{"title":"极端降雨条件下砂砾石支撑开挖穿墙冲刷破坏试验研究","authors":"Weizhen Jiang, Fangzhou Liu, Yong Tan","doi":"10.1007/s12665-025-12589-3","DOIUrl":null,"url":null,"abstract":"<div><p>Deep excavations in sandy gravel faced a high risk of seepage failure due to the increasing frequency of extreme rainfall events. Structural deficiencies in retaining walls, particularly leakage defects, exacerbated these failures by triggering through-wall leakage and subsurface erosion, resulting in hazardous ground movements that threaten nearby built environments. However, the influence of rainfall patterns, wall defects, and soil properties on erosion-induced instability remained insufficiently understood. This study conducted twelve reduced-scale 1<span>\\(\\:\\text{g}\\)</span> physical model tests to evaluate how defect dimensions, rainfall patterns, and gravel contents affect soil movements and structural performance under extreme rainfall. A semi-empirical ellipsoid-paraboloid model was developed to characterize the spatial and temporal evolution of erosion-induced failure zones. Key findings include: (1) the depth where defect was located was the dominant factor controlling erosion-induced soil movements, with defects at shallower depths accelerating erosion and surface subsidence due to reduced thickness of overlying soils; (2) rainfall patterns indirectly influenced erosion onset and surface instability timing by modulating groundwater responses, with the peak-advanced pattern intensifying hydraulic gradients and accelerating subsurface erosion zone development; and (3) the proposed model effectively described the transition from a confined ellipsoidal erosion cavity to an open paraboloidal failure zone in retained soil, driven by sapping erosion near the wall defect, matric suction loss, and rainwater scouring. These findings emphasized the critical role of defect geometry, hydraulic conditions, and soil gradings in erosion-induced excavation failures. The proposed framework offered a reference for predicting through-wall erosion failures and assessing instability in sandy gravel, providing insights that may contribute to climate change adaptation strategies and geotechnical risk mitigation in urban excavation projects.</p></div>","PeriodicalId":542,"journal":{"name":"Environmental Earth Sciences","volume":"84 20","pages":""},"PeriodicalIF":2.8000,"publicationDate":"2025-10-04","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Experimental investigation on through-wall erosion failure of braced excavation in sandy gravel under extreme rainfall\",\"authors\":\"Weizhen Jiang, Fangzhou Liu, Yong Tan\",\"doi\":\"10.1007/s12665-025-12589-3\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><p>Deep excavations in sandy gravel faced a high risk of seepage failure due to the increasing frequency of extreme rainfall events. Structural deficiencies in retaining walls, particularly leakage defects, exacerbated these failures by triggering through-wall leakage and subsurface erosion, resulting in hazardous ground movements that threaten nearby built environments. However, the influence of rainfall patterns, wall defects, and soil properties on erosion-induced instability remained insufficiently understood. This study conducted twelve reduced-scale 1<span>\\\\(\\\\:\\\\text{g}\\\\)</span> physical model tests to evaluate how defect dimensions, rainfall patterns, and gravel contents affect soil movements and structural performance under extreme rainfall. A semi-empirical ellipsoid-paraboloid model was developed to characterize the spatial and temporal evolution of erosion-induced failure zones. Key findings include: (1) the depth where defect was located was the dominant factor controlling erosion-induced soil movements, with defects at shallower depths accelerating erosion and surface subsidence due to reduced thickness of overlying soils; (2) rainfall patterns indirectly influenced erosion onset and surface instability timing by modulating groundwater responses, with the peak-advanced pattern intensifying hydraulic gradients and accelerating subsurface erosion zone development; and (3) the proposed model effectively described the transition from a confined ellipsoidal erosion cavity to an open paraboloidal failure zone in retained soil, driven by sapping erosion near the wall defect, matric suction loss, and rainwater scouring. These findings emphasized the critical role of defect geometry, hydraulic conditions, and soil gradings in erosion-induced excavation failures. The proposed framework offered a reference for predicting through-wall erosion failures and assessing instability in sandy gravel, providing insights that may contribute to climate change adaptation strategies and geotechnical risk mitigation in urban excavation projects.