Abstract
Due to the rapid economic development and urban construction and the high exploitation rate of groundwater and geothermal resource, Jimo district existed a potential threat of surface deformation. To clarify the characteristics and causations of surface deformation, this study firstly used SBAS-InSAR (Small Baseline Subset-Interferometric Synthetic Aperture Radar) technology to analyze the surface defor-mation distribution in the whole research area. Then, three areas with different surface cover conditions were selected to analyze the causations of surface deformation. Lastly, taking central urban area as the key research area, surface deformation causations were analyzed in detail based on PS-InSAR (Persistent Scatter-Interferometric Synthetic Aperture Radar) technology. The study found that, in coastal mollisol area, farmland area, and hot spring area, the maximum subsidence velocity reached up to 46.8 mm/a, 24 mm/a, and 19.1 mm/a, respectively. The factors, including surface loading, precipitation, and the groundwater level, were the causations of surface deformation in different research areas. The trend of the surface deformation curve was consistent with that of the groundwater level curve in the central urban area, but the response time of surface deformation lagged behind the change of groundwater level by approximately 4 months.
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Data availability
The original data in this study included GF-1 remote sensing image data, Landsat-8 remote sensing image data and Sentinel-1 remote sensing image data, which are shared free of charge online.
Abbreviations
- D-InSAR:
-
Differential Interferometric Synthetic Aperture Radar
- IW:
-
Interferometric Wides-wath
- PS:
-
Persistent Scatterer
- PS-InSAR:
-
Persistent Scatter -Interferometric Synthetic Aperture Radar
- SAR:
-
Synthetic Aperture Radar
- SLC:
-
Single Look Complex
- SBAS-InSAR:
-
Small Baseline Subset-Interferometric Synthetic Aperture Radar
- TS-InSAR:
-
Time-series Interferometric Synthetic Aperture Radar
References
Abidin HZ, Andreas H, Gamal M, Djaja R, Rajiyowiryono H (2005) Monitoring land subsidence of Jakarta (Indonesia) using leveling, GPS survey and InSAR techniques. International Association of Geodesy Symposia 128:61–566. https://doi.org/10.1007/3-540-27432-4_95
Andreas H, Abidin HZ, Sarsito DA, Pradipta D (2020) Remotes sensing capabilities on land subsidence and coastal water hazard and disaster studies. IOP Conf Ser: Earth Environ Sci 500:1–13. https://doi.org/10.1088/1755-1315/500/1/012036
Andrew H, Howard Z, Paul S, Bert K (2004) A new method for measuring deformation on volcanoes and other natural terrains using InSAR persistent scatterers. Res Lett 31:1–5. https://doi.org/10.1029/2004GL021737
Berardino P, Fornaro G, Lanari R, Sansosti E (2002) A new algorithm for surface deformation monitoring based on small baseline differential SAR interferograms. IEEE Trans Geosci Remote Sens 40:2375–2383. https://doi.org/10.1109/TGRS.2002.803792
Chen B, Gong H, Lei K, Li J, Zhou C, Gao M, Guan H, Lv W (2019) Land subsidence lagging quantification in the main exploration aquifer layers in Beijing plain, China. Int J Appl Earth Obs 75:54–67. https://doi.org/10.1016/j.jag.2018.09.003
Corbau C, Simeoni U, Zoccarato C, Mantovani G, Teatini P (2019) Coupling land use evolution and subsidence in the Po Delta, Italy: revising the past occurrence and prospecting the future management challenges. Sci Total Environ 654:1196–1208. https://doi.org/10.1016/j.scitotenv.2018.11.104
Dong HW (2000) Deduction of the vertical crustal movement in the Qingdao national leveling origin area using the mean sea level. Journal of Oceanography of Huanghai & Bohai Seas 18:25–28. https://doi.org/10.3969/j.issn.1671-6647.2000.02.004
