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GroMoPo Metadata for Beijing Mihuaishun plain GISFEFLOW model

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Created: Feb 08, 2023 at 3:51 a.m.
Last updated: Feb 08, 2023 at 3:52 a.m.
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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.

Subject Keywords



Coordinate System/Geographic Projection:
WGS 84 EPSG:4326
Coordinate Units:
Decimal degrees
Place/Area Name:
North Latitude
East Longitude
South Latitude
West Longitude


Additional Metadata

Name Value
DOI 10.1088/1755-1315/330/5/052037
Scale 101 - 1 000 km²
Purpose Groundwater resources
GroMoPo_ID 183
IsVerified True
Model Code Feflow
Model Link
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
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

GroMoPo, D. Kretschmer (2023). GroMoPo Metadata for Beijing Mihuaishun plain GISFEFLOW model, HydroShare,

This resource is shared under the Creative Commons Attribution CC BY.


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