2 edition of Simulation of a long-term aquifer test conducted near the Rio Grande, Albuquerque, New Mexico found in the catalog.
Simulation of a long-term aquifer test conducted near the Rio Grande, Albuquerque, New Mexico
Douglas P. McAda
by U.S. Dept. of the Interior, U.S. Geological Survey, Information Services [distributor] in Albuquerque, N.M. (5338 Montgomery Blvd. NE, ste. 400, Albuquerque 87109-1311), Denver, CO
Written in English
|Other titles||Simulation of a long term aquifer test conducted near the Rio Grande, Albuquerque, New Mexico|
|Statement||by Douglas P. McAda ; prepared in cooperation with the City of Albuquerque Public Works Department.|
|Series||Water-resources investigations report -- 99-4260|
|Contributions||Albuquerque (N.M.). Dept. of Public Works, Geological Survey (U.S.)|
|The Physical Object|
|Pagination||v, 66 p. :|
|Number of Pages||66|
The Albuquerque Basin (or Middle Rio Grande Basin) is one of the largest and deepest of the structural basins in the Rio Grande contains the city of Albuquerque, New Mexico.. Geologically, the Albuquerque Basin is a half-graben that slopes down towards the east to terminate on the Sandia and Manzano mountains. It has a semi-arid climate, with large areas Coordinates: 35°06′N °36′W / . The purpose of this investigation was to describe the water table configuration and its temporal variations, estimate aquifer properties, and evaluate the interaction of groundwater and surface water in the inner valley of the Rio Grande in southern Albuquerque, New Mexico, where groundwater contamination is a continuing concern. The upper ft of sedimentary deposits .
reach of the Río Grande in central New Mexico, United States. The stream-aquifer system near Escondida, New Mexico, was instrumented with temperature- and pressure-recording sensors to compare groundwater-level responses as a function of different streamflow conditions and determine forcing mechanisms driving diurnal stream-aquifer exchanges. Biogeochemistry at the zone of intermittent saturation: Field-based study of the shallow alluvial aquifer, Rio Grande, New Mexico Article in Geosphere 3(5) .
Model modification included splitting the four layers of the McAda-Wasiolek model (McAda, D.P., and Wasiolek, Maryann, , Simulation of the regional geohydrology of the Tesuque aquifer system near Santa Fe, New Mexico: U.S. Geological Survey Water- Resources Investigations Report , 71 p.) into eight layers to better simulate vertical. SOURCES OF SALINITY IN THE RIO GRANDE AND MESILLA BASIN GROUNDWATER WRRI Technical Completion Report No. James C. Witcher J. Phillip King John W. Hawley John F. Kennedy Jerry Williams Michael Cleary Lawrence R. Bothern NEW MEXICO WATER RESOURCES RESEARCH INSTITUTE New Mexico State University MSC Box Las Cruces, New Mexico .
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SIMULATION OF A LONG-TERM AQUIFER TEST CONDUCTED NEAR THE RIO GRANDE, ALBUQUERQUE, NEW MEXICO By Douglas P. McAda ABSTRACT A long-term aquifer test was conducted near the Rio Grande in Albuquerque during January and February using 22 wells and piezometers at nine sites, with the City of Albuquerque Griegos 1 production well Cited by: 1.
Get this from a library. Simulation of a long-term aquifer test conducted near the Rio Grande, Albuquerque, New Mexico. [Douglas P McAda; Albuquerque (N.M.). Department of Public Works.; Geological Survey (U.S.)]. supply. This report presents the results of a long- term aquifer test conducted near the Rio Grande in Albuquerque.
The long-term aquifer test was conducted during the winter of The City of Albuquerque Griegos 1 water production well was pumped continuously for 54 days at an average pumping rate of 2, gallons per minute.
DuringAuthor: Conde R. Thorn, Charles E. Heywood. Simulation of an Aquifer Test on the Tesuque Pueblo Grant, New Mexico By Glenn A.
Hearne Abstract An aquifer test was designed and conducted in the anisotropic dipping beds of the Tesuque Formation on the Tesuque Pueblo Grant, New Mexico. The three-di mensional digital model used to analyze the test approxiAuthor: Glenn A.
Hearne. Simulation of a long-term aquifer test conducted near the Rio Grande, Albuquerque, New Mexico / by Douglas P. McAda ; prepared in cooperation with the City of Albuquerque Public Works : Douglas P. McAda. Get this from a library. Analytical results of a long-term aquifer test conducted near the Rio Grande, Albuquerque, New Mexico.
