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June 26-27, 2001
Richmond, Virginia

Example of Possible Study Approach

The USGS, Office of Ground Water's Ground-Water Resources Program is currently funding the Southwest Ground-Water Resources (SWGR) project in the arid to semiarid basins in the southwestern states of California, Nevada, Utah, Arizona, and New Mexico.  Although the climate and aquifer systems in the Piedmont/Blue Ridge region differ from those of the southwestern states, the study approach of the SWGR project was used as a template for the discussion concerning the development of a science plan for the fractured rock aquifers in the Piedmont and Blue Ridge.

The approach of the SWGR project consists of (1) a regional synthesis of hydrologic and geologic information in the region and (2) integration of several networked research projects on topics (ground-water and surface-water interactions, recharge determinations, effects of ground-water development on riparian systems, and climatic effects on ground-water systems) specific to the assessment of availability and sustainability of water resources throughout the Desert Basins of the Southwest.

Examples from the SWGR website (http://az.water.usgs.gov/swgwrp/Pages/Overview.html) are shown below to illustrate the approach used by this project.


 

Link to U.S. Geological Survey
Southwest Ground-water Resources
sample side-bar

Regional Synthesis

One of the main aspects of the study is regional synthesis of hydrologic and geologic information from throughout the Southwest. The data are compiled and analyzed using geographic information systems (GIS) data sets, spreadsheet and statistical programs.

A major priority of this part of the project is to characterize ground-water and surface-water systems in terms of the potential for future overdraft, the value to riparian ecosystems, and the characteristics of the aquifers that may lead to potential overdraft.

 Data synthesis and analysis of the regional synthesis study include (see examples at following links):

Basin Categorization - GIS coverages are obtained or created to categorize the hydrologic setting of basins in the study area.

Depth to Ground Water - Data on water levels are compiled from USGS and other sources.  Hydrographs are plotted and GIS data sets (coverages) of depth to ground water are created for basins where data are available.

Water-Use Data - Data on water-use are compiled from USGS and other sources to help evaluate changes in water use.

Streamflow Data - Information on streamflow gaging stations are obtained and analyzed to illustrate base-flow conditions in streams for predevelopment and recent streamflow conditions.

Land Use - Land use conditions are obtained for the study area to analyze the relation between land-use changes and hydrologic conditions.

 


Link to U.S. Geological Survey
Southwest Ground-water Resources
sample side-bar

Regional Synthesis: Depth to Ground-water

Water-level data for ground-water monitoring sites in the study area have been compiled from U.S. Geological Survey databases and other sources. Hydrographs that illustrate the waterLong-term Ground-water Monitoring Sites map-level changes in most aquifer systems have been plotted. GIS data sets that represent pre-development or recent ground-water levels are being created, where possible.

 

well graph
well graph
The water-level data are used to evaluate the impact of changes in land use and water use on the aquifer systems. Changes in ground-water levels may also represent aquifer system response to climate variability.  Water-level data will also show areas where surface-water and ground-water interactions may play an important role in sustaining riparian habitat.

Link to U.S. Geological Survey
Southwest Ground-water Resources
sample side-bar

Recharge Projects

The objective of this part of the Southwest Ground-water Resources Project is to develop methods of quantifying ground-water recharge and ground-water/surface-water interactions. Recharge in southwestern alluvial basins occurs primarily along mountain fronts and in ephemeral and perennial streambeds where precipitation and runoff are concentrated and conveyed. In contrast, direct recharge through alluvial fans may account for the majority of recharge in many Basin and Range alluvial basins. The extent to which any location serves as a recharge (or discharge) area is a function of numerous factors, including lithology, slope, vegetative cover, climate, unsaturated-zone thickness, and hydraulic properties, and precipitation-event intensity and duration.

 As part of the effort to better understand recharge processes, the Southwest Ground-water Resources Project has developed both a networked series of studies and a set of individual studies.  The five networked recharge study sites have been established to cover the five-state study area in the Southwest.  For a synopsis of each project, check the Networked Recharge Studies map.

 The Individual Recharge Projects are concerned with the development of improved methods of quantifying recharge to ground-water systems from streams and application of these methods in the Southwest. Below is a table outlining each project.

 

Project Description Principal Investigator
Chloride Deposition in the southwestern United States - The chloride-mass- balance approach will be used to calculate evapotranspiration, recharge, and in the case of extremely dry desert environments, the time since water has infiltrated through the unsaturated zone to the underlying water table. John Izbicki,
San Diego, CA
Characterization of the temporal and spatial distribution of recharge mechanisms in the desert Southwest - The objective is to determine the relation between climate and physiographic features, including soil and bedrock properties, that leads to specific mechanisms of recharge and map out the occurrence of the mechanism over the region. A.L. Flint,
Sacramento, CA
The interaction of streambed infiltration and geomorphic changes in arroyos - The objectives include documenting channel changes at selected reaches in the Rio Puerco and quantifying streambed-infiltration rates at those sites. A.C. Gellis,
Albuquerque, NM
The response of surface-water/ground-water interactions to present-day climate variation: Amargosa Desert case study - Baseline data on surface-water flow and ground-water recharge will be established in the Upper Amargosa Basin under typical dry weather patterns. This data, along with previously collected data, will show the hydrologic response of the basin as it decays from El Niņo-induced wetter conditions to more typical drier conditions. D.A. Stonestrom,
Menlo Park, CA
Land-based thermal detection of the spatial and temporal distributions of streamflow on the San Pedro River - The objective is to quantify the spatial and temporal pattern flows in the San Pedro River. J. Constanz,
Menlo Park, CA

Contact: dlnelms@usgs.gov
U.S. Department of Interior, U.S. Geological Survey
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Last modified: July 09, 2002 09:02:17 AM
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