Size and spatial distribution of landslides induced by the 2015 Gorkha earthquake in the Bhote Koshi river watershed Size and spatial distribution of landslides induced by the 2015 Gorkha earthquake in the Bhote Koshi river watershed

最小化 最大化

Vol14 No.10: 1938-1950

Title】Size and spatial distribution of landslides induced by the 2015 Gorkha earthquake in the Bhote Koshi river watershed

Author】GUO Chen-wen1; HUANG Yi-dan1,2,3*; YAO Ling-kan1,2,3; ALRADI Helal1

Addresses】1 School of Civil Engineering, Southwest Jiaotong University, Chengdu 610031, China; 2 Road and Railway Engineering Research Institute, Sichuan Key Laboratory of Seismic Engineering and Technology, Chengdu 610031, China; 3 MOE Key Laboratory of High-speed Railway Engineering, Chengdu 610031 China

Corresponding author】huangyidan@home.swjtu.edu.cn

Citation】Guo CW, Huang YD, Yao LK, et al. (2017) Size and spatial distribution of landslides induced by the 2015 Gorkha earthquake in the Bhote Koshi river watershed. Journal of Mountain Science 14(10). https://doi.org/10.1007/s11629-016-4140-y

DOI】https://doi.org/10.1007/s11629-016-4140-y

Abstract】The Mw 7.8 Gorkha earthquake in Nepal on April 25, 2015, produced thousands of landslides in the Himalayan mountain range. After the earthquake, two field investigations along Araniko Highway were conducted. Then, using remote sensing technology and geographic information system (GIS) technology, 1481 landslides were identified along the Bhote Koshi river. Correlations between the spatial distribution of landslides with slope gradient and lithology were analyzed. The power-law relationship of the size distribution of earthquake-induced landslides was examined in both the Higher Himalaya and Lesser Himalaya. Possible reasons for the variability of the power exponent were explored by examining differences in the geological situations of these areas. Multi-threshold cellular automata were introduced to model the complexity of system components. Most of the landslides occurred at slope gradients of 30°–40°, and the landslide density was positively correlated with slope gradient. Landslides in hard rock areas were more common than in soft rock areas. The cumulative number-area distribution of landslides induced by the Gorkha earthquake exhibited a negative power-law relationship, but the power exponents were different: 1.13 in the Higher Himalaya, 1.36 and Lesser Himalaya. Furthermore, the geological conditions were more complex and varied in the Lesser Himalaya than in the Higher Himalaya, and the cellular automata simulation results indicated that, as the complexity of system components increased, the power exponent increased. Therefore, the variability of the power exponent of landslide size distribution should ascribe to the complexity of geological situations in the Bhote Koshi river watershed.

Keywords】Landslide distribution; Gorkha earthquake; Himalaya; Cellular automata; self-organized criticality