CNR-IRPI, Italy.
Department of Hydrology, IIT Roorkee, India.
J Contam Hydrol. 2023 Nov;259:104267. doi: 10.1016/j.jconhyd.2023.104267. Epub 2023 Nov 8.
Aquifer Storage and Recovery (ASR), a subset of Managed Aquifer Recharge (MAR) techniques, is a promising technique to address water scarcity issues by recharging depleted aquifers. The application of ASR in saline groundwater regions is challenging due to mixing of recharged freshwater with the ambient saline groundwater, decreasing the recoverable amount of freshwater. This paper aimed to investigate the feasibility of ASR techniques for freshwater storage and recovery in saline confined aquifers using a laboratory scale physical model (100 cm length x 30 cm width x 60 cm depth). The study then explored the impact of operational factors (freshwater storage duration, injected freshwater volume, number of injection/extraction cycles etc.) on freshwater recovery from an applied ASR. Firstly, the behaviour of stored freshwater in a saline-confined aquifer was investigated, and in the next step, the impact of ASR operational parameters on the recovery efficiency (RE) was evaluated. Along with the physical model, these effects were studied using a mathematical model (MODFLOW linked with SEAWAT) for the representative aquifer system. The movement and spreading of the stored freshwater were monitored over time. The experimental results presented in this study suggested that several factors significantly influence the efficiency of ASR systems. A negative correlation between ambient groundwater salinity and average recovery efficiency (ARE) was confirmed, with decreasing ARE observed as the salinity level increased. The injection volume of freshwater was found to have a positive influence on ARE, although the relationship was non-linear, a polynomial trend was observed. The longer freshwater was stored in the aquifer, the lower ARE was reported, indicating a negative impact of storage duration on ASR performance. Finally, the number of successive cycles of ASR operation was found to have a positive influence on ARE, but the effect decreased with each subsequent cycle. This research provided valuable insights into the application of ASR techniques for freshwater storage and its enhanced recovery in saline confined aquifers.
含水层储存与恢复(ASR)是管理型含水层补给(MAR)技术的一个分支,通过补给枯竭的含水层来解决水资源短缺问题是一种很有前景的技术。在咸地下水区域应用 ASR 存在挑战,因为补给的淡水与环境咸地下水混合会降低可回收淡水的数量。本研究旨在通过实验室规模的物理模型(100cm 长 x 30cm 宽 x 60cm 深)研究 ASR 技术在咸水封闭含水层中储存和回收淡水的可行性。然后,研究了操作因素(淡水储存时间、注入淡水体积、注入/提取循环次数等)对应用 ASR 中淡水回收的影响。首先,研究了储存在咸水封闭含水层中的淡水的行为,其次,评估了 ASR 操作参数对回收效率(RE)的影响。除了物理模型,还使用 MODFLOW 与 SEAWAT 链接的数学模型研究了代表性含水层系统中的这些效应。随着时间的推移,监测了储存淡水的移动和扩散。本研究的实验结果表明,有几个因素会显著影响 ASR 系统的效率。环境地下水盐度与平均回收效率(ARE)呈负相关,随着盐度的升高,ARE 呈下降趋势。注入淡水的体积对 ARE 有积极的影响,尽管关系是非线性的,但观察到了多项式趋势。储存在含水层中的淡水时间越长,ARE 越低,这表明储存时间对 ASR 性能有负面影响。最后,发现 ASR 操作的连续循环次数对 ARE 有积极的影响,但随着后续循环次数的增加,影响会减小。这项研究为 ASR 技术在咸水封闭含水层中储存和增强回收淡水方面的应用提供了有价值的见解。