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Evaluating impacts of recharging partially treated wastewater on groundwater aquifer in semi-arid region by integration of monitoring program and GIS technique

机译:通过融合监测计划和GIS技术评估对半干旱地区地下水含水层对地下水含水层的影响

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The current study investigates the impact of recharging of partially treated wastewater through an infiltration basin on the groundwater aquifer quality parameters. A monitoring program supported by a geographic information analysis (GIS) tool was used to conduct this study. Groundwater samples from the entire surrounding boreholes located downstream the infiltration basin, in addition to samples from the recharged wastewater coming from the Beit Lahia wastewater treatment (BLWWTP), were monitored and analysed between 2011 and 2014. The analysis was then compared with the available historical data since 2008. Results revealed a groundwater replenishment with the groundwater level increased by 1.0-2.0 m during the study period. It also showed a slight improvement in the groundwater quality parameters, mainly a decrease in TDS, Cl- and NO3- levels by 5.5, 17.1 and 20%, respectively, resulting from the relatively better quality of the recharged wastewater. Nevertheless, the level of boron and ammonium in the groundwater wells showed a significant increase over time by 96 and 100%, respectively. Moreover, the infiltration rate was slowed down in time due to the relatively high level of total suspended solid (TSS) in the infiltrated wastewater.
机译:目前的研究调查了通过在地下水含水层质量参数上渗透盆地进行部分处理的废水的冲击。通过地理信息分析(GIS)工具支持的监测程序进行了这项研究。从位于渗透盆地下游的整个周围钻孔的地下水样本,除了来自Beit Lahia废水处理(Blwwtp)的再充电废水的样品,于2011年和2014年间分析。然后将分析与可用的历史进行比较自2008年以来的数据。结果显示,在研究期间,地下水位达到了地下水位增加了1.0-2.0米。它还表现出地下水质量参数略有改善,主要是TDS,CL-和NO3的降低分别为5.5,17.1和20%,由充电废水的相对更好的质量产生。然而,地下水孔中的硼和铵的水平分别显着增加了96%和100%。此外,由于渗透废水中的相对高水平的悬浮固体(TS)含量相对较高,渗透速率在时间上减慢。

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