Department of Water and Water Structures Engineering, Faculty of Engineering, Zagazig University, Zagazig, 44519, Egypt.
Civil Engineering Department, College of Engineering, Shaqra University, Dawadmi, 11911, Saudi Arabia.
Environ Sci Pollut Res Int. 2020 Jun;27(18):23234-23245. doi: 10.1007/s11356-020-08891-1. Epub 2020 Apr 25.
Saltwater intrusion (SWI) is a physical problem that threatens many coastal aquifers all over the world. Saltwater intrusion is increasing with abstraction and rise in sea level. Coastal aquifer protection is essential to protect groundwater resources in these areas. A number of methods have been developed to protect coastal aquifers from SWI. This paper presents the impact of sea level rise on SWI in coastal aquifers and application of coastal earth fill as a new technique to control SWI. Different future sea level rise scenarios were studied and different coastal earth fill with an appropriate soil to extend the coastline towards the sea in order to control SWI was studied using SEAWAT model. The proposed control measure is numerically assessed by Henry's problem and then applied to a real case study of Biscayne aquifer, Florida, USA. For each aquifer, the corresponding relation was developed between the intrusion length of saltwater wedge and the width of fill. The results showed that increasing the fill width resulted in decreasing the intrusion length. In the case of Biscayne aquifer, increasing the fill width by 10, 20, 30, and 40% of the aquifer length resulted in retarding the intrusion to 329, 192, 42, and - 48 m respectively. Using 150- and 300-m fill widths retards the intrusion length by 32.3% and 60.5%. In addition, increasing the fill width to 465 m can retard SWI by 91.3%. This approach is capable to control the future risks of SWI and sea level rise.
海水入侵(SWI)是一种物理问题,威胁着世界各地的许多沿海含水层。随着开采量的增加和海平面的上升,海水入侵问题日益严重。保护沿海含水层对于保护这些地区的地下水资源至关重要。已经开发了许多方法来保护沿海含水层免受 SWI 的影响。本文介绍了海平面上升对沿海含水层中海水入侵的影响,并应用沿海填土作为控制海水入侵的新技术。研究了不同的未来海平面上升情景,并研究了不同的沿海填土,使用适当的土壤向海延伸海岸线,以控制海水入侵,使用 SEAWAT 模型。通过亨利问题对提出的控制措施进行了数值评估,然后将其应用于美国佛罗里达州比斯坎含水层的实际案例研究。对于每个含水层,都开发了咸水楔侵入长度与填土宽度之间的相应关系。结果表明,增加填土宽度会导致侵入长度减小。在比斯坎含水层的情况下,将填土宽度增加含水层长度的 10%、20%、30%和 40%,分别将入侵延迟到 329、192、42 和-48m。使用 150m 和 300m 的填土宽度,可将入侵长度延迟 32.3%和 60.5%。此外,将填土宽度增加到 465m 可以将 SWI 延迟 91.3%。这种方法能够控制未来海水入侵和海平面上升的风险。