稀性泥石流（diluted debris flow）又称紊流型泥石流（turbulence mudflow）。固体物质含量较低（体积分数10%～40%），容重1.3～1.5吨/立方米，黏度小于0.3帕·秒的泥石流。
试验表明，稀性泥石流阵性的起因首先决定于流域内形成的原始出流过程。
It is made clear that the formation of debris surge is firstly determined by the original hydrograph of the basin.
通过室内模型试验研究，对不同规模的水石流、稀性泥石流、黏性泥石流在堆积扇上输沙特征进行了研究。
The transporting characteristics of debris flow of different types (viscous, diluent and water stone) at Guxiang accumulation fan in the Tibet Autonomous region are studied by indoor model tests.
应用推荐