Chen Lixia, Mei Le, Zeng Bin, Yin Kunlong, Shrestha Dhruba Pikha, Du Juan
Institute of Geophysics and Geomatics, China University of Geosciences, Wuhan, 430074, China.
Environment Faculty, China University of Geosciences, Wuhan, 430074, China.
Sci Rep. 2020 Oct 5;10(1):16531. doi: 10.1038/s41598-020-73727-4.
Yadong County located in the southern Himalayan mountains in Tibet, China, is an import frontier county. It was affected by landslides after the 2011 Sikkim earthquake (Mw = 6.8) and the 2015 Gorkha earthquake (Mw = 7.8). Casualties and property damage were caused by shallow landslides during subsequent rainfall on the earthquake-destabilized slopes. Existing researches have generally examined rainfall- and earthquake-triggered landslides independently, whereas few studies have considered the combined effects of both. Furthermore, there is no previous study reported on landslide hazards in the study area, although the area is strategically applicable for trade as it is close to Bhutan and India. This study developed a new approach that coupled the Newmark method with the hydrological model based on geomorphological, geological, geotechnical, seismological and rainfall data. A rainfall threshold distribution map was generated, indicating that the southeast part of Yadong is prone to rainfall-induced landslides, especially when daily rainfall is higher than 45 mm/day. Permanent displacement predictions were used to identify landslide hazard zones. The regression model used to calculate these permanent displacement values was 71% accurate. Finally, landslide probability distribution maps were generated separately for dry and wet conditions with rainfall of varying intensities. Results can serve as a basis for local governments to manage seismic landslide risks during rainy seasons.
亚东县位于中国西藏喜马拉雅山脉南部,是一个重要的边境县。它在2011年锡金地震(Mw = 6.8)和2015年戈尔哈地震(Mw = 7.8)后受到山体滑坡影响。在地震使山坡失稳后的后续降雨期间,浅层滑坡造成了人员伤亡和财产损失。现有研究通常分别考察降雨引发的滑坡和地震引发的滑坡,而很少有研究考虑两者的综合影响。此外,尽管该地区靠近不丹和印度,具有重要的贸易战略地位,但此前没有关于该研究区域滑坡灾害的报道。本研究基于地貌、地质、岩土、地震和降雨数据,开发了一种将纽马克方法与水文模型相结合的新方法。生成了降雨阈值分布图,表明亚东县东南部容易发生降雨引发的滑坡,特别是当日降雨量高于45毫米/天时。利用永久位移预测来识别滑坡危险区。用于计算这些永久位移值的回归模型准确率为71%。最后,针对不同强度降雨的干燥和湿润条件分别生成了滑坡概率分布图。研究结果可为当地政府在雨季管理地震滑坡风险提供依据。