viscous debris flow

基本解釋

Intermittent debris flow is the most important moving form of viscous debris flows.
陣流是黏性泥石流的主要運(yùn)動(dòng)形式。
Some investigators maintain that large boulders must be supported by turbulence within a viscous debris flow .
有些調(diào)查者認(rèn)爲(wèi)大漂礫是通過粘性泥石流中的渦流搬運(yùn)的。
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The debris flow gullies of Banzi, Taoguan and Chediguan generate low frequency and low viscous debris flows or hyper-concentrated flows with an average interval of 20~50 years.
板子溝、桃關(guān)溝和徹底關(guān)溝均爲(wèi)低頻率泥石流或高含沙洪水，平均20～50年發(fā)生一次；