2 edition of Water-level changes in the High Plains aquifer--predevelopment to 1993 found in the catalog.
Water-level changes in the High Plains aquifer--predevelopment to 1993
Dugan, Jack T.
1994 by U.S. Dept. of the Interior, U.S. Geological Survey, Books and Open-File Reports, Open-File Reports Section [distributor] in Lincoln, Neb, Denver, Colo .
Written in English
|Other titles||Water level changes in the High Plains aquifer--predevelopment to 1993|
|Statement||by Jack T. Dugan and Dale A. Cox.|
|Series||Water-resources investigations report -- 94-4157|
|Contributions||Cox, Dale A., Geological Survey (U.S.)|
|The Physical Object|
|Pagination||vi, 60 p. :|
|Number of Pages||60|
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Get this from a library. Water-level changes in the High Plains aquifer--predevelopment to [T J McGrath; Jack T Dugan; Geological Survey (U.S.)]. Get this from a library. Water-level changes in the High Plains aquifer--predevelopment to [Jack T Dugan; Dale A Cox; Geological Survey (U.S.)].
You searched for: All Fields (("high plains" OR ) AND (aquifer OR watershed OR hydro OR model OR gage OR csrees OR compet) NOT (texas OR southern OR northern)) Remove constraint All Fields: (("high plains" OR ) AND (aquifer OR watershed OR hydro OR model OR gage OR csrees OR compet) NOT (texas OR southern OR northern)) Format Book OR Microfilm OR Map.
The report describes the High Plains aquifer, the factors that affect water levels in the aquifer, the history of development of the aquifer, water-level changes from predevelopment through the. McGrath, T. (Timothy J.): PIPECAR, version a microcomputer program for the structural analysis and design of circular and horizontal elliptical reinforced concrete pipe culverts:.
McGrath, T.S., and Dugan, J.T.,Water-level changes in the High Plains aquifer—Predevelopment to U.S. Geological Survey Water-Resources Investigations Report53 p. High Plains Water Levels. McGuire V L Water level changes in the high plains Aquifer, Predevelopment to –06, and – Scientific Investigations Report – Google Scholar Medellin-Azuara J, MacEwan D, Howitt R E, Koruakos G, Drogul E, Brush C, Kadir T, Harter T and Lund J R Hydro-economic analysis of groundwater pumping for California Cited by: 4.
Water-Level Changes in the High Plains Aquifer, Predevelopment totoand to USGS: Science Topics: groundwater USGS: Science Topics: surface-water level.
Water-level changes in the High Plains aquifer, predevelopment to and to U.S. Geological Survey Fact Sheet FS, 6 p. McLaughlin, D. Acquisition of improved time-varying gravity data would open a new class of important scientific problems to analysis, Water-level changes in the High Plains aquifer--predevelopment to 1993 book crustal motions associated with earthquakes and changes in groundwater levels, ice dynamics, sea-level changes, and atmospheric and oceanic circulation patterns.
The High Plains have a semi-arid, temperate climate, with surface elevations that follow a west-east gradient from~m in the west tõ m in the east (Dennehy et al., ); local relief is. The High Plains aquifer is the primary source of water for the production of food and fiber in the Great Plains area, central United States, and drives much of the economy of this region.
However, the saturated thickness of the central and southern portions of the aquifer has diminished since the early s because of an imbalance between Cited by: 3. The USGS post High Plains Aquifer Groundwater Levels Continue to Decline (6/16/17) summarizes the results from the USGS report Water-Level and Recoverable Water in Storage Changes, High Plains Aquifer, Predevelopment to and – Groundwater depletion is a serious issue in the southern and central parts of the High Plains Aquifer (HPA), USA.
A considerable imbalance exists between the recharge process and groundwater extractions in these areas, which threatens the long-term sustainability of the aquifer.
Irrigated agriculture has a major share in the economy, and it requires high pumping rates in regions vulnerable to. High application rates of chemical fertilizers, especially nitrogen (N) Biogeochemistry20, – [Google Scholar] V.L.
Water-Level Changes in the High Plains Aquifer, Predevelopment totoand to ; USGS Fact Sheet. Water-level changes in the High Plains aquifer, predevelopment to ; modified from McGuire, (USGS). Red areas are most severe. Red areas are most severe. Back to Ogallala rocks there’s another reason why they hold so much water.
The Our World in Data article Plastic Pollution by Hannah Ritchie and Max Roser (Sept ) is a detailed summary of plastics with 20 charts. For example, one of the charts is a time series of plastic production (downloaded and posted here) showing that, in.
Water-level changes in the High Plains aquifer, predevelopment to–08, and –09, and change in water storage, predevelopment to U.S. Geological Survey Scientific Investigations Report – Google ScholarAuthor: Dennis S. Ojima. This bibliography includes a majority of references used in the Colorado Ground Water Atlas along with pertinent entries gathered in the updating process.
McGuire, V.L., and Sharpe, J.B.,Water-level changes in the High Plains aquifer—Predevelopment to U.S. Geological Survey Water-Resources Investigations Report 97–, 2 pls.
