|Table of Contents|

Present-day Surface Subsidence Using Jointed InSAR Observations and Groundwater Numerical Modeling—A Case Study in Sanyuan Area of Shaanxi, China(PDF)

《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

Issue:
2025年第02期
Page:
274-284
Research Field:
大地测量、遥感与地学大数据
Publishing date:

Info

Title:
Present-day Surface Subsidence Using Jointed InSAR Observations and Groundwater Numerical Modeling—A Case Study in Sanyuan Area of Shaanxi, China
Author(s):
CAO Xi-yu1 GE Wei-peng12* ZHANG Bo1 ZHU Jun-wen1 PING Zi-fei1
(1. Lanzhou Institute of Seismology, China Earthquake Administration, Lanzhou 730000, Gansu, China; 2. Lanzhou National Geophysical Observation and Research Station, Lanzhou 730000, Gansu, China)
Keywords:
groundwater surface subsidence Sentinel-1A satellite InSAR technology numerical modeling MODFLOW software Guanzhong Basin
PACS:
P237; P641.2
DOI:
10.19814/j.jese.2024.02003
Abstract:
Groundwater exploitation and recharge in sedimentary basins can cause changes in the groundwater level of the basins, resulting in surface subsidence and uplift in the basins, and causing geologic hazards such as wide-scale geologic fissures and subsidence in the basins. In order to find the connection between groundwater level change and surface subsidence disaster in Guanzhong Basin, the up-orbit SAR data of Sentinel-1A satellite from 2015 to 2022 were processed to reveal the spatial and temporal distribution characteristics of regional surface deformation; the surface subsidence in the city area of Sanyuan county, Shaanxi province, which was surrounded by multiple active fractures, was significant, so the groundwater simulation was carried out by MODFLOW software to analyze the feedback mechanism of groundwater level change on surface subsidence. The results show that the deformation of surface subsidence in the study area is affected by the change of groundwater level, and the regional active fracture plays a role in blocking the distribution and flow of groundwater; InSAR technology combined with MODFLOW software can identify the groundwater level changes caused by groundwater mining and extraction and the resulting regional surface subsidence phenomenon, and contribute to explore the mechanism of surface subsidence disaster occurrence in sedimentary basins.

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