长江科学院院报 ›› 2009, Vol. 26 ›› Issue (10): 92-94.

• 全国水利工程渗流学术会专辑 • 上一篇    下一篇

非稳定渗流期骤降判别及均质土坝稳定分析

 王民侠, 张荣斌   

  • 出版日期:2009-10-01 发布日期:2012-07-03

Judgment of Reservoir Water level Sudden Drop and Stability Analysis of Homogeneous Earth Dam during Unsteady Seepage

 WANG  Min-Xia, ZHANG  Rong-Bin   

  • Online:2009-10-01 Published:2012-07-03

摘要: 在均质土坝设计中,水位骤降通常是拟定上游边坡时需控制的工况。水位降落期浸润线位置判别和确定,为大坝稳定计算提供依据,合理判别水位降落速度是浸润线计算的关键步骤,为此,用k/μv表示库水位相对于渗流自由面下降的速度,以区别库水位是缓降、快降还是骤降,并以此来判别和计算浸润线。渗透系数k值一般可通过试验给出比较精确的数值;给水度μ是确定浸润线位置的关键参数;黏性土μ值的研究目前还没有比较完善的确定方法。此次研究采用了公式计算和查表对比的方法确定合适的给水度值,并用不同公式进行了水位下降快慢的判别,提出了水位骤降期坝型调整和稳定计算指标合理性问题。

Abstract:  In the homogeneous earth dam design, reservoir water level sudden drawdown is often a control condition of the upstream slope. The judgment and determination of the wetting front location will provide a basis for dam stability calculation during reservoir water level lowering and a reasonably judging lowering rate of water level is a key step for calculating wetting front. The k/μv represents the rate of reservoir water level being relative to seepage free surface decline, which is used for distinguishing different drops of water level: gradual drop, quick drop or sudden drop, and from this value, the saturation line can be calculated. The permeability coefficient k can be given precisely by the test;the storativity μ is a key parameter to determine the saturation line location, but there is no perfect method to identify μ, and then this paper uses a suitable contrast value obtained from the formula calculation and relative table;the rate v to determine the pace of water level decline is given by different formulas. So, an issue on the reasonable judgment of damtype and the rational choice of stability calculation indexes during water level sudden drop is proposed.