Catastrophic debris flows triggered by a 14 August 2010 rainfall at the epicenter of the Wenchuan earthquake

Abstract

Catastrophic debris flows triggered by a 14 August 2010 rainfall at the epicenter of the Wenchuan earthquakeAbstract The Wenchuan earthquake of May 12, 2008 produced large amounts of loose material (landslide debris) that are still present on the steep slopes and in the gullies. This loose material creates an important hazard as strong rainfall can cause the development of devastating debris flows that will endanger the resettled population and destroy the result of reconstruction efforts. On 14 August 2010, a total of 21 debris flows were triggered by heavy rainfall around the town of Yingxue, located near the epicenter of the Wenchuan earthquake. One of these debris flows produced a debris dam, which then changed the course of the river and resulted in the flooding of the newly reconstructed Yinxue town. Prior to this catastrophic event, debris flow hazard had been recognized in the region, but its potential for such widespread and devastating impacts was not fully appreciated. Our primary objective for this study was to analyze the characteristics of the triggering rainfall and the sediment supply conditions leading to this event. Our field observations show that even small debris flow catchment areas have caused widespread sediment deposition on the existing fans. It is concluded that the whole of the area shaken by the Wenchuan earthquake is more susceptible to debris flows, initiated by localized heavy rainfall, than had been assumed earlier. The results of this study contribute to a better understanding of the conditions leading to catastrophic debris flow events in the earthquake-hit area. This is essential for the implementation of proper early warning, prevention, and mitigation measures as well as a better land use planning in this area.

Two multi-temporal datasets that track the enhanced landsliding after the 2008 Wenchuan earthquake

“…We believe that this important step will promote the standardisation of data collection and presentation, and facilitate meta-analyses and modelling efforts greatly. Several inven-tories were compiled for the Wenchuan earthquake-affected area (Gorum et al, 2011;Dai et al, 2011;Li et al, 2014;Tang et al, 2016). Landslides were mapped either as points (identifying the landslide scar) or polygons, with different degrees of accuracy (see Tang et al, 2016) and with or without distinction between landslide types (slides, flows, etc.).…”

Monitoring Earthquake-Damaged Vegetation after the 2008 Wenchuan Earthquake in the Mountainous River Basins, Dujiangyan County

“…Hence, large amounts of unconsolidated materials deposited on the steep slopes, which changed the hydrological processes (i.e., infiltration reduced, run-off increased and flow concentration expedited ) in the catchment [6]. Existing research indicates that the combination of steep slope, abundant fragmented materials, and high intensity rainfall naturally leads to the catastrophic debris flows in the earthquake-hit area [2,[42][43][44].…”

Mechanical state of gravel soil in mobilization of rainfall-induced landslides in the Wenchuan seismic area, Sichuan province, China

“…Based on the field surveys along Duwen highway, Niujuan valley and the literature review Fang et al, 2012;Tang et al, 2011;Yu et al, 2010), most of the rainfallinduced landslides are shallow. The range of the slope angle is 25-40 • , and its average value is 27 • .…”