State Key Laboratory of Lake Science and Environment, Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, Nanjing 210008, China; School of Freshwater Sciences, University of Wisconsin-Milwaukee, 600 E Greenfield Ave, Milwaukee, WI 53204, USA.
Key Laboratory of Surficial Geochemistry, Ministry of Education, School of Earth Sciences and Engineering, Nanjing University, Nanjing 210023, China.
Environ Pollut. 2018 Aug;239:205-214. doi: 10.1016/j.envpol.2018.03.108. Epub 2018 Apr 11.
Effects of photochemical and microbial degradation on variations in composition and molecular-size of dissolved organic matter (DOM) from different sources (algal and soil) and the subsequent influence on Cu(II) binding were investigated using UV-Vis, fluorescence excitation-emission matrices coupled with parallel factor analysis, flow field-flow fractionation (FlFFF), and metal titration. The degradation processes resulted in an initial rapid decline in the bulk dissolved organic carbon and chromophoric and fluorescent DOM components, followed by a small or little decrease. Specifically, photochemical reaction decreased the aromaticity, humification and apparent molecular weights of all DOM samples, whereas a reverse trend was observed during microbial degradation. The FlFFF fractograms revealed that coagulation of both protein- and humic-like DOM induced an increase in molecular weights for algal-DOM, while the molecular weight enhancement for allochthonous soil samples was mainly attributed to the self-assembly of humic-like components. The Cu(II) binding capacity of algal-derived humic-like and fulvic-like DOM consistently increased during photo- and bio-degradation, while the soil-derived DOM exhibited a slight decline in Cu(II) binding capacity during photo-degradation but a substantial increase during microbial degradation, indicating source- and degradation-dependent metal binding heterogeneities. Pearson correlation analysis demonstrated that the Cu(II) binding potential was mostly related with aromaticity and molecular size for allochthonous soil-derived DOM, but was regulated by both DOM properties and specific degradation processes for autochthonous algal-derived DOM. This study highlighted the coupling role of inherent DOM properties and external environmental processes in regulating metal binding, and provided new insights into metal-DOM interactions and the behavior and fate of DOM-bound metals in aquatic environments.
采用紫外-可见分光光度法、荧光激发-发射矩阵耦合平行因子分析、流动场流分离(FlFFF)和金属滴定法,研究了光化学和微生物降解对不同来源(藻类和土壤)溶解有机物(DOM)组成和分子大小变化的影响,以及随后对 Cu(II)结合的影响。降解过程导致初始时大量溶解有机碳以及发色和荧光 DOM 成分迅速下降,随后下降幅度较小或几乎没有下降。具体而言,光化学反应降低了所有 DOM 样品的芳香度、腐殖化程度和表观分子量,而微生物降解则呈现相反的趋势。FlFFF 馏分图表明,藻类 DOM 中蛋白型和腐殖型 DOM 的凝聚导致分子量增加,而所有外源土壤样品的分子量增强主要归因于腐殖型成分的自组装。在光解和生物降解过程中,藻类衍生的腐殖型和富里酸型 DOM 的 Cu(II)结合能力持续增加,而土壤衍生的 DOM 在光解过程中 Cu(II)结合能力略有下降,但在微生物降解过程中则显著增加,表明金属结合的不均一性与来源和降解过程有关。Pearson 相关分析表明,外源土壤衍生 DOM 的 Cu(II)结合潜力主要与芳香度和分子大小有关,而内源性 DOM 特性和特定的降解过程共同调节了自生藻类衍生 DOM 的 Cu(II)结合潜力。本研究强调了固有 DOM 特性和外部环境过程在调节金属结合方面的耦合作用,为金属-DOM 相互作用以及 DOM 结合金属在水生环境中的行为和归宿提供了新的认识。