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PREDICTION OF POREWATER PRESSURES IN THE CORE OF EARTH DAMS DURING CONSTRUCTION

机译:施工期土石坝中水压力的预测

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摘要

The stability of an earth dam with respect to a slope or foundation failure depends to a large extent on the pore pressures. During construction, it has been recognized that the positive and sometimes alarmingly high porewater pressures, associated with progressive consolidation, develop in impervious sections of some earth dams before there is any water in the reservoir to cause seepage pressures. The intensity and distribution of the pressures depend not only on the consolidation characteristics of the materials, which are changing as the dam is being constructed, and on the drainage conditions, but also to a large extent on the rate of construction. The pressures, which may develop at a given dam, can be predicted by analysis, and can be observed by piezometers during construction. The prediction is based on the adaptation of the theories of consolidation and the flow of water through porous media subject to the internal and external boundary conditions, and on a knowledge of the stress-deformation pore-pressure characteristics of the materials. A numerical technique was developed and a computer program was written to model the generation and dissipation of porewater pressures during construction. In this technique, a zoned dam and its foundation are discretized into elements. Each element is characterized by its geometry, total unit weight, cohesion and friction angle, horizontal and vertical hydraulic conductivity, maximum shear and bulk moduli, and initial degree of saturation and porosity. For a given time history of fill elevation, the analysis provides variations of pore pressures with time in the core of a dam. At each time step, the program calculates the total stresses as well as generation and dissipation of porewater pressures. The calculation cycle is repeated for the entire history of fill elevation. In this repetitive manner, the calculation marches with time providing deformations and movemnents of assemblage of elements in two-dimensional space. As time proceeds, static equilibrium of the dam is developed naturally. Analysis results are given for the West Dam of Diamond Valley Lake, California, to demonstrate the intensity and distribution of the porewater pressures during construction and compare them with the observed values from vibrating wire piezometers.
机译:土坝相对于边坡或基础破坏的稳定性在很大程度上取决于孔隙压力。在施工过程中,已经认识到,在水库中没有水引起渗流压力之前,一些土坝的不透水部分会出现与逐步固结相关的正,有时甚至是令人震惊的高孔隙水压力。压力的强度和分布不仅取决于材料的固结特性(随着大坝的建造而变化)以及排水条件,而且在很大程度上取决于施工速度。可以通过分析预测在给定大坝上可能产生的压力,并且可以在施工过程中通过压力计进行观察。该预测是基于固结理论和通过内部和外部边界条件的水通过多孔介质的流动的理论的适应,以及对材料的应力变形孔隙压力特性的了解。开发了一种数字技术,并编写了计算机程序来模拟施工过程中孔隙水压力的产生和消散。在这种技术中,分区坝及其基础被离散化为元素。每个元素的特征是其几何形状,总单位重量,内聚力和摩擦角,水平和垂直导水率,最大剪切模量和体积模量以及初始饱和度和孔隙度。对于给定的填充高度时间历史记录,该分析提供了坝心中孔隙压力随时间的变化。在每个时间步,程序都会计算总应力以及孔隙水压力的产生和消散。对整个填充高度历史记录重复计算周期。以这种重复的方式,计算随时间前进,从而在二维空间中提供了元素组合的变形和运动。随着时间的流逝,大坝的静态平衡自然发展。给出了加利福尼亚钻石谷湖西水坝的分析结果,以证明施工过程中孔隙水压力的强度和分布,并将其与振动线压计的观测值进行比较。

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