冰碛湖溃决型泥石流演化过程试验研究

党超; 褚娜娜

doi:10.13961/j.cnki.stbctb.2015.04.007

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冰碛湖溃决型泥石流演化过程试验研究

试验研究

- 冰碛湖溃决型泥石流演化过程试验研究
- Experimental Study on Evolution of Debris Flow Induced by Moraine Lake Outburst Floods
- 水土保持通报 2015年35卷第4期页码：29-33
- 作者机构：
  
  1. 三峡库区地质灾害教育部重点试验室,湖北,宜昌,443002
  2. 三峡大学土木与建筑学院,湖北,宜昌,443002
- 作者简介：
- 基金信息：
  
  湖北省教育厅科学技术研究计划优秀中青年人才项目"滑坡堰塞坝溃决预测模型的不确定性和非线性研究"(20151207)
- DOI：10.13961/j.cnki.stbctb.2015.04.007
  中图分类号：
- 纸质出版：2015
- 稿件说明：
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党超, 褚娜娜. 冰碛湖溃决型泥石流演化过程试验研究[J]. 水土保持通报, 2015,35(4):29-33.

DANG Chao, CHU Nana. Experimental Study on Evolution of Debris Flow Induced by Moraine Lake Outburst Floods[J]. Bulletin of Soiland Water Conservation, 2015, 35(4): 29-33.
党超, 褚娜娜. 冰碛湖溃决型泥石流演化过程试验研究[J]. 水土保持通报, 2015,35(4):29-33. DOI： 10.13961/j.cnki.stbctb.2015.04.007.

DANG Chao, CHU Nana. Experimental Study on Evolution of Debris Flow Induced by Moraine Lake Outburst Floods[J]. Bulletin of Soiland Water Conservation, 2015, 35(4): 29-33. DOI： 10.13961/j.cnki.stbctb.2015.04.007.

摘要

[目的] 分析冰湖溃决型泥石流演化过程中运动参数的变化特征

为冰湖溃决型泥石流的防治提供理论依据。[方法] 采用水槽试验

探讨冰碛湖溃决型泥石流形成和演化过程。[结果] 冰碛湖溃决泥石流属于典型的水力类泥石流;根据水沙两相流容重的变化

冰碛湖溃决型洪水演化为泥石流的过程可以概括为挟沙水流-泥石流-挟沙水流的演变

相对应的泥石流的粒径从粉砂到砾石

再到粉沙的变化过程;泥石流容重越大

一次泥石流过程中颗粒粒径越粗。从不同组次的试验结果来看

冰碛湖溃决泥石流粒径与其容重也存在正相关关系。[结论] 泥石流的运动和演化过程本质上取决于冰碛湖溃决型洪水功率和沟床堆积物的粒径特征。

Abstract

[Objective] Studying the characteristics of motion and evolution parameters of debris flow induced by glacier lake outburst floods(GLOFs) in order to provide countermeasures for debris flows prevention of this type. [Methods] Base on flume tests

the formation and evolution of debris flow due to moraine lake outburst floods were studied. [Results] The debris flow evolved from GLOFs was attributed to hydraulic reasons

the forming process could be divided into 5 phases. According to unit weight of water-sediment flow

the evolution process of debris flow could be summarized by successive sediment-laden flow

debris flow

sediment-laden flow. Correspondingly

The grain sizes of debris flow evolved from silts to gravels

and to silts in sequence. The outcomes from different sets of the test also showed that the grain sizes of the debris flow positively correlated to the unit weigh of the debris flow. [Conclusion] The motion processes of debris flow depend both on the hydraulic power of the GLOFs and on the grain sizes of bed materials.

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Keywords

references

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