Shi Min, Yang Yuesuo, Wang Dianlong, Wu Yuhui, Zhang Xi, Lu Ying
School of Environmental Science and Engineering, Southern University of Science and Technology, Shenzhen, 518055, China; Guangdong Provincial Key Laboratory of Soil and Groundwater Pollution Control, School of Environmental Science and Engineering, Southern University of science and Technology, Shenzhen 518055, China; Jilin Provincial Key Laboratory of Water Resources and Environment, Jilin University, Changchun 130021, China.
Jilin Provincial Key Laboratory of Water Resources and Environment, Jilin University, Changchun 130021, China.
Water Res. 2025 Sep 1;283:123778. doi: 10.1016/j.watres.2025.123778. Epub 2025 May 9.
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.
注入井周围过滤器和多孔介质中的铁沉积物会导致严重堵塞,从而限制地下水热泵(GWHP)系统的可持续性。在浅层富铁含水层注水过程中,铁堵塞在其组成和形成过程方面呈现出时空演变。本研究采用二维砂槽实验和连续多组分地下水,以探究注入井周围堵塞的时空演变。结果表明,上层堵塞主要由高结晶度的铁氧化物、针铁矿和纤铁矿主导,主要是由过滤器的氧化腐蚀引起的。下层堵塞的演变分阶段进行,具有明显的物质-机制-影响关系。初始阶段(0-15天):堵塞物由早期注水期间氧气富集和CO₂消耗诱导产生的碳酸钙和低结晶度铁氧化物组成,导致水头差增加10%。中期阶段(15-35天):随着水动力变化提高了pH值和氧化还原电位,微生物聚集体、SiO₂和低结晶度铁氧化物占主导地位,加速了微生物生长和铁氧化物沉积,使水头差放大到60%。稳定阶段(35天后):微生物群落分泌的生物膜和胞外聚合物(EPS)巩固了孔隙堵塞,维持了稳定的水力阻力。每个阶段从非生物矿物沉淀过渡到生物强化堵塞,通过协同的物理化学和微生物过程逐渐限制渗透率。本研究突出了对浅层富铁含水层中注入井内铁堵塞演变的新认识,并提出了针对堵塞缓解和控制的区域和阶段特定策略。