地质污染地下水中抗生素耐药性与砷代谢基因的相互作用:对砷迁移的影响

IF 5.9 1区 地球科学 Q1 ENGINEERING, CIVIL Journal of Hydrology Pub Date : 2024-12-12 DOI:10.1016/j.jhydrol.2024.132509
Junna Ning, Kunfu Pi, Xianjun Xie, Qianyong Liang, Philippe Van Cappellen, Yanxin Wang
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引用次数: 0

摘要

在受扰动的含水层环境中,地源性污染物和新出现的污染物经常同时出现,使地源性污染地下水的演变复杂化,并由此给人类带来健康风险。发现抗菌素耐药性(AMR)的发展影响了负责砷(As)动员的关键微生物活动,但从有限的实地调查中,潜在的过程和机制仍然被低估。通过联合野外实验、分子生物学分析和水文地球化学模拟,本研究为砷与抗生素交叉抗性对地下水中砷的生物转化和富集的影响提供了新的见解。盆地尺度的水文地质调查表明,第四纪地层的岩性特征和与之相关的区域地下水流动状况导致抗生素和砷浓度从补给区向排放区逐渐增加。地下水中抗生素耐药基因(ARGs)在补给区呈点状分布,而在排放区呈累积分布趋势。结果表明,在高剂量抗生素环境胁迫下,地下水中微生物介导的Fe(III)-氧化物还原受到抑制,而在高剂量抗生素环境胁迫下,微生物的SO42-还原得以维持。此外,ARGs积累后可能产生交叉抗性,从而促进As的生物转化和再迁移。因此,砷富集的主要机制可能从微生物对铁(III)氧化物的溶解转变为args驱动的砷在受抗生素影响的含水层中的生物迁移。这些发现突显了抗生素污染严重地区AMR对地源砷污染地下水演化的影响被低估。这项研究还保证了在受干扰的含水层环境中对原位地下水修复方法进行仔细的重新评估。
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Interactions between antibiotic resistance and arsenic metabolizing genes in geogenic contaminated groundwater: Consequence for arsenic migration
Geogenic contaminants and emerging contaminants co-occur frequently in disturbed aquifer environments, complicating the evolution of geogenic contaminated groundwater and resultant health risk posed to human beings. The development of antimicrobial resistance (AMR) was found to affect critical microbial activities responsible for arsenic (As) mobilization, yet the underlying processes and mechanism remain undervalued from limited field investigation. By virtue of joint field campaign, molecular biological analysis, and hydrogeochemical modeling, this research provides novel insights into influence of cross-resistance between As and antibiotics on As biotransformation and enrichment in groundwater. Our basin-scale hydrogeological investigation reveals that lithological characteristics of Quaternary formations and associated regional groundwater flow regime led to gradual co-increase of antibiotic and As concentrations from recharge area to discharge area. While antibiotic resistance genes (ARGs) in groundwater exhibited spotty distribution pattern in the recharge area, they tended to accumulate in the discharge area. Consequently, microbially-mediated Fe(III)-oxide reduction was inhibited in groundwater subject to high-level antibiotics, whereas microbial SO42- reduction was sustained under high-antibiotic environmental stress. Moreover, cross-resistance was likely to develop after the accumulation of ARGs, thereby enhancing As biotransformation and re-migration. Hence, primary mechanism underlying As enrichment probably shifted from microbial dissolution of Fe(III) oxides to ARGs-driven As bio-migration in antibiotic-affected aquifers. These findings highlight the underestimated impact of AMR on evolution of geogenic As-contaminated groundwater in areas with significant antibiotic pollution. This research additionally warrants a careful re-assessment of in-situ groundwater remediation approaches in disturbed aquifer environments.
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来源期刊
Journal of Hydrology
Journal of Hydrology 地学-地球科学综合
CiteScore
11.00
自引率
12.50%
发文量
1309
审稿时长
7.5 months
期刊介绍: The Journal of Hydrology publishes original research papers and comprehensive reviews in all the subfields of the hydrological sciences including water based management and policy issues that impact on economics and society. These comprise, but are not limited to the physical, chemical, biogeochemical, stochastic and systems aspects of surface and groundwater hydrology, hydrometeorology and hydrogeology. Relevant topics incorporating the insights and methodologies of disciplines such as climatology, water resource systems, hydraulics, agrohydrology, geomorphology, soil science, instrumentation and remote sensing, civil and environmental engineering are included. Social science perspectives on hydrological problems such as resource and ecological economics, environmental sociology, psychology and behavioural science, management and policy analysis are also invited. Multi-and interdisciplinary analyses of hydrological problems are within scope. The science published in the Journal of Hydrology is relevant to catchment scales rather than exclusively to a local scale or site.
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