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沟道松散堆积物形成泥石流的水动力条件分析及其数学模型

The Deposite Analysis of Water Dynamic Conditions to Form Debris Flow and to Set up Mathematical Model in Debris Flow Valley

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【作者】 解明曙王玉杰张洪江赵院赵合理

【Author】 Xie Mingshu Wang Yujie Zhang Hongjiang(College of Soil and Water Conservation, BFU, Beijing, 100083)Zhao Yuan(The Middle Reaches of the Yellow River Controling Agency, Xi’an 710000)Zhao Heli(Northwest Institute of Soil and Water Conservation, Yangling, Shaanxi, 712100)

【机构】 北京林业大学水土保持学院水利部黄委会黄河中游治理局中科院西北水保所 西安 710000陕西杨陵 712100

【摘要】 以泥沙运动和泥石流形成的理论力学为基础,重点论证了固相松散堆积物构成准泥石流体的条件,进行了相应的起动需水量模拟实验.通过准泥石流体屈服方程的建立,做出了武都地区泥石流沟道中准泥石流体起动数学模型,为该地区预报泥石流灾害发生发展提供了一定的科学依据.

【Abstract】 Based upon the theoretical mechanics of forming debris flow and silt movement,the paper proves mainly deposite conditions to form para-debris flowing body,and the simulated test of requiring water to start debris flow is also discussed.By setting up the yield equation of the pare-debris flowing body,the mathematical model of starting para-debris flow has been finished in debris flow valley of Wudu district,Gansu province.The model could be used to provide scientific basis for forecasting,the calamity of debris flow in the region.

【基金】 水利部长江水土保持局资助项目
  • 【文献出处】 北京林业大学学报 ,Journal of Beijing Forestry University , 编辑部邮箱 ,1993年04期
  • 【分类号】P642.23
  • 【被引频次】33
  • 【下载频次】386
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