Triggering conditions and depositional characteristics of a disastrous debris flow event in Zhouqu city, Gansu Province, northwestern China

On 7 August 2010, catastrophic debris flows were triggered by a rainstorm in the catchments of the Sanyanyu and Luojiayu torrents, Zhouqu County, Gansu Province northwestern China. These two debris flows originated shortly after a rainstorm with an intensity of 77.3 mm h<sup>−1<...

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Main Authors: C. Tang, N. Rengers, Th. W. J. van Asch, Y. H. Yang, G. F. Wang
Format: Article
Language:English
Published: Copernicus Publications 2011-11-01
Series:Natural Hazards and Earth System Sciences
Online Access:http://www.nat-hazards-earth-syst-sci.net/11/2903/2011/nhess-11-2903-2011.pdf
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spelling doaj-1e6ffda9ca5d414697ce69e043ef77152020-11-24T23:32:45ZengCopernicus PublicationsNatural Hazards and Earth System Sciences1561-86331684-99812011-11-0111112903291210.5194/nhess-11-2903-2011Triggering conditions and depositional characteristics of a disastrous debris flow event in Zhouqu city, Gansu Province, northwestern ChinaC. TangN. RengersTh. W. J. van AschY. H. YangG. F. WangOn 7 August 2010, catastrophic debris flows were triggered by a rainstorm in the catchments of the Sanyanyu and Luojiayu torrents, Zhouqu County, Gansu Province northwestern China. These two debris flows originated shortly after a rainstorm with an intensity of 77.3 mm h<sup>−1</sup> and transported a total volume of about 2.2 million m<sup>3</sup>, which was deposited on an existing debris fan and into a river. This catastrophic event killed 1765 people living on this densely urbanised fan. The poorly sorted sediment contains boulders up to 3–4 m in diameter. In this study, the geomorphological features of both debris flow catchment areas are analyzed based on the interpretation of high-resolution remote sensing imagery combined with field investigation. The characteristics of the triggering rainfall and the initiation of the debris flow occurrence are discussed. Using empirical equations, the peak velocities and discharges of the debris flows were estimated to be around 9.7 m s<sup>−1</sup> and 1358 m<sup>3</sup> s<sup>−1</sup> for the Sanyanyu torrent and 11 m s<sup>−1</sup> and 572 m<sup>3</sup> s<sup>−1</sup> for the Luojiayu torrent. The results of this study contribute to a better understanding of the conditions leading to catastrophic debris flow events.http://www.nat-hazards-earth-syst-sci.net/11/2903/2011/nhess-11-2903-2011.pdf
collection DOAJ
language English
format Article
sources DOAJ
author C. Tang
N. Rengers
Th. W. J. van Asch
Y. H. Yang
G. F. Wang
spellingShingle C. Tang
N. Rengers
Th. W. J. van Asch
Y. H. Yang
G. F. Wang
Triggering conditions and depositional characteristics of a disastrous debris flow event in Zhouqu city, Gansu Province, northwestern China
Natural Hazards and Earth System Sciences
author_facet C. Tang
N. Rengers
Th. W. J. van Asch
Y. H. Yang
G. F. Wang
author_sort C. Tang
title Triggering conditions and depositional characteristics of a disastrous debris flow event in Zhouqu city, Gansu Province, northwestern China
title_short Triggering conditions and depositional characteristics of a disastrous debris flow event in Zhouqu city, Gansu Province, northwestern China
title_full Triggering conditions and depositional characteristics of a disastrous debris flow event in Zhouqu city, Gansu Province, northwestern China
title_fullStr Triggering conditions and depositional characteristics of a disastrous debris flow event in Zhouqu city, Gansu Province, northwestern China
title_full_unstemmed Triggering conditions and depositional characteristics of a disastrous debris flow event in Zhouqu city, Gansu Province, northwestern China
title_sort triggering conditions and depositional characteristics of a disastrous debris flow event in zhouqu city, gansu province, northwestern china
publisher Copernicus Publications
series Natural Hazards and Earth System Sciences
issn 1561-8633
1684-9981
publishDate 2011-11-01
description On 7 August 2010, catastrophic debris flows were triggered by a rainstorm in the catchments of the Sanyanyu and Luojiayu torrents, Zhouqu County, Gansu Province northwestern China. These two debris flows originated shortly after a rainstorm with an intensity of 77.3 mm h<sup>−1</sup> and transported a total volume of about 2.2 million m<sup>3</sup>, which was deposited on an existing debris fan and into a river. This catastrophic event killed 1765 people living on this densely urbanised fan. The poorly sorted sediment contains boulders up to 3–4 m in diameter. In this study, the geomorphological features of both debris flow catchment areas are analyzed based on the interpretation of high-resolution remote sensing imagery combined with field investigation. The characteristics of the triggering rainfall and the initiation of the debris flow occurrence are discussed. Using empirical equations, the peak velocities and discharges of the debris flows were estimated to be around 9.7 m s<sup>−1</sup> and 1358 m<sup>3</sup> s<sup>−1</sup> for the Sanyanyu torrent and 11 m s<sup>−1</sup> and 572 m<sup>3</sup> s<sup>−1</sup> for the Luojiayu torrent. The results of this study contribute to a better understanding of the conditions leading to catastrophic debris flow events.
url http://www.nat-hazards-earth-syst-sci.net/11/2903/2011/nhess-11-2903-2011.pdf
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