3 edition of Steady-state simulation of ground-water flow in the Rush Springs aquifer, western Oklahoma found in the catalog.
Steady-state simulation of ground-water flow in the Rush Springs aquifer, western Oklahoma
Mark F Becker
by U.S. Dept. of the Interior, U.S. Geological Survey, Branch of Information Services [distributor] in [Reston, Va.?], Denver, CO
Written in English
|Other titles||Steady state simulation of ground water flow in the Rush Springs aquifer, western Oklahoma|
|Statement||by Mark F. Becker ; in cooperation with the Oklahoma Water Resources Board and Oklahoma Geological Survey|
|Series||Water-resources investigations report -- 98-4082|
|Contributions||Oklahoma Water Resources Board, Oklahoma Geological Survey, Geological Survey (U.S.)|
|The Physical Object|
|Pagination||iii, 74 p.,  p. :|
|Number of Pages||74|
Simulation of Ground-Water Flow and. Solute Transport in the Glen Canyon Aquifer, East-Central Utah. By Geoffrey W. Freethey and Bernard J. Stolp Prepared in cooperation with the Utah Department of Natural Resources, Division of Oil, Gas, and Mining. Scientific Investigations Report – U.S. Department of the Interior U.S. Geological. A C C E P T E D M A N U S C R I P T 5 aquifer system features, such as recharge modes, flow paths in the aquifer, flow regime, hydraulic conductivity and/or thickness of the unsaturated zone.
Steady State Flow Model of the Western Aquifer Basin SUSMAQ-MOD#23V July 1 Disclaimer This report is an output from the Flow Modelling and Hydrogeology Component, part of the SUSMAQ project. The findings, interpretations and conclusions expressed are . The hydraulic conductivity values used by Mark F. Becker (written commun., ) to simulate the ground-water flow in the Rush Springs aquifer are , , , , and feet per day. The hydraulic conductivity values are based on specific capacity data and aquifer tests.
In the ground-water flow model, Mark F. Becker defined the Rush Springs aquifer to include the Rush Springs Formation, alluvial and terrace deposits along major streams, and parts of the Marlow Formations, particularly in the eastern part of the aquifer boundary area. Urbanization is putting a great deal of pressure on the Aquifer's remaining resources. Rush Springs sits under square miles of western Oklahoma. It is the second most developed Aquifer in Oklahoma after the High Plains. It runs between and feet deep. It is a major asset for the agricultural economy that dominates this part of the.
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Abstract A simplified steady-state ground-water flow model was prepared for the Rush Springs aquifer in western Oklahoma. A 3-kilometer square grid was established over the area containing two layers with active nodes simulated in the model.
Steady-state simulation of ground-water flow in the Rush Springs aquifer, western Oklahoma [Mark F. Becker] on *FREE* shipping on qualifying offers. Book; Government Document Published [Reston, Va.?]: U.S. Dept. of the Interior, U.S. Geological Survey ; Denver, CO: Branch of Information Services [distributor], Language English Variant Title Steady state simulation of ground water flow in the Rush Springs aquifer, western Oklahoma Series Water-Resources Investigations Report SuDoc Number.
Get this from a library. Steady-state simulation of ground-water flow in the Rush Springs aquifer, western Oklahoma. [Mark F Becker; Oklahoma Water Resources Board.; Oklahoma Geological Survey.; Geological Survey (U.S.)]. Steady-state simulation of ground-water flow in the Rush Springs aquifer, western Oklahoma / By Mark F.
Becker, Geological Survey (U.S.), Oklahoma Geological Survey. and Oklahoma Water Resources Board. Abstract. Shipping list no.: es bibliographical references (p. ).Mode of access: Internet. Buy Steady-state simulation of ground-water flow in the Rush Springs aquifer, western Oklahoma (SuDoc I /) by Becker, Mark F.
(ISBN:) from Amazon's Book Store. Everyday low prices and free delivery on eligible : Mark F. Becker. STEADY-STATE SIMULATION OF GROUND WATER FLOW IN THE BLAINE AQUIFER, SOUTHWESTERN OKLAHOMA AND NORTHWESTERN TEXAS By D.L RUNKLE and J.S. McLEAN U.S. GEOLOGICAL SURVEY Open-File Report Prepared in cooperation with the OKLAHOMA WATER RESOURCES BOARD and the OKLAHOMA GEOLOGICAL SURVEY Oklahoma City, Oklahoma Cited by: 1.
