(1. School of Civil Engineering and Architecture, Xi?an University of Technology, Xi?an, Shaanxi 710048, China; 2. State Key Laboratory of Water Engineering Ecology and Environment in Arid Area, Xi'an University of Technology,
Xi?an, Shaanxi 710048, China; 3. Institute of New Energy Engineering, POWERCHINA Beijing Engineering
Corporation Limited, Beijing 100024, China)
Abstract:Considering the impact of particle non-uniformity on the tortuosity of soil is one approach to enhance the predictive accuracy of soil hydraulic conductivity. In response, a theoretical equation predicting average tortuosity was initially derived based on boundary layer theory and geometric analysis. This equation incorporates ten typical flow paths under varying conditions of particle overlap, selected from the pores of a representative element volume. Additionally, assemblies of square particles with different lengths were numerically simulated using COMSOL Multiphysics software. Several soil column flow tests were conducted under various rainfall intensities. The calculated curves from the proposed equation were then compared with these data, including both previously published simulation and test results. The results indicate that the proposed equation is well-suited to describe the evolution of hydraulic conductivity concerning porosity, as well as the large particle volume fraction and seepage drop relative to flow velocity. Further analysis of the effect of the particle length ratio reveals that soil tortuosity decreases with increasing ratios until this trend stabilizes. Finally, the proposed equation was used to predict the hydraulic conductivity of dam materials in the earth-rock dam with a straight core wall at Nuozhadu Hydropower Station. It was found that the proposed equation outperforms previously published equations due to its consideration of soil particle non-uniformity.
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