Journal of Jilin University(Earth Science Edition) ›› 2021, Vol. 51 ›› Issue (4): 1182-1192.doi: 10.13278/j.cnki.jjuese.20200047

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Spatio-Temporal Heterogeneity and Driving Factors of Land Subsidence in Middle-Lower Part of Chaobai River Alluvial Fan

Cheng Rui1,2,3,4, Zhu Lin1,2,3,4, Zhou Jiahui1,2,3,4, Guo Gaoxuan5, Guo Lin1,2,3,4, Li Huijun1,2,3,4, Chen Beibei1,2,3,4   

  1. 1. College of Resource Environment and Tourism, Capital Normal University, Beijing 100048, China;
    2. Beijing Laboratory of Water Resources Security, Capital Normal University, Beijing 100048, China;
    3. Key Laboratory of Land Subsidence Mechanism, Prevention and Control (Capital Normal University), Ministry of Education, Beijing 100048, China;
    4. Laboratory Cultivation Base of Environment Process and Digital Simulation, Beijing 100048, China;
    5. Beijing Institute of Hydrogeology and Engineering Geology, Beijing 100037, China
  • Received:2020-04-28 Online:2021-07-26 Published:2021-08-02
  • Supported by:
    Supported by Beijing Natural Science Foundation(8202008), Beijing Outstanding Young Scientist Program (BJJWZYJH01201910028032), Scientific and Technological Innovation Service Capacity Building-the Basic Scientific Research Business Cost (01119530050175) and the General Project of Science and Technology Plan of Beijing Municipal Commission of Education (KM202010028011)

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Abstract: To study the spatio-temporal distribution pattern and mechanism of land subsidence, the Chaobai River alluvial fan, a typical subsidence area in Beijing, was selected as the study area, and the spatial heterogeneity and the driving factors of land subsidence were analyzed by using PS-InSAR, global and local moran indices, and geographic detectors. The results showed that the temporal and spatial distribution characteristics of land subsidence in the study area from January 2017 to January 2019 were mainly general subsidence, the subsidence rate was[-133,3] mm/a, and the maximum cumulative subsidence was 261 mm. It was slightly distributed in the north, more severe in the middle, and lighter in the south. The severe and extremely severe land subsidence mainly occurred in eastern Houshayu of Shunyi and Lucheng town at the junction of the middle and lower parts. The land subsidence in different areas presents different spatial heterogeneity, that is, the uneven distribution characteristics are obvious. The middle and lower parts show low-low agglomeration characteristics. Different driving factors of land subsidence are different under different distribution characteristics. The main driving factors in the middle part are the groundwater level change in the second confined aquifer and the thickness of the compressible layers, while the driving factors in the lower part are the groundwater level change in the shallow groundwater and the groundwater level change in the first confined aquifer. This study suggestes that Moran index can be used to effectively analyze the spatial heterogeneity of land subsidence and identify the characteristics of agglomeration, and the geographic detector can be used to find out the causes of spatial heterogeneity of land subsidence and obtain the main driving factors. This study also provides data support and reference for the prevention and control of land subsidence in different hydrogeological units.

Key words: land subsidence, spatial heterogeneity, Moran index, geographical detector, driving factor, Chaobai River

CLC Number: 

  • P642.26
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