Zobrazeno 1 - 10
of 12
pro vyhledávání: '"Shuaixing Yan"'
Publikováno v:
地质科技通报, Vol 43, Iss 6, Pp 1-14 (2024)
Objective, Methods This study focus on debris flows in Huangniba gully, Muli County, Liangshan Prefecture, Sichuan Province, utilizing a mass flow numerical simulation platform. Through field investigations and the construction of numerical models, w
Externí odkaz:
https://doaj.org/article/4380432453f040ffad6b2ba0a7959b5a
Publikováno v:
Geotextiles and Geomembranes. 50:677-693
Publikováno v:
Journal of Hydraulic Research. 59:120-135
Debris flows are typical two-phase flows that commonly occur with entrainment. By involving sediment materials, the fluid viscosity of debris flow may change significantly along with the variety of...
Publikováno v:
Bulletin of Engineering Geology and the Environment. 79:3321-3335
In Western China, a large number of bridges are located in debris flow gullies and are exposed to a great risk of damage in case of a geological disaster. To ensure the safety of the bridge and extend its service period, in this study, we propose a m
Publikováno v:
Landslides. 16:777-785
The catastrophic Baige landslide occurred at 22:05:36 (Beijing time, UTC+8) on the 10th of October 2018 in Tibet, China. The large and rapid landslide generated strong long-period seismic signals that were recorded by broadband seismic stations. In t
Publikováno v:
Journal of Mountain Science. 16:414-427
Arrays of baffles are usually installed in front of protection site to attenuate the flow energy of rock avalanches in mountainous areas. Optimization design is crucial for efficiency promotion in hazard energy dissipation engineering. In this study,
Publikováno v:
Geophysical Research Letters. 47
Publikováno v:
Engineering Geology. 247:69-83
Construction solid waste (CSW) landslides are always characterized by high mobility, and thus pose much danger to surrounding residents and buildings. In this study, a back in situ analysis of the catastrophic CSW landslide occurred in Shenzhen in De
Publikováno v:
Landslides (Berl., Internet) 15 (2018): 2465–2474. doi:10.1007/s10346-018-1073-2
info:cnr-pdr/source/autori:Kaiheng Hu, Chaohua Wu, Jinbo Tang, Alessandro Pasuto, Yanji Li, Shuaixing Yan/titolo:New understandings of the June 24th 2017 Xinmo Landslide, Maoxian, Sichuan, China/doi:10.1007%2Fs10346-018-1073-2/rivista:Landslides (Berl., Internet)/anno:2018/pagina_da:2465/pagina_a:2474/intervallo_pagine:2465–2474/volume:15
info:cnr-pdr/source/autori:Kaiheng Hu, Chaohua Wu, Jinbo Tang, Alessandro Pasuto, Yanji Li, Shuaixing Yan/titolo:New understandings of the June 24th 2017 Xinmo Landslide, Maoxian, Sichuan, China/doi:10.1007%2Fs10346-018-1073-2/rivista:Landslides (Berl., Internet)/anno:2018/pagina_da:2465/pagina_a:2474/intervallo_pagine:2465–2474/volume:15
On June 24, 2017 (21:39 UTC, June 23rd), a catastrophic landslide occurred at Xinmo village of Mao County, Sichuan Province, China. Soon after the event, some research teams carried out field investigations in order to both support the emergency oper
Publikováno v:
Bulletin of Engineering Geology and the Environment. 78:2671-2680
The Dujiangyan-Wenchuan highway serves as a vital passage to and from the region severely damaged by the 5.12 Wenchuan Earthquake in China. Chediguan Bridge is located on the highway and spans the Minjiang River. During the earthquake, the bridge was