Experimental and numerical investigation on internal erosion induced by infiltration of defective buried pipe

IF 3.7 2区 工程技术 Q3 ENGINEERING, ENVIRONMENTAL Bulletin of Engineering Geology and the Environment Pub Date : 2025-01-03 DOI:10.1007/s10064-024-04073-2
Zi-Ye Wang, Jun-Cheng Liu, Yong Tan, Ying-Ying Long
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Abstract

Soil erosion induced by infiltration of a buried defective pipe is closely related to leaking locations, whereas it has received inadequate attention in literature. In this paper, the distinct effects of various leaking locations on internal erosion are investigated extensively using both experimental tests and numerical simulations. First, a series of experimental model tests are carried out to characterize the evolution of ground collapses due to pipe leaking at different defect locations and to quantify the related soil–water loss (SWL). The experimental results indicate that the defect location has a significant effect on the SWL rate and ground collapse. When the leaking location is changed from the pipe crown to its invert, both the soil- and water-loss rates accelerate dramatically, followed by a more severe ground collapse. Then, a validated two-dimensional (2D) finite-difference method and discrete-element method (FDM-DEM) coupling model is established to explore the distributions of earth pressure (EP), water pressure (WP) and water-earth pressure (WEP) against the pipe and to disclose the influence mechanism of different leaking locations. It is found that EP and WEP in the proximity of the defect reduce significantly after pipe leaking, while EP away from the defect increases due to seepage force and soil arching effect. In addition, the distribution of EP against the defective pipe during internal erosion can be divided into three typical zones: fluctuation, soil arching and stable zones. The findings of this study will be helpful for researchers and practitioners to understand the internal erosion of strata triggered by infiltration of defective buried pipeline.

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缺陷埋管入渗引起内侵蚀的试验与数值研究
埋置缺陷管道入渗引起的土壤侵蚀与泄漏位置密切相关,但文献对其重视不足。本文采用试验和数值模拟两种方法,广泛研究了不同泄漏位置对内侵蚀的不同影响。首先,进行了一系列的试验模型试验,表征了不同缺陷位置管道泄漏引起的地面塌陷的演变过程,并量化了相关的水土流失(SWL)。试验结果表明,缺陷位置对地基的SWL速率和地面塌陷有显著影响。当泄漏位置由管顶改为管顶时,土壤和水的流失速度急剧加快,随之而来的是更严重的地面塌陷。然后,通过验证二维有限差分法和离散元法(FDM-DEM)耦合模型,探索管道上土压力(EP)、水压力(WP)和水-土压力(WEP)的分布,揭示不同泄漏位置的影响机理。发现管道泄漏后,缺陷附近的EP和WEP显著降低,而远离缺陷的EP由于渗流力和土拱效应而增加。此外,内部侵蚀过程中对缺陷管道的EP分布可分为波动区、土拱区和稳定区三个典型区。本文的研究结果将有助于研究人员和实践人员了解埋地管道缺陷入渗引发的地层内部侵蚀。
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来源期刊
Bulletin of Engineering Geology and the Environment
Bulletin of Engineering Geology and the Environment 工程技术-地球科学综合
CiteScore
7.10
自引率
11.90%
发文量
445
审稿时长
4.1 months
期刊介绍: Engineering geology is defined in the statutes of the IAEG as the science devoted to the investigation, study and solution of engineering and environmental problems which may arise as the result of the interaction between geology and the works or activities of man, as well as of the prediction of and development of measures for the prevention or remediation of geological hazards. Engineering geology embraces: • the applications/implications of the geomorphology, structural geology, and hydrogeological conditions of geological formations; • the characterisation of the mineralogical, physico-geomechanical, chemical and hydraulic properties of all earth materials involved in construction, resource recovery and environmental change; • the assessment of the mechanical and hydrological behaviour of soil and rock masses; • the prediction of changes to the above properties with time; • the determination of the parameters to be considered in the stability analysis of engineering works and earth masses.
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