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ASSESSMENT OF GROUND WATER CONTAMINATION FROM AN INDUSTRIAL RIVER BY TIME SERIES-, FLOW MODELING- AND PARTICLE TRACKING METHODS

机译:按时间序列,流量建模和粒子跟踪方法评估工业河流污染的地面水污染

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The interaction of an industrial river and the groundwater aquifer in Florida are modeled by time scries-, flow modeling- and particle (racking methods, The major piuposc of the mcxleling ellbil is to delineate (lie possible contamination corridor in (lie aquifer as may be caused by llic infiltration cf polluted water from the industrial river. The interrelations of precipitation, river discharge and groundwater data series are first analyzed by methods of structural time series, in order to quantify the interdependence of the groundwater table and river gauge heights, and thus to statistically examine the hydraulic possibility of aquifer contamination. The interaction of the stream and the groundwater is simulated by tr?eUSGSMODFLOWmodel.For the calibration, simulated water tables are compared with the historical records of monitoring wells in the adjacent aquifer. Lateral 'stagnant' points of the water flow based on the transient simulation are connected to delineate the maximal contamination corridor along both sides of the stream. In addition, particle tracking simulations with varying water sources and forcing conditions are conducted to compute thedynamicmovementsofwatei'particlesoutandalongtheriver banks. The modeling results show that lateral migration of contaminants close to the industrial discharge point might be up to several thousands feet in cross-river direction during times when the normally gaining (effluent) stream becomes sectionally a losing (influent) stream. The last situation occurs especially during multiyear-long time spans with less-than-normal precipitation which, for Florida, happens during times between major El Niflo occurrences; i.e. during La Nina years.
机译:工业河流和地下水含水层在佛罗里达州的相互作用是通过时间脆弱的模型 - 流动建模和粒子(机架方法,McXLeling Ellbil的主要Piuposc是描绘(谎言可能的污染走廊(可能是含水层)由工业河流的LLIC渗透CF污水引起的。首先通过结构时间序列的方法分析降水,河流和地下水数据系列的相互关系,以量化地下水位和河流仪高度的相互依存,因此在统计上检查含水层污染的液压可能性。通过TRαeusgsmodflowModel模拟流和地下水的相互作用。与校准,模拟水表与相邻含水层中监测孔的历史记录进行比较。横向'停滞'基于瞬态仿真的水流点连接到界定最大续沿着溪流两侧的胺化走廊。此外,对具有不同水源和强制条件的粒子跟踪模拟,以计算ThedynamicMovementSofwatei'Particleoutandtheriver银行。建模结果表明,在正常增长(流出物)流变为损失(流水)流时,在近河上的横向循环迁移的横向迁移可能在跨河方向上高达几千英尺。最后的情况发生,特别是在多年度长时间的跨度,与佛罗里达州的沉淀不太正常的降水,在主要的El Niflo发生之间发生;即在La Nina期间。

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