[Condé R Thorn; Charles Albuquerque Heywood; Albuquerque (N.M.). Department of Public Works. Water Resources.; Geological Survey (U.S.)].
the Middle Rio Grande Basin near Albuquerque, New Mexico, as part of the U.S. Geological Survey National Water-Quality Assessment Program. The Santa Fe Group aquifer system in the Middle Rio Grande Basin regional study area is represen-tative of the Basin and Range basin-fill aquifers of the south.
Hearne GA () Mathematical model of the Tesuque aquifer system near Pojoaque, New Mexico US Government Printing Office Hearne GA, Dewey J () Hydrologic analysis of the Rio Grande Basin north of Embudo, New Mexico; Colorado, and New Mexico Huff G () Simulation of ground-water flow in the basin-fill aquifer of the Tularosa basin.
WATER-QUALITY DATA FOR THE RIO GRANDE BETWEEN PICACHO BRIDGE NEAR LAS CRUCES AND CALLE DEL NORTE BRIDGE NEAR MESILLA, NEW MEXICO, By G.F.
Huff U.S. GEOLOGICAL SURVEY Open-File Report Prepared in cooperation with the CITY OF LAS CRUCES Albuquerque, New Mexico Author: G.F. Huff. Hydrogeologic Setting and Groundwater. Flow Simulation of the Middle Rio Grande Basin Regional Study Area, New Mexico.
By Laura M. Bexfield, Charles E. Heywood, Leon J. Kauffman, Gordon W. Rattray, and Eric T. Vogler. Section 2 of. Hydrogeologic Settings and Groundwater-Flow Simulations for.
Regional Investigations of the Transport of. Ground-water flow modeling is an important tool frequently used in studies of ground-water systems. Reviewers and users of these studies have a need to evaluate the accuracy or reasonableness of the ground-water flow model. This report provides some guidelines and discussion on how to evaluate complex ground-water flow models used in the investigation of.
Anthropogenic sulfate loads in the Rio Grande, New Mexico (USA) Article in Chemical Geology () April with Reads How we measure 'reads'. New Mexico aeromagnetic and gravity maps and data: a web site for distribution of data.
Open-File Report Thorn, Conde R.; Heywood, Charles E., Analytical results of a long-term aquifer test conducted near the Rio Grande, Albuquerque, New Mexico, with a section on piezometric-extensometric test results.
Analytical results of a long-term aquifer test conducted near the Rio Grande, Albuquerque, New Mexico, with a section on piezometric-extensometric test results,Water-Resources Investigations Report The Albuquerque area of New Mexico has two principal sources of water: (1) groundwater from the Santa Fe Group aquifer system, and (2) surface water from the Rio Grande.
From topumping from the Santa Fe Group aquifer system caused groundwater levels to decline more than feet while water-level declines along the Rio Grande in Albuquerque were. Geochemical Characterization of Ground-Water Flow in the Santa Fe Group Aquifer System, Middle Rio Grande Basin, New Mexico Book January.
Institutional Adjustments for Coping with Prolonged and Severe Drought in the Rio Grande Basin. Las Cruces: New Mexico Water Resources Research Institute. Watkins, A. The Impact of Climate Change on New Mexico’s Water Supply and Ability to Manage Water Resources. Santa Fe: New Mexico Office of the State Engineer.
SIMULATED MASS TRANSPORT OF 1,2-DIBROMOETHANE IN GROUNDWATER OF SOUTHEAST ALBUQUERQUE, NEW MEXICO By Scott Ellinger ABSTRACT A three-dimensional groundwater flow and contaminant transport model was developed to study the mass transport of 1,2-dibromoethane (EDB) in the Santa Fe Group aquifer system of southeast Albuquerque, New : Scott Ellinger.
Simulation of ground-water flow in the Mojave River basin, California. Request This. Title Analytical results of a long-term aquifer test conducted near the Rio Grande, Albuquerque, New Mexico.
Thorn, Condé R. GBW no The Basin of Mexico is located in the central part of the Trans-Mexican Volcanic Belt and has an approximate area of 9, square kilometers. The basin, at an altitude of 2, meters above sea level, is the highest valley in the region, and is surrounded by mountains that reach elevations of over 5, meters above sea level.
A study done by USGS projected groundwater would rise 25 to 50 feet over 40 years once Albuquerque cut back on its pumping. For Rio Grande Valley water users, both human and natural, the recharge.The more than 3, square miles of the Middle Rio Grande Basin includes the Albuquerque Basin and aquifer.
The semiarid climate of this region is a constant challenge to recharge, although this groundwater supply has successfully supplied Albuquerque's population of over(38% of the New Mexico population) with its municipal and.Ground Displacements Caused by Aquifer-system Water-level Variations Observed using Interferometric Synthetic Aperture Radar Near Albuquerque, New Mexico Article (PDF Available) January