Abstract
The Jianshanying landslide in Guizhou province, China, is a typical mining-induced landslide with its complex formation in karst mountainous area. However, the spatiotemporal deformation characteristics and failure mechanism are still unknown. In this paper, the surface deformation time series from 2017 to 2020 is firstly estimated by combining multi-temporal synthetic aperture radar (SAR) interferometry and improved offset-tracking methods to overcome the difficulties caused by the large gradient surface deformation and surface material changes. Then, the spatiotemporal characteristics of Jianshanying landslide is analyzed in terms of line-of-sight (LOS) deformation with stacking InSAR method and two-dimensional (2D) deformation with improved SAR offset-tracking method. And the different deformation features between sliding body and surrounding areas are uncovered. Accordingly, we point out the “three-section” surface deformation model. We further analyze the deformation time series by considering the joint effects of rainfall and underground mining. Finally, we conceptualize the landslide failure mode for the Jianshanying landslide, which can be extended to the similar landslide in karst mountainous areas of southwestern China.
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Acknowledgements
We would like to thank JAXA, Japan, to provide the ALOS/PALSAR-2 data. And one arc-second SRTM DEM is freely downloaded from the website https://e4ftl01.cr.usgs.gov/MEASURES/. Some mapping software, such as ArcGIS and Origin are used.
Funding
This work was funded by the National Key Research and Development Program of China (Grant No. 2018YFC1504805) and the Natural Science Foundation of China (Grant Nos. 41731066, 41874005, 41929001).
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Chen, L., Zhao, C., Li, B. et al. Deformation monitoring and failure mode research of mining-induced Jianshanying landslide in karst mountain area, China with ALOS/PALSAR-2 images. Landslides 18, 2739–2750 (2021). https://doi.org/10.1007/s10346-021-01678-6
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DOI: https://doi.org/10.1007/s10346-021-01678-6