Gomez-Alvarez Vicente, Liu Hong, Pressman Jonathan G, Wahman David G
Center for Environmental Solutions & Emergency Response, U.S. Environmental Protection Agency, Cincinnati, Ohio 45268, United States.
Oak Ridge Institute for Science and Education (ORISE), Post-Doctoral Fellow at U.S. Environmental Protection Agency, Cincinnati, Ohio 45268, United States.
ACS ES T Water. 2021;1(5):1283-1294. doi: 10.1021/acsestwater.1c00016.
Sediment accumulation in drinking water storage facilities may lead to water quality degradation, including biological growth and disinfectant decay. The current research evaluated the microbiome present in a sediment after sequential exposure to monochloramine, free chlorine, and monochloramine. Chemical profiles within the sediment based on microelectrodes showed evidence of nitrification, and monochloramine slowly penetrated the sediment but was not measurable at lower depths. A metagenomic approach was used to characterize the microbial communities and functional potential of top (0-1 cm) and bottom (1-2 cm) layers in sediment cores. Differential abundance analysis revealed both an enrichment and depletion associated with depth of microbial populations. We assembled 30 metagenome-assembled genomes (MAGs) representing bacterial and archaeal microorganisms. Most metabolic functions were represented in both layers, suggesting the capability of the microbiomes to respond to environmental fluctuations. However, niche-specific abundance differences were identified in biotransformation processes (e.g., nitrogen). Metagenome-level analyses indicated that nitrification and denitrification can potentially occur simultaneously in the sediments, but the exact location of their occurrence within the sediment will depend on the localized physicochemical conditions. Even though monochloramine was maintained in the bulk water there was limited penetration into the sediment, and the microbial community remained functionally diverse and active.
饮用水储存设施中的沉积物积累可能导致水质恶化,包括生物生长和消毒剂衰减。当前的研究评估了沉积物在依次暴露于一氯胺、游离氯和一氯胺后存在的微生物群落。基于微电极的沉积物化学剖面显示出硝化作用的证据,一氯胺缓慢渗透到沉积物中,但在较浅深度无法检测到。采用宏基因组学方法来表征沉积物岩芯顶部(0-1厘米)和底部(1-2厘米)层的微生物群落和功能潜力。差异丰度分析揭示了与微生物种群深度相关的富集和耗竭情况。我们组装了30个代表细菌和古细菌微生物的宏基因组组装基因组(MAG)。大多数代谢功能在两层中都有体现,这表明微生物群落有能力应对环境波动。然而,在生物转化过程(如氮)中发现了特定生态位的丰度差异。宏基因组水平的分析表明,硝化作用和反硝化作用可能在沉积物中同时发生,但其在沉积物中的具体发生位置将取决于局部的物理化学条件。尽管一氯胺在主体水中得以维持,但对沉积物的渗透有限,并且微生物群落仍然功能多样且活跃。