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Last modified
5/14/2010 8:58:17 AM
Creation date
9/30/2006 10:12:13 PM
Metadata
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Template:
Publications
Year
1998
Title
Ground Water and Surface Water A Single Resource U.S. Geological Survey Circular 1139
CWCB Section
Interstate & Federal
Author
T.C. Winter, J.W. Harvey, O.L. Franke, W.M. Alley
Description
Overview of current understandimg of interaction of ground water and surface water in terms of quality and quantity
Publications - Doc Type
Historical
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<br /> <br />commonly returns to the river as base flow <br />directly downstream from the dam. In addition, <br />reservoirs can cause temporary bank storage at <br />times when reservoir levels are high. In some <br />cases, this temporary storage of surface water in <br />the ground-water system has been found to be a <br />significant factor in reservoir management (see <br />BoxQ). <br />Human-controlled reservoir releases and <br />accumulation of water in storage may cause high <br />flows and low flows to differ considerably in <br />magnitude and timing compared to natural flows. <br />As a result, the environmental conditions in river <br />valleys downstream from a dam may be altered as <br />organisms try to adjust to the modified flow condi- <br />tions. For example, the movement of water to and <br />from bank storage under controlled conditions <br />would probably be much more regular in timing <br />and magnitude compared to the highly variable <br />natural flow conditions, which probably would <br />lead to less biodiversity in river systems down- <br />stream from reservoirs. The few studies that have <br />been made of riverine ecosystems downstream <br />from a reservoir indicate that they are different <br />from the pre-reservoir conditions, but much more <br />needs to be understood about the effects of reser- <br />voirs on stream channels and riverine ecosystems <br />downstream from dams. <br /> <br />REMOVAL OF NATURAL VEGETATION <br /> <br />To make land available for agriculture and <br />urban growth, development sometimes involves <br />cutting of forests and removal of riparian vegeta- <br />tion and wetlands. Forests have a significant role <br />in the hydrologic regime of watersheds. Deforesta- <br />tion tends to decrease evapotranspiration, increase <br />storm runoff and soil erosion, and decrease infil- <br />tration to ground water and base flow of streams. <br />From the viewpoint of water-resource quality and <br />management, the increase in storm runoff and soil <br />erosion and the decrease in base flow of streams <br />are generally viewed as undesirable. <br />In the western United States, removal of <br />riparian vegetation has long been thought to result <br />in an increase in streamflow. It commonly is <br />believed that the phreatophytes in alluvial valleys <br />transpire ground water that otherwise would flow <br />to the river and be available for use (see Box R). <br />Some of the important functions of riparian vege- <br />tation and riparian wetlands include preservation <br />of aquatic habitat, protection of the land from <br />erosion, flood mitigation, and maintenance of <br />water quality. Destruction of riparian vegetation <br />and wetlands removes the benefits of erosion <br />control and flood mitigation, while altering <br />aquatic habitat and chemical processes that main- <br />tain wafer quality. <br /> <br />69 <br />
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