financially supported by the Open Fund of State Key Laboratory of Geohazard Prevention and Geoenvironment(No.SKLGP2021K008);the National Natural Science Foundation of China(41907247)。
The failure of the 2017 Xinmo catastrophic rockslide in Maoxian County, Sichuan, Southwest China was a combined effect of long-term and shortterm triggering factors. Field investigation, historical data collection, la...
the support of the National Key R&D Program of China (2017YFC1501102);the National Natural Science Foundation of China (51639007);the Youth Science and Technology Fund of Sichuan Province (2016JQ0011)
A pair of flumes with variable inclinations were employed to investigate the entrainment mechanics and dynamical evolution of a debris avalanche/flow. A fixed quantity of solid and water mixture was released from a co...
funded by CRSRI Open Research Program (CKWV2013203/KY);Fundamental Research Funds for the Central Universities of China (Grant No. BLX2014-12);the National Natural Science Foundation (Grant No. 41601004)
Debris flows can be extremely destructive because they can increase in magnitude via progressive entrainment. In this paper, a total of 18landslide-type debris flows and 268 channelized debris flows in Wenchuan earthq...
funded by the Key Research Program of the Chinese Academy of Sciences (Grant No.KZZD-EW-05-01);the National Natural Science Foundation of China (Grant No.41371039);the Open Foundation of State Key Laboratory of Hydraulics and Mountain River Engineering,Sichuan University (Grant No.SKHL1426)
On-spot observation and field reconnaissance of debris flows have revealed that inflexion points in the longitudinal profile of a movable channel may easily become unstable points that significantly affect their entra...
partially supported by Grant-in-Aid for Scientific Research 26292077, 2014, from the Ministry of Education, Science, Sports, and Culture of Japan;by the River Fund in charge of the River Foundation, Japan
Debris flow simulations are useful for predicting the sediment supplied to watersheds from upstream areas. However, the topographic conditions upstream are more complicated than those downstream and the relationship b...