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    Volume 50 Issue 4
    Apr.  2025
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    Lu Shuaishuai, Zhou Nianqing, Cai Yi, Guo Mengshen, Xia Mingrui, Liu Kehao, Shan Hongcui, 2025. Ecological Stoichiometric Characteristics of Carbon, Nitrogen, and Phosphorus in Sediments of Hyporheic Zone within Lake Wetland. Earth Science, 50(4): 1651-1662. doi: 10.3799/dqkx.2024.069
    Citation: Lu Shuaishuai, Zhou Nianqing, Cai Yi, Guo Mengshen, Xia Mingrui, Liu Kehao, Shan Hongcui, 2025. Ecological Stoichiometric Characteristics of Carbon, Nitrogen, and Phosphorus in Sediments of Hyporheic Zone within Lake Wetland. Earth Science, 50(4): 1651-1662. doi: 10.3799/dqkx.2024.069

    Ecological Stoichiometric Characteristics of Carbon, Nitrogen, and Phosphorus in Sediments of Hyporheic Zone within Lake Wetland

    doi: 10.3799/dqkx.2024.069
    • Received Date: 2023-12-15
      Available Online: 2025-05-10
    • Publish Date: 2025-04-25
    • In order to study the ecological stoichiometric characteristics and influencing factors of carbon (C), nitrogen (N), phosphorus (P) in sediments of the hyporheic zone within the lake wetland, 4 monitoring transections and 16 boreholes were set up in the wetland at the entrance of the Xiangjiang River in South Dongting Lake. A total of 156 sediment samples were collected for parameter testing within a depth range of 0-10 m. Correlation analysis, redundancy analysis and structural equation modeling were applied in the investigation. The results indicate that the average contents of total carbon (TC), organic carbon (SOC), total nitrogen (TN), and total phosphorus (TP) in sediment are 8.99, 7.30, 0.93, and 0.46 g/kg, respectively, which show a decreasing trend with increasing sampling depth (H). The average ratios of C/N, C/P, and N/P in sediments are 10.46, 46.51, and 5.06, respectively, with strong spatial variability. The lower C/N and C/P indicate that organic N and organic P are prone to mineralization, while lower N/P indicates that sediments are mainly limited by N. TC, SOC, TN and TP contents have a significant negative correlation with H and redox potential (Eh), and a significant positive correlation with water content (ω). H, Eh and ω are the main driving factors influencing C, N and P contents and their ecological stoichiometric characteristics in wetland sediments.

       

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