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| 1 | Size and spatial distribution of landslides induced by the2015 Gorkha earthquake in the Bhote Koshi river watershed显示文摘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. | GUO Chen-wen HUANG Yi-dan YAO Ling-kan ALRADI Helal | 2017 | Journal of Mountain Science2017，14，10： | 6 |
| 2 | 非透过性泥石流拦砂坝研究现状及展望显示文摘由于泥石流动力过程的复杂性和理论研究的不完善,拦砂坝防治工程中关键参数计算与拦砂坝结构设计仍然存在诸多不足。首先,简要介绍了拦砂坝工程防治的发展历程及其重要作用。然后,从溢流口过流能力计算、坝体所受泥石流冲击力、坝后冲刷深度与基础埋深以及坝体结构稳定性4个方面详细评述了非透过性泥石流拦砂坝研究取得的主要成果及存在的问题。最后,从设计参数计算方法、新型拦砂坝结构、新型抗冲耐磨材料的研发与应用以及拦砂坝防治体系建设等方面探讨了非透过性泥石流拦砂坝研究的发展趋势。 | 陈华勇 柳金峰 赵万玉 唐金波 | 2016 | 防灾减灾工程学报2016，36，2： | 4 |
| 3 | Effects of spillway types on debris flow trajectory and scour behind a sabo dam显示文摘Debris flows are one of the common natural hazards in mountainous areas.They often cause devastating damage to the lives and property of local people.The sabo dam construction along a debris flow valley is considered to be a useful method for hazard mitigation.Previous work has concentrated on the different types of sabo dams such as close-type sabo dam,open-type sabo dam.However,little attention has been paid to the spillway structure of sabo dam.In the paper,a new type of spillway structure with lateral contraction was proposed.Debris flow patterns under four different spillway structures were investigated.The projection theory was employed to predict trajectory of debris flow out from the spillway and to estimate the incident angle and terminal velocity before it plunged into the scour hole behind the sabo dam.The results indicated that the estimated data were in good agreement with the experimental ones.The discrepancy between the estimated and experimental values of main parameters remained below 21.82%(relative error).Additionally,the effects of debris flow scales under different spillway structures were considered to study the scour law.Although the debris flow pattern and scour law behind the sabo dam under different operating conditions was analyzed in this paper,further study on the scour mechanism andthe maximum scour depth estimation based on scour theory is still required in the future. | CHEN Hua-yong CUI Peng CHEN Jian-gang TANG Jin-bo | 2016 | Journal of Mountain Science2016，13，2： | 3 |
| 4 | 大型深层滑坡灾害及其预测显示文摘为了进一步探明大型深层滑坡发生机制,对今后发生潜在大型深层滑坡区域进行预测,通过对比分析近年来亚洲地区发生的多起大型深层滑坡,从诱发大型深层滑坡的地震与降雨两个主要方面,分析了特殊地层岩性在化学风化作用影响下与多种坡体结构在重力作用影响下的深层滑坡特征,以及降雨对于该类滑坡的形成所具有的促进作用.研究结果表明,对于由地震作用诱发的深层滑坡,应主要根据不同岩石种类的化学风化情况、深层滑坡形成的力学演化机制以及先行降雨对地震滑坡潜在位置进行预测;对于由降雨诱发的深层滑坡,应主要根据重力边坡变形与内部地质结构的地形特征对深层滑坡发生位置进行预测. | 千木良雅弘 | 2016 | 西南交通大学学报2016，51，5： | 3 |
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