Identification of Potential Landslide Hazards Using Time-Series InSAR in Xiji County, Ningxia

被引:6
|
作者
Zhang, Jia [1 ,2 ]
Gong, Yongfeng [1 ,2 ]
Huang, Wei [2 ]
Wang, Xing [3 ,4 ,5 ]
Ke, Zhongyan [6 ]
Liu, Yanran [3 ,4 ,5 ]
Huo, Aidi [3 ,4 ,5 ]
Adnan, Ahmed [3 ,4 ,5 ]
Abuarab, Mohamed EL-Sayed [7 ]
机构
[1] China Univ Geosci, Sch Environm Studies, Wuhan 430074, Peoples R China
[2] NingXia Survey & Monitor Inst Land & Resources, Yinchuan 750001, Peoples R China
[3] Changan Univ, Key Lab Subsurface Hydrol & Ecol Effects Arid Reg, Minist Educ, Xian 710054, Peoples R China
[4] Changan Univ, Sch Water & Environm, Xian 710054, Peoples R China
[5] Changan Univ, Xian Monitoring Modelling & Early Warning Watershe, Xian 710054, Peoples R China
[6] Changan Univ, Sch Humanities, Xian 710054, Peoples R China
[7] Cairo Univ, Fac Agr, Giza 12613, Egypt
基金
中国国家自然科学基金;
关键词
southern mountainous region of Ningxia; time-series InSAR; potential landslide identification; spatiotemporal characteristics; RADAR INTERFEROMETRY;
D O I
10.3390/w15020300
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Potential landslide identification and monitoring are essential to prevent geological disasters. However, in mountainous areas where the surface gradient changes significantly, the leveling effect is not completely removed, affecting the deformation results. In this paper, the SBAS-InSAR and PS-InSAR time-series processing methods were combined to interfere with the SAR image data of the ascending orbit in the southern mountainous area of Ningxia and its surrounding regions. Based on the obtained surface deformation monitoring results and optical images, landslide hazard identification was successfully carried out within the coverage area of 3130 km(2) in Xiji County. The results show that the whole study area presented a relatively stable state, most of the deformation rates were concentrated in the range of 0 mm/a to -10 mm/a, and the deformation in the southwest area was larger. A total of 11 large potential landslides (which were already registered potential danger points of geological disasters) were identified in the study area, including three historical collapses. The landslide identification results were highly consistent with the field survey results after verification. The timing analysis of the typical landslide point of the Jiaowan landslide was further carried out, which showed that the Jiaowan landslide produced new deformation during the monitoring time, but it was still in a basically stable state. It can do a good job in disaster prevention and reduction while strengthening monitoring. The results of this study have a guiding effect on landslide prevention and mitigation in the mountainous areas of southern Ningxia.
引用
收藏
页数:12
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