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Has the Role of Estuaries as Sources or Sinks of Dissolved Inorganic Phosphorus Changed Over Time? Results of a K_d Study

机译:河口作为溶解无机磷源或汇的作用是否随时间而改变? K_d研究的结果

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There are literature reports suggesting that some estuaries are sinks for dissolved inorganic phosphorus (DIP) whilst other estuaries appear to be sources of DIP. Here a simple K_d model is presented that is able to rationalize these disparate patterns of behaviour. This model suggests that riverine DIP levels are an important regulator of DIP behaviour in estuaries. DIP concentrations have increased in many rivers over the last 50 years as a result of human activity. The model results presented suggest that increases in riverine DIP concentrations from < 1 to > 5 μM, consistent with documented changes in some systems over the last 50 years, can change estuaries from being sources to sinks for DIP. The model results demonstrate that suspended solid concentrations in estuaries (based on simulations over the range 100-2000 mg l~(-1)) are also an important regulator of DIP behaviour and hence the modification of suspended solids via dredging and land reclamation activities in estuaries can alter their DIP removal capacity.
机译:有文献报道表明某些河口是溶解性无机磷(DIP)的汇,而其他河口似乎是DIP的来源。这里提出了一个简单的K_d模型,该模型能够合理化这些不同的行为模式。该模型表明河流DIP水平是河口DIP行为的重要调节器。在过去的50年中,由于人类活动,许多河流的DIP浓度有所增加。提出的模型结果表明,河流DIP浓度从<1增至> 5μM,与过去50年某些系统中已记录的变化相一致,可以使河口从DIP的源头变为汇点。模型结果表明,河口中的悬浮物浓度(基于100-2000 mg l〜(-1)范围内的模拟)也是DIP行为的重要调节剂,因此通过疏in和土地开垦活动改变了悬浮物的浓度。河口可以更改其DIP清除能力。

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