS scientists have detected fresh groundwater in submarine environments in Mid-Atlantic coastal waters. The new data will help define sources and quantities of nutrients entering the coastal bays of Delaware, Maryland, and Virginia and refine groundwater flow models. A special "streamer resistivity survey" technique was used to measure the electrical resistance of bottom sediments.

Normal saltwater sediments are good conductors of electricity. However, bottom sediments permeated by fresh waters are poor conductors of electricity, and act like semi-insulators. To conduct the streamer resistivity survey, a 360-foot electrical cable called a streamer was towed behind boats. Continuous measurements of electrical potential at variable spacings revealed the presence of fresh ground water beneath the bays at distances from a few hundred meters to one kilometer from shore. The researchers were able to map fresh, salt and mixed water layers to more than 100 feet below the sea floor.

Studying submarine discharges in the Delmarva Peninsula, an area that includes the Rehoboth, Indian River, Chincoteague, and other saltwater coastal bays, is important because these areas receive very high concentrations of nutrients. The high nutrient supply causes undesirable effects such as algal fouling and changes in bottom sediment environments. The data from the streamer resistivity survey will define pathways of freshwater inflow, and help resource managers plan remediation efforts to reduce nutrients entering the coastal bays. Accurate information may minimize remediation impacts on local farming, recreation and other activities in the coastal areas.

In some areas, up to 80 percent of freshwater enters the bays not from streams or rain, but by groundwater discharge. The pathways of entry however, are poorly understood. The current survey in the Delmarva Peninsula is one of the first systematic detailings of regional estuarine groundwater properties using the electrical resistivity method. It has mapped the distribution of submarine freshwater discharge and confirmed remote sensing tests conducted from aircraft. The latter studies were part of regional research by the University of Delaware and Delaware Geological Survey, in cooperation with the USGS. The seagoing electrical resistivity technique offers major breakthroughs because it recovers data at rates 30 to 70 times those for comparable studies on land.

The results of this streamer resistivity measurements were presented at the Symposium for the Application of Geophysics to Environmental and Engineering Problems (SAGEEP) in Las Vegas, Feb. 10-14 by USGS Coastal and Marine and Water Resources scientists along with industry and regional partners. The report can be viewed at http://woodshole.er.usgs.gov/epubs/SAGEEP/.

The USGS serves the Nation by providing reliable scientific information to: describe and understand the Earth; minimize the loss of life and property from natural disasters; manage water, biological, energy and mineral resources; and enhance and protect our quality of life.

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U.S. Geological Survey, MS119 National Center, Reston, VA 20192, USA
URL http://www.usgs.gov/public/press/public_affairs/press_releases/pr1572m.html
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Last Modification: 3-18-2002@3:04pm(BK)