Connectivity of earthquake-triggered landslides with the fluvial network: Implications for landslide sediment transport after the 2008 Wenchuan earthquake

doi:10.1002/2015JF003718

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	Connectivity of earthquake-triggered landslides with the fluvial network: Implications for landslide sediment transport after the 2008 Wenchuan earthquake
	Li, Gen 1; West, A. Joshua 1; Densmore, Alexander L.2,3; Hammond, Douglas E.1; Jin, Zhangdong 4; Zhang, Fei 4; Wang, Jin 4; Hilton, Robert G.2,3
	2016-04-01
发表期刊	JOURNAL OF GEOPHYSICAL RESEARCH-EARTH SURFACE
卷号	121 期号:4 页码:703-724
文章类型	Article
摘要	Evaluating the influence of earthquakes on erosion, landscape evolution, and sediment-related hazards requires understanding fluvial transport of material liberated in earthquake-triggered landslides. The location of landslides relative to river channels is expected to play an important role in postearthquake sediment dynamics. In this study, we assess the position of landslides triggered by the M-w 7.9 Wenchuan earthquake, aiming to understand the relationship between landslides and the fluvial network of the steep Longmen Shan mountain range. Combining a landslide inventory map and geomorphic analysis, we quantify landslide-channel connectivity in terms of the number of landslides, landslide area, and landslide volume estimated from scaling relationships. We observe a strong spatial variability in landslide-channel connectivity, with volumetric connectivity (xi) ranging from similar to 20% to similar to 90% for different catchments. This variability is linked to topographic effects that set local channel densities, seismic effects (including seismogenic faulting) that regulate landslide size, and substrate effects that may influence both channelization and landslide size. Altogether, we estimate that the volume of landslides connected to channels comprises 43 + 9/-7% of the total coseismic landslide volume. Following the Wenchuan earthquake, fine-grained (90% of the total landslide volume) may be more significantly affected by landslide locations.
WOS标题词	Science & Technology ; Physical Sciences
DOI	10.1002/2015JF003718
关键词[WOS]	TEMPERATE MONTANE FOREST ; MOUNTAIN DRAINAGE BASINS ; THRESHOLD HILLSLOPES ; TIBETAN PLATEAU ; GROUND MOTION ; EROSION ; TOPOGRAPHY ; EVOLUTION ; DENSITY ; TAIWAN
收录类别	SCI
语种	英语
WOS研究方向	Geology
WOS类目	Geosciences, Multidisciplinary
WOS记录号	WOS:000382579600004
引用统计	被引频次：84[WOS] [WOS记录] [WOS相关记录]
文献类型	期刊论文
条目标识符	http://ir.ieecas.cn/handle/361006/5677
专题	加速器质谱中心
作者单位	1.Univ So Calif, Dept Earth Sci, Los Angeles, CA 90007 USA 2.Univ Durham, Inst Hazard Risk & Resilience, Durham, England 3.Univ Durham, Dept Geog, Durham, England 4.Chinese Acad Sci, Inst Earth Environm, State Key Lab Loess & Quaternary Geol, Xian, Peoples R China
推荐引用方式 GB/T 7714	Li, Gen,West, A. Joshua,Densmore, Alexander L.,et al. Connectivity of earthquake-triggered landslides with the fluvial network: Implications for landslide sediment transport after the 2008 Wenchuan earthquake[J]. JOURNAL OF GEOPHYSICAL RESEARCH-EARTH SURFACE,2016,121(4):703-724.
APA	Li, Gen.,West, A. Joshua.,Densmore, Alexander L..,Hammond, Douglas E..,Jin, Zhangdong.,...&Hilton, Robert G..(2016).Connectivity of earthquake-triggered landslides with the fluvial network: Implications for landslide sediment transport after the 2008 Wenchuan earthquake.JOURNAL OF GEOPHYSICAL RESEARCH-EARTH SURFACE,121(4),703-724.
MLA	Li, Gen,et al."Connectivity of earthquake-triggered landslides with the fluvial network: Implications for landslide sediment transport after the 2008 Wenchuan earthquake".JOURNAL OF GEOPHYSICAL RESEARCH-EARTH SURFACE 121.4(2016):703-724.