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MODFLOW-NWT model used in simulation of groundwater flow and availability in the North Fork Red River aquifer, southwest Oklahoma, 1980-2013

Dates

Release Date
2017-01-01
Start Date
1980-01-01
End Date
2013-12-31
Publication Date

Citation

Smith, S.J., Ellis, J.H., Wagner, D.L., and Peterson, S.M., 2017, MODFLOW-NWT model used in simulation of groundwater flow and availability in the North Fork Red River aquifer, southwest Oklahoma, 1980-2013: U.S. Geological Survey data release, https://doi.org/10.5066/F7JQ0ZXH.

Summary

In 2017 the U.S. Geological Survey, in cooperation with the Oklahoma Water Resources Board, published a calibrated numerical groundwater-flow model and associated model documentation report that evaluated the effects of potential groundwater withdrawals on groundwater flow and availability in the North Fork Red River aquifer in southwest Oklahoma. The results of groundwater-availability scenarios run on the calibrated numerical groundwater-flow model could be used by the Oklahoma Water Resources Board to reevaluate the maximum annual yield of groundwater from the North Fork Red River aquifer in Oklahoma. The numerical groundwater-flow model was built on a hydrogeologic framework and a conceptual groundwater-flow model derived from [...]

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Attached Files

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sir2017-5098.xml
Original FGDC Metadata

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18.98 KB application/fgdc+xml
output.zip 901.01 MB application/zip
sir2017-5098Thumbnail.jpg thumbnail 113.51 KB image/jpeg
source.zip 20.97 MB application/zip
ancillary.zip 464.02 MB application/zip
model.zip 57.31 MB application/zip
georef.zip 43.51 KB application/zip
bin.zip 3.77 MB application/zip
modelgeoref.txt 1.13 KB text/plain
readme.txt 48.06 KB text/plain

Purpose

The 1973 Oklahoma Water Law (82 OK Stat § 82-1020.5) requires the Oklahoma Water Resources Board to conduct hydrologic investigations of the State’s aquifers to support a determination of the maximum annual yield (MAY) for each groundwater basin. The MAY is defined as the amount of fresh groundwater that can be withdrawn annually while ensuring a minimum 20-year life of the groundwater basin. For alluvium and terrace aquifers, the groundwater-basin-life requirement is satisfied if, after 20 years of MAY withdrawals, 50 percent of the groundwater basin retains a saturated thickness of at least 5 ft. When a MAY has been established, the amount of land owned or leased by a permit applicant determines the annual volume of water allocated to that permit applicant. The annual volume of water allocated per acre of land is known as the equal-proportionate-share (EPS) pumping rate. The Oklahoma Water Resources Board established the MAY (343,042 acre-feet per year) and EPS pumping rate (1.0 acre-foot per acre per year) for the North Fork Red River aquifer in 1981 based on hydrologic investigations by Kent (1980) and Paukstaitis (1981) that used a numerical groundwater-flow model to evaluate the effects of potential groundwater withdrawals on groundwater availability in the North Fork Red River aquifer. Every 20 years, the Oklahoma Water Resources Board is statutorily required to update the hydrologic investigation on which the MAY and EPS were based. Because 20 years have elapsed since the MAY and EPS were established, the U.S. Geological Survey, in cooperation with the Oklahoma Water Resources Board, conducted an updated hydrologic investigation and developed a calibrated numerical groundwater-flow model to evaluate the effects of potential groundwater withdrawals on groundwater flow and availability in the North Fork Red River aquifer. Groundwater-availability scenarios were performed by using the calibrated numerical groundwater-flow model to (1) estimate the EPS pumping rate that guarantees a minimum 20-, 40-, and 50-year life of the aquifer, (2) quantify the potential effects of projected well withdrawals on groundwater storage over a 50-year period, and (3) simulate the potential effects of a hypothetical (10-year) drought on groundwater storage and lake storage. The results of these groundwater-availability scenarios could be used by the Oklahoma Water Resources Board to reevaluate the maximum annual yield of groundwater from the North Fork Red River aquifer in Oklahoma. The development of the model input and output files included in this data release are documented in the U.S. Geological Survey Scientific Investigations Report 2017-5098 (https://doi.org/10.3133/sir20175098).
Image showing the model domain with active and inactive areas of the numerical groundwater-flow model for the North Fork Red River aquifer in southwest Oklahoma
Image showing the model domain with active and inactive areas of the numerical groundwater-flow model for the North Fork Red River aquifer in southwest Oklahoma

Map

Communities

  • Model Data Management Function (MDMF)

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Provenance

These data were originally released on the Water Mission Area National Spatial Data Infrastructure Node and were migrated to sciencebase.gov in 2023.

Additional Information

Identifiers

Type Scheme Key
DOI https://www.sciencebase.gov/vocab/category/item/identifier doi:10.5066/F7JQ0ZXH

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