Effects of organic matter content and composition on ammonium adsorption in lake sediments
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  • 作者:Li Zhang ; Shengrui Wang ; Lixin Jiao…
  • 关键词:Organic matter ; Ammonium ; Adsorption ; Sediment ; Fourier transform infrared spectrometry ; Scanning electron microscopy
  • 刊名:Environmental Science and Pollution Research
  • 出版年:2016
  • 出版时间:April 2016
  • 年:2016
  • 卷:23
  • 期:7
  • 页码:6179-6187
  • 全文大小:577 KB
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  • 作者单位:Li Zhang (1) (2) (3)
    Shengrui Wang (1) (2) (3)
    Lixin Jiao (1) (2) (3)
    Yanping Li (1) (2) (3)
    Jiachun Yang (1) (2) (3)
    Rui Zhang (1) (2) (3)
    Shuang Feng (1) (2) (3)
    Juan Wang (1) (2) (3)

    1. State Key Laboratory of Environmental Criteria and Risk Assessment, Chinese Research Academy of Environmental Sciences, Beijing, 100012, China
    2. State Environmental Protection Key Laboratory for Lake Pollution Control, Research Center of Lake Eco-environment, Chinese Research Academy of Environmental Sciences, Beijing, 100012, China
    3. Dongting Lake Ecological Observation and Research Station Chinese Research Academy of Environmental Sciences, Yueyang, Hunan Province, 414000, China
  • 刊物类别:Earth and Environmental Science
  • 刊物主题:Environment
    Environment
    Atmospheric Protection, Air Quality Control and Air Pollution
    Waste Water Technology, Water Pollution Control, Water Management and Aquatic Pollution
    Industrial Pollution Prevention
  • 出版者:Springer Berlin / Heidelberg
  • ISSN:1614-7499
文摘
The nature of the influence of organic matter (OM) on ammonium adsorption in lake sediments remains disputed. In this study, the kinetics and thermodynamics of ammonium adsorption were investigated on sediment samples with different OM contents (ignoring the effects of OM mineralization) previously collected from Lake Wuli, a northern bay of Lake Taihu, a shallow lake in southern China. The mechanisms of ammonium adsorption in these samples were characterized by Fourier transform infrared spectrometry and scanning electron microscopy. The results show that the ammonium adsorption capacity of the sediments is highly correlated with their OM content and with the humic content of the OM. The ammonium adsorption capacity of OM varies with its composition, i.e., with the surface properties of the different functional groups present. Indeed, humic acid was found to have a greater ammonium adsorption capacity by itself than when mixed with kerogen and black carbon, the mixture of the latter two components proving a better adsorbent than pure black carbon.

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