Consiglio Nazionale delle Ricerche, Istituto di Ricerca sulle Acque, Reparto di Chimica e Tecnologia delle Acque, via Francesco De Blasio, 5, 70132 Bari, Italy.
J Environ Manage. 2013 Nov 30;130:306-12. doi: 10.1016/j.jenvman.2013.08.021. Epub 2013 Oct 5.
This study investigates the feasibility of management of aquifer recharge (MAR) in Lebanon by designing well barriers to remove seawater intrusion from the fractured carbonate aquifers. Groundwater flow and saltwater/freshwater 50% sharp interface have been modeled along the coastal area using the Ghyben-Herzberg theory. The groundwater flow simulations have been supported by field transmissivity estimations and depth measurements carried out on 44 wells during 2003. Results have shown the seawater intrusion in coastal aquifers at Jieh and Damour regions. Three well-injection barriers have been proposed. The water volumes for recharge and the barrier positions have been defined by means of groundwater flow simulations. MAR can provide a valuable contribution to colloid (even pathogen) removal from injectant water, although during water infiltration in subsoil the reduction of aquifer permeability causes clogging. A simple new model for estimating the soil-rock permeability reduction due to the well clogging has been presented. The MAR, including the soil aquifer treatment at Damour and Jieh regions, has been studied by considering aquifer transmissivity (and soil porosity) reduction caused by clogging. Furthermore, the appropriate mixing of the injectant water by using reclaimed water, groundwater and surface water can be simulated using the proposed models. The time required to achieve 5% of rock permeability reduction at the proposed well barriers ranged from 71 to 935 d, by changing water quality and flow rate for recharge. This study can assist regional governments with water management in areas affected by scarcity of freshwater by implementing appropriate well-barrier projects.
本研究通过设计井障来管理含水层补给(MAR),以去除滨海断裂碳酸盐含水层中的海水入侵,从而探讨了在黎巴嫩管理含水层补给的可行性。利用基希贝格-赫茨伯格理论,沿沿海地区对地下水流动和咸水/淡水 50%锐界面进行了建模。地下水流动模拟得到了 2003 年在 44 口井进行的现场渗透率估计和深度测量的支持。结果表明,在杰伊赫和达穆尔地区的滨海含水层中存在海水入侵。提出了三个注水屏障。通过地下水流动模拟确定了补给的水量和屏障的位置。MAR 可以为胶体(甚至病原体)从注入水中去除提供有价值的贡献,尽管在地下水入渗到地下时,含水层渗透率的降低会导致堵塞。提出了一种简单的新模型,用于估算由于井堵塞而导致的土壤-岩石渗透率降低。通过考虑由于堵塞而导致的含水层渗透率(和土壤孔隙率)降低,研究了包括达穆尔和杰伊赫地区的土壤含水层处理在内的 MAR。此外,可以使用提出的模型模拟通过再利用水、地下水和地表水来适当混合注入水。通过改变补给的水质和流量,在建议的井障处达到岩石渗透率降低 5%所需的时间范围为 71 至 935 天。本研究可以通过实施适当的井障项目,为受淡水短缺影响的地区的政府提供水资源管理方面的帮助。