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| Created: | Feb 07, 2023 at 7:10 p.m. | |
| Last updated: | Feb 07, 2023 at 7:11 p.m. | |
| Citation: | See how to cite this resource |
| Sharing Status: | Public |
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Abstract
A multicell groundwater model was constructed to investigate the potential improvement in the modelling of karstic aquifers by using a mixed equation suitable for both the free surface and pressure flow conditions in karstic conduits. To estimate the model parameters the shuffled complex evolution (SCE) optimisation method was used. This ensured a fast and objective model calibration. The model was applied to two real-world karstic aquifers and it became clear that in case of absence of water level measurements, the use of the mixed equation did not improved the performance. In cases where both spring discharge and water level measurements were available, the use of the mixed equation proved to be advantageous in reproducing the features of the observed time series especially of the water level. (c) 2005 Elsevier B.V. All rights reserved.
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Additional Metadata
| Name | Value |
|---|---|
| DOI | 10.1016/j.jhydrol.2005.10.021 |
| Depth | |
| Scale | |
| Layers | |
| Purpose | 3D Karstic Flow Model |
| GroMoPo_ID | 94 |
| IsVerified | True |
| Model Code | 3dkflow |
| Model Link | https://doi.org/10.1016/j.jhydrol.2005.10.021 |
| Model Time | |
| Model Year | 2006 |
| Model Authors | E. Rozos, D. Koutsoyiannis |
| Model Country | Greece |
| Data Available | Report/paper only |
| Developer Email | rozos@itia.ntua.gr |
| Dominant Geology | Carbonate (including karst) |
| Developer Country | Greece |
| Publication Title | A multicell karstic aquifer model with alternative flow equations |
| Original Developer | No |
| Additional Information | 3dkflow was built and used for hydrological simulations in karstic catchments |
| Integration or Coupling | MODFLOW |
| Evaluation or Calibration | Shuffled complex evolution (SCE) and mix of spring discharge and water level measurements |
| Geologic Data Availability |
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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