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Type: | Resource | |
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Created: | Feb 08, 2023 at 1:47 p.m. | |
Last updated: | Feb 08, 2023 at 1:48 p.m. | |
Citation: | See how to cite this resource |
Sharing Status: | Public |
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Views: | 540 |
Downloads: | 213 |
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Abstract
This paper demonstrates that analytic element models have potential as powerful screening tools that can facilitate or improve calibration of more complicated finite-difference and finite-element models. We demonstrate how a two-dimensional analytic element model was used to identify errors in a complex three-dimensional finite difference model caused by incorrect specification of boundary conditions. An improved finite-difference model was developed using boundary conditions developed from a far-field analytic element model. Calibration of a revised finite-difference model was achieved using fewer zones of hydraulic conductivity and lake bed conductance than the original finite-difference model, Calibration statistics were also improved in that simulated base-flows were much closer to measured values. The improved calibration is due mainly to improved specification of the boundary conditions made possible by first solving the far-field problem with an analytic element model.
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Additional Metadata
Name | Value |
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DOI | 10.1111/j.1745-6584.1998.tb02108.x |
Depth | 53 |
Scale | 11 - 101 km² |
Layers | 5 |
Purpose | Scientific investigation (not related to applied problem) |
GroMoPo_ID | 244 |
IsVerified | True |
Model Code | MODFLOW |
Model Link | https://doi.org/10.1111/j.1745-6584.1998.tb02108.x |
Model Time | 1991 |
Model Year | 1998 |
Model Authors | Hunt, RJ; Anderson, MP; Kelson, VA |
Model Country | United States |
Data Available | Report/paper only |
Developer Email | rjhunt@usgs.gov; andy@geology.wisc.edu; vkelson@indiana.edu |
Dominant Geology | Unconsolidated sediments |
Developer Country | USA |
Publication Title | Improving a complex finite-difference ground water flow model through the use of an analytic element screening model |
Original Developer | No |
Additional Information | Paper shows that analytical element models can be initially used to improve complex finite-difference models. |
Integration or Coupling | None of the above |
Evaluation or Calibration | Dynamic 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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