McMahon, P.B.,A reconnaissance study of the effect of irrigated agriculture on water quality in the Ogallala Formation, central High Plains aquifer. MSU Scholars and Faculty Insight.
MSU Scholars () is Michigan State University’s instance of Academic Analytics’ public-facing version of their Research Discovery Suite. MSU Scholars highlights the visibility and research activity of MSU faculty and academic staff, identifying experts for local, state, national, and international research and business communities.
Water-level changes in the High Plains Aquifer—Predevelopment to U.S. Geol. Surv. Water-Resource Investigations Report Food and Agriculture Organization ().Cited by: and associated changes in intensities and frequencies of wet and dry periods, even though projections in space and time are uncertain.
Potential feedbacks of groundwater on the global climate system are largely unknown, but may be stronger than previously assumed. Groundwater has been depleted in manyCited by: 5. Estimation of the water requirement for beef production in the United States, Journal of Animal Science, 71, Changes in water level and storage in the High Plains aquifer, predevelopment to U.S.
Geological Survey Fact Sheet Retrieved Novem Water-Level Changes in the High Plains Aquifer. Box 22 Folder 5 Water-Level Changes in the High Planins Aquifer- Predevelopment to ; Box 22 Folder 6 Caring for the Kaw: A Citizen's Guide to Protecting Water Quality ; Box 22 Folder 7 Lawrence our future ; Box 22 Folder 8 Business Directory of Lawrence, K.T.
; Box 22 Folder 9 Planning Commission Minutes, Staff Reports. Water level measurements from to in 56 wells were separated into 10 time intervals; and, statistically they compared well to model output for the same time period.
Ten wells completed in the deep sandstone aquifer had long-term semicontinuous records, which were compared to simulated water-level trends for the same periods.
Full text of "Conservation of Great Plains Ecosystems: Current Science, Future Options [electronic resource]" See other formats. Water level changes and changes in storage in the High Plains Aquifer, predevelopment to and Texas Water Journal, Volume 7, Number 1 Conjunctive groundwater management as a.
Ina group of scientists at Colorado State University (McKee et al., ) developed a new drought index, the Standardized Precipitation Index (SPI). Extensive studies showed that the PDSI was highly correlated (typically r > ) with precipitation at certain timescales (almost always 6–12 months), and therefore temperature added.
FIGURE Water-level declines in the High Plains aquifer, – SOURCE: USGS, About this PDF file: This new digital representation of the original work has been recomposed from XML files created from the original paper book, not from the.
Full text of "Ecological Economics-Principles and Applications" See other formats. The modeled water-level decline is compared with data from ACCWF wells and irrigation wells in the vicinity on the basis of relative change from the water level (steady-state conditions).
Groundwater budget for the south-central High Plains aquifer during pre-development and in ; values are in million acre-feet per year (from McGuire et al., ). Figure 4. Generalized groundwater flow for (A) natural conditions and (B) pumped conditions.
Laurence Smith. The World in Four Forces Shaping Civilization's Northern Future. Smith, a UCLA geography professor, explores megatrends through computer model projections to describe "with reasonable scientific credibility, what our world might look like in forty years' time, should things continue as they are now." Laying out "ground rules" for himself--including an assumption of.
Katherine L. Rankin, Special Formats Catalog Librarian, WAML Information Bulletin Book Review Editor and former WAML President, was given the University of Nevada, Las Vegas Libraries' McPhee Librarian of the Year Award for Congratulations Kathy.
Water-level changes in the High Plains aquifer, predevelopment totoand. Technology as prospective ontology - Arie Rip - Synthese – pdf Кб. Ecological Economics - Free ebook download as PDF File .pdf), Text File .txt) or read book online for free. The Monetary Sector / Combining IS and LM / Exogenous Changes in IS and LM / IS-LM and Monetary and Fiscal Policy / IS-LM in the Real World / Adapting IS-LM to Ecological Economics / Big Ideas to Remember 5/5(4).
More than 96% of the water pumped from the aquifer has been used for irrigation. From predevelopment to the area weighted average water-level changes in the High Plains aquifer declined by m ( ft) (Table ). In South Dakota water level rose slightly during that period.
In Texas, water levels declined by m (35 ft) (Figure ). Characterization of trends in reservoir storage, streamflow, and precipitation in the Canadian River watershed in New Mexico and Texas. Water-level changes in the High Plains Aquifer, predevelopment to–06, Stored water declined in andCited by: 3.
- Free download as PDF File .pdf), Text File .txt) or read online for free. Scribd is the world's largest social reading and publishing site. The High Plains (Ogallala) Aquifer System Extending the Water Supply C H A P T E R Ore Deposits Types of Mineral Deposits Igneous Rocks and Magmatic Deposits Hydrothermal Ores Desalination Sedimentary Deposits Contents 13 Mineral and Rock Resources Interbasin Water Transfer xii Case Study Suspects.We can get at least a feel here for the magnitude of the changes of water level due to Holocene isostatic readjustment from the sea level data shown in Fig.
Displayed are the elevations relative to modern sea level of the Bristol Channel, United Kingdom, site for the last 8 .Geosystems Combination of satellite Terra MODIS sensor image and GOES satellite image produces a true-color view of North and South America f km (22, mi) in space.