Since “Groundwater and surface water–A single resource”: some U.S. Geological Survey advances in modeling groundwater/surface-water interactions
Daniel T. Feinstein
2012, Acque Sotterranee: Italian Journal of Groundwater (1) 9-24
Field and interpretive studies conducted by T.C. Winter and U.S. Geological Survey colleagues, and summarized in the 1998 publication “Groundwater and Surface Water – A Single Resource”, inspired a new generation of research centered on extensions of the groundwater-flow code MODFLOW to more sophisticated simulation of coupled...
User guide for MODPATH version 6—A particle-tracking model for MODFLOW
David W. Pollock
2012, Techniques and Methods 6-A41
MODPATH is a particle-tracking post-processing model that computes three-dimensional flow paths using output from groundwater flow simulations based on MODFLOW, the U.S. Geological Survey (USGS) finite-difference groundwater flow model. This report documents MODPATH version 6. Previous versions were documented in USGS Open-File Reports 89-381 and 94-464. The program uses a...
Groundwater flow and water budget in the surficial and Floridan aquifer systems in east-central Florida
Nicasio Sepulveda, Claire R. Tiedeman, Andrew M. O’Reilly, Jeffery B. Davis, Patrick Burger
2012, Open-File Report 2012-1132
A numerical transient model of the surficial and Floridan aquifer systems in east-central Florida was developed to (1) increase the understanding of water exchanges between the surficial and the Floridan aquifer systems, (2) assess the recharge rates to the surficial aquifer system from infiltration through the unsaturated zone and (3)...
Groundwater simulation and management models for the upper Klamath Basin, Oregon and California
Marshall W. Gannett, Brian J. Wagner, Kenneth E. Lite Jr.
2012, Scientific Investigations Report 2012-5062
The upper Klamath Basin encompasses about 8,000 square miles, extending from the Cascade Range east to the Basin and Range geologic province in south-central Oregon and northern California. The geography of the basin is dominated by forested volcanic uplands separated by broad interior basins. Most of the interior basins once...
Preliminary investigation of the effects of sea-level rise on groundwater levels in New Haven, Connecticut
David M. Bjerklie, John R. Mullaney, Janet Radway Stone, Brian J. Skinner, Matthew A. Ramlow
2012, Open-File Report 2012-1025
Global sea level rose about 0.56 feet (ft) (170 millimeters (mm)) during the 20th century. Since the 1960s, sea level has risen at Bridgeport, Connecticut, about 0.38 ft (115 mm), at a rate of 0.008 ft (2.56 mm + or - 0.58 mm) per year. With regional subsidence, and with...
Simulation of groundwater conditions and streamflow depletion to evaluate water availability in a Freeport, Maine, watershed
Martha G. Nielsen, Daniel B. Locke
2012, Scientific Investigations Report 2011-5227
In order to evaluate water availability in the State of Maine, the U.S. Geological Survey (USGS) and the Maine Geological Survey began a cooperative investigation to provide the first rigorous evaluation of watersheds deemed "at risk" because of the combination of instream flow requirements and proportionally large water withdrawals. The...
RIP-ET: A riparian evapotranspiration package for MODFLOW-2005
Thomas Maddock III, Kathryn J. Baird, R. T. Hanson, Wolfgang Schmid, Hoori Ajami
2012, Techniques and Methods 6-A39
A new evapotranspiration package for the U.S. Geological Survey's groundwater-flow model, MODFLOW, is documented. The Riparian Evapotranspiration Package (RIP-ET) provides flexibility in simulating riparian and wetland transpiration not provided by the Evapotranspiration (EVT) or Segmented Function Evapotranspiration (ETS1) Packages for MODFLOW 2005. This report describes how the RIP-ET package was...
On modeling weak sinks in MODPATH
Daniel B. Abrams, Henk Haitjema, Leon J. Kauffman
2012, Ground Water (51) 597-602
Regional groundwater flow systems often contain both strong sinks and weak sinks. A strong sink extracts water from the entire aquifer depth, while a weak sink lets some water pass underneath or over the actual sink. The numerical groundwater flow model MODFLOW may allow a sink cell to act as...
Evaluation of MODFLOW-LGR in connection with a synthetic regional-scale model
T.N. Vilhelmsen, S. Christensen, Steffen W. Mehl
2012, Ground Water (50) 118-132
This work studies costs and benefits of utilizing local‐grid refinement (LGR) as implemented in MODFLOW‐LGR to simulate groundwater flow in a buried tunnel valley interacting with a regional aquifer. Two alternative LGR methods were used: the shared‐node (SN) method and the ghost‐node (GN) method. To conserve flows the SN method...
