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Hazard Assessment of Co-seismic Landslides Based on Information Value Method: A Case in 2018 MW6.6 Hokkaido Earthquake, Japan
作者姓名:WEN Boyu  XU Chong  HE Xiangli  MA Siyuan  SHAO Xiaoyi  LI Kai  ZHANG Zhongjian  LI Zhengfang
作者单位:Key Laboratory of Active Tectonics and Volcano, Institute of Geology, China Earthquake Administration, Beijing 100029, China;School of Engineering and Technology, China University of Geosciences(Beijing), Beijing 100083, China,Key Laboratory of Active Tectonics and Volcano, Institute of Geology, China Earthquake Administration, Beijing 100029, China;Institute of Crustal Dynamics, China Earthquake Administration, Beijing 100085, China,Institute of Crustal Dynamics, China Earthquake Administration, Beijing 100085, China,Key Laboratory of Active Tectonics and Volcano, Institute of Geology, China Earthquake Administration, Beijing 100029, China,Key Laboratory of Active Tectonics and Volcano, Institute of Geology, China Earthquake Administration, Beijing 100029, China,School of Engineering and Technology, China University of Geosciences(Beijing), Beijing 100083, China,School of Engineering and Technology, China University of Geosciences(Beijing), Beijing 100083, China,Key Laboratory of Active Tectonics and Volcano, Institute of Geology, China Earthquake Administration, Beijing 100029, China
基金项目:This project is supported by the Basic Scientific Fund of the Institute of Geology, China Earthquake Administration (IGCEA1604).
摘    要:An MW6.6 earthquake occurred in eastern Hokkaido, Japan on September 6th, 2018. Based on the pre-earthquake image from Google Earth and the post-earthquake image from high resolution (3 m) planet satellite, we manually interpret 9 293 coseismic landslides and select 7 influencing factors of seismic landslide, such as elevation, slope, slope direction, road distance, flow distance, peak ground acceleration (PGA) and lithology. Then, 9 293 landslide points are randomly divided into training samples and validation samples with a proportion of 7:3. In detail, the training sample has 6 505 landslide points and the validation sample has 2 788 landslide points. The hazard risk assessment of seismic landslide is conducted by using the information value method and the study area is further divided into five risk grades, including very low risk area, low risk area, moderate risk area high risk area and very high risk area. The results show that there are 7 576 landslides in high risk area and very high risk area, accounting for 81.52% of the total landslide number, and the landslide area is 22.93 km2, accounting for 74.35% of the total area. The hazard zoning is in high accordance with the actual situation. The evaluation results are tested by using the curve of cumulative percentage of hazardous area and cumulative percentage of landslides number. The results show that the success rate of the information value method is 78.50% and the prediction rate is 78.43%. The evaluation results are satisfactory, indicating that the hazard risk assessment results based on information value method may provide scientific reference for landslide hazard risk assessment as well as the disaster prevention and mitigation in the study area.

关 键 词:Hokkaido  earthquake  Co-seismic  landslides  Hazard  risk  assessment  Information  value  method
收稿时间:2019/11/5 0:00:00
修稿时间:2020/1/14 0:00:00

Hazard Assessment of Co-seismic Landslides Based on Information Value Method: A Case in 2018 MW6.6 Hokkaido Earthquake, Japan
WEN Boyu,XU Chong,HE Xiangli,MA Siyuan,SHAO Xiaoyi,LI Kai,ZHANG Zhongjian,LI Zhengfang.Hazard Assessment of Co-seismic Landslides Based on Information Value Method: A Case in 2018 MW6.6 Hokkaido Earthquake, Japan[J].Earthquake Research in China,2020,34(1):64-80.
Authors:WEN Boyu  XU Chong  HE Xiangli  MA Siyuan  SHAO Xiaoyi  LI Kai  ZHANG Zhongjian and LI Zhengfang
Institution:Key Laboratory of Active Tectonics and Volcano, Institute of Geology, China Earthquake Administration, Beijing 100029, China;School of Engineering and Technology, China University of Geosciences(Beijing), Beijing 100083, China,Key Laboratory of Active Tectonics and Volcano, Institute of Geology, China Earthquake Administration, Beijing 100029, China;Institute of Crustal Dynamics, China Earthquake Administration, Beijing 100085, China,Institute of Crustal Dynamics, China Earthquake Administration, Beijing 100085, China,Key Laboratory of Active Tectonics and Volcano, Institute of Geology, China Earthquake Administration, Beijing 100029, China,Key Laboratory of Active Tectonics and Volcano, Institute of Geology, China Earthquake Administration, Beijing 100029, China,School of Engineering and Technology, China University of Geosciences(Beijing), Beijing 100083, China,School of Engineering and Technology, China University of Geosciences(Beijing), Beijing 100083, China and Key Laboratory of Active Tectonics and Volcano, Institute of Geology, China Earthquake Administration, Beijing 100029, China
Abstract:An MW6.6 earthquake occurred in eastern Hokkaido, Japan on September 6th, 2018. Based on the pre-earthquake image from Google Earth and the post-earthquake image from high resolution (3 m) planet satellite, we manually interpret 9 293 coseismic landslides and select 7 influencing factors of seismic landslide, such as elevation, slope, slope direction, road distance, flow distance, peak ground acceleration (PGA) and lithology. Then, 9 293 landslide points are randomly divided into training samples and validation samples with a proportion of 7:3. In detail, the training sample has 6 505 landslide points and the validation sample has 2 788 landslide points. The hazard risk assessment of seismic landslide is conducted by using the information value method and the study area is further divided into five risk grades, including very low risk area, low risk area, moderate risk area high risk area and very high risk area. The results show that there are 7 576 landslides in high risk area and very high risk area, accounting for 81.52% of the total landslide number, and the landslide area is 22.93 km2, accounting for 74.35% of the total area. The hazard zoning is in high accordance with the actual situation. The evaluation results are tested by using the curve of cumulative percentage of hazardous area and cumulative percentage of landslides number. The results show that the success rate of the information value method is 78.50% and the prediction rate is 78.43%. The evaluation results are satisfactory, indicating that the hazard risk assessment results based on information value method may provide scientific reference for landslide hazard risk assessment as well as the disaster prevention and mitigation in the study area.
Keywords:Hokkaido earthquake  Co-seismic landslides  Hazard risk assessment  Information value method
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