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基于核磁共振的土体孔隙水形态与渗透性研究

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为探究水力梯度及孔隙水形态对土体渗透性的影响,测定重塑土样在0~500 kPa等8级吸力作用下的核磁共振T2曲线;将孔隙水划分为可动水和不动水,定量分析可动水与吸力/水力梯度关系,并将水力梯度、可动水引入Coates渗透模型进行修正.结果表明:随着吸力从0 kPa增加至500 kPa(水力梯度从0增加到50),土体T2曲线面积和T2最大值逐渐减小,T2最小值几乎不变;可动水含量随吸力/水力梯度的增加先迅速增大,随后增速减小,最后趋于稳定,二者之间可用指数函数很好地拟合;不动水含量随吸力/水力梯度增加呈指数减小;可动水与不动水比值(FFI/BVI)和水力梯度呈良好的线性关系;简化Coates模型显示土体渗透率与水力梯度的二次方成正比;孔径是影响孔隙水渗流的关键因素,吸力/水力梯度作用下,土体孔隙水排出过程可用Young-Laplace方程描述,土体孔隙水由大孔隙开始排水,并逐渐向小孔隙发展,大孔隙先完成排水过程;水力梯度的增大会提高可动水占比,导致更多可动水参与渗流作用,导致土体渗透率显著增大;简化Coates模型直观展示了水力梯度-孔隙水形态-渗透率关系,该模型仅含有水力梯度一个未知数,可为路基稳定性分析与防护设计提供理论参考.
NMR-Based Study on Pore Water Form and Permeability of Soil
In order to explore the effects of hydraulic gradient and pore water form on soil permeability,the NMR T2 curves of disturbed soil are measured under 8 kinds of suction such as 0-500 kPa.The pore water is divided into movable water and immobile water,the relationship between movable water and suction/hydraulic gradient is quantitatively analyzed,and the hydraulic gradient and movable water are introduced into Coates permeability model to be corrected.The result shows that (1) the T2 curve area of soilmass and the maximum value of T2 gradually decrease as the suction increases from 0 kPa to 500 kPa ( the hydraulic gradient increases from 0 to 50),and the minimum value of T2 is almost unchanged;(2) with the increase of suction/hydraulic gradient,the movable water first increases rapidly,then increases slowly,and tends to be stable finally;(3) these two can be well fitted with an exponential function,and the immobile water content decreases exponentially with the increase of suction/hydraulic gradient;(4) the ratio of movable water to immovable water (FFI/BVI) and hydraulic gradient is fitted with a linear function;(5) the simplified Coates model shows that the permeability of soil is directly proportional to the quadratic hydraulic gradient;(6) pore radius is the key factor affecting seepage of soil,under the influence of suction/hydraulic gradient,the process of water drainage can be described with Young-Laplace equation,the pore water starts to drain from macropores and gradually develops to micro-pores,and the macro-pores complete the drainage process firstly;(7) the increase of hydraulic gradient raises the proportion of movable water,leading to more movable water participating in seepage and a significantly increase of soil permeability.The simplified Coates model visually shows the relationship among hydraulic gradient,pore water form and permeability,containing only an unknown ( hydraulic gradient ),and providing a theoretical reference for subgrade stability analysis and protection design.

road engineeringpermeability modelnuclear magnetic resonancehydraulic gradientpore water form

钟悦鹏、冯楚桥

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江西省赣南公路勘察设计院有限公司,江西 赣州 341000

华南理工大学 土木与交通学院,广东 广州 510641

武汉大学 水资源与水电工程科学国家重点实验室,湖北 武汉 430070

道路工程 渗透率模型 核磁共振 (NMR) 水力梯度 孔隙水形态

国家自然科学基金项目

51809200

2024

公路交通科技
交通运输部公路科学研究院

公路交通科技

CSTPCD北大核心
影响因子:1.007
ISSN:1002-0268
年,卷(期):2024.41(7)
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