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[浑河与太子河流域淡水中分级胶体有机物的荧光特性]

[Fluorescence characteristics of fractionated colloidal organic matter in freshwater from Hunhe and Taizihe watersheds].

作者信息

Liu Na-Na, Li Bin, Liu Rui-Xia, Song Yong-Hui, Wu Wei

出版信息

Huan Jing Ke Xue. 2014 Nov;35(11):4103-10.

Abstract

The ultrafiltration system with molecular mass of 100 x 10(3) and 1 x 10(3) membrane was used for the fractionation of total dissolved organic matter (DOM) in waters from Hunhe and Taizihe Watersheds. The fluorescence properties of colloidal organic matter with different sizes were investigated using a three-dimension excitation-emission matrix (3-D EEM) fluorescence spectroscopy. It was shown that the tryptophan-, fuvic-and humic-like materials were presented in the waters from Hunhe and Taizihe Watersheds, of which fuvic-and humic-like materials were mainly in colloidal form with small size (relative molecular mass < 100 x 10(3)) and truly dissolved phase (relative molecular mass < 1 x 10(3)). The adsorption of protein-like matters onto the colloid particles made the majority of these materials in colloidal phase though they had a low molecular mass. The higher percentages of small colloidal and truly dissolved organic carbon in total dissolved organic carbon (DOC) were observed in the water samples collected in wet season. Fluorescence index (FI), index of recent autochthonous contribution (BIX) and humification index (HIX) indicated that humic-like components in truly dissolved phase were mainly originated from autochthonous source and colloidal humic-like components were mainly derived from terrestrial organic matter. The recent autochthonous organic matter made a major contribution to truly dissolved phase. The humic-like matter was the domain of DOC content, but the contribution of protein-like materials to the organic carbon was not negligible due to the pollution of waterbody by industrial wastewater discharge.

摘要

采用截留分子量为100×10³和1×10³的超滤系统对浑河和太子河流域水体中的总溶解有机物(DOM)进行分级。利用三维激发-发射矩阵(3-D EEM)荧光光谱研究了不同尺寸胶体有机物的荧光特性。结果表明,浑河和太子河流域水体中存在色氨酸类、富里酸类和腐殖酸类物质,其中富里酸类和腐殖酸类物质主要以小尺寸胶体形式(相对分子量<100×10³)和真正溶解态(相对分子量<1×10³)存在。尽管蛋白质类物质分子量较低,但它们在胶体颗粒上的吸附使得这些物质大部分处于胶体相。在湿季采集的水样中,总溶解有机碳(DOC)中较小胶体态和真正溶解态有机碳的百分比更高。荧光指数(FI)、近期自生源贡献指数(BIX)和腐殖化指数(HIX)表明,真正溶解态中的腐殖酸类组分主要来源于自生源,胶体态腐殖酸类组分主要来源于陆源有机物。近期自生源有机物对真正溶解态贡献较大。腐殖酸类物质是DOC含量的主要组成部分,但由于工业废水排放对水体的污染,蛋白质类物质对有机碳的贡献也不可忽视。

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