Southeast Environmental Research Center and Department of Chemistry and Biochemistry, Florida International University, Miami, FL 33199, USA.
Southeast Environmental Research Center and Department of Chemistry and Biochemistry, Florida International University, Miami, FL 33199, USA.
Water Res. 2014 Sep 15;61:181-90. doi: 10.1016/j.watres.2014.03.075. Epub 2014 May 22.
Dissolved organic carbon (DOC) measurements and optical properties were applied to assess the photo- and bio-reactivity of dissolved organic matter (DOM) from different sources, including biomass leaching, soil leaching and surface waters in a subtropical wetland ecosystem. Samples were exposed to light and/or dark incubated through controlled laboratory experiments. Changes in DOC, ultraviolet (UV-Vis) visible absorbance, and excitation-emission matrix (EEM) fluorescence combined with parallel factor analysis (PARAFAC) were performed to assess sample degradation. Degradation experiments showed that while significant amounts of DOC were consumed during bio-incubation for biomass leachates, a higher degree of bio-recalcitrance for soil leachate and particularly surface waters was displayed. Photo- and bio-humification transformations were suggested for sawgrass, mangrove, and seagrass leachates, as compared to substantial photo-degradation and very little to almost no change after bio-incubation for the other samples. During photo-degradation in most cases the EEM-PARAFAC components displayed photo-decay as compared to a few cases which featured photo-production. In contrast during bio-incubation most EEM-PARAFAC components proved to be mostly bio-refractory although some increases and decreases in abundance were also observed. Furthermore, the sequential photo- followed by bio-degradation showed, with some exceptions, a "priming effect" of light exposure on the bio-degradation of DOM, and the combination of these two processes resulted in a DOM composition more similar to that of the natural surface water for the different sub-environments. In addition, for leachate samples there was a general enrichment of one of the EEM-PARAFAC humic-like component (Ex/Em: <260(305)/416 nm) during photo-degradation and an enrichment of a microbial humc-like component (Ex/Em: <260(325)/406 nm and of a tryptophan-like component (Ex/Em: 300/342 nm) during the bio-degradation process. This study exemplifies the effectiveness of optical property and EEM-PARAFAC in the assessment of DOM reactivity and highlights the importance of the coupling of photo- and bio-degradation processes in DOM degradation.
溶解有机碳(DOC)测量和光学特性被用于评估来自不同来源的溶解有机物(DOM)的光和生物反应性,包括生物质浸出物、土壤浸出物和亚热带湿地生态系统中的地表水。通过控制实验室实验,将样品暴露在光照或黑暗中进行孵育。通过进行 DOC、紫外(UV-Vis)可见吸收、激发-发射矩阵(EEM)荧光和并行因子分析(PARAFAC)的变化来评估样品降解。降解实验表明,尽管生物质浸出物的生物孵育过程中消耗了大量的 DOC,但土壤浸出物和特别是地表水表现出更高程度的生物稳定性。与其他样品的生物孵育后发生大量光降解和几乎没有变化相比,对锯草、红树林和海草浸出物则显示出光和生物腐殖化转化。在大多数情况下,与少数显示光生成的情况相比,EEM-PARAFAC 组分在光降解过程中显示出光衰减。相比之下,在生物孵育过程中,大多数 EEM-PARAFAC 组分被证明主要是生物难降解的,尽管也观察到一些丰度的增加和减少。此外,顺序光降解随后是生物降解,除了一些例外情况,光暴露对 DOM 生物降解的“启动效应”,以及这两个过程的组合导致 DOM 组成与不同子环境的天然地表水更相似。此外,对于浸出物样品,在光降解过程中,EEM-PARAFAC 腐殖质样组分之一(Ex/Em:<260(305)/416nm)普遍富集,而在生物降解过程中,微生物腐殖质样组分(Ex/Em:<260(325)/406nm 和色氨酸样组分(Ex/Em:300/342nm)富集。本研究例证了光学特性和 EEM-PARAFAC 在评估 DOM 反应性方面的有效性,并强调了光和生物降解过程耦合在 DOM 降解中的重要性。