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Basic characteristics and starting mode of debris flow in Tieshanzhang Mining Area under typhoon

机译:铁山张矿区台风泥石流的基本特征与始发模式。

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Through field investigation and test, the distribution characteristics, formation conditions, and starting mode of the typical mine debris flow in Tieshanzhang Mining Area were studied, and the density, flow velocity, flow, and other dynamical parameters of the debris flow were calculated based on the dynamic principle, which provided a reliable basis for the design of debris flow prevention engineering. The results showed that the debris flow was currently in the development stage, belonged to the rainstorm gully-shaped, high-frequency, non-viscous, mining slag debris flow, and its starting mode was collapsing-jamming-bursting type. From the topography point of view, large relative height difference of the gully basin, steep terrain, and large longitudinal slope of the gully helped the formation and starting of the debris flow; from the source point of view, arbitrary discharge of large-scale mining waste provided a rich loose solid source for the debris flow; heavy rainfall brought by landing of typhoon was a trigger for the debris flow.
机译:通过现场调查和试验,研究了铁山章矿区典型矿山泥石流的分布特征,形成条件和起爆方式,并基于此计算出泥石流的密度,流速,流量等动力参数。动态原理为泥石流防治工程的设计提供了可靠的依据。结果表明,泥石流目前处于发育阶段,属于暴雨沟状,高频,无粘性矿渣渣流,其起步方式为塌陷—突涌型。从地形角度看,沟壑盆地的相对高度差大,地形陡峭,沟壑的纵向坡度大,有助于泥石流的形成和开始。从源头上看,任意排放大型采矿废物为泥石流提供了丰富的疏松固体源。台风登陆带来的大雨是泥石流的诱因。

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