2 edition of Model-estimated ground-water recharge and hydrograph of ground-water discharge to a stream found in the catalog.
Model-estimated ground-water recharge and hydrograph of ground-water discharge to a stream
A. T. Rutledge
by U.S. Dept. of the Interior, U.S. Geological Survey, Information Services [distributor] in Reston, Va, Denver, CO
Written in English
|Other titles||Model estimated ground water recharge and hydrograph of ground-water discharge to a stream.|
|Statement||by A.T. Rutlege.|
|Series||Water-resources investigations report -- 97-4253.|
|Contributions||Geological Survey (U.S.)|
|The Physical Object|
|Pagination||vi, 29 p. :|
|Number of Pages||29|
EPA//R/ November TMDL Model Evaluation and Research Needs By Leslie Shoemaker, Ting Dai, and Jessica Koenig Tetra Tech, Inc. Fairfax, Virginia Contract C Mohamed Hantush Land Remediation and Pollution Control Division National Risk Management Research Laboratory Cincinnati, Ohio National Risk Management . River cross sectional discharge calculation Stream discharge measurements were carried out as detailed in Section Values of flow velocity were obtained at m intervals across the river at a level of m of the total river depth at each measurement location.
Recharge is estimated from period was percent greater than for PULSE by taking the user-supplied estimates of ground-water recharge that produced a simulated ground-water discharge Because base flow does not account for losses of recharge hydrograph from PULSE fitting the recession segments of the caused by. Remote Sensing Applications Compiled and Edited by Dr. P. S. Roy, Deputy Director, Remote Sensing & GIS Applications Area, NRSC Dr. R.S. Dwivedi and n RS & GIS Applications Area, NRSC Published by National Remote Sensing Centre Indian Space Research Organisation Dept. of Space, Govt. of India, Balanagar, Hyderabad –
Download the abstract book. - Society of Environmental Toxicology. Hugo Navarro ecological risk and ground water pollution of organic pollutantsor in short LIBERA- TION. The presentation includes examples on how to scale and integrate the results from various scientific disciplines. increased river discharge into the Arctic Basin. sir - Free download as PDF File .pdf), Text File .txt) or read online for free. Automata.
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Model-Estimated Ground-Water Recharge and Hydrograph of Ground-Water Discharge to a Stream: USGS WRIR This report documents the theoretical basis and mathematical model.
The program user should read this report. Considerations for Use of the Rora Program to Estimate Ground-Water Recharge from Streamflow Records: USGS OFR Model-Estimated Ground-Water Recharge and Hydrograph of Ground-Water Discharge to a Stream By A.T.
Rutledge Abstract The computer model PULSE, described in this report, can be used to construct a hydrograph of ground-water discharge to a stream.
The model is applicable to a ground-water flow system that is driven by areally uniformFile Size: KB. Get this from a library. Model-estimated ground-water recharge and hydrograph of ground-water discharge to a stream.
[A T Rutledge; Geological Survey (U.S.)]. Estimates of Ground-Water Recharge Based on Streamflow-Hydrograph Methods: Pennsylvania By Dennis W.
Risser, Randall W. Conger, James E. Ulrich, and Michael P. Asmussen U.S. Department of the Interior U.S. Geological Survey In cooperation with the Pennsylvania Department of Conservation and Natural Resources, Bureau of Topographic and Geologic.
PULSE: Model-Estimated Ground-Water Recharge and Hydrograph of Ground-Water Discharge to a Stream PART: A computerized method of base-flow-record estimation RECESS: A method for analysis of streamflow recession.
The mean annual recharge of Al-Khazir Gomal Basin was estimated as a basis for decision makers regarding the renewability and sustainability of groundwater.
For this purpose, two approaches were used: hydrograph analysis and water table fluctuation (WTF). The long-term mean daily stream-flow records of Al-Khazir River (–) were used to estimate Cited by: A. T Rutledge has written: 'Model-estimated ground-water recharge and hydrograph of ground-water discharge to a stream' -- subject(s): Artificial groundwater recharge, Computer simulation.
