GroMoPo Metadata for Daxing Beijing Model
Authors: | |
---|---|
Owners: | gromopo_admin |
Type: | Resource |
Storage: | The size of this resource is 1.5 KB |
Created: | Feb 08, 2023 at 3:25 p.m. |
Last updated: | Feb 08, 2023 at 3:25 p.m. |
Citation: | See how to cite this resource |
Sharing Status: | Public |
---|---|
Views: | 694 |
Downloads: | 232 |
+1 Votes: | Be the first one to this. |
Comments: | No comments (yet) |
Abstract
The use of groundwater flow models is prevalent in the field of environmental hydrogeology. Models have been applied to investigate a wide variety of hydrogeological conditions. Recently, groundwater models have been applied to predict the fate and transport of contaminants for risk evaluation purposes. In this paper, a transient groundwater flow model in Daxing district of Beijing, China was developed. The conceptual model was built by analyzing the hydrogeological data. Hydraulic conductivities have been calibrated by the steady state model. The storage coefficients are calibrated by the transient model based on the available data observed from 1995 to 2000, which provides insights to understand the dynamic behavior of groundwater systems and to predict spatial-temporal distributions of groundwater levels in responding to changes. The model results help to identify the aquifer properties and to analyze the groundwater flow dynamics, the changes of groundwater levels, in addition, the improvement of the groundwater level monitoring network will be proposed through the analysis of groundwater levels. The calibrated transient model will be used later to predict the impacts of water resources management schemes on groundwater in the study area. (C) 2011 Published by Elsevier Ltd. Selection and/or peer-review under responsibility of the organizing committee of 2nd International Conference on Advances in Energy Engineering (ICAEE).
Subject Keywords
Coverage
Spatial












Content
Additional Metadata
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