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三峡库区消落带水体DOM不同分子量组分三维荧光特征
摘要点击 2897  全文点击 1215  投稿时间:2015-08-31  修订日期:2015-11-11
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中文关键词  溶解性有机质  超滤  三维荧光光谱  三峡库区  消落带  水体有机胶体
英文关键词  dissolved organic matter(DOM)  ultrafiltration  three-dimensional fluorescence spectrum  Three Gorges Reservoir areas  water-level fluctuation zones  water organic colloid
作者单位E-mail
陈雪霜 西南大学资源环境学院, 三峡库区生态环境教育部重点实验室, 重庆市农业资源与环境研究重点实验室, 重庆 400716 401602312@qq.com 
江韬 西南大学资源环境学院, 三峡库区生态环境教育部重点实验室, 重庆市农业资源与环境研究重点实验室, 重庆 400716
Department of Forest Ecology and Management, Swedish University of Agricultural Sciences, Sweden Umeå
SE-90183 
Jiangtower666@163.com 
卢松 西南大学资源环境学院, 三峡库区生态环境教育部重点实验室, 重庆市农业资源与环境研究重点实验室, 重庆 400716  
魏世强 西南大学资源环境学院, 三峡库区生态环境教育部重点实验室, 重庆市农业资源与环境研究重点实验室, 重庆 400716  
王定勇 西南大学资源环境学院, 三峡库区生态环境教育部重点实验室, 重庆市农业资源与环境研究重点实验室, 重庆 400716  
闫金龙 西南大学资源环境学院, 三峡库区生态环境教育部重点实验室, 重庆市农业资源与环境研究重点实验室, 重庆 400716  
中文摘要
      本研究利用超滤技术和三维荧光光谱,以三峡库区典型消落带水体溶解性有机质(DOM)不同分子量组分为对象,分析和讨论了不同分子量级分的组成差异和输入来源. 结果表明,该区域DOM分子量分布情况较为分散,但胶体(Mr1×103~0.22 μm)和真溶态组分(Mr<1×103)均对DOC总质量贡献相当. 不同分子量级分中均存在A、C、B、T峰,其相对含量分配均呈现出一致趋势,即真溶态(Mr<1×103)>低分子量组分(Mr 1×103~10×103)>中分子量组分(Mr 10×103~30×103)>高分子量组分(Mr 30×103~0.22 μm). 另外,DOM随超滤分子量等级降低,FI和BIX值增加,"内源"输入特征增强; 腐殖化程度降低(HIX值下降). 陆源输入主要影响高、中分子组分,而内源输入主要影响低分子及真溶态部分. 同时,沿岸不同土地利用类型对水体DOM性质和组成影响明显. 土地利用类型多样性、生态景观结构复杂程度越高,水体DOM不同分子量等级中各荧光组分也越复杂.
英文摘要
      The study of the molecular weight (MW) fractions of dissolved organic matter (DOM) in aquatic environment is of interests because the size plays an important role in deciding the biogeochemical characteristics of DOM. Thus, using ultrafiltration (UF) technique combined with three-dimensional fluorescence spectroscopy, DOM samples from four sampling sites in typical water-level fluctuation zones of Three Gorge Reservoir areas were selected to investigate the differences of properties and sources of different DOM MW fractions. The results showed that in these areas, the distribution of MW fractions was highly dispersive, but the approximately equal contributions from colloidal (Mr 1×103-0.22 μm) and true dissolved fraction (Mr<1×103) to the total DOC concentration were found. Four fluorescence signals (humic-like A and C; protein-like B and T) were observed in all MW fractions including bulk DOM, which showed the same distribution trend: true dissolved>low MW (Mr 1×103-10×103)>medium MW (Mr 10×103-30×103)>high MW (Mr 30×103-0.22 μm). Additionally, with decreasing MW fraction, fluorescence index (FI) and freshness index (BIX) increased suggesting enhanced signals of autochthonous inputs, whereas humification index (HIX) decreased indicating lower humification degree. It strongly suggested that terrestrial input mainly affected the composition and property of higher MW fractions of DOM, as compared to lower MW and true dissolved fractions that were controlled by autochthonous sources such as microbial and alga activities, instead of allochthonous sources. Meanwhile, the riparian different land-use types also affected obviously on the characteristics of DOM. Therefore, higher diversity of land-use types, and also higher complexity of ecosystem and landscapes, induced higher heterogeneity of fluorescence components in different MW fraction of DOM.

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