Articles | Volume 382
https://doi.org/10.5194/piahs-382-291-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/piahs-382-291-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Analysis of land subsidence changes on the Beijing Plain from 2004 to 2015
Lin Guo
College of Resource Environment and Tourism, Capital Normal
University, Beijing 100048, China
Beijing Laboratory of Water Resources Security, Capital Normal
University, Beijing 100048, China
Huili Gong
CORRESPONDING AUTHOR
College of Resource Environment and Tourism, Capital Normal
University, Beijing 100048, China
Beijing Laboratory of Water Resources Security, Capital Normal
University, Beijing 100048, China
Xiaojuan Li
College of Resource Environment and Tourism, Capital Normal
University, Beijing 100048, China
Beijing Laboratory of Water Resources Security, Capital Normal
University, Beijing 100048, China
College of Resource Environment and Tourism, Capital Normal
University, Beijing 100048, China
Beijing Laboratory of Water Resources Security, Capital Normal
University, Beijing 100048, China
Wei Lv
Chinese Academy of Calligraphy Culture, Capital Normal University,
Beijing 100048, China
Mingyuan Lyu
College of Resource Environment and Tourism, Capital Normal
University, Beijing 100048, China
Beijing Laboratory of Water Resources Security, Capital Normal
University, Beijing 100048, China
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Land subsidence is a serious geo-hazard in Beijing Plain, which has threatened the safety of the operation of the metropolis. This study derived the vertical and the East-West deformation, and the spatial variation and the impact factors of the vertical and the East-West deformation were analyzed. It found that the extraction of groundwater is the dominant factor affecting the spatial distribution of the vertical displacement, while the dominant factor of East-West deformation is not obvious.
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The earth fissures of geological structure are visualized in three dimensional domains through a volumetric modeling method. The topological relations between TIN, triangular prism and lines are constructed for further spatial calculation. This method can facilitate the mechanism for studying fissures.
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