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首页> 外文期刊>Journal of Freshwater Ecology >The diffusion fluxes and sediment activity of phosphorus in the sediment-water interface of Poyang Lake
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The diffusion fluxes and sediment activity of phosphorus in the sediment-water interface of Poyang Lake

机译:Po阳湖沉积物-水界面中磷的扩散通量和沉积物活性

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摘要

The dissolved reactive phosphorous (DRP) in pore water releases into the water body through the sediment-water interface. The DRP concentrations in the water and sediment of Poyang Lake were determined by high-resolution pore diffusion balance (HR-Peeper) and Zr-oxide diffusive gradients in thin films (Zr-oxide DGT) techniques. The range of the DRP concentrations in the pore water samples of different sampling sites was 30-360 ng/cm(3). The diffusion fluxes of DRP in the sediment-water interface were calculated based on the DRP concentration gradients. The range of DRP flux in Poyang Lake was 4.78-40.5ng m(-2) d(-1) with an average value of 14.7ng m(-2) d(-1). The results showed that the P diffusion flux was higher in the middle of the Poyang Lake than both upstream and downstream of the lake.
机译:孔隙水中溶解的反应性磷(DRP)通过沉积物-水界面释放到水体中。 high阳湖水体和底泥中DRP的浓度是通过高分辨率孔扩散平衡法(HR-Peeper)和薄膜中Zr-氧化物扩散梯度(Zr-氧化物DGT)技术确定的。不同采样点的孔隙水样品中DRP浓度范围为30-360 ng / cm(3)。根据DRP浓度梯度计算DRP在沉积物-水界面中的扩散通量。 Po阳湖的DRP通量范围为4.78-40.5ng m(-2)d(-1),平均值为14.7ng m(-2)d(-1)。结果表明,P阳湖中部磷的扩散通量高于其上游和下游。

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