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Tuesday, October 6, 2020 | History

2 edition of Computer model of two-dimensional solute transport and dispersion in ground water found in the catalog.

Computer model of two-dimensional solute transport and dispersion in ground water

Leonard F. Konikow

Computer model of two-dimensional solute transport and dispersion in ground water

by Leonard F. Konikow

  • 82 Want to read
  • 5 Currently reading

Published by U.S. Govt. Print. Off. in Washington .
Written in English

    Subjects:
  • Groundwater flow -- Mathematical models.,
  • Dispersion -- Mathematical models.

  • Edition Notes

    Other titlesAutomated data processing and computations.
    Statementby L. E. Konikow and J. D. Bredehoeft.
    SeriesTechnique of water-resources investigations of the United States Geological Survey -- bk. 7, ch. C2.
    ContributionsBredehoeft, J. D.
    The Physical Object
    Paginationvi, 90 p. :
    Number of Pages90
    ID Numbers
    Open LibraryOL16007962M

    "Computer Model of Two-Dimensional Solute Transport and Dispersion in Ground Water", USGS Techniques of Water Resources Investigations, Book 7, Chap. C2, . The discrete-fracture, finite-element model HydroGeoSphere (Therrien et al. ) and a discrete-fracture implementation of MT3DMS (Zheng ) were used to model solute transport in a single.

    Computer Model of Two-Dimensional Solute Transport and Dispersion in Ground Water. U.S. Geological Survey Water-Resources Investigations Book 7, Chap. C2, 90 pp. Google ScholarCited by: Computer model of two-dimensional solute transport and dispersion in ground water. Techniques of Water-Resource Investigations of the United States Geological Survey, Book 7, Chapt. C2.

    This paper presents a study of solute transport through ground water in the saturated zone and the resulting breakthrough curves (BTCs), using a field-scale numerical model that incorporates the. 7-C2. Computer model of two-dimensional solute transport and dispersion in ground water, by L. F. Konikow and J. D. Bredehoeft: USGS— TWRI Book 7, Chapter C2. 90 pages. 7-C3. A model for simulation of flow in singular and interconnected channels, by R. W. Schaffranek, R. A. Baltzer, andFile Size: KB.


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Computer model of two-dimensional solute transport and dispersion in ground water by Leonard F. Konikow Download PDF EPUB FB2

This report presents a model that simulates solute transport in flowing ground water. The model is both general and flexible in that it can be applied to a wide range of problem types.

It is applicable to one- or two-dimensional problems involving steady-state or transient flow. The model computes changes in concentration over time caused by the processes of convective transport, hydrodynamic.

Computer Model of Two-Dimensional Solute Transport and Dispersion in Ground Water U.S. Geological Survey, Techniques of Water-Resources Investigations, Book. COMPUTER MODEL OF TWO-DIMENSIONAL SOLUTE TRANSPORT AND DISPERSION IN GROUND WATER. By L. Konikow and J. Bredehoeft Abstract. This report presents a model that simulates solute transport in flowing ground water.

The model is both general and flexible in that it can be applied to a wide range of problem types. Updates of the computer code associated with "Computer model of two-dimensional solute transport and dispersion in ground water" UNITED STATES DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY RESTON, VA.

In Reply Refer To: March 4, WGS-Mail Stop OFFICE OF GROUND WATER TECHNICAL MEMORANDUM NO. Subject: GROUND WATER--Updates of the computer code associated with "Computer model.

NAME moc - Two-dimensional method-of-characteristics ground-water flow and transport model ABSTRACT This model simulates solute transport in flowing ground water. It is applicable to one- or two-dimensional problems involving steady- state or transient flow. The model computes changes in concentration over time caused by the processes of advective transport, hydrodynamic dispersion.

Get this from a library. Computer model of two-dimensional solute transport and dispersion in ground water. [Leonard F Konikow; J D Bredehoeft]. Ground Water Monitoring & Remediation, v.

20, no. 4, p. Merritt, M.L., and Konikow, L.F.,Documentation of a computer program to simulate lake-aquifer interaction using the MODFLOW ground-water flow model and the MOC3D solute-transport model: U.S. Geological Survey Water-Resources Investigations Reportp. NAME biomoc - A multispecies solute-transport model with biodegradation ABSTRACT BIOMOC is a two-dimensional model that can simulate the transport and biotransformation of multiple reacting solutes.

