ISSN 1000-3665 CN 11-2202/P

    基于原位浸水载荷试验的风积砂湿陷特性及评价模型

    Collapsibility characteristics and factor analysis of aeolian sand based on in-situ water immersion load test

    • 摘要: 目前湿陷性研究主要集中在黄土,风积砂也有湿陷性,但是研究内容主要为特定地区的湿陷影响因素研究,毛乌素沙漠南缘风积砂的湿陷特性、湿陷机理及评价方法研究还较欠缺,阻碍了沙漠地区开发油气资源及建设油气场站的发展。以毛乌素沙漠南缘风积砂为研究对象,基于原位浸水载荷试验及室内基本物理性质试验,研究了风积砂的湿陷程度与湿陷变形特性,分析了含水率、干密度、孔隙比、饱和度与湿陷系数的关系;采用多元线性回归方法,建立了主要物性指标与湿陷系数之间的多元线性回归关系。结果表明:(1)研究区风积砂湿陷程度主要为轻微湿陷,少部分为无湿陷。(2)原位浸水载荷试验所得到的荷载-沉降量曲线呈折线型,可分为线弹性变形阶段、弹塑性变形阶段和湿陷变形阶段,主要对应荷载为0~100 kPa、100~200 kPa、>200 kPa;浸水段沉降量-时间曲线呈折线型,可分为浸水骤降段和变形稳定段,前150 min湿陷变形随浸水历时增加而骤增,随后湿陷变形逐渐平稳。(3)风积砂湿陷系数与初始含水率、饱和度及干密度呈负相关关系,与孔隙比呈正相关关系。(4)基于多元线性回归的风积砂湿陷性评价模型能够较好地预测湿陷系数,拟合度为0.879,未来可通过扩大样本量和引入非线性回归方法进一步提升模型的普适性和准确性。研究结果可为毛乌素沙漠地区工程建设提供理论依据,为同类型场地湿陷性研究提供借鉴。

       

      Abstract: The collapsibility of aeolian sand poses significant challenges to oil and gas resource development and the construction of related infrastructure in desert regions. This study focused on aeolian sand distributed along the southern margin of the Mu Us Desert. A combination of in-situ immersion load tests and laboratory physical property analyses was conducted to investigate the collapsibility characteristics and deformation behavior of the sand. The relationships between collapsibility and variables such as water content, dry density, porosity, and saturation were analyzed. Furthermore, a multiple linear regression (MLR) method was established to quantify the relationship between major physical indices and the collapsibility coefficient. It shows that the collapsibility of aeolian sand in this area is mainly slight, with a small proportion classified as non-collapsible. The load-settlement curve obtained from in-situ immersion loading test exhibits a polygonal pattern, which can be divided into three distinct stages: the linear elastic deformation stage (0−100 kPa), the elastoplastic deformation stage (100−200 kPa), and the collapse deformation stage (>200 kPa). Similarly, the immersion-induced settlement-time curve demonstrates a segmented characteristic, consisting of a rapid collapse phase during immersion (0−150 min) followed by a deformation stabilization phase. Notably, the collapse deformation shows a dramatic increase during the initial 150 minutes of immersion, then progressively stabilizes with prolonged immersion duration. The collapsibility coefficient of aeolian sand presents a negative correlation with initial water content, saturation, and dry density, but a positive correlation with porosity. The collapsibility evaluation model of aeolian sand based on multivariate linear regression can predict the collapsibility coefficient well, with a fitting degree of 0.879. In the future, the universality and accuracy of the model can be further improved by expanding the sample size and introducing nonlinear regression methods. These results provide a theoretical foundation for engineering projects in the Mu Us Desert and offer valuable insights into the collapsibility behavior of aeolian sand at similar sites.

       

    /

    返回文章
    返回