联合下水道中有机固体的来源和侵蚀

M Ahyerre, G Chebbo, M Saad
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引用次数: 38

摘要

下水道沉积物在合流下水道溢流中扮演着重要的污染源角色。本文的目的是利用下水道长度的直接方法,确定不同沉积物中有机固体的主要来源及其侵蚀过程。研究的不同沉积物是下水道底部的大型无机固体,下水道壁上的生物膜和水床界面的有机固体。所采用的方法首先包括非常精确地分析(质量和污染物负荷)沿着一条150米长的污水管道的三种沉积物中的固体。然后,利用自来水对沉积物进行原位冲刷试验。最后,将沿下水道长度方向侵蚀颗粒的性质和质量与各类下水道沉积物的性质和固体质量进行比较,以确定下水道中有机固体的主要来源。结果表明,水床界面有机层是侵蚀固体的主要来源。在连续观察下进行的侵蚀试验证实,有机层实际上受到了侵蚀。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Sources and erosion of organic solids in a combined sewer

Sewer deposits play a significant role as a source of pollution in combined sewer overflows. The objective of this paper is to identify, using a direct approach on a sewer length, the main source of organic solids among the different deposits and their erosion processes. The different deposits studied were large inorganic solids at the bottom of the sewer, biofilms on the walls of the sewer and organic solids at the water–bed interface. The method applied consisted firstly of analysing very precisely (mass and pollutant loads) the solids in the three types of deposits along a sewer line with a length of 150 m. Then, the deposits were eroded by in situ flushing experiments using tap water. Finally the nature and the mass of particles eroded along the length of the sewer were compared with the nature and the mass of solids in each type of sewer sediment in order to identify the main source of organic solids in the sewers. This comparison indicates that the organic layer at water–bed interface is the main source of eroded solids. An erosion test carried out under continuous observation confirms that the organic layer is actually eroded.

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