Mapping ground subsidence induced by aquifer overexploitation using advanced Differential SAR Interferometry: Vega Media of the Segura River (SE Spain) case study

Tomás, Roberto; Márquez, Yolanda; López-Sánchez, Juan M.; Delgado, José; Blanco, Pablo; Mallorquí, Jordi J.; Martínez, Mónica M.; Herrera, Gerardo; Mulas, J.

doi:10.1016/j.rse.2005.08.003

Cited by 120 publications

(77 citation statements)

References 10 publications

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“…This technique has been mostly applied for monitoring tectonic motions (Kimura and Yamaguchi, 2000;Bürgmann et al, 2006;Delouis et al, 2002;Johanson and Bürgmann, 2005;Wright et al, 2004;Bürgmann et al, 2002). It has also been used successfully for surface effects of subsidence induced by natural causes or man made activities (Poland et al, 2006;Amelung et al, 1999;Tomas et al, 2005;Dixon et al, 2006;Fernandez et al, 2009). However, InSAR technique, for deformation monitoring, depends a lot on local conditions such as topography, vegetation, atmosphere as well as resolution of data.…”

Section: Detecting Surface Deformations Using Insar Techniquementioning

confidence: 99%

Monitoring subsidence effects in the urban area of Zonguldak Hardcoal Basin of Turkey by InSAR-GIS integration

Akçın

Kutoğlu

Kemaldere

et al. 2010

Nat. Hazards Earth Syst. Sci.

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Section: Detecting Surface Deformations Using Insar Techniquementioning

confidence: 99%

Monitoring subsidence effects in the urban area of Zonguldak Hardcoal Basin of Turkey by InSAR-GIS integration

Akçın

Kutoğlu

Kemaldere

et al. 2010

Nat. Hazards Earth Syst. Sci.

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“…Therefore, the dynamic temporal and spatial distribution of three-dimensional (3-D) deformations is vital to determine the most severely damaged areas, to mitigate (or even eliminate) the causes of ground deformations [7], to provide information for the interpretation of deformation mechanism and to predict deformation evolution resulting from future underground fluid withdrawal.…”

Section: Introductionmentioning

confidence: 99%

“…MT-InSAR has been successfully and extensively used in monitoring the deformations Remote Sens. 2017, 9, 1129 2 of 22 induced by exploitation of underground fluids, such as groundwater [7,[14][15][16][17][18][19][20][21], oil [22][23][24][25][26][27][28][29][30][31], natural gas [14,30,[32][33][34][35][36][37], and geothermal [38][39][40][41][42][43][44][45], because of its low cost, wide spatial coverage, high measurement precision, and fine spatial resolution. However, MT-InSAR can capture only one-dimensional (1-D) time-series deformation that includes the sum of projections on the line-of-sight (LOS) direction of actual 3-D time series ground deformations.…”

Section: Introductionmentioning

confidence: 99%

Deriving 3-D Time-Series Ground Deformations Induced by Underground Fluid Flows with InSAR: Case Study of Sebei Gas Fields, China

Liu

Sun

et al. 2017

Remote Sensing

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Multi-temporal Interferometric Synthetic Aperture Radar (MT-InSAR) technique has proven to be a powerful tool for the monitoring of time-series ground deformations along the line-of-sight (LOS) direction. However, the one-dimensional (1-D) measurements cannot provide comprehensive information for interpreting the related geo-hazards. Recently, a novel method has been proposed to map the three-dimensional (3-D) deformation associated with underground fluid flows based on single-track InSAR LOS measurements and the deformation modeling associated with the Green's function. In this study, the method is extended in temporal domain by exploiting the MT-InSAR measurements, and applied for the first time to investigate the 3-D time series deformation over Sebei gas field in Qinghai, Northwest China with 37 Sentinel-1 images acquired during October 2014-July 2017. The estimated 3-D time series deformations provide a more complete view of ongoing deformation processes as compared to the 1-D time series deformations or the 3-D deformation velocities, which is of great importance for assessing the possible geohazards. In addition, the extended method allows for the retrieval of time series of fluid volume changes due to the gas extraction in the Sebei field, which agrees well with those from the PetroChina Qinghai Oilfield Company Yearbooks (PQOCYs). This provides a new way to study the variations of subsurface fluids at unprecedented resolution.

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“…The systematic cov-erage and frequent observations (e.g. approximately monthly repeat-cycle for ERS and ASAR) provided by SAR sensors allows the extraction of information on the spatial and temporal evolution of ground deformation at more frequent intervals than traditional techniques (Massonnet and Feigl, 1998;Baer et al, 2002;Tomás et al, 2005;Herrera et al, 2007). The availability since 1992 of a large archive of satellite acquisitions allows an analysis of historical deformation.…”

Section: Introductionmentioning

confidence: 99%

Spatio-temporal evolution of aseismic ground deformation in the Mexicali Valley (Baja California, Mexico) from 1993 to 2010, using differential SAR interferometry

Sarychikhina

Glowacka

2015

Proc. IAHS

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Abstract. Ground deformation in Mexicali Valley, Baja California, Mexico, the southern part of the MexicaliImperial valley, is influenced by active tectonics and human activity, mainly that of geothermal fluid extraction in the Cerro Prieto Geothermal Field. Significant ground deformation, mainly subsidence ( ∼ 18 cm yr −1 ), and related ground fissures cause severe damage to local infrastructure.The technique of Differential Synthetic Aperture Radar Interferometry (DInSAR) has been demonstrated to be a very effective remote sensing tool for accurately measuring the spatial and temporal evolution of ground displacements over broad areas. In present study ERS-1/2 SAR and ENVISAT ASAR images acquired between 1993 and 2010 were used to perform a historical analysis of aseismic ground deformation in Mexicali Valley, in an attempt to evaluate its spatio-temporal evolution and improve the understanding of its dynamic. For this purpose, the conventional 2-pass DInSAR was used to generate interferograms which were used in stacking procedure to produce maps of annual aseismic ground deformation rates for different periods. Differential interferograms that included strong co-seismic deformation signals were not included in the stacking and analysis.The changes in the ground deformation pattern and rate were identified. The main changes occur between 2000 and 2005 and include increasing deformation rate in the recharge zone and decreasing deformation rate in the western part of the CPGF production zone. We suggested that these changes are mainly caused by production development in the Cerro Prieto Geothermal Field.

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Mapping ground subsidence induced by aquifer overexploitation using advanced Differential SAR Interferometry: Vega Media of the Segura River (SE Spain) case study

Cited by 120 publications

References 10 publications

Monitoring subsidence effects in the urban area of Zonguldak Hardcoal Basin of Turkey by InSAR-GIS integration

Monitoring subsidence effects in the urban area of Zonguldak Hardcoal Basin of Turkey by InSAR-GIS integration

Deriving 3-D Time-Series Ground Deformations Induced by Underground Fluid Flows with InSAR: Case Study of Sebei Gas Fields, China

Spatio-temporal evolution of aseismic ground deformation in the Mexicali Valley (Baja California, Mexico) from 1993 to 2010, using differential SAR interferometry

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