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Full-Text Articles in Environmental Sciences
A Brief History And Summary Of The Effects Of River Engineering And Dams On The Mississippi River System And Delta, Jason S. Alexander, Richard C. Wilson, W. Reed Green
A Brief History And Summary Of The Effects Of River Engineering And Dams On The Mississippi River System And Delta, Jason S. Alexander, Richard C. Wilson, W. Reed Green
United States Geological Survey: Water Reports and Publications
The United States Geological Survey Forecast Mekong project is providing technical assistance and information to aid management decisions and build science capacity of institutions in the Mekong River Basin. A component of this effort is to produce a synthesis of the effects of dams and other engineering structures on large-river hydrology, sediment transport, geomorphology, ecology, water quality, and deltaic systems. The Mississippi River Basin (MRB) of the United States was used as the backdrop and context for this synthesis because it is a continental scale river system with a total annual water discharge proportional to the Mekong River, has been …
Altitude, Age, And Quality Of Groundwater, Papio-Missouri River Natural Resources District, Eastern Nebraska, 1992 To 2009, Virginia L. Mcguire, Derek W. Ryter, Amanda T. Flynn
Altitude, Age, And Quality Of Groundwater, Papio-Missouri River Natural Resources District, Eastern Nebraska, 1992 To 2009, Virginia L. Mcguire, Derek W. Ryter, Amanda T. Flynn
United States Geological Survey: Water Reports and Publications
The United States Geological Survey (USGS), in cooperation with the Papio-Missouri River Natural Resources District (PMRNRD), conducted this study to map the water-level altitude of 2009 within the Elkhorn River Valley, Missouri River Valley, and Platte River Valley alluvial aquifers; to present the predevelopment potentiometric-surface altitude within the Dakota aquifer; and to describe the age and quality of groundwater in the five principal aquifers of the PMRNRD in eastern Nebraska using data collected from 1992 to 2009. In addition, implications of alternatives to the current PMRNRD groundwater-quality monitoring approach are discussed.
In the PMRNRD, groundwater altitude, relative to National Geodetic …
Saturated Thickness And Water In Storage In The High Plains Aquifer, 2009, And Water-Level Changes And Changes In Water In Storage In The High Plains Aquifer, 1980 To 1995, 1995 To 2000, 2000 To 2005, And 2005 To 2009, Virginia L. Mcguire, Kris D. Lund, Brenda K. Densmore
Saturated Thickness And Water In Storage In The High Plains Aquifer, 2009, And Water-Level Changes And Changes In Water In Storage In The High Plains Aquifer, 1980 To 1995, 1995 To 2000, 2000 To 2005, And 2005 To 2009, Virginia L. Mcguire, Kris D. Lund, Brenda K. Densmore
United States Geological Survey: Water Reports and Publications
The High Plains aquifer underlies about 112 million acres (about 175,000 square miles) in parts of eight States—Colorado, Kansas, Nebraska, New Mexico, Oklahoma, South Dakota, Texas, and Wyoming. Water levels declined in parts of the High Plains aquifer soon after the onset of substantial irrigation with groundwater (about 1950). This report presents the volume of saturated aquifer material and drainable water in storage in the High Plains aquifer in 2009; water-level changes in the High Plains aquifer from 1980 to 1995, 1995 to 2000, 2000 to 2005, and 2005 to 2009; and changes in the volume of drainable water in …
Hydrostratigraphic Interpretation Of Test-Hole And Surface Geophysical Data, Elkhorn And Loup River Basins, Nebraska, 2008 To 2011, Christopher M. Hobza, Paul A. Bedrosian, Benjamin R. Bloss
Hydrostratigraphic Interpretation Of Test-Hole And Surface Geophysical Data, Elkhorn And Loup River Basins, Nebraska, 2008 To 2011, Christopher M. Hobza, Paul A. Bedrosian, Benjamin R. Bloss
United States Geological Survey: Water Reports and Publications
The Elkhorn-Loup Model (ELM) was begun in 2006 to understand the effect of various groundwater-management scenarios on surface-water resources. During phase one of the ELM study, a lack of subsurface geological information was identified as a data gap. Test holes drilled to the base of the aquifer in the ELM study area are spaced as much as 25 miles apart, especially in areas of the western Sand Hills. Given the variable character of the hydrostratigraphic units that compose the High Plains aquifer system, substantial variation in aquifer thickness and characteristics can exist between test holes. To improve the hydrogeologic understanding …