Spatial Analysis of Land Subsidence in the San Luis Potosi Valley Induced by Aquifer Overexploitation Using the Coherent Pixels Technique (CPT) and Sentinel-1 InSAR Observation

被引:18
|
作者
Ines Navarro-Hernandez, Maria [1 ]
Tomas, Roberto [2 ]
Lopez-Sanchez, Juan M. [3 ]
Cardenas-Tristan, Abraham [1 ]
Mallorqui, Jordi J. [4 ]
机构
[1] Univ San Luis Potosi, Engn Fac, Ctr Res & Posgrad Studies, Av Dr Manuel Nava 8, San Luis Potosi 78210, San Luis Potosi, Mexico
[2] Univ Alicante, Escuela Politecn Super, Dept Civil Engn, POB 99, E-03080 Alicante, Spain
[3] Univ Alicante, Inst Comp Res IUII, POB 99, E-03080 Alicante, Spain
[4] Univ Politecn Cataluna, Dept Signal Theory & Commun, CommSensLab, C Jordi Girona 1-3,D-3, ES-08034 Barcelona, Spain
关键词
land subsidence; groundwater withdrawal; coherent pixel technique; InSAR; Sentinel-1; Mexico; spatial analysis; SYNTHETIC-APERTURE RADAR; PERSISTENT SCATTERER INTERFEROMETRY; CENTRAL MEXICO; GROUNDWATER EXPLOITATION; METROPOLITAN-AREA; BEIJING PLAIN; CITY; DEFORMATION; BASIN; SPAIN;
D O I
10.3390/rs12223822
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The San Luis Potosi metropolitan area has suffered considerable damage from land subsidence over the past decades, which has become visible since 1990. This paper seeks to evaluate the effects of groundwater withdrawal on land subsidence in the San Luis Potosi Valley and the development of surface faults due to the differential compaction of sediments. For this purpose, we applied the Coherent Pixels Technique (CPT), a Persistent Scatterer Interferometry (PSI) technique, using 112 Sentinel-1 acquisitions from October 2014 to November 2019 to estimate the deformation rate. The results revealed that the deformation areas in the municipality of Soledad de Graciano Sanchez mostly exhibit subsidence values between -1.5 and -3.5 cm/year; whereas in San Luis Potosi these values are between -1.8 and -4.2 cm/year. The PSI results were validated by five Global Navigation Satellite System (GNSS) benchmarks available, providing a data correlation between the results obtained with both techniques of 0.986. This validation suggests that interferometric derived deformations agree well with results obtained from GNSS data. The strong relationship between trace fault, land subsidence,e and groundwater extraction suggests that groundwater withdrawal is resulting in subsidence induced faulting, which follows the pattern of structural faults buried by sediments.
引用
收藏
页码:1 / 23
页数:23
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