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GroMoPo Metadata for Shanghai subsidence model


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Created: Feb 08, 2023 at 7:38 p.m.
Last updated: Feb 08, 2023 at 7:38 p.m.
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Abstract

Shanghai city has been suffering land subsidence caused by overly exploitation of ground water since 1921, which is a serious problem for this coastal city with altitude of 2.2-4.8m above mean sea level. The largest cumulative land subsidence amounted to 2.6m in the downtown area. Measures to decrease the ground water exploitation, change the pumping aquifers, and increase aquifer artificial recharge have been used to mitigate land subsidence since 1961. It is necessary to develop a proper numerical model to simulate and predict land subsidence. In this study, a decoupled three-dimensional (3-D) finite element land subsidence model including a 3-D ground water flow model and a 3-D geo-mechanical model was developed to simulate the 3-D deformation of the aquifer systems in the center area of Shanghai. The area of downtown Shanghai is 660 km(2), with 10 million inhabitants, dense high buildings, and 11 metro lines. The simulation spans the period from 1979 to 1995. Two different assumptions have been tested on the side boundary, i.e., precluding the three components of the displacement, or assuming a free-displacement condition. The distribution of calculated land subsidence and horizontal displacements in different aquifers was analyzed. The computed vertical displacement fitted well with the available observations. It has been verified that the two different assumptions on the lateral boundaries in the geo-mechanical model caused different results just limited on nodes close to boundary. The developed 3-D land subsidence model is reasonable and can be used to simulate and predict 3-D movement of aquifer systems in the center area of Shanghai, which could provide scientific support to local government in controlling land subsidence and differential movements of the land surface.

Subject Keywords

Coverage

Spatial

Coordinate System/Geographic Projection:
WGS 84 EPSG:4326
Coordinate Units:
Decimal degrees
Place/Area Name:
China
North Latitude
31.4849°
East Longitude
121.3042°
South Latitude
31.2173°
West Longitude
121.1136°

Content

Additional Metadata

Name Value
DOI 10.5194/piahs-372-443-2015
Depth
Scale 101 - 1 000 km²
Layers 10
Purpose Subsidence
GroMoPo_ID 378
IsVerified True
Model Code Unknown
Model Link https://doi.org/10.5194/piahs-372-443-2015
Model Time 1979-1995
Model Year 2015
Model Authors Ye, S; Luo, Y; Wu, J; Teatini, P; Wang, H; Jiao, X
Model Country China
Data Available Report/paper only
Developer Email sjye@nju.edu.cn
Dominant Geology Model focuses on multiple geologic materials
Developer Country Peoples R China; Italy
Publication Title Three dimensional numerical modeling of land subsidence in Shanghai
Original Developer No
Additional Information
Integration or Coupling
Evaluation or Calibration Dynamic water levels
Geologic Data Availability No

How to Cite

GroMoPo, D. Kretschmer (2023). GroMoPo Metadata for Shanghai subsidence model, HydroShare, http://www.hydroshare.org/resource/a88867afa25745dca4732d824009f53e

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

http://creativecommons.org/licenses/by/4.0/
CC-BY

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