MT3DMS: Model use, calibration, and validation
C. Zheng, Mary C. Hill, G. Cao, R. Ma
2012, Transactions of the ASABE (55) 1549-1559
MT3DMS is a three-dimensional multi-species solute transport model for solving advection, dispersion, and chemical reactions of contaminants in saturated groundwater flow systems. MT3DMS interfaces directly with the U.S. Geological Survey finite-difference groundwater flow model MODFLOW for the flow solution and supports the hydrologic and discretization features of MODFLOW. MT3DMS contains...
Modifications to the conduit flow process mode 2 for MODFLOW-2005
Thomas Reimann, S. Birk, C. Rehrl, W. Barclay Shoemaker
2012, Ground Water (50) 144-148
As a result of rock dissolution processes, karst aquifers exhibit highly conductive features such as caves and conduits. Within these structures, groundwater flow can become turbulent and therefore be described by nonlinear gradient functions. Some numerical groundwater flow models explicitly account for pipe hydraulics by coupling the continuum model with...
MODFLOW-NWT – Robust handling of dry cells using a Newton Formulation of MODFLOW-2005
Randal J. Hunt, Daniel T. Feinstein
2012, Ground Water (50) 659-663
The first versions of the widely used groundwater flow model MODFLOW (McDonald and Harbaugh 1988) had a sure but inflexible way of handling unconfined finite-difference aquifer cells where the water table dropped below the bottom of the cell—these "dry cells" were turned inactive for the remainder of the simulation. Problems...
MODFLOW-style parameters in underdetermined parameter estimation
Marco D. D’Oria, Michael N. Fienen
2012, Groundwater (50) 149-153
In this article, we discuss the use of MODFLOW-Style parameters in the numerical codes MODFLOW_2005 and MODFLOW_2005-Adjoint for the definition of variables in the Layer Property Flow package. Parameters are a useful tool to represent aquifer properties in both codes and are the only option available in the adjoint version. Moreover, for overdetermined parameter...
Comment on “An unconfined groundwater model of the Death Valley Regional Flow System and a comparison to its confined predecessor” by R.W.H. Carroll, G.M. Pohll and R.L. Hershey [Journal of Hydrology 373/3–4, pp. 316–328]
Claudia C. Faunt, Alden M. Provost, Mary C. Hill, Wayne R. Belcher
2011, Journal of Hydrology (397) 306-309
Carroll et al. (2009) state that the United States Geological Survey (USGS) Death Valley Regional Flow System (DVRFS) model, which is based on MODFLOW, is “conceptually inaccurate in that it models an unconfined aquifer as a confined system and does not simulate unconfined drawdown in transient pumping simulations.” Carroll et...
Programming PHREEQC calculations with C++ and Python a comparative study
Scott R. Charlton, David L. Parkhurst, Mike Muller
2011, Conference Paper, Proceedings for MODFLOW and More 2011: Integrated Hydrologic Modeling
The new IPhreeqc module provides an application programming interface (API) to facilitate coupling of other codes with the U.S. Geological Survey geochemical model PHREEQC. Traditionally, loose coupling of PHREEQC with other applications required methods to create PHREEQC input files, start external PHREEQC processes, and process PHREEQC output files. IPhreeqc eliminates...
A data-input program (MFI2005) for the U.S. Geological Survey modular groundwater model (MODFLOW-2005) and parameter estimation program (UCODE_2005)
Arien W. Harbaugh
2011, Open-File Report 2010-1057
The MFI2005 data-input (entry) program was developed for use with the U.S. Geological Survey modular three-dimensional finite-difference groundwater model, MODFLOW-2005. MFI2005 runs on personal computers and is designed to be easy to use; data are entered interactively through a series of display screens. MFI2005 supports parameter estimation using the UCODE_2005...
Simulations of groundwater flow and particle-tracking analysis in the zone of contribution to a public-supply well in San Antonio, Texas
Richard L. Lindgren, Natalie A. Houston, MaryLynn Musgrove, Lynne S. Fahlquist, Leon J. Kauffman
2011, Scientific Investigations Report 2011-5149
In 2006, a public-supply well in San Antonio, Texas, was selected for intensive study to assess the vulnerability of public-supply wells in the Edwards aquifer to contamination by a variety of compounds. A local-scale, steady-state, three-dimensional numerical groundwater-flow model was developed and used in this study to evaluate the movement...
