Spatial features of debris flows and their rainfall thresholds in the Wenchuan earthquake-affected area

被引:38
作者
Guo, Xiaojun [1 ,2 ,3 ]
Cui, Peng [1 ,2 ,4 ]
Li, Yong [1 ,2 ]
Zhang, Jianqiang [1 ,2 ]
Ma, Li [5 ]
Mahoney, William B. [6 ]
机构
[1] Chinese Acad Sci, Inst Mt Hazards & Environm, Key Lab Mt Surface Proc & Hazards, Chengdu 610041, Peoples R China
[2] Asian Network Debris Flow, Chengdu 610041, Peoples R China
[3] Univ Chinese Acad Sci, Beijing 100049, Peoples R China
[4] Chinese Acad Sci, Ctr Excellencein Tibetan Plateau Earth Sci, Beijing 100101, Peoples R China
[5] Sichuan Meteorol Adm, Chengdu 610072, Peoples R China
[6] Int Eros Control Assoc, Denver, CO 80207 USA
关键词
Debris flow; I-D relationship; Spatial distribution; Rainfall; Wenchuan earthquake; SHALLOW LANDSLIDES; DURATION CONTROL; INTENSITY; INITIATION;
D O I
10.1007/s10346-015-0608-z
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
The 2008 Wenchuan earthquake greatly altered the thresholds for rainfall-triggered debris flows within the affected area. Debris flows were widely and densely distributed, and they exhibited a range of differing local rainfall thresholds. This study looked at 518 debris flow events that occurred post-earthquake in order to analyze their spatial characteristics. The duration D (in h) and the average rainfall intensity I (in mm/h) that triggered the debris flows were determined for 252 of these events in order to analyze the spatial features of rainfall thresholds. Results show that 49 % of debris flows occurred in the highest-intensity seismic zone, 58 % occurred within 10 km of active faults, and 49 % occurred in areas with humid climate. Rainfall thresholds in these three regions were persistently lower than others. Moreover, debris flows were most frequent in watersheds smaller than 5 km(2), and rainfall thresholds tended to decrease with a decrease in watershed size. Given the abundant loose materials available throughout the study area, 11 extreme debris flow-prone sub-regions were selected to illustrate the spatial features of rainfall thresholds in relation to local climate conditions. The lowest and highest I-D thresholds in the sub-regions examined were I = 5.94D (-0.70) (2 < D < 53) and I = 21.4D (-0.58) (3 < D < 50), respectively. The lowest and mean rainfall intensities needed to trigger debris flows were power-related with the local maximum 1- and 24-h rainfall. By normalizing the rainfall intensity (I) by mean annual precipitation (MAP), the I (MAP)-D thresholds were determined. Normalized results showed that the lowest and highest I (MAP)-D thresholds were I (MAP) = 0.0034D (-0.55) (2 < D < 53) and I (MAP) = 0.0090D (-0.40) (3 < D < 51), respectively. Such results are useful for debris flow forecasting based on empirical rainfall thresholds and have implications for hazard and risk assessment in this region.
引用
收藏
页码:1215 / 1229
页数:15
相关论文
共 45 条
[1]   A warning system for rainfall-induced shallow failures [J].
Aleotti, P .
ENGINEERING GEOLOGY, 2004, 73 (3-4) :247-265
[2]  
[Anonymous], NEW J TRADIT CHIN ME
[3]  
[Anonymous], 2009, ATLAS SEISMOLOGICAL
[4]  
[Anonymous], SICHUAN J MT SCI
[5]   Rainfall thresholds for the possible occurrence of landslides in Italy [J].
Brunetti, M. T. ;
Peruccacci, S. ;
Rossi, M. ;
Luciani, S. ;
Valigi, D. ;
Guzzetti, F. .
NATURAL HAZARDS AND EARTH SYSTEM SCIENCES, 2010, 10 (03) :447-458
[6]  
Burchfiel B.C., 1995, INT GEOL REV, V37, P661, DOI [DOI 10.1080/00206819509465424, 10.1080/00206819509465424]
[7]   THE RAINFALL INTENSITY - DURATION CONTROL OF SHALLOW LANDSLIDES AND DEBRIS FLOWS [J].
CAINE, N .
GEOGRAFISKA ANNALER SERIES A-PHYSICAL GEOGRAPHY, 1980, 62 (1-2) :23-27
[8]   Storm rainfall conditions for floods and debris flows from recently burned areas in southwestern Colorado and southern California [J].
Cannon, Susan H. ;
Gartner, Joseph E. ;
Wilson, Raymond C. ;
Bowers, James C. ;
Laber, Jayme L. .
GEOMORPHOLOGY, 2008, 96 (3-4) :250-269
[9]   Rainfall duration and debris-flow initiated studies for real-time monitoring [J].
Chen, CY ;
Chen, TC ;
Yu, FC ;
Yu, WH ;
Tseng, CC .
ENVIRONMENTAL GEOLOGY, 2005, 47 (05) :715-724
[10]  
[陈兴长 Chen Xingzhang], 2011, [地理科学, Scientia Geographica Sinica], V31, P1500