地质调查与研究Issue(1)：34-38,5.
北川县樱桃沟泥石流地质特征与动力学参数分析
Geological Characteristics and Dynamics Features of the Debris Flow in Yingtao Gully of Beichuan County, Sichuan Province
摘要
Abstract
The debris flow in Yingtao gully is a typical gully debris flow, which is located in Beichuan County,"5. 12"Earthquake epicenter, Sichuan Province. Based on the basic features of the valley, the characteristics of the debris flow and forming conditions like topography, water source and sediment sources, are firstly analyzed. Then according to the dynamic parameters, the bulk density, flow rate, flow capacity and sediment flush-out, are calculated. It is suggested that the fluid dense of debris flow is 1.686 t/m3,flow rate is 6.45 m/s, whole impact force is 35.56 kPa, maximum surge wave height is 0.72 m, debris flow climb-up is 1.15 m, super elevation in bend is 0.41 m. The results can offer theory basis for setting debris flow control structure reasonably.关键词
樱桃沟/泥石流/地质特征/动力学参数Key words
Yingtao gully/debris flow/geological characteristic/dynamic parameter分类
地质学引用本文复制引用
师书冉,涂良权,沈卫立..北川县樱桃沟泥石流地质特征与动力学参数分析[J].地质调查与研究,2014,(1):34-38,5.基金项目
四川省地震灾后恢复重建地质灾害防治专项 （）
