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Seawater induced release and transformation of organic and inorganic phosphorus from river sediments

机译:海水诱导河流沉积物中有机磷和无机磷的释放和转化

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This paper reports an investigation of the release of organic and inorganic phosphorus from a riverine sediment subjected to salinity conditions typical of estuarine mixing. Freshwater sediment was mixed with filtered river water in a thermostatted reactor, and allowed to equilibrate under aerobic conditions for 3 days. Salinity was then increased in a stepwise manner by addition of filtered low-nutrient seawater over a period of 4 days. A control experiment was performed in a second reactor by substituting ultrapure water for seawater. Using a flow injection analysis method for measurement of filterable reactive phosphorous (FRP, the so-called inorganic fraction) and filterable organic phosphorous (FOP), it was found that rapid releases of both FOP and FRP occurred at salinities of ≥ 10per thousand. Over the 4-day experimental period, sediment release increased the filterable P concentration by approx. 50 μgL~(-1), and of this, nearly half was initially present as FOP, which subsequently underwent rapid mineralisation to FRP. The observed behaviour may be explained by a combination of salinity induced plasmolysis of sediment bacteria and ion exchange by suspended sediment particles.
机译:本文报道了在河口混合典型盐度条件下河流沉积物中有机磷和无机磷的释放情况的研究。在恒温反应器中将淡水沉积物与过滤的河水混合,并在有氧条件下平衡3天。然后在4天的时间内,通过添加过滤的低营养海水,逐步提高盐度。通过用超纯水代替海水在第二个反应器中进行了对照实验。使用流动注射分析方法测量可过滤的活性磷(FRP,所谓的无机级分)和可过滤的有机磷(FOP),发现在盐分≥10时,FOP和FRP都会快速释放。在4天的实验期内,沉淀物的释放使可过滤的P浓度增加了约5%。 50μgL〜(-1),其中近一半最初以FOP的形式存在,随后迅速矿化成FRP。观察到的行为可以用盐度引起的沉积物细菌的质解和悬浮沉积物颗粒的离子交换共同解释。

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