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| Type: | Resource | |
| Storage: | The size of this resource is 1.6 KB | |
| Created: | Feb 08, 2023 at 3:51 a.m. | |
| Last updated: | Feb 08, 2023 at 3:52 a.m. | |
| Citation: | See how to cite this resource |
| Sharing Status: | Public |
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| Views: | 293 |
| Downloads: | 199 |
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Abstract
A three dimensional finite element model (FEFLOW) has been used for regional ground water flow modeling of Mihuaishun plain located in the south of Beijing, China. The numerical groundwater flow model is developed considering recharge components (precipitation infiltration, river leakage, and irrigation return flow). GIS interface is created for each source of recharge. Hydraulic conductivities and storage coefficient have been calibrated by the steady state model using the recorded data from 2007 to 2009. The model results is useful to identify the aquifer characteristics and to analyze the groundwater dynamics. The groundwater level monitoring network will be improved by analyzing groundwater levels. The future development scenarios are proposed to predict the trend changes of groundwater levels.
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Additional Metadata
| Name | Value |
|---|---|
| DOI | 10.1088/1755-1315/330/5/052037 |
| Depth | |
| Scale | 101 - 1 000 km² |
| Layers | |
| Purpose | Groundwater resources |
| GroMoPo_ID | 183 |
| IsVerified | True |
| Model Code | Feflow |
| Model Link | https://doi.org/10.1088/1755-1315/330/5/052037 |
| Model Time | |
| Model Year | 2019 |
| Model Authors | B. Ren, J. Liang, J. Dai, X. Li, T. Sun, Y. Han |
| Model Country | China |
| Data Available | Report/paper only |
| Developer Email | renborenbo1999@163.com |
| Dominant Geology | Unconsolidated sediments |
| Developer Country | China |
| Publication Title | Trend prediction of regional groundwater level with GIS-FEFLOW model in Beijing Mihuaishun plain, China |
| Original Developer | No |
| Additional Information | |
| Integration or Coupling | |
| Evaluation or Calibration | Dynamic water levels |
| 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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