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首页> 外文期刊>Photochemistry and Photobiology: An International Journal >Utilization of PARAFAC-Modeled Excitation-Emission Matrix (EEM) Fluorescence Spectroscopy to Identify Biogeochemical Processing of Dissolved Organic Matter in a Northern Peatland
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Utilization of PARAFAC-Modeled Excitation-Emission Matrix (EEM) Fluorescence Spectroscopy to Identify Biogeochemical Processing of Dissolved Organic Matter in a Northern Peatland

机译:利用PARAFAC模拟的激发发射矩阵(EEM)荧光光谱法确定北部泥炭地中溶解有机物的生物地球化学过程

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摘要

In this study, we contrast the fluorescent properties of dissolved organic matter (DOM) in fens and bogs in a Northern Minnesota peatland using excitation emission matrix fluorescence spectroscopy with parallel factor analysis (EEM-PARAFAC). EEM-PARAFAC identified four humic-like components and one protein-like component and the dynamics of each were evaluated based on their distribution with depth as well as across sites differing in hydrology and major biological species. The PARAFAC-EEM experiments were supported by dissolved organic carbon measurements (DOC), optical spectroscopy (UV-Vis), and compositional characterization by ultrahigh resolution Fourier transform ion cyclotron resonance mass spectroscopy (FT-ICR MS). The FT-ICR MS data indicate that metabolism in peatlands reduces the molecular weights of individual components of DOM, and oxygen-rich less aromatic molecules are selectively biodegraded. Our data suggest that different hydrologic and biological conditions within the larger peat ecosystem drive molecular changes in DOM, resulting in distinctly different chemical compositions and unique fluorescent fingerprints. PARAFAC modeling of EEM data coupled with ultrahigh resolution FT-ICR MS has the potential to provide significant molecular-based information on DOM composition that will support efforts to better understand the composition, sources, and diagenetic status of DOM from different terrestrial and aquatic systems.
机译:在这项研究中,我们使用激发发射矩阵荧光光谱和并行因子分析(EEM-PARAFAC),对比了明尼苏达州北部泥炭地和沼泽中溶解性有机物(DOM)的荧光特性。 EEM-PARAFAC确定了4种腐殖质样成分和1种蛋白质样成分,并根据它们的深度分布以及跨水文学和主要生物种类的不同地点评估了它们的动力学。 PARAFAC-EEM实验得到了溶解有机碳测量(DOC),光谱学(UV-Vis)和超高分辨率傅里叶变换离子回旋共振质谱(FT-ICR MS)的成分表征的支持。 FT-ICR MS数据表明,泥炭地中的代谢降低了DOM各个成分的分子量,富氧少的芳香族分子被选择性地生物降解。我们的数据表明,较大的泥炭生态系统中不同的水文和生物学条件驱动DOM中的分子变化,从而导致化学成分和独特的荧光指纹显着不同。 EEM数据的PARAFAC建模与超高分辨率FT-ICR MS结合使用,有可能提供有关DOM组成的基于分子的重要信息,这将有助于人们更好地了解来自不同陆地和水生系统的DOM的组成,来源和成岩状态。

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