Min Shi, Yuesuo Yang, Dianlong Wang, Yuhui Wu, Xi Zhang, Ying Lu
{"title":"浅层富铁含水层地下水补给过程中注水井周围铁堵塞机制:来自时空演化的洞察","authors":"Min Shi, Yuesuo Yang, Dianlong Wang, Yuhui Wu, Xi Zhang, Ying Lu","doi":"10.1016/j.watres.2025.123778","DOIUrl":null,"url":null,"abstract":"Iron deposits in the filters and porous media around injection wells could induce severe clogging, thereby limiting the sustainability of groundwater heat pump (GWHP) systems. During the water injection in shallow iron-rich aquifers, iron clogging exhibits both spatial and temporal evolution in terms of its composition and formation processes. This study employed a two-dimensional sand tank experiment with continuous multicomponent groundwater to explore the spatiotemporal evolution of clogging around the injection well. The results suggested that upper-layer clogging was dominated by high-crystallinity iron oxides, goethite, and lepidocrocite, primarily caused by oxidation corrosion of filter. The evolution of lower-layer clogging occurred in stages with distinct material-mechanism-impact relationships. The initial phase (0–15 days): clogging comprised of calcium carbonate and low-crystallinity iron oxides induced by oxygen enrichment and CO₂ depletion during the early injection period, causing a 10% hydraulic head difference to increase. Mid-stage (15–35 days): microbial aggregates, SiO₂, and lower-crystallinity iron oxides dominated as hydrodynamic shifts elevated pH and redox potential, accelerating microbial growth and iron oxide deposition, amplifying hydraulic head difference to 60%. Stabilization phase (after 35 days): biofilms and extracellular polymeric substances (EPS) secretion by microbial communities consolidated pore occlusion, sustaining stable hydraulic resistance. Each stage transitioned from abiotic mineral precipitation to biologically reinforced clogging, progressively restricting permeability through synergistic physicochemical and microbial processes. This study highlighted a novel understanding of the evolution of iron clogging within an injection well located in a shallow iron-rich aquifer, and proposed region- and stage-specific strategies for clogging mitigation and control.","PeriodicalId":443,"journal":{"name":"Water Research","volume":"110 1","pages":""},"PeriodicalIF":11.4000,"publicationDate":"2025-05-06","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Iron clogging mechanism around injection wells during groundwater recharge in shallow iron-rich aquifer: insight from spatiotemporal evolution\",\"authors\":\"Min Shi, Yuesuo Yang, Dianlong Wang, Yuhui Wu, Xi Zhang, Ying Lu\",\"doi\":\"10.1016/j.watres.2025.123778\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"Iron deposits in the filters and porous media around injection wells could induce severe clogging, thereby limiting the sustainability of groundwater heat pump (GWHP) systems. During the water injection in shallow iron-rich aquifers, iron clogging exhibits both spatial and temporal evolution in terms of its composition and formation processes. This study employed a two-dimensional sand tank experiment with continuous multicomponent groundwater to explore the spatiotemporal evolution of clogging around the injection well. The results suggested that upper-layer clogging was dominated by high-crystallinity iron oxides, goethite, and lepidocrocite, primarily caused by oxidation corrosion of filter. The evolution of lower-layer clogging occurred in stages with distinct material-mechanism-impact relationships. The initial phase (0–15 days): clogging comprised of calcium carbonate and low-crystallinity iron oxides induced by oxygen enrichment and CO₂ depletion during the early injection period, causing a 10% hydraulic head difference to increase. Mid-stage (15–35 days): microbial aggregates, SiO₂, and lower-crystallinity iron oxides dominated as hydrodynamic shifts elevated pH and redox potential, accelerating microbial growth and iron oxide deposition, amplifying hydraulic head difference to 60%. Stabilization phase (after 35 days): biofilms and extracellular polymeric substances (EPS) secretion by microbial communities consolidated pore occlusion, sustaining stable hydraulic resistance. Each stage transitioned from abiotic mineral precipitation to biologically reinforced clogging, progressively restricting permeability through synergistic physicochemical and microbial processes. This study highlighted a novel understanding of the evolution of iron clogging within an injection well located in a shallow iron-rich aquifer, and proposed region- and stage-specific strategies for clogging mitigation and control.