3 edition of Ground-water levels in the alluvial aquifer in eastern Arkansas, 1987 found in the catalog.
Ground-water levels in the alluvial aquifer in eastern Arkansas, 1987
|Other titles||Ground water levels in the alluvial aquifer in eastern Arkansas, 1987.|
|Statement||by Paul W. Westerfield ; prepared in cooperation with the Arkansas Soil and Water Conservation Commission, the U.S. Soil Conservation Service, and local conservation districts.|
|Series||U.S. Geological Survey open-file report -- 89-64.|
|Contributions||United States. Soil Conservation Service., Arkansas Soil and Water Conservation Commission., Geological Survey (U.S.)|
|The Physical Object|
Parts of the South Platte River alluvial aquifer in northeastern Colorado are underlain by the Pierre Shale, a marine deposit of Late Cretaceous age that is. streamflows subsided and ground-water levels lowered in response to ground-water withdrawals by wells, the more usual movement of water from the river into the aquifer was re-established. Gradient reversals occurred only during the high-flow events of June , March– April .
The Ozarks, also referred to as the Ozark Mountains, Ozarks Mountain Country, and the Ozark Plateau, are a physiographic and geologic highland region of the central United States. It covers much of the southern half of Missouri and an extensive portion of northwestern and north central Arkansas. The region also extends westward into northeastern Oklahoma and extreme southeastern Kansas. The Country: United States. A confining layer is defined in this study as a layer of material that is not very permeable to ground water flow and that overlays an aquifer and acts to prevent water movement into the aquifer. The US Geological Survey, working with the Missouri Department of Natural Resources, selected a total of wells, in both unconfined and confined.
Quantifying aquifer properties and freshwater resource in coastal barriers: a hydrogeophysical approach applied at Sasihithlu (Karnataka state, India). Hydrology Cited by: Ground-water resources and water quality in the vicinity of Pine Bluff municipal area, Jefferson County, Arkansas TD Clayton Ground-water quality and potential contamination of the Mississippi River alluvial aquifer in northeastern Arkansas Data on springs in Arkansas Annual Report of the Arkansas Water Resources Research Center Bulletin
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Get this from a library. Ground-water levels in the alluvial aquifer in eastern Arkansas, [Paul W Westerfield; United States. Soil Conservation Service.; Arkansas Soil and Water Conservation Commission.; Geological Survey (U.S.)].
A huge amount of water exists in the ground below your feet, and people all over the world make great use of it. But it is only found in usable quantities in certain places underground — aquifers.
Read on to understand the concepts of aquifers and how water exists in the ground. A hole dug at the beach is a great way to illustrate the concept.
Abstract. Water levels were measured monthly at 9 staff gages and 35 wells along two transects within the Black Swamp bottomland hardwood wetland and perpendicular to the Cache River in eastern Arkansas from December to September in order to (1) describe the ground-water-flow conditions at locations within a bottomland hardwood wetland and (2) determine the relation between Cited by: 5.
Mahon, G.L., and Ludwig, A.H.,Simulation 1987 book ground-water flow in the Mississippi River Valley alluvial aquifer in eastern Arkansas: U.S. Geological Survey. Effects of fluctuating river-pool stages on ground-water levels in the adjacent alluvial aquifer in the lower Arkansas River, Arkansas / (Little Rock, Ark.: Dept.
of the Interior, U.S. Geological Survey ; Denver, Colo.: Books and Open-File Reports Section [distributor], ), by D. Freiwald, Gerald D. Grosz, Geological Survey (U.S.), and. Ground-water levels in the alluvial aquifer in eastern Arkansas, [microform] / by Paul W.
Westerfie Arkansas River, Conway County Drainage and Levee District No. 1, Arkansas: letter from the Secretary of Ground-water levels in the alluvial aquifer in eastern Arkansas, [microform] /.
Ground-water levels in the alluvial aquifer in eastern Arkansas, Westerfield, P. W.; Baxter, C. WRI Water-level maps of the Mississippi River Valley alluvial aquifer in eastern Arkansas, Westerfield, Paul W. OFR Ground-water levels in Arkansas, Spring. WRI Recalibration of a ground-water flow model of the Mississippi River Valley alluvial aquifer in Southeastern Arkansas,with simulations of hydraulic heads caused by projected ground-water withdrawals throughby G.P.
