首页> 外文会议>2011 International Symposium on Water Resource and Environmental Protection >Forming conditions and movement features of debris flow disasters in East Channel of Yuanfang in PingShan County of HeBei Province
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Forming conditions and movement features of debris flow disasters in East Channel of Yuanfang in PingShan County of HeBei Province

机译:河北省屏山县原坊东航道泥石流灾害形成条件及运动特征

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The formation mechanism and dynamics features of the debris flow were analyzed based on the survey of a debris flow site in East Channel of Yuanfang in Pingshan County. This paper adopted rain-flood modifying and mud trace investigation methods of making the known rainstorm characteristic values under different design frequencies to translate into responding flood peak value flux. This method educed some characteristic values about debris flow peak value flux, including the gross amount of transporting sand etc. In addition, the occurring frequencies analysis of debris flow was valuated on engineering projects. According to movement feature, this debris flow break out at 50 years return period, and the scale of this debris flow is medium, and its development trend has been accelerated. Meanwhile, engineering and biological measures should be combined on the prevention of debris flow.
机译:在对平山县圆方东航道泥石流场进行调查的基础上,分析了泥石流的形成机理和动力学特征。本文采用雨洪改造和泥质痕量调查方法,将不同设计频率下的已知暴雨特征值转化为响应洪峰峰值通量。该方法得出了泥石流峰值通量的一些特征值,包括运沙总量等。此外,还对工程中泥石流的发生频率进行了评估。根据运动特征,该泥石流在50年的返还期就爆发了,该泥石流的规模中等,其发展趋势得到了加速。同时,在防治泥石流方面应结合工程和生物学措施。

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