Yuandong Huang , Chenchen Xie , Tao Li , Chong Xu , Xiangli He , Xiaoyi Shao , Xiwei Xu , Tao Zhan , Zhaoning Chen
{"title":"这是2022年9月5日中国泸定6.8级地震引发的山体滑坡的公开清单","authors":"Yuandong Huang , Chenchen Xie , Tao Li , Chong Xu , Xiangli He , Xiaoyi Shao , Xiwei Xu , Tao Zhan , Zhaoning Chen","doi":"10.1016/j.eqrea.2022.100181","DOIUrl":null,"url":null,"abstract":"<div><p>This study constructs a preliminary inventory of landslides triggered by the <em>M</em><sub>S</sub> 6.8 Luding earthquake based on field investigation and human-computer interaction visual interpretation on optical satellite images. The results show that this earthquake triggered at least 5 007 landslides, with a total landslide area of 17.36 km<sup>2</sup>, of which the smallest landslide area is 65 m<sup>2</sup> and the largest landslide area reaches 120 747 m<sup>2</sup>, with an average landslide area of about 3 500 m<sup>2</sup>. The obtained landslides are concentrated in the IX intensity zone and the northeast side of the seismogenic fault, and the area density and point density of landslides are 13.8%, and 35.73 km<sup>−2</sup> peaks with 2 km as the search radius. It should be noted that the number of landslides obtained in this paper will be lower than the actual situation because some areas are covered by clouds and there are no available post-earthquake remote sensing images. Based on the available post-earthquake remote sensing images, the number of landslides triggered by this earthquake is roughly estimated to be up to 10 000. This study can be used to support further research on the distribution pattern and risk evaluation of the coseismic landslides in the region, and the prevention and control of landslide hazards in the seismic area.</p></div>","PeriodicalId":100384,"journal":{"name":"Earthquake Research Advances","volume":"3 1","pages":"Article 100181"},"PeriodicalIF":0.0000,"publicationDate":"2023-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"19","resultStr":"{\"title\":\"An open-accessed inventory of landslides triggered by the MS 6.8 Luding earthquake, China on September 5, 2022\",\"authors\":\"Yuandong Huang , Chenchen Xie , Tao Li , Chong Xu , Xiangli He , Xiaoyi Shao , Xiwei Xu , Tao Zhan , Zhaoning Chen\",\"doi\":\"10.1016/j.eqrea.2022.100181\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><p>This study constructs a preliminary inventory of landslides triggered by the <em>M</em><sub>S</sub> 6.8 Luding earthquake based on field investigation and human-computer interaction visual interpretation on optical satellite images. The results show that this earthquake triggered at least 5 007 landslides, with a total landslide area of 17.36 km<sup>2</sup>, of which the smallest landslide area is 65 m<sup>2</sup> and the largest landslide area reaches 120 747 m<sup>2</sup>, with an average landslide area of about 3 500 m<sup>2</sup>. The obtained landslides are concentrated in the IX intensity zone and the northeast side of the seismogenic fault, and the area density and point density of landslides are 13.8%, and 35.73 km<sup>−2</sup> peaks with 2 km as the search radius. It should be noted that the number of landslides obtained in this paper will be lower than the actual situation because some areas are covered by clouds and there are no available post-earthquake remote sensing images. Based on the available post-earthquake remote sensing images, the number of landslides triggered by this earthquake is roughly estimated to be up to 10 000. This study can be used to support further research on the distribution pattern and risk evaluation of the coseismic landslides in the region, and the prevention and control of landslide hazards in the seismic area.</p></div>\",\"PeriodicalId\":100384,\"journal\":{\"name\":\"Earthquake Research Advances\",\"volume\":\"3 1\",\"pages\":\"Article 100181\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2023-01-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"19\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Earthquake Research Advances\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/S2772467022000720\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Earthquake Research Advances","FirstCategoryId":"1085","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S2772467022000720","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
An open-accessed inventory of landslides triggered by the MS 6.8 Luding earthquake, China on September 5, 2022
This study constructs a preliminary inventory of landslides triggered by the MS 6.8 Luding earthquake based on field investigation and human-computer interaction visual interpretation on optical satellite images. The results show that this earthquake triggered at least 5 007 landslides, with a total landslide area of 17.36 km2, of which the smallest landslide area is 65 m2 and the largest landslide area reaches 120 747 m2, with an average landslide area of about 3 500 m2. The obtained landslides are concentrated in the IX intensity zone and the northeast side of the seismogenic fault, and the area density and point density of landslides are 13.8%, and 35.73 km−2 peaks with 2 km as the search radius. It should be noted that the number of landslides obtained in this paper will be lower than the actual situation because some areas are covered by clouds and there are no available post-earthquake remote sensing images. Based on the available post-earthquake remote sensing images, the number of landslides triggered by this earthquake is roughly estimated to be up to 10 000. This study can be used to support further research on the distribution pattern and risk evaluation of the coseismic landslides in the region, and the prevention and control of landslide hazards in the seismic area.