The Aquifer The Rush Springs aquifer underlies approximately 2, square miles in west central Oklahoma, including large portions of Caddo, Custer, Washita, and Grady counties. It is the second most developed aquifer in the state after the Ogallala.
Caddo County is ranked fourth statewide in the amount of permitted groundwater per Size: 1MB. MODFLOW is a groundwater modelling program. It can be compiled and remedied according to the practical applications.
Because structure and fixed data format, MODFLOW can be integrated with geographic information system (GIS) for ground water resource management.
Groundwater is a distinguished component of the hydrologic cycle. Groundwater is the water which Cited by: Becker, M.F.,Steady-State Simulation of Ground-Water Flow in the Rush Springs Aquifer, Western Oklahoma: U.S.
Geological Survey Water-Resources Investigations Report Steady-State Simulation of Ground-Water Flow in the Rush Springs Aquifer, Western Oklahoma By Mark F. Becker ABSTRACT A simplified steady-state ground-water flow model was prepared for the Rush Springs aquifer in western Oklahoma. A 3-kilometer square grid was established over the area containing two layers with active nodes simulated in the : M.F.
Becker. Hydrogeology and Simulation of Groundwater Flow in the Central Oklahoma (Garber-Wellington) Aquifer, Oklahoma, toand Simulation of Available Water in Storage, – A numerical groundwater-flow model of the Rush Springs aquifer was constructed by using MODFLOW with the Newton solver.
Groundwater flow was simulated for January –December by using monthly stress periods, and an initial steady-state stress period was configured to represent mean annual inflows and : John Ellis.
Modify your heat/diffusion code to solve the 1-D transient ground water flow equation. We wish to simulate temporal changes in the confined aquifer heads between two reservoirs (shown below).
Assume the aquifer is m long, has a T of m2 min-1, and a storage coefficient of Hydrogeology, Simulation of Ground-Water Flow, and Land-Surface Subsidence in the Chicot, Evangeline, and Jasper Aquifers, Houston Area, Texas Mark C. Kasmarek & Eric W. Strom In Cooperation with the Texas Water Development Board and.
Simulation of ground-water flow and solute transport in the Glen Canyon aquifer, East-Central Utah: USGS Scientific Investigations Report [Geoffrey W.
Freethey, Bernard J. Stolp] on *FREE* shipping on qualifying offers. The extraction of methane from coal beds in the Ferron coal trend in central Utah started in the : Geoffrey W. Freethey. Interpretive Reports. Science Center Objects.
Overview; Becker, Mark F.,Steady-state simulation of ground-water flow in the Rush Springs aquifer, western Oklahoma: U.S. Geological Survey Water-Resources Investigations Report Description: Steady-state simulation of ground-water flow in the Rush Springs Aquifer, western Oklahoma.
Survey Date: Print Date: Two Sided: No. Pieces: 1. Languages: English. $ Available + Add $4 Product to Cart. the aquifer are decreased. The quantity of flow, which can be calculated from the flow net using the methods of Sectionis increased. One result of the increased flow is a larger discharge area, made necessary by the need for the large flows in the aquifer to escape to the surface as the influence of the left-hand boundary is Size: 2MB.
Hydrogeology and Steady-State Numerical Simulation of Groundwater Flow in the Lost Creek Designated Ground Water Basin, Weld, Adams, and Arapahoe Counties, Colorado 88 by U.S. Department of the Interior U.S. Department of the InteriorPages:. Hydrogeology and simulation of groundwater flow in the central Oklahoma (Garber-Wellington) Aquifer, Oklahoma, toand simulation of available water in storage, / by: Mashburn, Shana L.
Published: ().Steady-state simulation of ground-water flow in the Rush Springs aquifer, western Oklahoma / ([Reston, Va.?]: U.S.
Dept. of the Interior, U.S. Geological Survey ; Denver, CO: Branch of Information Services [distributor], ), by Mark F. Becker, Geological Survey (U.S.), Oklahoma Geological Survey, and Oklahoma Water Resources Board (page.In this lesson, our focus is to analyze the steady flow to pumping wells, and hence it is also assumed that flow towards the well is under steady-state conditions.
Steady Radial Flow in Confined Aquifers. For analyzing steady radial flow in a confined aquifer, apart from the above assumptions, the following additional assumptions are.