Different hydrodynamic conditions on the deposition of organic carbon in sediment of two reservoirs

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• 作者：Zhao Luo ; Ji-Ming Ma ; Shuang-Ling Zheng ; Chun-Zi Nan ; Lin-Mei Nie
• 关键词：Hydrodynamic condition ; Mixing model ; Sedimentary organic carbon ; Stable isotope ; Water level fluctuation
• 刊名：Hydrobiologia
• 出版年：2016
• 出版时间：February 2016
• 年：2016
• 卷：765
• 期：1
• 页码：15-26
• 全文大小：811 KB
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• 作者单位：Zhao Luo (1)
  Ji-Ming Ma (1)
  Shuang-Ling Zheng (1)
  Chun-Zi Nan (1)
  Lin-Mei Nie (2)
  
  1. The State Key Laboratory of Hydroscience and Engineering, Department of Hydraulic Engineering, Tsinghua University, Beijing, 100084, China
  2. SINTEF Building and Infrastructure, P.O. Box 124, Blindern, 0314, Oslo, Norway
  
• 刊物类别：Biomedical and Life Sciences
• 刊物主题：Life Sciences
  Hydrobiology
  Ecology
  
• 出版者：Springer Netherlands
• ISSN：1573-5117

文摘

In regulated freshwater ecosystems, the deposition process of organic carbon (OC) in sediment could be affected by all the changes of physical, chemical, and biological factors. To assess different hydrodynamic conditions on the deposition of OC in sediment, the combination of elemental and stable isotope analyses was carried out in two reservoirs: the Huairou Reservoir (HR), which undergoes seasonal water level fluctuation (WLF) like natural lakes, and the Shisanling Reservoir (SR), which undergoes daily WLF for the operation of pumped storage power station. In general, OC concentration and its variation were comparable in the two reservoirs, whereas the OC distribution showed completely different features. The OC burial rate in SR was nearly two times more than in the HR, which reflect the impact of WLFs on the erosion of soil. For the relative contribution of phytoplankton-derived OC (P-OC), macrophyte-derived OC (M-OC), and terrestrial OC (T-OC) in sediment, the T-OC and M-OC in the SR were both higher than those of the HR, whereas the P-OC was markedly lower. Furthermore, the classification of nearshore and offshore sediments suggested that hydrodynamic conditions affected the T-OC import by physical processes and the in situ contributions of P-OC and M-OC with a spatial difference. Keywords Hydrodynamic condition Mixing model Sedimentary organic carbon Stable isotope Water level fluctuation