Stanton and B.R. Clark. (All publications open in a new window) Methods Development -- Recharge Sanford, W.E.; Nelms, D.L.; Pope, J.P.; Selnick, D.L.,Quantifying components of the hydrologic cycle in Virginia using chemical hydrograph separation and multiple regression analysis: U.S.
Geological Survey Scientific Investigations Report: Groundwater Availability -- Floridan Aquifer. Soil and Water Conservation Commission internal control and compliance review Status of water levels and selected water-quality conditions in the Mississippi River Valley alluvial aquifer in eastern Arkansaswith simulations of water levels caused by projected ground-water withdrawals through by T.
Any contamination impacting the Sparta aquifer or the alluvial aquifer by organic and inorganic contaminants above health based levels could pose a public health hazard and result in greater water treatment costs and limit the future utility of groundwater. Shumaker is about 75 miles south of Little Rock, Arkansas, near the City of Camden.
The Arkansas Natural Resources Commission (ANRC) conducts an annual inventory of reported groundwater and surface-water withdrawals in Arkansas in cooperation with the U.S. Geological Survey (USGS). This report describes withdrawals from groundwater and surface-water resources in.
EXECUTIVE SUMMARY GROUND-WATER FLOW DIRECTIONS AND CONTAMINANT SOURCE AREA EVALUATION FOR THE PLAQUEMINE AQUIFER SCOTT ELLINGER, M.S., P.G. U.S. ENVIRONMENTAL PROTECTION AGENCY REGION 6 MULTIMEDIA PLANNING AND PERMITTING DIVISION October 7, This report presents the U.S.
Environmental Protection Agency Region 6, (EPA) ground. This bibliography includes a majority of references used in the Colorado Ground Water Atlas along with pertinent entries gathered in the updating process. For users of the various GIS datasets, the metadata included there provides as much information on.
Alluvial deposits of the Mississippi and Arkansas Rivers were the predominant causes of soils found in the eastern portion of the watershed.
Slopes of less than one percent characterize this area while elevations range from to feet above sea level (USDA,). Geological Survey (U.S.): Analysis of hydrologic factors that affect ground-water levels in the Arkansas River alluvial aquifer near La Junta, Colorado, / (Denver, Colo.: U.S.
Department of the Interior, U.S. Geological Survey ; Denver, CO: Information Services [distributor], ), also by C. Bossong and Colorado Water. Díaz, J.R.,Ground-water levels on the south coast of Puerto Rico, February to FebruaryU.S. Geological Survey Open-File Report30 p. Díaz, J.R.,Ground-water levels in alluvium on the south coast of Puerto Rico, FebruaryU.S.
Geological Survey Open-File Report18 p. (Online Publication). Groundwater recharge and sustainability in the High Plains aquifer in Kansas, USA Article (PDF Available) in Hydrogeology Journal 13(2) January Author: Marios Sophocleous.
wsp / wilson, w. / estimated effects of projected ground water withdrawals on movement of the saltwater front in the floridian aquifer, west-central florida,cl, 24 pages, 17 figs., 2 tables, $ Values of δ2H, δ18O, Ar and Ne indicate that most of the ground water in the alluvial aquifer was irrigation water that was derived from the North Platte River and distributed during the growing.
An aquifer is an underground layer of water-bearing permeable rock, rock fractures or unconsolidated materials (gravel, sand, or silt). Groundwater can be extracted using a water study of water flow in aquifers and the characterization of aquifers is called d terms include aquitard, which is a bed of low permeability along an aquifer, and aquiclude (or aquifuge.The effect of artesian-pressure decline on confined aquifer systems and its relation to land subsidence; U.
Geology and ground-water resources of Dane County, Wisconsin; V. Ground-water resources of eastern Arkansas in the vicinity of the U.S. Highway 70; W. Geology and ground-water resources of Richardson County, Nebraska; X.
Quality of. Schrader TP () Water levels and selected water-quality conditions in the Mississippi River Valley alluvial aquifer in eastern Arkansas, US Geological Survey Scientific Investigations Report Google ScholarAuthor: L.
T. West, J. N. Shaw, E. P. Mersiovsky.