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首页> 外文期刊>Applied Geochemistry: Journal of the International Association of Geochemistry and Cosmochemistry >Comparative study of dissolved organic matter from groundwater and surface water in the Florida coastal Everglades using multi-dimensional spectrofluorometry combined with multivariate statistics
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Comparative study of dissolved organic matter from groundwater and surface water in the Florida coastal Everglades using multi-dimensional spectrofluorometry combined with multivariate statistics

机译:多维分光光度法结合多元统计数据对佛罗里达沿海大沼泽地地下水和地表水中溶解有机物的比较研究

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摘要

Dissolved organic matter (DOM) in groundwater and surface water samples from the Florida coastal Everglades were studied using excitation-emission matrix fluorescence modeled through parallel factor analysis (EEM-PARAFAC). DOM in both surface and groundwater from the eastern Everglades S332 basin reflected a terrestrial-derived fingerprint through dominantly higher abundances of humic-like PARAFAC components. In contrast, surface water DOM from northeastern Florida Bay featured a microbial-derived DOM signature based on the higher abundance of microbial humic-like and protein-like components consistent with its marine source. Surprisingly, groundwater DOM from northeastern Florida Bay reflected a terrestrial-derived source except for samples from central Florida Bay well, which mirrored a combination of terrestrial and marine end-member origin. Furthermore, surface water and groundwater displayed effects of different degradation pathways such as photodegradation and biodegradation as exemplified by two PARAFAC components seemingly indicative of such degradation processes. Finally, Principal Component Analysis of the EEM-PARAFAC data was able to distinguish and classify most of the samples according to DOM origins and degradation processes experienced, except for a small overlap of S332 surface water and groundwater, implying rather active surface-to-ground water interaction in some sites particularly during the rainy season. This study highlights that EEM-PARAFAC could be used successfully to trace and differentiate DOM from diverse sources across both horizontal and vertical flow profiles, and as such could be a convenient and useful tool for the better understanding of hydrological interactions and carbon biogeochemical cycling.
机译:利用通过平行因子分析(EEM-PARAFAC)建立的激发-发射矩阵荧光,研究了佛罗里达沿海大沼泽地的地下水和地表水样品中的溶解性有机物(DOM)。东部大沼泽地S332盆地的地表水和地下水中的DOM均通过大量富含腐殖质的PARAFAC成分反映了陆源指纹。相反,来自东北佛罗里达湾的地表水DOM具有微生物衍生的DOM特征,其特征是与其海洋来源一致的微生物类腐殖质和蛋白质类成分含量较高。出乎意料的是,来自佛罗里达湾东北部的地下水DOM反映了一种源自地面的水源,但来自佛罗里达湾中部井的样本却反映了陆源和海洋末段来源的组合。此外,地表水和地下水表现出不同降解途径的影响,例如光降解和生物降解,这两个表面活性剂似乎表明了这种降解过程。最后,对EEM-PARAFAC数据的主成分分析能够根据DOM来源和经历的降解过程对大多数样品进行区分和分类,除了S332地表水和地下水有少量重叠,这意味着地表相当活跃一些地点的水相互作用,尤其是在雨季。这项研究突出表明,EEM-PARAFAC可以成功地用于跟踪和区分DOM在水平和垂直流动剖面中来自各种来源,因此可以作为方便和有用的工具来更好地了解水文相互作用和碳生物地球化学循环。

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