Experimental and Numerical Simulation Study of Water Infiltration Impact on Soil-Pile Interaction in Expansive Soil

IF 1.2 4区 地球科学 Q3 GEOCHEMISTRY & GEOPHYSICS Geofluids Pub Date : 2024-01-17 DOI:10.1155/2024/6642676
Waleed Awadalseed, Xingli Zhang, Yunpeng Ji, XiangJin Wang, Yuntian Bai, Honghua Zhao
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Abstract

A laboratory model of a single pile embedded in Nanyang expansive soil and subjected to water infiltration is applied in this study to examine the interaction between the expansive soil and pile foundation upon water infiltration. The soil matric suction decreases as a result of the rising soil-water content. The amount of soil ground heave reaches its peak of 10.7 mm after 200 hours of water infiltration. As matric suction decreases, pile shaft friction also declines, which causes more of the load at the pile head to be carried by the pile base resulting in more pile settlements. A new numerical simulation method is provided to simulate this issue by coupling the subsurface flow, soil deformation, and hygroscopic swelling to investigate the expansive soil-pile response upon water infiltration. From the numerical simulation model, hygroscopic strain arises as a result of elevated moisture levels resulting from the entry of water, and due to ground heave and the mobilization of lateral soil swelling, the shear stress at the interface between the soil and the pile gradually increases over time. It reaches its maximum value of 4420 Pa at upper depths around 200 hours after the infiltration. The comparison between the lab model testing data and the numerical model results demonstrates a good level of concurrence.

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水渗透对膨胀土中土桩相互作用影响的实验和数值模拟研究
本研究应用了一个单桩嵌入南阳膨胀土并承受水渗透的实验室模型,以检验水渗透时膨胀土与桩基之间的相互作用。土壤母吸力随着土壤含水量的增加而减小。渗水 200 小时后,土壤地表隆起量达到峰值 10.7 毫米。随着基底吸力的减小,桩轴摩擦力也随之减小,从而导致桩头的荷载更多地转移到桩基上,造成更多的桩基沉降。本文提供了一种新的数值模拟方法,通过耦合地下流动、土壤变形和吸湿膨胀来模拟这一问题,从而研究水渗入时膨胀土-桩的响应。从数值模拟模型中可以看出,吸湿应变是由于水的进入导致湿度升高而产生的,由于地表隆起和土体横向膨胀的作用,土体与桩体界面处的剪应力随着时间的推移逐渐增大。在渗水后 200 小时左右,上部深度的剪应力达到最大值 4420 Pa。实验室模型试验数据与数值模型结果之间的比较显示出了良好的一致性。
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来源期刊
Geofluids
Geofluids 地学-地球化学与地球物理
CiteScore
2.80
自引率
17.60%
发文量
835
期刊介绍: Geofluids is a peer-reviewed, Open Access journal that provides a forum for original research and reviews relating to the role of fluids in mineralogical, chemical, and structural evolution of the Earth’s crust. Its explicit aim is to disseminate ideas across the range of sub-disciplines in which Geofluids research is carried out. To this end, authors are encouraged to stress the transdisciplinary relevance and international ramifications of their research. Authors are also encouraged to make their work as accessible as possible to readers from other sub-disciplines. Geofluids emphasizes chemical, microbial, and physical aspects of subsurface fluids throughout the Earth’s crust. Geofluids spans studies of groundwater, terrestrial or submarine geothermal fluids, basinal brines, petroleum, metamorphic waters or magmatic fluids.
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