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[南水北调东线工程中线关键湖泊中发色溶解性有机物的特征分析]

[Characterizing Chromophoric Dissolved Organic Matter in Key Lakes in the Middle Reaches of the East Route of the South-North Water Diversion Project].

作者信息

Zhang Liu-Qing, Peng Kai, Zhou Lei, Shi Yu, Li Yuan-Peng, Zhou Yong-Qiang, Gong Zhi-Jun, Zhang Yun-Lin, Yang Yan

机构信息

College of Environment Science and Engineering, China West Normal University, Nanchong 637000, China.

State Key Laboratory of Lake Science and Environment, Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, Nanjing 210008, China.

出版信息

Huan Jing Ke Xue. 2019 Jul 8;40(7):3018-3029. doi: 10.13227/j.hjkx.201811137.

Abstract

Lake Hongze and Lake Luoma are two key lakes located in the middle reaches of the east line of the South-to-North Water Diversion Project. We attempted to unravel the sources and optical composition of CDOM for samples collected from these lakes using excitation-emission matrices (EEMs) and parallel factor analysis (PARAFAC). ① Three fluorescent components were obtained using PARAFAC, including a terrestrial humic-like C1, a tryptophan-like C2, and a tyrosine-like C3. The sources and optical composition of CDOM in the two lakes were, to a large extent, affected by upstream inflow. ② Specifically, fluorescence intensity () of the three components C1-C3 in the inflowing river mouths of the two lakes was notably higher than in the other lake regions, and of the three components during the flood season was significantly higher than during the dry season (-test, <0.01). During the flood season, the fluorescence intensity of the terrestrial humic-like component was the highest. This indicates that the source and composition of CDOM in the two lakes are greatly affected by the inflow from the upstream water system, and that the hydrological processes control the abundance and sources of CDOM, especially the terrestrial humic-like C1.③ Significant positive relationships were found between the terrestrial humic-like C1 and the DOC concentrations and CDOM absorption (254) (=0.60, <0.01; =0.88, <0.01), and the correlation was higher than the other two components. This indicated that the terrestrial humic-like component was the main source of CDOM. In addition, the terrestrial humic-like C1 had a significant positive correlation with SUVA, , and the integration ratio of the fluorescence peak C to peak T (:) (=0.49, <0.01; =0.61, <0.01; =0.93, <0.01). It is further revealed that the source and composition of CDOM in the two lakes are greatly affected by land sources. This study reveals the response of CDOM source and composition in Lake Hongze and Lake Luoma to different hydrological scenarios and water transfer processes. Based on these results, the water quality management of the rivers entering the lake should be strengthened during the flood season.

摘要

洪泽湖和骆马湖是南水北调东线工程中线的两个关键湖泊。我们试图利用激发-发射矩阵(EEMs)和平行因子分析(PARAFAC),对从这些湖泊采集的样本中溶解性有色有机物(CDOM)的来源和光学组成进行解析。①利用PARAFAC得到了三种荧光成分,包括一种陆源腐殖质类C1、一种色氨酸类C2和一种酪氨酸类C3。两个湖泊中CDOM的来源和光学组成在很大程度上受到上游入流的影响。②具体而言,两个湖泊入河口处三种成分C1 - C3的荧光强度()显著高于其他湖区,且三种成分在汛期的荧光强度显著高于枯水期(t检验,<0.01)。在汛期,陆源腐殖质类成分的荧光强度最高。这表明两个湖泊中CDOM的来源和组成受上游水系入流的影响很大,且水文过程控制着CDOM的丰度和来源,尤其是陆源腐殖质类C1。③陆源腐殖质类C1与溶解性有机碳(DOC)浓度和CDOM吸收(254)之间存在显著正相关(=0.60,<0.01;=0.88,<0.01),且相关性高于其他两种成分。这表明陆源腐殖质类成分是CDOM的主要来源。此外,陆源腐殖质类C1与SUVA、以及荧光峰C与峰T的积分比值(:)之间存在显著正相关(=0.49,<0.01;=0.61,<0.01;=0.93,<0.01)。进一步表明两个湖泊中CDOM的来源和组成受陆源的影响很大。本研究揭示了洪泽湖和骆马湖中CDOM来源和组成对不同水文情景和调水过程的响应。基于这些结果,在汛期应加强入湖河流的水质管理。

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