Seawater Intrusion Mapping Using Geophysical Methods, Piezometry, and Hydrochemical Data Analysis: Application in the Coastal Aquifer of Nador Wadi Plain in Tipaza (Algeria)

IF 1.9 4区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS pure and applied geophysics Pub Date : 2024-08-30 DOI:10.1007/s00024-024-03565-2
Mohamed Amine Bechkit, Abdelmadjid Boufekane, Gianluigi Busico, Giuseppe Francesco Cesare Lama, Fayçal Chafiheddine Mouhoub, Moussa Aichaoui, Khiereddine Arrache, Seid Bourouis
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Abstract

Nowadays the salinization of freshwater resources due to seawater intrusion represent a worldwide issue. Accordingly, this study aims to identify and locate the freshwater-saltwater interface in the downstream part of the Nador wadi plain (Algeria), a coastal area characterized by a semi-arid mediterranean climate using a multi-methodologies approach including geophysical methods, hydrostatics approach, hydrochemical method, and piezometry situation. The investigation was carried out by the electrical survey and refraction seismic methods in the period of April-May 2018. Moreover, the hydrochemical and piezometry methods were used to confirm the results of the geophysical technique. The results of the present study case showed that the seawater intrusion interface is located at 420–1380 m from the shoreline. Additionally, the presence of the bedrock bulge (clay formation) at a distance ranging between 550 and 1050 m from the shoreline, plays the role of the natural hydraulic barrier for the seawater advance. The findings indicate that the identified seawater intrusion interface and the natural hydraulic barrier formed by the bedrock bulge are critical for managing groundwater resources in the Nador wadi plain. This methodology can be applied to other coastal plains worldwide to address the challenges of seawater intrusion and groundwater salinization.

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利用地球物理方法、压强测量和水化学数据分析绘制海水入侵图:在提帕扎纳多尔瓦迪平原沿海含水层中的应用(阿尔及利亚)
如今,海水入侵导致淡水资源盐碱化已成为世界性问题。因此,本研究旨在采用多种方法(包括地球物理方法、水文方法、水化学方法和压强测量法)确定纳祖尔瓦迪平原(阿尔及利亚)下游地区淡水-盐水界面的位置,该沿海地区的特点是半干旱地中海气候。调查于 2018 年 4 月至 5 月期间通过电测法和折射地震法进行。此外,还使用了水化学方法和压强测量方法来确认地球物理技术的结果。本研究案例的结果显示,海水入侵界面位于距离海岸线 420-1380 米处。此外,在距离海岸线 550 米至 1050 米处存在基岩隆起(粘土层),为海水入侵起到了天然水力屏障的作用。研究结果表明,已确定的海水入侵界面和基岩隆起形成的天然水力屏障对于纳祖尔瓦迪平原的地下水资源管理至关重要。这一方法可应用于全球其他沿海平原,以应对海水入侵和地下水盐碱化的挑战。
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来源期刊
pure and applied geophysics
pure and applied geophysics 地学-地球化学与地球物理
CiteScore
4.20
自引率
5.00%
发文量
240
审稿时长
9.8 months
期刊介绍: pure and applied geophysics (pageoph), a continuation of the journal "Geofisica pura e applicata", publishes original scientific contributions in the fields of solid Earth, atmospheric and oceanic sciences. Regular and special issues feature thought-provoking reports on active areas of current research and state-of-the-art surveys. Long running journal, founded in 1939 as Geofisica pura e applicata Publishes peer-reviewed original scientific contributions and state-of-the-art surveys in solid earth and atmospheric sciences Features thought-provoking reports on active areas of current research and is a major source for publications on tsunami research Coverage extends to research topics in oceanic sciences See Instructions for Authors on the right hand side.
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