Imaging land subsidence induced by groundwater extraction in Beijing (China) using satellite radar interferometry

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Abstract

Beijing is one of the most water-stressed cities in the world. Due to over-exploitation of groundwater, the Beijing region has been suffering from land subsidence since 1935. In this study, the Small Baseline InSAR technique has been employed to process Envisat ASAR images acquired between 2003 and 2010 and TerraSAR-X stripmap images collected from 2010 to 2011 to investigate land subsidence in the Beijing region. The maximum subsidence is seen in the eastern part of Beijing with a rate greater than 100 mm/year. Comparisons between InSAR and GPS derived subsidence rates show an RMS difference of 2.94 mm/year with a mean of 2.41 ± 1.84 mm/year. In addition, a high correlation was observed between InSAR subsidence rate maps derived from two different datasets (i.e., Envisat and TerraSAR-X). These demonstrate once again that InSAR is a powerful tool for monitoring land subsidence. InSAR derived subsidence rate maps have allowed for a comprehensive spatio-temporal analysis to identify the main triggering factors of land subsidence. Some interesting relationships in terms of land subsidence were found with groundwater level, active faults, accumulated soft soil thickness and different aquifer types. Furthermore, a relationship with the distances to pumping wells was also recognized in this work.

Figures

  • Figure 1. (a) Location of the study area; (b) geology of the Beijing plain (China); (c) hydrogeological cross-section of the studied aquifer (adapted from [20]).
  • Figure 2. Networks of the small baseline interferograms obtained from (a) Envisat ASAR and (b) TerraSAR-X images used for SBAS InSAR analysis for land subsidence in Beijing.
  • Figure 3. Mean LOS displacement rates derived from Envisat ASAR (2003~2010) in the Beijing basin. Figure 3. Mean LOS displacement rates derived from Envisat ASAR (2003~2010) in the Beijing basin.
  • Figure 4. Spatio-temporal evolution of InSAR-derived accumulated LOS displacement in Beijing from Envisat-ASAR images. Note that for simplicity, the displacement patterns of only 8 of the 41 acquisition dates are shown (i.e., one per year).
  • Figure 5. Comparison of GPS and Envisat InSAR results for points G1–G6. See GPS stations location in Figure 3.
  • Figure 6. Displacement rates along LOS derived from (a) Envisat ASAR (2007~2010) and (b) TerraSAR-X (2010~2011) images. (c) Correlation and (d) differences analysis between Envisat ASAR and TerraSAR-X data.
  • Figure 7. (a) Subsidence bowls located in the NE of Beijing; (b) extension of the subsidence bowls. Mapped InSAR results along LOS have been derived from Envisat ASAR images acquired from 2003 to 2010.
  • Figure 8. LOS displacements difference in Beijing obtained from Envisat ASAR images between the acquisition dates selected in Figure 4.

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APA

Chen, M., Tomás, R., Li, Z., Motagh, M., Li, T., Hu, L., … Gong, X. (2016). Imaging land subsidence induced by groundwater extraction in Beijing (China) using satellite radar interferometry. Remote Sensing, 8(6). https://doi.org/10.3390/rs8060468

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