Anderson Lindsay E, DeMont Isobel, Dunnington Dewey D, Bjorndahl Paul, Redden Dave J, Brophy Michael J, Gagnon Graham A
Centre for Water Resources Studies, Department of Civil & Resource Engineering, Dalhousie University, 1360 Barrington St. Halifax, Nova Scotia, Canada.
Centre for Water Resources Studies, Department of Civil & Resource Engineering, Dalhousie University, 1360 Barrington St. Halifax, Nova Scotia, Canada.
Sci Total Environ. 2023 Feb 1;858(Pt 1):159699. doi: 10.1016/j.scitotenv.2022.159699. Epub 2022 Oct 25.
Reduced atmospheric acid deposition has given rise to recovery from acidification - defined as increasing pH, acid neutralization capacity (ANC), or alkalinity in surface waters. Strong evidence of recovery has been reported across North America and Europe, driving chemical responses. The primary chemical responses identified in this review were increasing concentration and changing character of natural organic matter (NOM) towards predominantly hydrophobic nature. The concentration of NOM also influenced trace metal cycling as many browning surface waters also reported increases in Fe and Al. Further, climate change and other factors (e.g., changing land use) act in concert with reductions in atmospheric deposition to contribute to widespread browning and will have a more pronounced effect as deposition stabilizes. The observed water quality trends have presented challenges for drinking water treatment (e.g., increased chemical dosing, poor filter operations, formation of disinfection by-products) and many facilities may be under designed as a result. This comprehensive review has identified key research areas to be addressed, including 1) a need for comprehensive monitoring programs (e.g., larger timescales; consistency in measurements) to assess climate change impacts on recovery responses and NOM dynamics, and 2) a better understanding of drinking water treatment vulnerabilities and the transition towards robust treatment technologies and solutions that can adapt to climate change and other drivers of changing water quality.
大气酸沉降的减少已促使水体从酸化状态中恢复——酸化被定义为地表水的pH值升高、酸中和能力(ANC)增强或碱度增加。北美和欧洲各地都报告了水体恢复的有力证据,这推动了化学响应。本综述确定的主要化学响应是天然有机物(NOM)的浓度增加,且其性质逐渐向主要为疏水性转变。NOM的浓度还影响了痕量金属的循环,因为许多呈现褐变的地表水还报告了铁和铝含量的增加。此外,气候变化和其他因素(如土地利用变化)与大气沉降的减少共同作用,导致水体普遍褐变,并且随着沉降趋于稳定,这种影响将更加显著。观察到的水质趋势给饮用水处理带来了挑战(如化学药剂投加量增加、过滤操作不佳、消毒副产物的形成),许多设施可能因此设计不足。这项全面的综述确定了有待解决的关键研究领域,包括:1)需要开展全面的监测计划(如更长的时间尺度;测量的一致性),以评估气候变化对恢复响应和NOM动态的影响;2)更好地了解饮用水处理的脆弱性,以及向能够适应气候变化和其他水质变化驱动因素的稳健处理技术和解决方案的转变。