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Effects of water depth and water level fluctuation on the total and bio- available element concentrations in riverine reed stands

机译:水深和水位波动对河流芦苇架的总和生物可用元素浓度的影响

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摘要

This paper evaluates the chemical composition of reed stands grown in different riverine habitats. In addition to the total concentrations, we first present data on the bio-available element fractions of the sediment of reed stands.The results demonstrate clear separation between the plant and sediment samples and reveal the same concentration order of organs in all of the investigated sites irrespective of the water depth and water level fluctuation of the habitats.In reed stands with static water depth gradient, both the total and the bio-available element concentrations of the sediment increase towards the deep water. In habitats regularly flooded by the river, the deposition of suspended matter homogenizes the surface layer of the sediment and, therefore, total element concentrations in that layer is not influenced by the deepening river bed. After the flood event, however, the water depth gradient does influence the bio-available fractions. Finally, it is also demonstrated that chemistry in reed stands can indicate redox conditions in the rhizosphere and anthropogenic pollution sources.
机译:本文评估了在不同河流栖息地种植的芦苇架的化学成分。除了总浓度外,我们首先存在关于簧片沉积物的生物可用元素分数的数据。结果表明植物和沉积物样品之间的清晰分离,并揭示了所有研究部位中的器官相同的浓度顺序无论栖息地的水深和水位波动如何波动。芦苇稳定水深梯度,沉积物的总和生物可用元素浓度朝向深水增加。在栖息地经常被河流淹没,悬浮物的沉积均匀化沉淀物的表面层,因此,该层中的总元素浓度不受深化河床的影响。然而,在洪水事件之后,水深梯度确实会影响生物可用级分。最后,还证明了芦苇架中的化学可以表明根际和人为污染源中的氧化还原条件。

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