ISSN 1003-8035 CN 11-2852/P

    地下水位回升与降雨入渗作用下西安黄土地裂缝场地变形规律研究

    Study on the regularity of rainfall infiltration and deformation in ground fissure zones of loess in Xi’an City under the background of rising groundwater level

    • 摘要: 研究旨在探讨地下水位回升与降雨入渗共同作用下西安黄土地裂缝场地变形规律。在梳理西安地裂缝灾害、地下水位和降雨等特征的基础上,基于室内土工试验,研究了地裂缝带黄土的物理力学特性和湿陷特征,并利用有限差分数值模拟研究了地下水位回升背景下西安市黄土地裂缝场地的降雨入渗变形规律。研究结果表明:西安市地裂缝场地的黄土湿陷性强且抗拉强度低;在降雨入渗作用下,黄土地裂缝场地产生“悬臂梁式”变形,地层形变量为毫米级;而在地下水位回升和降雨入渗共同作用下,黄土地裂缝场地形变量可达数厘米,且以受拉破坏为主,上盘受拉强度高于下盘。以上结果表明,地下水位回升与降雨入渗产生协同放大效应,导致黄土地裂缝场地受拉破坏风险增大。

       

      Abstract: This study aims to investigate the deformation patterns of loess ground fissure sites in Xi’an under the combined effects of rising groundwater levels and rainwater infiltration. Based on the characterization of ground fissure disasters, groundwater levels, and rainfall, and supported by laboratory geotechnical tests, the physical-mechanical properties and collapsibility characteristics of the loess in fissured zones were studied. Moreover, finite difference numerical simulations were employed to analyze the deformation behavior induced by rainwater infiltration under the influence of groundwater level rise at the loess fissure sites of Xi’an. The results indicate that the loess in these fissured sites exhibits strong collapsibility and low tensile strength. Under rainfall infiltration alone, the loess fissure zones exhibit “cantilever beam” type deformation, with with displacements on the order of millimeters. Under the combined effects of rising groundwater levels and rainfall infiltration, deformation magnitues can reach several centimeters, predominantly resulting in tensile failure, with the upper layer demonstrating higher tensile strength than the lower layer. These findings suggest that the synergistic interaction of groundwater level rise and rainwater infiltration produces a amplification effect, and increases the risk of tensile failure in loess ground fissure areas.

       

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