Magnitude-frequency relationship of debris flows in the Jiangjia Gully, China

被引:0
|
作者
GAO Yan-chao [1 ,2 ,3 ]
CHEN Ning-sheng [1 ]
HU Gui-sheng [1 ]
DENG Ming-feng [1 ,3 ]
机构
[1] Key Laboratory of Mountain Hazards and Land Surface Process, Institute of Mountain Hazards and Environment, CAS
[2] Chengdu Center,China Geological Survey
[3] University of Chinese Academy of Sciences
基金
中国国家自然科学基金;
关键词
Debris flow; Magnitude; Cumulative frequency; Drainage area; Precipitation; Jiangjia Gully;
D O I
暂无
中图分类号
P642.23 [泥石流];
学科分类号
0837 ;
摘要
The magnitude-frequency(MF) relationship of debris flows is the basis for engineering designs and risk quantification. However, because of the lack of debris flow monitoring data, research progress in this area has been relatively slow. The MF relationship of debris flows in Jiangjia Gully, Yunnan Province was evaluated based on a regression analysis of 178 debris flow events that occurred from 1987-2004. The magnitude-cumulative frequency(MCF) relationship of the debris flows in the Jiangjia Gully is consistent with the linear logarithmic transformation function. Moreover, observed data for debris flows in Hunshui Gully of Yunnan Province and Huoshao Gully, Liuwan Gully, and Niwan Gully of Gansu Province were used to verify the function. The results showed that the MCF relationship of highfrequency debris flows is consistent with the power law equation, although the regression coefficients in the equation are considerably different. Further analysis showed a strong correlation between the differences in the constants and the drainage area and daily maximum precipitation.
引用
收藏
页码:1289 / 1299
页数:11
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