The program is general and flexible, allowing for any combination of biodegradation processes. A number of expressions for biological transformation rates have been included as options in the code.

Salt water intrusion is investigated in a coastal groundwater system in the northern part of the province Noord-Holland, The Netherlands. Density dependent groundwater flow is modeled in three-dimensions with MOCDENS3D.

This computer code is a version of MOC3D (Konikow et al., ) that has been adapted to simulate transient density-driven groundwater by: A mathematical model consists of differential equations developed from ana-lyzing groundwater flow (or solute transport in groundwater) and are known to govern the physics of flow (and transport).

The reliability of model predic-tions depends on how well the model approximates the actual situation in the. Computer Model of Two-Dimensional Solute Transport and Dispersion in Ground Water.

USGS Techniques of Water-Resources Investigations. Book 7, Chap. C2, 90 pp. Ligget, J.A. and P.L-F. Liu. The Boundary Integral Equation Method for Porous Media Flow. Allen. Computer model of two-dimensional solute transport and dispersion in ground water.

TWRI, Book 7, Chapter C2, U.S. Geological Survey, Reston, Virginia. Google ScholarCited by: 2. Computer model of two-dimensional solute transport and dispersion in ground water. Techniques of Water-Resources Investigations, Book 7, ch. U.S. Geological Survey. McDonald, M.G.

and A.W. Harbaugh. A modular three-dimensional finite-difference ground-water flow model. Techniques of Water-Resources Investigations of the USGS, ch. Konikow, L.F. and J.D. Bredehoeft () Computer Model of Two-Dimensional Solute Transport and Dispersion in Ground Water.

Techniques of Water-Resources Investigations. Book 7, Chapter C2. U.S. Geological Survey, Reston, Virginia. Google Scholar.

@article{osti_, title = {Groundwater transport: handbook of mathematical models}, author = {Javandel, I and Doughty, C and Tsang, C F}, abstractNote = {This monograph discusses selected analytical solutions, semianalytical methods and numerical approaches used to study solute transport in groundwater.

It discusses their strengths. Finite difference model for aquifer simulation in two dimensions with results of numerical experiments, by PC. Trescott. G.F. Pinder, and S.P. Larson. pages. Computer model of two-dimensional solute transport and dispersion in ground water, by L.F.

Konikow and J.D. Bredehoeft. pages. @article{osti_, title = {FTWORK: A three-dimensional groundwater flow and solute transport code}, author = {Faust, C R and Sims, P N and Spalding, C P and Andersen, P F and Stephenson, D E}, abstractNote = {The three-dimensional, finite-difference model, FTWORK, may be used to simulate groundwater flow and solute transport processes in fully saturated porous media.

L.F. Konikow, and J.D. Bredehoeft, Computer model of two-dimensional solute transport and dispersion in groundwater. U.S. Geological Survey Techniques of Water Resources Investigations. Book 7, Automated Data Processing and Computation, Chapter C2, Cited by: 2. MOCGRAF is a menu-driven graphics program specifically designed for use with MOC, the USGS "Computer Model of Two-dimensional Solute Transport and Dispersion in Ground Water." MOCGRAF can generate two-dimensional contour plots of ending concentrations and heads for each time step and pumping period of the simulation.

Finite difference model for aquifer simulation in two dimensions with results of numerical experiments, by P.C. Trescott, G.F. Pinder, and S.P. Larson. pages. Computer model of two-dimensional solute transport and dispersion in ground water, by L.F.

Konikow and J.D. Bredehoeft. 90 pages. The mathematical model of solute transport and dispersion of Koni Kow & Bredehoeft () has been modified so that density- difference effects can be taken into account.Role of numerical simulation in analysis of ground-water quality problems Mountain Arsenal, Colorado, U.S.

Geol. Surv. Water-Supply Paper, 43 pp. 11 L.F. Konikow and J.D. Bredehoeft, Computer model of two-dimensional solute transport and dispersion in ground water, U.S.

Geological Survey Techniques of Water-Resources Inv., Book 7.HST3D ( Win32) - Computer code for simulation of heat and solute transport in three-dimensional groundwater flow systems. JUPITER API - The Joint Universal Parameter IdenTification and Evaluation of Reliability Application Programming Interface.

MOC ()- Two-dimensional method-of-characteristics ground-water flow and transport model.