Abstract

As Egypt’s population increases, the demand for fresh groundwater extraction will intensify. Consequently, the groundwater quality will deteriorate, including an increase in salinization. On the other hand, salinization caused by saltwater intrusion in the coastal Nile Delta Aquifer (NDA) is also threatening the groundwater resources. The aim of this article is to assess the situation in 2010 (since this is when most data is sufficiently available) regarding the available fresh groundwater resources and to evaluate future salinization in the NDA using a 3D variable-density groundwater flow model coupled with salt transport that was developed with SEAWAT. This is achieved by examining six future scenarios that combine two driving forces: increased extraction and sea level rise (SLR). Given the prognosis of the intergovernmental panel on climate change (IPCC), the scenarios are used to assess the impact of groundwater extraction versus SLR on the seawater intrusion in the Delta and evaluate their contributions to increased groundwater salinization. The results show that groundwater extraction has a greater impact on salinization of the NDA than SLR, while the two factors combined cause the largest reduction of available fresh groundwater resources. The significant findings of this research are the determination of the groundwater volumes of fresh water, brackish, light brackish and saline water in the NDA as a whole and in each governorate and the identification of the governorates that are most vulnerable to salinization. It is highly recommended that the results of this analysis are considered in future mitigation and/or adaptation plans.

Highlights

  • The Nile Delta in Egypt, along with its fringes, covers an area of approximately 30,000 km2 [1].It is occupied by the most populated governorates in Egypt

  • The results showed that the combined impact of sea-level rise (SLR)-induced land inundation and recharge rate variation is more significant compared to SLR impacts alone

  • This article presented an assessment of the impacts of sea-level rise (SLR) and groundwater extraction on saltwater intrusion (SWI) in the Nile Delta aquifer (NDA)

Read more

Summary

Introduction

The Nile Delta in Egypt, along with its fringes, covers an area of approximately 30,000 km2 [1]. It is occupied by the most populated governorates in Egypt. About 60% of Egypt’s population lives in the Nile Delta region. The Nile Delta aquifer (NDA) is a vast aquifer located between Cairo and the Mediterranean Sea [3]. The NDA was formed by Quaternary deposits with a wide variety of hydrogeological characteristics and spatially varying salinity levels [4].

Objectives
Methods
Results
Conclusion
Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call