MODFLOW-CDSS, a version of MODFLOW-2005 with modifications for Colorado Decision Support Systems
Edward R. Banta
2011, Open-File Report 2011-1213
MODFLOW-CDSS is a three-dimensional, finite-difference groundwater-flow model based on MODFLOW-2005, with two modifications. The first modification is the introduction of a Partition Stress Boundaries capability, which enables the user to partition a selected subset of MODFLOW's stress-boundary packages, with each partition defined by a separate input file. Volumetric water-budget components...
Numerical simulation of groundwater flow for the Yakima River basin aquifer system, Washington
D.M. Ely, M.P. Bachmann, J. J. Vaccaro
2011, Scientific Investigations Report 2011-5155
A regional, three-dimensional, transient numerical model of groundwater flow was constructed for the Yakima River basin aquifer system to better understand the groundwater-flow system and its relation to surface-water resources. The model described in this report can be used as a tool by water-management agencies and other stakeholders to quantitatively...
Application of the Local Grid Refinement package to an inset model simulating the interaction of lakes, wells, and shallow groundwater, northwestern Waukesha County, Wisconsin
D. T. Feinstein, C. P. Dunning, P. F. Juckem, R. J. Hunt
2011, Scientific Investigations Report 2010-5214
Groundwater use from shallow, high-capacity wells is expected to increase across southeastern Wisconsin in the next decade (2010-2020), owing to residential and business growth and the need for shallow water to be blended with deeper water of lesser quality, containing, for example, excessive levels of radium. However, this increased pumping...
Application of MODFLOW for oil reservoir simulation during the Deepwater Horizon Crisis
Paul A. Hsieh
2011, Ground Water (49) 319-323
When the Macondo well was shut in on July 15, 2010, the shut-in pressure recovered to a level that indicated the possibility of oil leakage out of the well casing into the surrounding formation. Such a leak could initiate a hydraulic fracture that might eventually breach the seafloor, resulting in...
MODPATH-LGR; documentation of a computer program for particle tracking in shared-node locally refined grids by using MODFLOW-LGR
Jesse E. Dickinson, R. T. Hanson, Steffen W. Mehl, Mary C. Hill
2011, Techniques and Methods 6-A38
The computer program described in this report, MODPATH-LGR, is designed to allow simulation of particle tracking in locally refined grids. The locally refined grids are simulated by using MODFLOW-LGR, which is based on MODFLOW-2005, the three-dimensional groundwater-flow model published by the U.S. Geological Survey. The documentation includes brief descriptions of...
Geohydrology, simulation of regional groundwater flow, and assessment of water-management strategies, Twentynine Palms area, California
Zhen Li, Peter Martin
2011, Scientific Investigations Report 2010-5249
The Marine Corps Air Ground Combat Center (MCAGCC) Twentynine Palms, California, overlies the Surprise Spring, Deadman, Mesquite, and Mainside subbasins of the Morongo groundwater basin in the southern Mojave Desert. Historically, the MCAGCC has relied on groundwater pumped from the Surprise Spring subbasin to provide all of its potable water...
Numerical simulation of the groundwater-flow system in the Chambers-Clover Creek Watershed and Vicinity, Pierce County, Washington
Kenneth H. Johnson, Mark E. Savoca, Burt Clothier
2011, Scientific Investigations Report 2011-5086
A groundwater-flow model was developed to contribute to an improved understanding of water resources in the Chambers-Clover Creek Watershed. The model covers an area of about 491 square miles in western Pierce County, Washington, and is bounded to the northeast by the Puyallup River valley, to the southwest by the...
MODFLOW-LGR-Modifications to the streamflow-routing package (SFR2) to route streamflow through locally refined grids
Steffen W. Mehl, Mary C. Hill
2011, Techniques and Methods 6-A34
This report documents modifications to the Streamflow-Routing Package (SFR2) to route streamflow through grids constructed using the multiple-refined-areas capability of shared node Local Grid Refinement (LGR) of MODFLOW-2005. MODFLOW-2005 is the U.S. Geological Survey modular, three-dimensional, finite-difference groundwater-flow model. LGR provides the capability to simulate groundwater flow by using one...