\",\"PeriodicalId\":443,\"journal\":{\"name\":\"Water Research\",\"volume\":\"110 1\",\"pages\":\"\"},\"PeriodicalIF\":11.4000,\"publicationDate\":\"2025-05-06\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Water Research\",\"FirstCategoryId\":\"93\",\"ListUrlMain\":\"https://doi.org/10.1016/j.watres.2025.123778\",\"RegionNum\":1,\"RegionCategory\":\"环境科学与生态学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q1\",\"JCRName\":\"ENGINEERING, ENVIRONMENTAL\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Water Research","FirstCategoryId":"93","ListUrlMain":"https://doi.org/10.1016/j.watres.2025.123778","RegionNum":1,"RegionCategory":"环境科学与生态学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"ENGINEERING, ENVIRONMENTAL","Score":null,"Total":0}
Iron clogging mechanism around injection wells during groundwater recharge in shallow iron-rich aquifer: insight from spatiotemporal evolution
Iron deposits in the filters and porous media around injection wells could induce severe clogging, thereby limiting the sustainability of groundwater heat pump (GWHP) systems. During the water injection in shallow iron-rich aquifers, iron clogging exhibits both spatial and temporal evolution in terms of its composition and formation processes. This study employed a two-dimensional sand tank experiment with continuous multicomponent groundwater to explore the spatiotemporal evolution of clogging around the injection well. The results suggested that upper-layer clogging was dominated by high-crystallinity iron oxides, goethite, and lepidocrocite, primarily caused by oxidation corrosion of filter. The evolution of lower-layer clogging occurred in stages with distinct material-mechanism-impact relationships. The initial phase (0–15 days): clogging comprised of calcium carbonate and low-crystallinity iron oxides induced by oxygen enrichment and CO₂ depletion during the early injection period, causing a 10% hydraulic head difference to increase. Mid-stage (15–35 days): microbial aggregates, SiO₂, and lower-crystallinity iron oxides dominated as hydrodynamic shifts elevated pH and redox potential, accelerating microbial growth and iron oxide deposition, amplifying hydraulic head difference to 60%. Stabilization phase (after 35 days): biofilms and extracellular polymeric substances (EPS) secretion by microbial communities consolidated pore occlusion, sustaining stable hydraulic resistance. Each stage transitioned from abiotic mineral precipitation to biologically reinforced clogging, progressively restricting permeability through synergistic physicochemical and microbial processes. This study highlighted a novel understanding of the evolution of iron clogging within an injection well located in a shallow iron-rich aquifer, and proposed region- and stage-specific strategies for clogging mitigation and control.
期刊介绍:
Water Research, along with its open access companion journal Water Research X, serves as a platform for publishing original research papers covering various aspects of the science and technology related to the anthropogenic water cycle, water quality, and its management worldwide. The audience targeted by the journal comprises biologists, chemical engineers, chemists, civil engineers, environmental engineers, limnologists, and microbiologists. The scope of the journal include:
•Treatment processes for water and wastewaters (municipal, agricultural, industrial, and on-site treatment), including resource recovery and residuals management;
•Urban hydrology including sewer systems, stormwater management, and green infrastructure;
•Drinking water treatment and distribution;
•Potable and non-potable water reuse;
•Sanitation, public health, and risk assessment;
•Anaerobic digestion, solid and hazardous waste management, including source characterization and the effects and control of leachates and gaseous emissions;
•Contaminants (chemical, microbial, anthropogenic particles such as nanoparticles or microplastics) and related water quality sensing, monitoring, fate, and assessment;
•Anthropogenic impacts on inland, tidal, coastal and urban waters, focusing on surface and ground waters, and point and non-point sources of pollution;
•Environmental restoration, linked to surface water, groundwater and groundwater remediation;
•Analysis of the interfaces between sediments and water, and between water and atmosphere, focusing specifically on anthropogenic impacts;
•Mathematical modelling, systems analysis, machine learning, and beneficial use of big data related to the anthropogenic water cycle;
•Socio-economic, policy, and regulations studies.