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Implications of using measured sediment oxygen demand data vs. Estimated valuesin water quality modeling

机译:在水质模型中使用测得的沉积物需氧量数据与估算值的含义

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Sediment oxygen demand (SOD) is one of the primary sediment-water interactions which contributes to poor surface water quality. It is a key parameter in computer models for simulating the dissolved oxygen (DO) balance in natural wate bodies which receive wastwater discharges. Accurate estimates of SOD rates are needed in these water quality models to correctly design the allowable waste loads for discharge permits. However, in spite of historical documented evidence that SOD can be responsible for a large portioin of observed DO deficits, the use of measured SOD data for computation of waste load allocations and permit limits is not a standard procedure. This paper documents how inaccurate SOD estimates can lead to errors in understanding the governing pheomena responsible for observed water quality problems related to disolved oxygen concentrations.
机译:沉积物需氧量(SOD)是主要的沉积物与水之间的相互作用之一,它导致了较差的地表水质量。它是计算机模型中用于模拟接收废水排放的天然水体中溶解氧(DO)平衡的关键参数。在这些水质模型中,需要准确估算SOD率,以正确设计排放许可的允许废物负荷。但是,尽管有历史文献证明SOD可能是造成大量观察到的DO缺陷的原因,但使用测量的SOD数据来计算废物负荷分配和许可限值并不是一个标准程序。本文记录了不正确的SOD估算值如何导致在理解导致与溶解氧浓度有关的水质问题的治理现象方面出现错误。

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