推导了渗流控制指标及渗流破坏的动力相似条件

S. Fukuoka, Kosuke Tabata
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引用次数: 1

摘要

建立汛期堤防渗流弱点估算方法,为流域准备大洪水时制定适当的堤防加固和风险管理措施提供依据。洪涝灾害发生时,堤体内具有较大潜水面梯度的内部水流往往集中在堤侧坡脚附近,可能引发堤溃。研究表明,堤防破坏思想对堤防渗流危险破坏位置的初步选择是有效的。首先,控制土壤渗流的唯一动态指标SFn(渗流数)是通过对一般渗流的理查兹控制方程进行无量纲化而得到的。其次,将SFn应用于堤防渗流,导出堤防易损指数t*,其表达式为动态无因次量。采用非定常准二维渗流分析方法,推导了透水地基上堤防的易损性指标。最后,对实际现场堤防和模型堤防试验中发生渗漏、滑动或崩塌溃决等各种破坏模式的脆弱性指数t*进行计算。由此证实,t*在相同破坏模式的现场堤防和模型堤防中呈现近似相同的值。由此证明,t*给出了渗流引起的堤防破坏现象和堤防破坏程度判断的动态相似条件。
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DERIVATION OF THE INDEX GOVERNING THE SEEPAGE FLOW AND DYNAMIC SIMILARITY CONDITION OF LEVEE FAILURES DUE TO SEEPAGE FLOW
It is necessary to establish an estimation method of levee weak points due to seepage flow during floods for making appropriate levee reinforcements and risk management measures in a river basin preparing for large-scale floods. The internal flow with large phreatic surface gradient in the body of the levee tends to concentrate around the landside toe of the levee during a flood event, which may trigger the levee failure. This study shows that the idea of the levee failure is effective for primary selection of dangerous levee failure positions to the seepage flow. First, the only dynamic index governing the seepage flow in soils, SFn (Seepage Flow number) is derived by nondimensionalizing Richards' governing equation for a general seepage flow. Next, by applying SFn to the seepage flow in the levee, levee vulnerability index t* is derived in the expression of a dynamic dimensionless quantity. Also, the vulnerability index of the levee on the permeable foundation is derived by using unsteady quasi two-dimensional seepage flow analysis method. Finally, the vulnerability index t* is calculated for the actual field levee and model levee experiment in which each failure mode such as leakage, sliding or collapse and breach occurred. As a result, it is confirmed that t* shows approximately common values in the field levee and model levee taking the same failure mode. Therefore, it is demonstrated that t* gives a dynamic similarity condition on the levee failure phenomena due to the seepage flow and the judge of the degree of levee failures.
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