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Groundwater intrusion into leaky sewer systems.

机译:地下水侵入泄漏的下水道系统。

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摘要

Vast volumes of groundwater are drained by urban sewer systems. This unwanted flow component intrudes into sewer systems through leaky joints or connected house drains. However, unlike urban storm drainage, it has a high seasonal variation corresponding to groundwater storage and long slow recessions similar to baseflow in rivers also fed by shallow groundwater exfiltrating into the surface waters. By applying the nonlinear reservoir algorithm as used for baseflow separation from total flow in a river, groundwater flow is separated from daily measured influents to treatment plants in Lower Saxony and Baden-Württemberg, Germany and in the Terkos Lake watershed near Istanbul, Turkey. While waste water flows vary only moderately within a year, separated intruded groundwater flows show recessions and seasonal variations correlated to baseflow in neighbouring rivers. It is possible to conclude that recession characteristics of treatment plant influents allow quantification and prediction of groundwater intrusion into sewer systems.
机译:大量的地下水通过城市下水道系统排出。这种多余的流量成分通过泄漏的接头或相连的房屋排水管侵入下水道系统。但是,与城市暴雨排水不同,它的季节性变化大,对应于地下水的蓄积,而长期缓慢的衰退类似于河流中的底流,同样是由浅层地下水渗入地表水来补充的。通过应用用于从河流总流量中进行底流分离的非线性水库算法,将地下水流量与每日测得的入流水分离,分离到位于德国下萨克森州和巴登-符腾堡州以及土耳其伊斯坦布尔附近的Terkos湖流域的处理厂。虽然废水流量在一年之内变化不大,但单独的入侵地下水流量却显示出衰退和季节性变化,与邻近河流的基础流量有关。可以得出这样的结论,即污水处理厂进水口的衰退特性可以量化和预测地下水进入下水道系统。

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