Case study of a giant debris flow in the Wenjia Gully, Sichuan Province, China

Bin Yu (), Yu Ma and Yufu Wu

Natural Hazards: Journal of the International Society for the Prevention and Mitigation of Natural Hazards, 2013, vol. 65, issue 1, 835-849

Abstract: The debris flow, which was triggered in the Wenjia Gully on August 13, 2010, is an extreme example of mass movement events, which occurred after the Wenchuan earthquake of May 12, 2008. This Earthquake triggered in the Wenjia Gully the second largest co-seismic landslide, which can be classified as a rockslide-debris avalanche. A lot of loose sediments was deposited in the basin. In the main so called Deposition Area II of this landslide, with a volume of 30 × 10 6 m 3 , flash floods can easily trigger debris flows because of the steep bottom slope and the relative small grain sizes of the sediments. The largest debris flow of August 13, 2010 destroyed the most downstream dam in the catchment during a heavy rain storm. The debris flow with a peak discharge of 1,530 m 3 /s and a total volume of 3.1 × 10 6 m 3 caused the death of 7 persons, 5 persons were missing, 39 persons were injured and 479 houses buried. After three rainy seasons, only 16 % of the landslide-debris deposition was taken away by 5 large-scale debris flow events. Since the threshold for rainfall triggered debris flows in the Wenjia Gully and other catchments drastically decreased after the Wenchuan Earthquake, new catastrophic events are expected in the future during the rainy season. Copyright Springer Science+Business Media B.V. 2013

Keywords: Wenchuan earthquake; Wenjia Gully; Co-seismic rockslide-debris avalanche; Rainfall triggered debris flows; Yield strength; Peak discharges; Meteorological threshold for debris flows (search for similar items in EconPapers)
Date: 2013
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DOI: 10.1007/s11069-012-0395-y

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