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ZHANG Yu, MING Dongping, ZHAO Wenyi, XU Lu, ZHAO Zhi, LIU Ran. 2023. The extraction and analysis of Luding earthquake-induced landslide based on high-resolution optical satellite images. Remote Sensing for Natural Resources, 35(1): 161-170. doi: 10.6046/zrzyyg.2022434
Citation: ZHANG Yu, MING Dongping, ZHAO Wenyi, XU Lu, ZHAO Zhi, LIU Ran. 2023. The extraction and analysis of Luding earthquake-induced landslide based on high-resolution optical satellite images. Remote Sensing for Natural Resources, 35(1): 161-170. doi: 10.6046/zrzyyg.2022434
shu

The extraction and analysis of Luding earthquake-induced landslide based on high-resolution optical satellite images

  • 1. School of Information Engineering, China University of Geosciences (Beijing), Beijing 100083, China；

  • 2. China Geological Environment Monitoring Institute, Beijing 100081, China

Received Date:  07 November 2022
Revised Date:  15 March 2023
Publish Date:  20 March 2023
    Abstract
  • On September 5, 2022, a Ms 6.8 earthquake occurred in Luding County, Ganzi Prefecture, Sichuan Province, inducing numerous landslides. This study collected the pre- and post-earthquake images from the GF-2 and GF-6 satellites, as well as the DEM data of Luding. Then, using the object-oriented method, the stepwise optimization multi-scale segmentation method, and the nearest neighbor classification method, this study extracted the landslide information according to the spectrum, thematic index, geometric texture, and topographic features of the objects in the experimental area. The overall identification accuracy of pre- and post-earthquake landslides was 92.3% and 95.4%, respectively. The comprehensive analysis of the distribution of pre- and post-earthquake landslide landslides shows that 23.91 km2 of new landslides were induced by the earthquake. This study summarized the distribution characteristics of post-earthquake landslides through the spatial statistical analysis of seven topographic factors. The results are as follows: ① The post-earthquake landslides were mainly affected by the Xianshuihe fault zone, and they show a banded distribution along rivers and a lamellar, dense distribution along the hillsides and valleys near the fault zone; ② Compared with the historical landslides, the new landslides have a relatively stable elevation range and a large slope range. Moreover, there is a significantly negative correlation between the area of the post-earthquake landslides and the surface roughness.
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