基于孔隙介质饱和-非饱和渗流理论,将物理模型试验与数值模拟相结合,研究了库水位周期升降时,粘土心墙坝上游坝壳浸润线及坝坡稳定性的变化规律及其影响因素。结果表明,坝体内部的渗流场较库水位变化具有滞后性。上游坝壳渗透系数是影响浸润线位置和坝坡稳定性的主要因素,上游坝壳渗透系数小1个数量级,上游浸润线位置要高2.60~3.00 m
Rowshon Jadid,Brina M. Montoya,Victoria Bennett,Mohammed A. Gabr.Effect of repeated rise and fall of water level on seepage-induced deformation and related stability analysis of Princeville levee[J].Engineering Geology,2020.
Shuyang Yu,Xuhua Ren,Jixun Zhang,Haijun Wang,Junlei Wang,Wenwei Zhu.Seepage, Deformation, and Stability Analysis of Sandy and Clay Slopes with Different Permeability Anisotropy Characteristics Affected by Reservoir Water Level Fluctuations[J].Water,2020.