Zi-Ye Wang, Jun-Cheng Liu, Yong Tan, Ying-Ying Long
{"title":"Experimental and numerical investigation on internal erosion induced by infiltration of defective buried pipe","authors":"Zi-Ye Wang, Jun-Cheng Liu, Yong Tan, Ying-Ying Long","doi":"10.1007/s10064-024-04073-2","DOIUrl":null,"url":null,"abstract":"<div><p>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.</p></div>","PeriodicalId":500,"journal":{"name":"Bulletin of Engineering Geology and the Environment","volume":"84 1","pages":""},"PeriodicalIF":3.7000,"publicationDate":"2025-01-03","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Bulletin of Engineering Geology and the Environment","FirstCategoryId":"5","ListUrlMain":"https://link.springer.com/article/10.1007/s10064-024-04073-2","RegionNum":2,"RegionCategory":"工程技术","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q3","JCRName":"ENGINEERING, ENVIRONMENTAL","Score":null,"Total":0}
引用次数: 0
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.
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.