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Spectroscopic characterization and molecular weight distribution of dissolved organic matter in sediment porewaters from Lake Erhai, Southwest China.

机译:西南Er海沉积物孔隙水中溶解有机物的光谱表征和分子量分布

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摘要

Dissolved organic matter (DOM) in sediment porewaters from Lake Erhai, Southwest China was investigated using dissolved organic carbon (DOC) concentration, UV absorbance, fluorescence and molecular weight distribution. DOC exhibited a high concentration at the sediment-water interface with a rapid decrease to the oxic-anoxic interface at approximately 7 cm, and then increased with depth. Similar trends were also found for the UV absorption coefficients at 254 and 280 nm in the porewaters. DNA in the sediment was also measured, which confirmed the high abundance of aerobic bacteria in the upper layer of the sediment. Both humic-like (peaks A and C) and protein-like (peaks B and D) fluorescence were observed in the porewater DOM, and their fluorescence intensities exhibited a similar porewater profile as DOC concentration. A strong correlation was found between the peak fluorescence intensity ratio r(A, C) and r(D, B). Both the fluorescence index and UV absorption coefficient at 254 nm suggested a dramatic increase in aromaticity of porewater DOM across the oxic-anoxic interface. Porewater DOM exhibited a multimodal distribution of molecular weight with a relatively low polydispersity. The results of this study offer significant insight into the nature and properties of DOM in freshwater ecosystems..
机译:利用溶解有机碳(DOC)浓度,紫外线吸收率,荧光和分子量分布,研究了西南Er海沉积物孔隙水中的溶解有机物(DOM)。 DOC在沉积物-水界面处表现出高浓度,并在约7 cm处迅速下降至有氧-缺氧界面,然后随深度增加。对于孔隙水中在254和280 nm处的紫外线吸收系数,也发现了类似的趋势。还测量了沉积物中的DNA,这证实了沉积物上层中有大量的需氧细菌。在孔隙水DOM中均观察到腐殖质样(峰A和C)和蛋白质样(峰B和D)荧光,并且它们的荧光强度表现出与DOC浓度相似的孔隙水特征。发现峰值荧光强度比r(A,C)和r(D,B)之间有很强的相关性。 254 nm处的荧光指数和UV吸收系数均表明,在有氧-无氧界面上,孔隙水DOM的芳香度显着增加。孔隙水DOM表现出分子量的多峰分布,且多分散性较低。这项研究的结果为淡水生态系统中DOM的性质和性质提供了重要的见识。

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