Zheng Wenjing, Chen Yan, Niu Yalin, Xu Pengcheng, Hao Huayi, Dong Bingzhi
Key Laboratory of Yellow River Water Environment in Gansu Province, Lanzhou Jiaotong University, Lanzhou 730070, China; College of Environment and Municipal Engineering, Lanzhou Jiaotong University, Lanzhou 730070, China.
Key Laboratory of Yellow River Water Environment in Gansu Province, Lanzhou Jiaotong University, Lanzhou 730070, China; College of Environment and Municipal Engineering, Lanzhou Jiaotong University, Lanzhou 730070, China.
Sci Total Environ. 2025 Jan 1;958:177891. doi: 10.1016/j.scitotenv.2024.177891. Epub 2024 Dec 7.
Seasonal fluctuations present significant challenges to drinking water treatment by altering the properties of Dissolved Organic Matter (DOM) within watersheds, thereby influencing the potential for disinfection by-product (DBP) formation. DOM is a complex mixture of organic matter that serves as a critical DBP precursor and is closely linked to adverse health outcomes. The prediction of DBP formation is complicated by the variability in DOM concentrations and compositions in lake source water, a situation exacerbated by seasonal changes in water systems. We examined the seasonality of lake DBP formation potential (DBPFP) and the dynamics of precursors across four distinct seasons based on water temperature. Utilizing the Excitation-Emission Matrix (EEM) coupled with parallel factorial (PARAFAC) analysis, three-dimensional fluorescence difference spectroscopy (3D-FDS), and molecular weight distribution (MWD), we elucidated the compositions and fates of lake DBP precursors. The findings revealed that DBPFP (THMFP and HAAFP) were markedly influenced by seasonal variations, with peak fluorescence intensity occurring during the summer. Contributions to the water system were dominated by microbial metabolites (region IV) and protein-like substances (region I and region II). 3D-FDS analysis further substantiated the low homogeneity of DBP precursors between summer and autumn, with fulvic acid (FA) substances comprising up to 36.89 % of the variance. Distinct fluorescence intensities were detected at Peak B (266.29 A.U.) and Peak T (376.19 A.U.). Throughout the year, a total of four fluorescent components were characterized, encompassing humic-like substances (C3) and protein-like substances (C1, C2, C4), indicative of biogenic pollution. The source of DBP precursors was identified as small molecular weight organic matter (0.2-5 KDa), resulting from microbial metabolic processes and the degradation of aquatic plants. In addition, external factors such as chlorination, pH levels, and contact time significantly influence THMFP and HAAFP. Overall, these findings advance our comprehension of the transport and fate of DBP precursors within drinking water sources and lake ecosystems. This knowledge is pivotal for optimizing water treatment protocols in relevant water treatment facilities.
季节性波动给饮用水处理带来了重大挑战,它改变了流域内溶解有机物(DOM)的性质,从而影响了消毒副产物(DBP)形成的可能性。DOM是一种复杂的有机物混合物,是关键的DBP前体,与不良健康后果密切相关。湖泊源水中DOM浓度和组成的变化使得DBP形成的预测变得复杂,而水系统的季节性变化加剧了这种情况。我们根据水温研究了湖泊DBP形成潜力(DBPFP)的季节性以及前体在四个不同季节的动态变化。利用激发-发射矩阵(EEM)结合平行因子分析(PARAFAC)、三维荧光差异光谱(3D-FDS)和分子量分布(MWD),我们阐明了湖泊DBP前体的组成和归宿。研究结果表明,DBPFP(三卤甲烷形成潜力和卤乙酸形成潜力)受到季节变化的显著影响,夏季荧光强度达到峰值。对水系统的贡献主要来自微生物代谢产物(区域IV)和类蛋白质物质(区域I和区域II)。3D-FDS分析进一步证实了夏季和秋季之间DBP前体的低同质性,富里酸(FA)物质占方差的比例高达36.89%。在峰B(266.29 A.U.)和峰T(376.19 A.U.)处检测到不同的荧光强度。全年共鉴定出四种荧光成分,包括类腐殖质物质(C3)和类蛋白质物质(C1、C2、C4),表明存在生物源污染。DBP前体的来源被确定为微生物代谢过程和水生植物降解产生的小分子有机物(0.2-5 kDa)。此外,氯化、pH值和接触时间等外部因素对三卤甲烷形成潜力和卤乙酸形成潜力有显著影响。总体而言,这些发现增进了我们对饮用水源和湖泊生态系统中DBP前体的迁移和归宿的理解。这些知识对于优化相关水处理设施的水处理方案至关重要。