</p></div>\",\"PeriodicalId\":542,\"journal\":{\"name\":\"Environmental Earth Sciences\",\"volume\":\"84 20\",\"pages\":\"\"},\"PeriodicalIF\":2.8000,\"publicationDate\":\"2025-10-04\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Environmental Earth Sciences\",\"FirstCategoryId\":\"93\",\"ListUrlMain\":\"https://link.springer.com/article/10.1007/s12665-025-12589-3\",\"RegionNum\":4,\"RegionCategory\":\"环境科学与生态学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q3\",\"JCRName\":\"ENVIRONMENTAL SCIENCES\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Environmental Earth Sciences","FirstCategoryId":"93","ListUrlMain":"https://link.springer.com/article/10.1007/s12665-025-12589-3","RegionNum":4,"RegionCategory":"环境科学与生态学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q3","JCRName":"ENVIRONMENTAL SCIENCES","Score":null,"Total":0}
Experimental investigation on through-wall erosion failure of braced excavation in sandy gravel under extreme rainfall
Deep excavations in sandy gravel faced a high risk of seepage failure due to the increasing frequency of extreme rainfall events. Structural deficiencies in retaining walls, particularly leakage defects, exacerbated these failures by triggering through-wall leakage and subsurface erosion, resulting in hazardous ground movements that threaten nearby built environments. However, the influence of rainfall patterns, wall defects, and soil properties on erosion-induced instability remained insufficiently understood. This study conducted twelve reduced-scale 1\(\:\text{g}\) physical model tests to evaluate how defect dimensions, rainfall patterns, and gravel contents affect soil movements and structural performance under extreme rainfall. A semi-empirical ellipsoid-paraboloid model was developed to characterize the spatial and temporal evolution of erosion-induced failure zones. Key findings include: (1) the depth where defect was located was the dominant factor controlling erosion-induced soil movements, with defects at shallower depths accelerating erosion and surface subsidence due to reduced thickness of overlying soils; (2) rainfall patterns indirectly influenced erosion onset and surface instability timing by modulating groundwater responses, with the peak-advanced pattern intensifying hydraulic gradients and accelerating subsurface erosion zone development; and (3) the proposed model effectively described the transition from a confined ellipsoidal erosion cavity to an open paraboloidal failure zone in retained soil, driven by sapping erosion near the wall defect, matric suction loss, and rainwater scouring. These findings emphasized the critical role of defect geometry, hydraulic conditions, and soil gradings in erosion-induced excavation failures. The proposed framework offered a reference for predicting through-wall erosion failures and assessing instability in sandy gravel, providing insights that may contribute to climate change adaptation strategies and geotechnical risk mitigation in urban excavation projects.
期刊介绍:
Environmental Earth Sciences is an international multidisciplinary journal concerned with all aspects of interaction between humans, natural resources, ecosystems, special climates or unique geographic zones, and the earth:
Water and soil contamination caused by waste management and disposal practices
Environmental problems associated with transportation by land, air, or water
Geological processes that may impact biosystems or humans
Man-made or naturally occurring geological or hydrological hazards
Environmental problems associated with the recovery of materials from the earth
Environmental problems caused by extraction of minerals, coal, and ores, as well as oil and gas, water and alternative energy sources
Environmental impacts of exploration and recultivation – Environmental impacts of hazardous materials
Management of environmental data and information in data banks and information systems
Dissemination of knowledge on techniques, methods, approaches and experiences to improve and remediate the environment
In pursuit of these topics, the geoscientific disciplines are invited to contribute their knowledge and experience. Major disciplines include: hydrogeology, hydrochemistry, geochemistry, geophysics, engineering geology, remediation science, natural resources management, environmental climatology and biota, environmental geography, soil science and geomicrobiology.