Dong SC, Sergey S, Yin HW, Ye SJ, Cao YR (2014) Time-series analysis of subsidence associated with rapid urbanization in Shanghai, China measured with SBAS InSAR method. Environ Earth Sci 72:677–769. https://doi.org/10.1007/s12665-013-2990-y
Faunt CC, Sneed M, Traum J, Brandt JT (2016) Water availability and land subsidence in the Central Valley, California, USA. Hydrogeol J 24:675–684. https://doi.org/10.1007/s10040-015-1339-x
Ferretti A, Prati C, Rocca F (2001) Permanent scatterers in SAR interferometry. IEEE Trans Geosci Remote Sens 39:8–20. https://doi.org/10.1109/36.898661
Fu YL, Luo ZJ, Jin WZ, Chen XX, Tan JZ (2017) Impact of high-rise building load on land subsidence in Nantong. Journal of Jiangsu University (Natural Science Edition) 38:336–342+360. https://doi.org/10.3969/j.issn.1671-7775.2017.03.015
Gao ML, Gong HL, Chen BB, Li XJ, Zhou CF, Shi M, Si Y, Chen Z, Duan GY (2018) Regional land subsidence analysis in eastern Beijing plain by InSAR time series and wavelet transforms. Remote Sens 10:365–382. https://doi.org/10.3390/rs10030365
Guang YD, Hui LG, Huan HL, You QZ, Bei BC, Kun CL (2016) Monitoring and analysis of land subsidence along Beijing-Tianjin inter-city railway. J Indian Soc Remote 44:915–931. https://doi.org/10.1007/s12524-016-0556-7
Guo H, Bai J, Zhang Y, Wang L, Wang H (2017) The evolution characteristics and mechanism of the land subsidence in typical areas of the North China Plain. Geol China 44:1115–1127. https://doi.org/10.12029/gc20170606
Hu Z, Li B, Liu Y, Niu X (2019) Research on quality improvement method of deformation monitoring data based on InSAR. J Vis Commun Image Represent 64:1–8. https://doi.org/10.1016/j.jvcir.2019.102652
Lanari R, Casu F, Manzo M, Zeni G, Berardino P, Manunta M, Pepe A (2007) An overview of the small baseline subset algorithm: a DInSAR technique for surface deformation analysis. Deformation and Gravity Change: Indicators of Isostasy, Tectonics, Volcanism, and Climate Change. Pageoph Topical Volumes. Birkhäuser Basel. 164:637–661. https://doi.org/10.1007/978-3-7643-8417-3_2
Lanari R, Mora O, Manunta M, Mallorquí JJ, Berardino P, Sansosti E (2004) A small-baseline approach for investigating deformations on full-resolution differential SAR interferograms. IEEE Trans Geosci Remote Sens 42:1377–1386. https://doi.org/10.1109/TGRS.2004.828196
Liu MH, Ren LH, Zhang WJ, Ren PF (2018) Influence of super El Niño events on the frequency of spring and summer extreme precipitation over eastern China. Acta Meteorol Sinica 76:49–63. https://doi.org/10.11676/qxxb2018.021
Li RH, Zhao Z, Duan MY, Wang ZY, Wang P (2015) An analysis of surface subsidence in chiba using PSInSAR technique. 2015 International Workshop on Image and Data Fusion, Kona, Hawaii, USA.81–85. https://doi.org/10.5194/isprsarchives-XL-7-W4-81-2015
Mokadem N, Boughario E, Mudarra M, Brahim FB, Andreo B, Hamed Y, Bouri S (2018) Mapping potential zones for groundwater recharge and its evaluation in arid environments using a GIS approach: case study of North Gafsa Basin (Central Tunisia). J Afr Earth Sci 141:107–117. https://doi.org/10.1016/j.jafrearsci.2018.02.007
San MJ, Hai GW, Shou SZ, Yong L (2007) A tentative study of the mechanism of land subsidence in Beijing. City Geol 1:20–26. https://doi.org/10.3969/j.issn.1007-1903.2007.01.005
Shu JY, Yu QX, Ji CW, Xue XY, Jun Y (2016) Progression and mitigation of land subsidence in China. Hydrogeol J 24:685–693. https://doi.org/10.1007/s10040-015-1356-9
Suddeepong A, Chai JC, Shen SL, Carter JP (2015) Deformation behaviour of clay under repeated one-dimensional unloading-reloading. Can Geotech J 52:1035–1044. https://doi.org/10.1139/cgj-2014-0216
Xu YS, Yuan Y, Shen SL, Yin ZY, Wu HN, Ma L (2015) Investigation into subsidence hazards due to groundwater pumping from Aquifer II in Changzhou, China. Nat Hazards 78:281–296. https://doi.org/10.1007/s11069-015-1714-x
