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    Volume 43 Issue 11
    Nov.  2018
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    Article Navigation >  Earth Science  > 2018  >  43(11): 4109-4119
    Pan Feng, Guo Zhanrong, Liu Huatai, Wang Bo, Li Zhiwei, Zhuang Zhenjie, 2018. High-Resolution Distribution and Biogeochemical Behavior of Phosphorus and Iron at Sediment-Water Interface of Tidal Flat. Earth Science, 43(11): 4109-4119. doi: 10.3799/dqkx.2018.177
    Citation: Pan Feng, Guo Zhanrong, Liu Huatai, Wang Bo, Li Zhiwei, Zhuang Zhenjie, 2018. High-Resolution Distribution and Biogeochemical Behavior of Phosphorus and Iron at Sediment-Water Interface of Tidal Flat. Earth Science, 43(11): 4109-4119. doi: 10.3799/dqkx.2018.177
    shu

    High-Resolution Distribution and Biogeochemical Behavior of Phosphorus and Iron at Sediment-Water Interface of Tidal Flat

    doi: 10.3799/dqkx.2018.177
    • 1.

      College of Ocean and Earth Sciences, Xiamen University, Xiamen 361102, China

    • 2.

      College of the Environment and Ecology, Xiamen University, Xiamen 361102, China

    • Received Date: 2018-03-19
    • Publish Date: 2018-11-15
      Abstract
    • To find out distribution and coupling pattern of iron and phosphorus, as well as impact on phosphorus release in microenvironment of intertidal region. with the help of diffusive gradients in thin films technique (ZrO-Chelex DGT), we obtained in-situ high-resolution DRP and Fe2+ concentrations in porewater profiles of mangrove tidal flat in Jiulong River estuary, as well as the corresponding sediment properties in this study. The results show:(1) In surface porewater, the remarkable positive correlation between DRP and Fe2+ verified the coupling relationship of these two elements and the crucial effects of sediment iron (Ⅲ) (oxyhydr) oxides on the absorption/desorption of phosphorus; (2) in deep anoxic porewater, on account of sediment heterogeneity and absorption by mangrove plants, DRP concentrations presented obvious fluctuations compared with Fe2+; (3) the molecular diffusion flux was estimated ranging from 0.000 64 to 0.006 00 μg·cm-2·d-1 based on DRP concentrations gradient in surface porewater, which are much lower than results of general lake research. The main reason is P-Fe coupling in this iron-rich tidal flat sediment with deep oxidation zone which effectively restrains phosphorus release.

       

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