石流是一个汉语词语，读音是shí liú，指石山中的溪流。
水石流是秦岭山地泥石流主要类型之一。 分布广泛，发育典型，灾害严重。
Water-rock debris flow is a main type of debris flow in Qinling mountain with a wide distribution, typical development and serious disaster.
针对水石流颗粒粗、粘性小的特点，提出了利用水槽进行分段模拟水石流的设想。
In light of thicker grain and smaller viscosity of debris flow, a segmented simulation of the debris flow with flume is presented.
研究表明，水石流中细颗粒的存在，其输沙浓度比相同纵坡下没有细颗粒时有很大提高。
It is found that due to the existence of fine particles in flow, the transport concentration of solid will increase with the same slope of gully.
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