Zhang JZ, Huang HJ, Bi HB (2015) Land subsidence in the modern Yellow River Delta based on InSAR time series analysis. Nat Hazards 75:2385–2397. https://doi.org/10.1007/s11069-014-1434-7
Zhou C, Gong H, Chen B, Li X, Ji Li, Wang X, Gao M, Si Y, Guo L, Shi M, Duan G (2019) Quantifying the contribution of multiple factors to land subsidence in the Beijing Plain, China with machine learning technology. Geomorphology 335:48–61. https://doi.org/10.1016/j.geomorph.2019.03.017
Acknowledgements
Thanks for the shared data provided by the “European Space Agency,” “National Aeronautics and Space Administrationand,” and “Chinese Center for Resources Satellite Data and Application.” Thanks to editors and reviewers.
Funding
This research was funded by the National Science Fund for Distinguished Young Scholars—“Construction and application of remote sensing ecological index model of Tamarix shrubbery forest(grant number 42107496),” the Introduction and Cultivation Plan for Young Innovative Talents of Colleges and Universities by the Education Department of Shandong Province, the project of “One Project One Discussion” on introducing top talents in Shandong Province—“Research and development of key technologies and high-end equipment of water environment health in the Yellow River Basin (Shandong)” and the Research Project of Academician Innovation Platform of Hainan Province, China- “Ecological environment monitoring, protection and restoration of tropical marine islands based on intelligent robot (grant number YSPTZX202149).”
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J. W. was a major contributor in methodology, validation, writing, original draft preparation, writing review and editing. P. H. performed the formal analysis. Z. L. performed the investigation. G.L., B.L., and F.C. provided the fund support. All authors read and approved the final manuscript.
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Highlights
• Overall, Jimo district displayed a trend of surface uplift in the southwest, with a maximum uplift rate of 23.5 mm/a, and surface subsidence in the northeast, with a maximum subsidence rate of 46.8 mm/a.
• The most obvious subsidence occurred along the southern bank of Dingzi Bay and near where the Wulong River enters the Huanghai sea. This region is characterized by thick and loose Quaternary sediment. It was speculated that the causes of surface subsidence in this region are consolidation and compaction, which are influenced by the load from buildings and the self-weight from the mollisol foundation.
• The region in the suburbs of Jimo district, is mainly covered by farmland with a disperse distribution of rural dwellings. The results suggested that the excessive exploitation of groundwater for farmland irrigation is one of main factors promoting surface deformation in this region.
• The region located near the hot spring park in the southeastern part of Jimo district, is characterized by developed hot spring tourism and abundant geothermal resources. It was concluded that surface deformation in this region is related to the exploitation of hot spring geothermal resources, precipitation, and the building load.
• The trend of the surface deformation curve was consistent with that of the groundwater level curve in the central urban area. But the response time of surface deformation lagged behind the change of the groundwater level by approximately 4 months.
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Wang, J., Liang, Z., Han, P. et al. Analysis of the characteristics and causations of surface deformation based on TS-InSAR: a case study of Jimo district, China. Environ Sci Pollut Res 30, 40049–40061 (2023). https://doi.org/10.1007/s11356-022-25099-7
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DOI: https://doi.org/10.1007/s11356-022-25099-7