Analysis of the Deformation Behavior and Sinkhole Risk in Kerdabad, Iran Using the PS-InSAR Method

被引:21
作者
Azar, Mahdi Khoshlahjeh [1 ]
Hamedpour, Amir [2 ,3 ]
Maghsoudi, Yasser [1 ,4 ]
Perissin, Daniele [5 ]
机构
[1] KN Toosi Univ Technol, Photogrammetry & Remote Sensing Dept, Geomat Engn Fac, Tehran 1543319967, Iran
[2] Agr Univ Iceland, Fac Environm & Forest Sci, IS-311 Borgarnes, Iceland
[3] Svarmi, Data Co Specialized Remote Sensing & Drones, Arleyni 22, IS-112 Reykjavik, Iceland
[4] Univ Leeds, Sch Earth & Environm, COMET, Leeds LS2 9JT, W Yorkshire, England
[5] RASER Ltd, Radar & Software Engn Res Co, 9 Wing Hong St, Hong Kong, Peoples R China
基金
英国自然环境研究理事会;
关键词
radar interferometry; persistent scatterers; PSI; sinkhole; Sentinel-1; subsidence; DEAD-SEA; PERMANENT SCATTERERS; SAR INTERFEROMETRY; EVAPORITE KARST; LAND SUBSIDENCE; TIME-SERIES; HAZARDS; AREAS; GROUNDWATER; HAMADAN;
D O I
10.3390/rs13142696
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The unexpected collapse of land surface due to subsidence is one of the most significant geohazards that threatens human life and infrastructure. Kabudrahang and Famenin are two Iranian plains experiencing several sinkholes due to the characteristics of the underground soil layers and extreme groundwater depletion. In this study, space-based Synthetic Aperture Radar images are used to investigate the ground displacement behavior to examine the feasibility of Sentinel-1 data in detecting precursory deformation proceeding before the sinkhole formation. The selected sinkhole occurred in August 2018 in the vicinity of Kerdabad village in Hamedan province with a 40 m diameter and depth of similar to 40 m. Time series of the European constellation Sentinel-1 data, spanning from January 2015 to August 2018, is analyzed, and the results revealed a 3 cm annual subsidence (similar to 3 cm/year) along with the line-of-sight direction. Time-series analysis demonstrated that the driving mechanism of the sinkhole formation had a gradual process. Displacement of persistent scatterers (PSs) near the cave area had an acceleration by approaching the sinkhole formation date. In contrast, other areas that are far from the cave area show linear subsidence behavior over time. Additionally, the one-kilometer deformation profile over the cave area indicates a high subsidence rate precisely at the location where the sinkhole was formed later on 20 August 2018.
引用
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页数:18
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