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Type: | Resource | |
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Created: | Feb 08, 2023 at 4:08 p.m. | |
Last updated: | Feb 08, 2023 at 4:08 p.m. | |
Citation: | See how to cite this resource |
Sharing Status: | Public |
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Views: | 532 |
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Abstract
A three-dimensional fractured medium flow model was developed for the Bear Creek Valley (BCV) S-3 site of the Oak Ridge Reservation (ORR) using SWIFT III. The numerical modeling for this site focused on a conceptual model established through the analysis of heterogeneous geologic units and matrix fracture properties of the subsurface in the BCV area. The SWIFT III modeling analysis was based on the previous modeling studies that used MODFLOW and MODPATH. A rigorous calibration was obtained first by comparing simulated results with the existing data on ground water levels and then by comparing pumping test results with the simulated ground water levels. A satisfactory agreement between observed and simulated results was obtained. The calibrated model was used to determine sustained yield from a ground water interceptor trench. Different withdrawal rates were used to simulate the performance of the trench for the sustained withdrawal of ground water.
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Additional Metadata
Name | Value |
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DOI | 10.1111/j.1752-1688.2003.tb03697.x |
Depth | |
Scale | 11 - 101 km² |
Layers | 5 |
Purpose | Groundwater contamination |
GroMoPo_ID | 339 |
IsVerified | True |
Model Code | MODFLOW;SWIFT III |
Model Link | https://doi.org/10.1111/j.1752-1688.2003.tb03697.x |
Model Time | SS |
Model Year | 2003 |
Model Authors | Ahmed, S; Khan, A; Salpas, P |
Model Country | United States |
Data Available | Report/paper only |
Developer Email | NA |
Dominant Geology | Siliciclastic sedimentary (sandstones, shales) |
Developer Country | USA |
Publication Title | Development of a fractured medium flow model for a waste site |
Original Developer | No |
Additional Information | |
Integration or Coupling | Solute transport |
Evaluation or Calibration | Static water levels |
Geologic Data Availability | No |
How to Cite
This resource is shared under the Creative Commons Attribution CC BY.
http://creativecommons.org/licenses/by/4.0/
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