Checking for non-preferred file/folder path names (may take a long time depending on the number of files/folders) ...
This resource contains some files/folders that have non-preferred characters in their name. Show non-conforming files/folders.
This resource contains content types with files that need to be updated to match with metadata changes. Show content type files that need updating.
Authors: |
|
|
---|---|---|
Owners: |
|
This resource does not have an owner who is an active HydroShare user. Contact CUAHSI (help@cuahsi.org) for information on this resource. |
Type: | Resource | |
Storage: | The size of this resource is 1.6 KB | |
Created: | Feb 08, 2023 at 2:09 p.m. | |
Last updated: | Feb 08, 2023 at 2:09 p.m. | |
Citation: | See how to cite this resource |
Sharing Status: | Public |
---|---|
Views: | 554 |
Downloads: | 211 |
+1 Votes: | Be the first one to this. |
Comments: | No comments (yet) |
Abstract
The construction of 3D hydrogeological models for unconsolidated sedimentary aquifers remains particularly challenging, especially in Quaternary deposits. Simplifications at small or large scale are part of groundwater flow modeling and are often required due on the usual inherent complexity of the stratigraphic systems. This study analyzes the effects of hydrostratigraphic simplifications on the accuracy of 3D numerical groundwater flow models. Such investigation is conducted from an initial detailed model of an aquifer located in the Saguenay-Lac-St-Jean region in Canada and the considered simplifications are based on using the equivalent hydraulic conductivity concept. Different levels or approaches of simplification are applied to numerical simulated models and the results of the different scenarios are compared. A root mean square (RMS) calibration result of 3.79 m on the groundwater levels is obtained for the most detailed model, while the RMS ranges between 4.01 and 4.83 m with the simplified models. Such results illustrate a gain obtained in the calibration of the model with increasing level of hydrostratigraphic details, but that this gain is relatively limited. The proposed methodology for simplifying the hydrostratigraphic settings could be used by hydrogeological modellers for a wide variety of aquifers constituted of sedimentary granular material.
Subject Keywords
Coverage
Spatial
Content
Additional Metadata
Name | Value |
---|---|
DOI | 10.1007/s12665-015-4439-y |
Depth | 44 |
Scale | 101 - 1 000 km² |
Layers | 5 |
Purpose | Groundwater resources;Scientific investigation (not related to applied problem) |
GroMoPo_ID | 256 |
IsVerified | True |
Model Code | Feflow |
Model Link | https://doi.org/10.1007/s12665-015-4439-y |
Model Time | SS |
Model Year | 2015 |
Model Authors | Hudon-Gagnon, E; Chesnaux, R; Cousineau, PA; Rouleau, A |
Model Country | Canada |
Data Available | Report/paper only |
Developer Email | romain_chesnaux@uqac.ca |
Dominant Geology | Unconsolidated sediments |
Developer Country | Canada |
Publication Title | A hydrostratigraphic simplification approach to build 3D groundwater flow numerical models: example of a Quaternary deltaic deposit aquifer |
Original Developer | No |
Additional Information | |
Integration or Coupling | |
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/
Comments
There are currently no comments
New Comment