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 1.7 KB | |
| Created: | Feb 08, 2023 at 2:22 p.m. | |
| Last updated: | Feb 08, 2023 at 2:22 p.m. | |
| Citation: | See how to cite this resource |
| Sharing Status: | Public |
|---|---|
| Views: | 275 |
| Downloads: | 189 |
| +1 Votes: | Be the first one to this. |
| Comments: | No comments (yet) |
Abstract
Ground water flow modeling in a karst aquifer presents many difficulties. In particular, the hydrodynamic properties and the now behavior can vary over time. History matching of transient-state conditions is required to test the accuracy of the model under varying hydrodynamic conditions. The objective of this study was to illustrate how transient-state conditions can be used to history match a ground water flow model of a large aquifer, the La Rochefoucauld karst (Charente, France). The model used a porous medium equivalent and was based on a steady-state calibration of hydraulic conductivities. The history match consisted of studying the simulated heads and spring flow rates to test the capacity of the model to reproduce different aspects of the aquifer behavior, The simulated heads and flow rates were analyzed as new data using correlation and spectral analyses to compare the temporal structures of the measured and simulated time series. The analyses provided information on the storage capacity of the aquifer, the input-output delays, the degree of correlation between input and output, and the length of the impulse response of the aquifer, These data were used to study the impact of the hypotheses underlying the model (hydraulic conductivities, storage coefficient, representation of rivers, use of a porous medium equivalent). The results show that the model adequately simulates the overall behavior of the studied aquifer, The model can be used under variable hydrodynamic conditions to simulate ground water flow on a regional scale. This case study illustrates how a complete history match of a simplified representation of reality can lead to an adequate mathematical tool.
Subject Keywords
Coverage
Spatial
Content
Additional Metadata
| Name | Value |
|---|---|
| DOI | 10.1111/j.1745-6584.2000.tb00694.x |
| Depth | |
| Scale | 101 - 1 000 km² |
| Layers | |
| Purpose | Scientific investigation (not related to applied problem) |
| GroMoPo_ID | 265 |
| IsVerified | True |
| Model Code | GMS;HPP-GMS |
| Model Link | https://doi.org/10.1111/j.1745-6584.2000.tb00694.x |
| Model Time | 1994-1995 |
| Model Year | 2000 |
| Model Authors | Larocque, M; Banton, O; Razack, M |
| Model Country | France |
| Data Available | Report/paper only |
| Developer Email | NA |
| Dominant Geology | Carbonate (including karst) |
| Developer Country | France; Canada |
| Publication Title | Transient-state history matching of a karst aquifer ground water flow model |
| Original Developer | No |
| Additional Information | This study iis sued to illustrate the use of transient-state conditions for history matching using groundwater flow modeling of a karst aquifer in the La Rochefoucauld karst in Charente, France. |
| Integration or Coupling | None of the above |
| Evaluation or Calibration | Static water levels;Baseflow |
| 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