| 河流-湖泊系统中溶解有机质的示踪及迁移 |
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| 引用本文： | 黎文,吴丰昌,王静,郭建阳,王立英,白英臣,张润宇. 河流-湖泊系统中溶解有机质的示踪及迁移[J]. 环境科学研究, 2012, 25(2): 133-139 |
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| 作者姓名： | 黎文 吴丰昌 王静 郭建阳 王立英 白英臣 张润宇 |
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| 作者单位： | 1.中国科学院地球化学研究所,环境地球化学国家重点实验室 |
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| 基金项目： | 国家自然科学基金，中国科学院"西部之光"人才培养计划"西部博士项目" |
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| 摘 要： | 应用同步和三维荧光光谱对夏季贵州红枫湖、百花湖河流-湖泊系统的DOM(溶解有机质)进行识别和示踪,重点揭示了人为来源DOM的迁移和影响.结果表明,人为来源DOM比例较大的水体r(287 nm/332 nm)(同步荧光光谱指数)均大于1,r(B/C)(三维荧光光谱指数)较高,287 nm处的同步荧光峰是有机污染物的特征峰.与红枫湖表层水相比,百花湖表层水出现明显的类蛋白荧光峰,且r(287 nm/332 nm)(2.7)远大于红枫湖(0.7),指示百花湖中人为来源ρ(DOM)高于红枫湖.东门桥河向百花湖输送了较多人为来源DOM,但在百花湖水体纵向剖面4 m以下受到的影响较小.经过稀释和净化百花湖出口人为来源的ρ(DOM)已降至较低水平.同步荧光和三维荧光光谱联合可用来识别和示踪水体中人为来源ρ(DOM).
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| 关 键 词： | 同步荧光光谱 三维荧光光谱 溶解有机质 湖泊 |
Tracing the Transport of Dissolved Organic Matter in a River-Lake System |
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| LI Wen,WU Feng-chang,WANG Jing,GUO Jian-yang,WANG Li-ying,BAI Ying-chen and ZHANG Run-yu. Tracing the Transport of Dissolved Organic Matter in a River-Lake System[J]. Research of Environmental Sciences, 2012, 25(2): 133-139 |
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| Authors: | LI Wen WU Feng-chang WANG Jing GUO Jian-yang WANG Li-ying BAI Ying-chen ZHANG Run-yu |
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| Affiliation: | 1.State Key Laboratory of Environmental Geochemistry,Institute of Geochemistry,Chinese Academy of Sciences,Guiyang 550002,China2.State Environmental Protection Key Laboratory for Lake Pollution Control,Chinese Research Academy of Environmental Sciences,Beijing 100012,China |
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| Abstract: | By using synchronous fluorescence spectroscopy and three-dimensional excitation emission matrix(EEM) spectroscopy,dissolved organic matter(DOM) in the Hongfeng and Baihua Lakes in Guizhou Province and their surrounding rivers were identified and traced during summer,with specific focus on the transport and influences of the anthropogenic DOMs.The results showed that the synchronous fluorescence spectroscopy index r(287 nm/332 nm) of the water with high proportion of anthropogenic DOM was larger than 1.The characteristic peak was at about 287 nm,and its EEM spectroscopy index r(B/C) was larger than that of the DOM with low portion of anthropogenic sources.The synchronous fluorescence spectroscopy index r(287 nm/332 nm) of the surface water of Lake Baihua(2.7) was much higher than that of Lake Hongfeng(0.7).There was an obvious protein-like fluorescence peak in the spectroscopy of Lake Baihua,which indicated a higher portion of anthropogenic DOM.The results also demonstrated that a large amount of anthropogenic DOM was transported to Lake Baihua by Dongmenqiao River,and this inflow mainly affected the water layer of 0 m to 4 m depth.After dilution and degradation,ρ(DOM) decreased to a very low level by the time the water was discharged from Lake Baihua.It is useful to combine synchronous fluorescence spectroscopy with three-dimensional excitation emission matrix fluorescence spectroscopy for anthropogenic DOM identification and tracing in river-lake water systems. |
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| Keywords: | synchronous fluorescence spectroscopy three-dimensional excitation emission matrix fluorescence spectroscopy dissolved organic matter lake |
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