Computer programs for describing the recession of ground-water discharge and for estimating mean ground-water recharge and discharge from stream-flow. Rutledge, A.T.,Model-estimated ground-water recharge and hydrograph of ground-water discharge to a stream.
Water Resources Investigations Report,US Geological Survey, Denver, 29 p. Google ScholarCited by: 6. PDF | On Jan 1,Dennis W Risser and others published Ground-Water Resources Program Comparison of Methods for Estimating Ground-Water Recharge and Base Flow at a Small Watershed Underlain by.
Certainly the most common method of assessing ground water discharge to streams is to separate a stream hydrograph into baseflow and quickflow and then assume that baseflow represents ground water discharge (Winter, ).
If hydrographs are not available, current meter measurements may be taken under low-flow conditions, and the difference in Cited by: Model-estimated ground-water recharge and hydrograph of ground-water discharge to a stream / (Reston, Va.: U.S. Dept. of the Interior, U.S. Geological Survey ; Denver, CO: Information Services [distributor], ), by A.
Rutledge and Geological Survey (U.S.) (page images at. Simulation of Ground-Water Flow. The GFLOW model domain includes all major drainage basins in the vicinity of the Bayfield Peninsula, ranging from the Bois Brule River in the west to the Bad River in the east (fig. Other surface-water features include Lake Superior to the north and several lakes and streams to the south.
Optimal hydrograph separation (OHS) uses a two-parameter recursive digital filter that applies specific conductance mass-balance constraints to estimate the base flow contribution to total streamflow at stream gages where discharge and specific conductance are measured.
OHS was applied to U.S. Geological Survey (USGS) stream gages across the conterminous United Author: Sydney S. Foks, Jeff P. Raffensperger, Colin A. Penn, Jessica M. Driscoll.
Hydrograph separation techniques range in complexity from graphical approaches that separate the hydrograph into base flow (a proxy for groundwater discharge to streams) and runoff components using only a record of stream discharge (e.g., recession curve [Barnes, ] or digital filter [Nathan and McMahon, ] methods), to two‐component Cited by: Base flow (b) and runoff (Q Stream – b) estimates served as proxies for groundwater and runoff discharge to the stream, respectively, and are hereafter referred to as groundwater discharge (Q GWD) and runoff discharge (Q RO).
Lumping of many different flow paths into these two end‐members is a simplification of the system, necessitated by Cited by: Therefore, we replaced the ground-water component of SWAT with the more detailed and sophisticated ground-water simulator MODFLOW.
The linkage between the two programs is shown schematically in Fig. 3, and is intended to represent the significant interactions among a watershed and its stream network and the associated aquifer according to the Cited by: The activities eligible for the grant program include research, planning, ground water assessments, demonstration programs, enforce- ment, technical assistance, and education and training to protect the quality of ground water and to prevent contam- ination of ground water from nonpoint sources of pollution.
Carmel watershed, the model- estimated groundwater phosphorus concentration is mg/L. The GWLF manual provides estimated backgroundgroundwater phosphorus concentrations for ≥90% forested land in the eastern United States, which is mg/L.
Consequently, about 60% of the groundwater load ( lbs/yr) can be attributed to naturalFile Size: 2MB. Understanding ground water flow on an aquifer or basin scale became possible with the analog model in the s. Improvements in computer technology in the s and s led to the development of digital computer models or numerical models of.
Full text of "Selected water resources abstracts" See other formats.Enhanced PDF; Standard PDF ( MB) ; 1. Introduction  Streambed seepage and hydraulic conductivity are important for hydrological and ecological studies. High seepage loss rates along a stream are indicative of focused groundwater recharge [Winter et al., ].Seepage controls mixing between surface water and groundwater, which is important for biological cycling of .Unlike past work that considers estimates of groundwater recharge and river flow as measures of supply, we use precipitation as the renewable water supply endogenous to the area, and consider natural and human uses of this water.
The reliance on imported river water or mined ground water is exposed in the process.