Time-series evolution patterns of land subsidence in the eastern Beijing Plain, China

• Published in: Remote sensing (Basel, Switzerland) Switzerland), 2019-03, Vol.11 (5), p.539
• Main Authors: Zuo, Junjie, Gong, Huili, Chen, Beibei, Liu, Kaisi, Zhou, Chaofan, Ke, Yinghai
• Format: Article
• Language: English
• Subjects: Algorithms; Aquifers; compressible sediment layer; Entropy; Evolution; Evolutionary algorithms; Geologic depressions; Geology; Groundwater; Groundwater data; groundwater level; Groundwater levels; Hydrogeology; Interferometric synthetic aperture radar; Interferometry; Land subsidence; Permutations; Precipitation; Radarsat; Remote sensing; SDE; Spatial data; Studies; Subsidence; Time series
• ISSN: 2072-4292; 2072-4292
• DOI: 10.3390/rs11050539

Land subsidence in the Eastern Beijing Plain has a long history and is always serious. In this paper, we consider the time-series evolution patterns of the eastern of Beijing Plain. First, we use the Persistent Scatterer Interferometric Synthetic Aperture Radar (PSI) technique, with Envisat and Radarsat-2 data, to monitor the deformation of Beijing Plain from 2007 to 2015. Second, we adopt the standard deviation ellipse (SDE) method, combined with hydrogeological data, to analyze the spatial evolution patterns of land subsidence. The results suggest that land subsidence developed mainly in the northwest–southeast direction until 2012 and then expanded in all directions. This process corresponds to the expansion of the groundwater cone of depression range after 2012, although subsidence is restricted by geological conditions. Then, we use the permutation entropy (PE) algorithm to reverse the temporal evolution pattern of land subsidence, and interpret the causes of the phenomenon in combination with groundwater level change data. The results show that the time-series evolution pattern of the land subsidence funnel edge can be divided into three stages. From 2009 to 2010, the land subsidence development was uneven. From 2010 to 2012, the land subsidence development was relatively even. From 2012 to 2013, the development of land subsidence became uneven. However, subsidence within the land subsidence funnel is divided into two stages. From 2009 to 2012, the land subsidence tended to be even, and from 2012 to 2015, the land subsidence was relatively more even. The main reason for the different time-series evolution patterns at these two locations is the annual groundwater level variations. The larger the variation range of groundwater is, the higher the corresponding PE value, which means the development of the land subsidence tends to be uneven.