Time evolution and spatial accumulation of progressive failure for Xinhua slope in the Dagangshan reservoir, Southwest China
Time evolution and spatial accumulation of progressive failure for Xinhua slope in the Dagangshan reservoir, Southwest China
复制标题
大岗山水库新华斜坡渐进破坏的时间演化与空间累积
DOI:
10.1007/s10346-018-0946-8
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发表时间:
2018-01
期刊:
影响因子:
6.7
通讯作者:
Jia-wen Zhou
中科院分区:
文献类型:
--
作者:
Ming-liang Chen;Peng-fei Lv;Shi-lin Zhang;Xing-ze Chen;Jia-wen Zhou
This paper presents a preliminary study of time evolution and spatial accumulation of progressive failure for ancient landslide deposits in Xinhua slope. According to the geological response after impoundment, the Xinhua slope has shown the spatial accumulation of deformation, such as ground cracks in the rear edge, toe collapse, local shallow slides in intense rainfall, and progressive creep displacement. Approximately 2 years of monitoring was performed for the Xinhua slope with the assistance of the global navigation satellite system (GNSS), unmanned aerial vehicles (UAVs), and field investigations. The deformation process of a reservoir landslide is considered to be a comprehensive and complicated combination of geological influence from various adverse factors. Field investigations and monitoring indicate that the major serious influence after completion of dam construction comes from the initial large-scale impoundment, the fluctuation of water level, and the existence of a flood season. The creep/slip deformation of slope deposits is a result of integration with adverse hydraulic conditions, e.g., strong rainfall, intense currents and transient seepage flow inside the slope deposits, and activation by water level fluctuation, which can be verified from the twofold evident deformation in the flood season. For the reservoir with daily regulation ability, the occurrence of evident deformations in July highlights that the regulation plan for water level in the flood season is important for controlling the deformation of slope deposits, where the fluctuation of the water level is no more than 10 m in the operation period.
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影响因子:
6.7
作者:
A. Chelli;G. Mandrone;G. Truffelli
通讯作者:
A. Chelli;G. Mandrone;G. Truffelli
影响因子:
6.7
作者:
D. M. Duc
通讯作者:
D. M. Duc
DOI:
10.1007/978-3-642-32238-9_42
发表时间:
2013
期刊:
--
影响因子:
--
作者:
Masao Yamada;Kensuke Ichikawa;Takeshi Kuwano;Tomonari Takeuchi;Atsushi Nakagawa
通讯作者:
Masao Yamada;Kensuke Ichikawa;Takeshi Kuwano;Tomonari Takeuchi;Atsushi Nakagawa
DOI:
--
发表时间:
2011
期刊:
Journal of Sichuan University
影响因子:
--
作者:
Huang Run-qiu
通讯作者:
Huang Run-qiu
DOI:
10.1659/mrd.mm068
发表时间:
2010-05
期刊:
--
影响因子:
--
作者:
D. Petley
通讯作者:
D. Petley