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| Type: | Resource | |
| Storage: | The size of this resource is 1.7 KB | |
| Created: | Feb 08, 2023 at 1:54 p.m. | |
| Last updated: | Feb 08, 2023 at 1:55 p.m. | |
| Citation: | See how to cite this resource |
| Sharing Status: | Public |
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| Views: | 340 |
| Downloads: | 187 |
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Abstract
The groundwater pollution case at Mercier is a very complex one. Groundwater flow modeling has been a valuable tool in the assessment of this large environmental problem. However, due to the complexity of the hydrogeological setting, the modeling has been performed with various simple case models in lieu of a large complex model. Here we report the results of one of these piecewise modeling tasks that proved very useful in the explanation of the strong upward gradients observed in the bedrock aquifer. These results and their interpretation prove the usefulness of the piecewise modeling strategy in this case.
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Additional Metadata
| Name | Value |
|---|---|
| DOI | 10.1139/t92-076 |
| Depth | 60 |
| Scale | Other |
| Layers | 6 |
| Purpose | Scientific investigation (not related to applied problem) |
| GroMoPo_ID | 246 |
| IsVerified | True |
| Model Code | Galerkin weighting method with a network of first-order triangular elements to numerically resolve the Laplace equation |
| Model Link | https://doi.org/10.1139/t92-076 |
| Model Time | SS |
| Model Year | 1992 |
| Model Authors | ISABEL, D; GELINAS, P; LOCAT, J |
| Model Country | Canada |
| Data Available | Report/paper only |
| Developer Email | NA |
| Dominant Geology | Unconsolidated sediments |
| Developer Country | Canada |
| Publication Title | USE OF A GROUNDWATER-FLOW MODEL TO EXPLAIN STRONG UPWARD GRADIENTS IN ROCK FORMATION UNDERNEATH THE MERCIER SITE |
| Original Developer | No |
| Additional Information | Numerical modeling of a complex hydrogeologic site near Montreal, Canada in order to explain strong upward hydraulic gradients. |
| Integration or Coupling | None of the above |
| 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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