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利用卡马西平作为示踪剂对碳酸盐含水层中的污水渗漏和运移进行建模。

Modeling sewage leakage and transport in carbonate aquifer using carbamazepine as an indicator.

机构信息

Zuckerberg Institute for Water Research, J. Blaustein Institutes for Desert Research, Ben-Gurion University of the Negev, Israel; Etgar A. Engineering Ltd., Israel.

Zuckerberg Institute for Water Research, J. Blaustein Institutes for Desert Research, Ben-Gurion University of the Negev, Israel.

出版信息

Water Res. 2018 Jan 1;128:157-170. doi: 10.1016/j.watres.2017.10.044. Epub 2017 Oct 31.

Abstract

The Western Mountain Aquifer (Yarkon-Taninim) of Israel is one of the country's major water resources and partially flows through a karst system. During late winter 2013, maintenance actions were performed on a central sewage pipe that caused sewage to leak into the creek located in the study area. Carbamazepine (CBZ) was used as an indicator for the presence of sewage in the groundwater. The research goal was to develop a mathematical model for quantifying flow and contaminant transport processes in the karst/fractured-porous unsaturated zone and groundwater system. The model was used to simulate CBZ transport during and after an observed sewage leakage event. A quasi-3D dual permeability numerical model represents the 'vadose zone - aquifer' system, by a series of 1D vertical flow and transport equations solved in a variably-saturated zone and by 3D-saturated flow and transport equation in groundwater. The results of simulation showed that after the leakage stopped, significant amounts of CBZ were retained in the porous matrix of the unsaturated zone below the creek. Water redistribution and slow recharge during the dry summer season contributed to a continuous supply of CBZ to the groundwater in the vicinity of the creek and hundreds of meters downstream.

摘要

以色列西山含水层(雅尔孔-塔尼尼姆)是该国的主要水资源之一,部分流经喀斯特系统。2013 年底冬,对一条中央污水管进行了维护,导致污水泄漏到研究区域的小溪中。卡马西平(CBZ)被用作地下水存在污水的指示剂。研究目标是开发一种数学模型,以量化喀斯特/裂隙-多孔非饱和带和地下水系统中的水流和污染物运移过程。该模型用于模拟观测到的污水泄漏事件期间和之后的 CBZ 运移。准 3D 双重渗透率数值模型通过一系列在非饱和带中求解的 1D 垂直流动和传输方程以及在地下水 3D 饱和流动和传输方程来表示“包气带-含水层”系统。模拟结果表明,泄漏停止后,小溪下方非饱和带多孔基质中仍保留了大量 CBZ。干旱夏季的水分再分配和缓慢补给导致小溪附近和数百米下游地下水中 CBZ 的持续供应。

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