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dc.contributor.advisorMaddock III, Thomasen
dc.contributor.authorRomero, Dave
dc.creatorRomero, Daveen
dc.date.accessioned2018-02-28T18:12:29Z
dc.date.available2018-02-28T18:12:29Z
dc.date.issued1996
dc.identifier.urihttp://hdl.handle.net/10150/626899
dc.description.abstractThe U.S. Geological Survey modular groundwater model (MOD FLOW) by McDonald and Harbaugh ( 1988) implements a finite-difference technique in its numerical scheme. Because of this, the spatial discretization of the flow domain in two-dimensions is limited to rectangular cells. This paper presents a package that adapts MODFLOW' s numerical scheme into a non-generalized integrated finite-difference technique which allows flow to be simulated through a curvilinear grid. The curvilinearity is discretized into piecewise linear segments which creates a two-dimensional grid with trapezoidal cells. The new model is termed MODIFD: A Modular Three-Dimensional Integrated Finite-Difference Groundwater Flow Model. The modifications made to the source code of MODFLOW are documented in Appendix A.
dc.language.isoen_USen
dc.publisherThe University of Arizona.en
dc.rightsCopyright © is held by the author. Digital access to this material is made possible by the University Libraries, University of Arizona. Further transmission, reproduction or presentation (such as public display or performance) of protected items is prohibited except with permission of the author.en
dc.titleIFD: An integrated finite-difference package for use with modflowen_US
dc.typetexten
dc.typeThesis-Reproduction (electronic)en
thesis.degree.grantorUniversity of Arizonaen
thesis.degree.levelmastersen
dc.contributor.committeememberMaddock III, Thomasen
thesis.degree.disciplineGraduate Collegeen
thesis.degree.disciplineHydrology and Water Resourcesen
thesis.degree.nameM.S.en
dc.description.noteDigitized from paper copies provided by the Department of Hydrology & Atmospheric Sciences.en
refterms.dateFOA2018-08-15T05:59:10Z
html.description.abstractThe U.S. Geological Survey modular groundwater model (MOD FLOW) by McDonald and Harbaugh ( 1988) implements a finite-difference technique in its numerical scheme. Because of this, the spatial discretization of the flow domain in two-dimensions is limited to rectangular cells. This paper presents a package that adapts MODFLOW' s numerical scheme into a non-generalized integrated finite-difference technique which allows flow to be simulated through a curvilinear grid. The curvilinearity is discretized into piecewise linear segments which creates a two-dimensional grid with trapezoidal cells. The new model is termed MODIFD: A Modular Three-Dimensional Integrated Finite-Difference Groundwater Flow Model. The modifications made to the source code of MODFLOW are documented in Appendix A.


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