Groundwater-flow model for the Wood River Valley aquifer system, south-central Idaho
Links
- Document: Report (10 MB pdf)
- Appendixes:
- Appendix A (2.2 MB pdf) An Introduction to the R-Package ‘wrv’
- Appendix B (525 KB pdf) Manual for Functions and Datasets in the R-Package ‘wrv’
- Appendix C (6.9 MB pdf) Creating Datasets for the R-Package ‘wrv’
- Appendix D (11 MB pdf) Uncalibrated Groundwater-Flow Model for the Wood River Valley Aquifer System, South-Central Idaho
- Appendix E (6.8 MB pdf) Tributary Basin Underflow into the Wood River Valley Aquifer System, South-Central Idaho
- Appendix F (8.5 MB pdf) Natural Groundwater Recharge and Discharge in the Wood River Valley Aquifer System, South-Central Idaho
- Appendix G (15 MB pdf) Incidental Groundwater Recharge and Pumping Demand in the Wood River Valley Aquifer System, South-Central Idaho
- Appendix H (9 MB pdf) Calibration of the Wood River Valley Groundwater Flow Model
- Companion Files:
- Download citation as: RIS | Dublin Core
Abstract
A three-dimensional numerical model of groundwater flow was developed for the Wood River Valley (WRV) aquifer system, Idaho, to evaluate groundwater and surface-water availability at the regional scale. This mountain valley is located in Blaine County and has a drainage area of about 2,300 square kilometers (888 square miles). The model described in this report can serve as a tool for water-rights administration and water-resource management and planning. The model was completed with support from the Idaho Department of Water Resources, and is part of an ongoing U.S. Geological Survey effort to characterize the groundwater resources of the WRV. A highly reproducible approach was taken for constructing the WRV groundwater-flow model. The collection of datasets, source code, and processing instructions used to construct and analyze the model was distributed as an R statistical-computing and graphics package.
Flow in the WRV aquifer was simulated using the MODFLOW-USG groundwater flow model. The transient flow model simulates groundwater flow between 1995 and 2010. The model uses a 100-meter (328-feet) uniform grid spacing with 54,922 active model cells distributed over three model layers. A confining unit in the south-central part of the Bellevue fan necessitated the use of a multi-layer model. Specified-flow boundaries were used to simulate the groundwater inflows from each of the major tributary basins (also known as tributary basin underflow) and the areal recharge of precipitation and applied irrigation. Head‑dependent flow boundaries were used to simulate the stream-aquifer flow exchange in river reaches and the groundwater discharge at the outlet boundaries of Stanton Crossing and Silver Creek. The model was calibrated by adjusting aquifer hydraulic properties to match simulated and measured water levels and stream-aquifer flow exchange, using the parameter-estimation program PEST. The model reasonably simulated the measured water-table elevation, orientation, and gradients. Stream-aquifer flow exchange along river reaches also was reasonably simulated by the model.
Inflow into the WRV aquifer system originates from three sources (from largest to smallest):
- Streamflow loss from the Big Wood River and Silver Creek,
- Areal recharge of precipitation and applied irrigation, and
- Tributary basin underflow.
Outflow from the WRV aquifer system originates from five sources (from largest to smallest):
- Aquifer discharge into the Big Wood River and Silver Creek,
- Production-well pumping,
- Discharge across the water table into the vadose zone,
- Subsurface outflow beneath Silver Creek near Picabo, and
- Subsurface outflow beneath the Big Wood River near Stanton Crossing.
Temporal changes in aquifer storage are most affected by areal recharge and groundwater pumping, and also contribute to changes in streamflow gains.
Suggested Citation
Fisher, J.C., Bartolino, J.R., Wylie, A.H., Sukow, Jennifer, and McVay, Michael, 2016, Groundwater-flow model of the Wood River Valley aquifer system, south-central Idaho: U.S. Geological Survey Scientific Investigations Report 2016–5080, 71 p., http://dx.doi.org/10.3133/sir20165080.
ISSN: 2328-0328 (online)
Study Area
Table of Contents
- Abstract
- Introduction
- Description of Groundwater-Flow System
- Calibrated Groundwater Flow Model
- Model Limitations and Suggestions for Future Work
- Summary
- References Cited
- Appendixes A-H
Publication type | Report |
---|---|
Publication Subtype | USGS Numbered Series |
Title | Groundwater-flow model for the Wood River Valley aquifer system, south-central Idaho |
Series title | Scientific Investigations Report |
Series number | 2016-5080 |
DOI | 10.3133/sir20165080 |
Year Published | 2016 |
Language | English |
Publisher | U.S. Geological Survey |
Publisher location | Reston, VA |
Contributing office(s) | Idaho Water Science Center |
Description | Report: viii, 71 p.; Appendixes A-H; Model Archive; Data Repository |
Country | United States |
State | Idaho |
Other Geospatial | Wood River Valley |
Online Only (Y/N) | Y |
Additional Online Files (Y/N) | N |
Google Analytic Metrics | Metrics page |