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首页> 外文期刊>Estuaries and coasts >Fate and Transport of Hydrophobic Organic Chemicals in the Lower Passaic River: Insights from 2,3,7,8- Tetrachlorodibenzo-p-Dioxin
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Fate and Transport of Hydrophobic Organic Chemicals in the Lower Passaic River: Insights from 2,3,7,8- Tetrachlorodibenzo-p-Dioxin

机译:低Passaic河中疏水性有机化学物质的结局和运输:从2,3,7,8-四氯二苯并-p-二恶英的见解

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The fate and transport of hydrophobic organic chemicals (HOCs) is particularly complex in estuaries because of bidirectional longitudinal currents, density stratification, the tendency to trap sediments, and significant dilution in the downstream bay or ocean. Investigations of HOCs in estuaries are further complicated because HOCs typically enter from multiple sources. The distribution of contaminants in estuarine sediment beds reflect a time integration of a complex balance of time- and space-variable fate and transport processes and loading history. A unique opportunity to study HOC fate and transport exists in the Lower Passaic River (LPR), where a pesticide manufacturer was the dominant source of 2,3,7,8-tetrachlorodibenzo-p-dioxin (2,3,7,8- TCDD) to the estuary and the distribution of this "tracer of opportunity" provides insights about fate and transport processes in estuarine systems. This paper presents observed sediment 2,3,7,8-TCDD patterns within the LPR and the adjacent Newark Bay, and interprets them in terms of fate and transport processes that likely distributed the contaminant from its dominant source, drawing upon other physical datasets as needed. Major observations include that estuarine transport processes have distributed 2,3,7,8-TCDD approximately 18 km upstream of the source and downstream across Newark Bay, and that, generally, HOC trapping processes within the LPR have been highly effective, particularly near the 2,3,7,8-TCDD source and in downstream areas. The present LPR surface sediment 2,3,7,8-TCDD distribution indicates spatially variable recovery, which appears broadly driven by historical net sedimentation patterns, though the dominant processes may be shifting as the system continues to evolve.
机译:疏水性有机化学物质(HOC)的命运和运输在河口中特别复杂,这是因为双向纵向水流,密度分层,捕获沉积物的趋势以及下游海湾或海洋的大量稀释。由于HOC通常是从多个来源进入的,因此对河口HOC的调查更加复杂。河口沉积床中污染物的分布反映了时间和空间变化的命运,运输过程和装载历史的复杂平衡的时间积分。在较低的Passaic河(LPR)中,存在研究HOC命运和运输的独特机会,那里的农药生产商是2,3,7,8-四氯二苯并-p-二恶英(2,3,7,8- TCDD)到河口,这种“机会追踪者”的分布提供了有关河口系统中命运和运输过程的见解。本文介绍了在LPR和邻近的纽瓦克湾内观察到的沉积物2,3,7,8-TCDD模式,并根据可能从主要来源分配污染物的命运和运输过程来解释它们,并利用其他物理数据集需要。主要的观察结果包括,河口的运输过程在震源上游和下游穿过纽瓦克湾约18 km处分布了2,3,7,8-TCDD,并且一般而言,LPR内的HOC捕集过程非常有效,特别是在河床附近。 2,3,7,8-TCDD源和下游地区。目前的LPR表面沉积物2,3,7,8-TCDD分布表明空间变量的恢复,这似乎是由历史上的净沉积模式驱动的,尽管随着系统的不断发展,主要过程可能正在转移。

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