Groundwater quality assessment along the West of New Damietta Coastal City of Egypt using an integrated geophysical and hydrochemical approaches
Environmental Earth Sciences
(2023) 82:107
https://doi.org/10.1007/s12665-023-10762-0
ORIGINAL ARTICLE
Groundwater quality assessment along the West of New
Damietta Coastal City of Egypt using an integrated geophysical
and hydrochemical approaches
Gehad Gamal1 · Taher Mohammed Hassan2 · Ahmed Gaber1 · Mohamed Abdelfattah1
Received: 10 August 2022 / Accepted: 14 January 2023
© The Author(s) 2023
Abstract
Recently, the groundwater became very important source for the Egyptian water balance. Therefore, assessing its quality and
quantity is necessary before initiating any developmental plans using this resource. In this research, a new operated power
plant, which is located in the coastal area of West New Damietta City, north-east of Egypt was designed to work using the
coastal groundwater aquifer. Therefore, an integrated approaches of both geophysical methods and hydrochemical analysis
were applied to identify the subsurface lithology, the water-bearing layers and determine the potential use of such coastal
groundwater. Therefore, a total of seventeen vertical electrical soundings (VES) and five time-domain electromagnetic
soundings (TEM) were performed. Moreover, groundwater samples were collected from seven existing wells to be analyzed
for water quality assessment. The geophysical results identified five geoelectric layers. The first geoelectric layer has a
resistivity of 1–7.9 Ω m and a thickness range of 7–9 m. The second layer has a resistivity of 0.9–4.4 Ω m and a thickness
range of 7–8 m. The third layer is 10–21 m thick with a resistivity value of 0.5–2 Ω m. The fourth layer, which is thicker (29
to 42 m), has a resistivity of 0.7–3 Ω m, while the last layer has a resistivity of 1.7–9 Ω m. According to the hydrochemical
analysis, the aquifer is dominated by Na–Cl water type. The brackish nature of the water is revealed by the TDS range of
7035 mg/l to 7735 mg/l. The results collected demonstrate the groundwater's quantity and quality availability for the power
plant’s sustainable use.
Keywords Groundwater assessment · Hydrochemistry · Geophysics · Coastal aquifer · West New Damietta · Egypt
Abbreviations
VES Vertical electrical soundings
TEM Time-domain electromagnetic
TDS The total dissolved solids
EC Electric conductivity
S.W.L Static water level
WHO World Health Organization
ppm Part per million
* Gehad Gamal
1
Geology Department, Faculty of Science, Port Said
University, Port Said, Egypt
2
National Water Research Centre, Research Institute
for Groundwater, Cairo, Egypt
Introduction
Coastal areas have become progressively developed around
the world. They cover over 10% of the planet’s surface and
contain more than half of the world's population, as well as
human activities (Chatton et al. 2016). The Egyptian coastal
region is undergoing tremendous demographic, environmental, economic, and social developments with a high concentration of water-demanding human activities (De Filippis
et al. 2016). Development projects, including agriculture,
domestic water use, and electricity generation, require a
sustainable supply of fresh water. In the absence of applicability of the nearby surface water resources, the demand
for groundwater resources is the alternative (Eltarabily and
Negm 2019).
West New Damietta is one of Egypt’s coastal regions,
located northeast of the Nile Delta, where the increase in
human demands and the expansion of national projects
have necessitated the need for long-term water supplies.
Therefore, this research is to investigate the groundwater
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potentiality within the study area by using geophysical
techniques. Regarding the direct relationship between the
hydraulic characteristics of geological formations and
existing fluids, electrical and electromagnetic geophysical
techniques have been widely used in coastal hydrogeological investigations (Freeze and Cherry 1979; Stewart 1981;
Fitterman and Stewart 1986; Duque et al. 2008; Zarroca
et al. 2011). Electrical method is the most widely utilized
technology for investigating groundwater resources due to
its excellent performance (De breuck and De moor 1969;
Choudhury and Saha 2004; Adepelumi et al. 2009; Himi
et al. 2017). Recently, numerous research also has shown
the accuracy of the TEM approach (Meju et al. 2000; Guérin et al. 2001; Danielsen et al. 2003; Tsourlos et al. 2004;
Kontar and Ozorovich 2006; Metwaly et al. 2006; Barlow
and Reichard 2010; Soupios et al. 2010; Trabelsi et al. 2013;
Herckenrath et al. 2013; Kanta et al. 2013; Gonçalves et al.
2017; Himi et al. 2017) due to its sensitivity to conductive
anomalies (Abdelfattah et al. 2021).
Groundwater quality is critical because it affects the capability of water for numerous applications. It is very important to define groundwater quality and its hydrogeochemical
characterization for assessing whether or not this water is
suitable for various purposes.
Chemicals that are dissolved in water may have long-term
negative effects on human health as well as cause cosmetic
problems (Ahmed et al. 2019). As a result, anthropogenic
activity and waste outflow with hazardous mixtures generate
major problems for aquatic ecosystem communities and have
a potential impact on human health (Duruibe et al. 2007).
The valuable resources such as water resources have been
polluted by land- and water-based societal activities, and
in certain cases, the exploitation of these resources might
contaminate the nearby aquifers (Vasanthavigar et al. 2010).
Fig. 1 Location map of the
power plant (study area)
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Environmental Earth Sciences
(2023) 82:107
Many studies were carried out on groundwater quality
evaluation and hydrochemical characterization (Brindha
et al. 2014; Sajil Kumar et al. 2014; Wu et al. 2014, 2015;
Bouzourra et al. 2015; Vetrimurugan and Elango 2015; Li
et al. 2016). In addition, many researchers in Egypt have
focused on groundwater resources in terms of quality
(Masoud 2014; Armanuos et al. 2016; Negm and Armanuos
2017; El-Rawy et al. 2019; Salem et al. 2019; Ding et al.
2020; Hegazy et al. 2020; Mansour 2020; El-Kholy et al.
2022).
The physical and chemical properties of groundwater
are influenced by both natural and anthropogenic causes.
Natural factors include lithology, groundwater velocity,
water–rock interaction, evaporation/crystallization, oxidation or reduction reactions, salt solubility and recharge water
quality; anthropogenic factors entail agriculture, industry,
mining, urban development, etc. (Jeong 2001; Hussein 2004;
Hosseinifard and Mirzaei Aminiyan 2015). Numerous investigations focused on evaluating the hydrochemical changes
and showing their spatial distributions using geographic
information systems (GIS) (Ahmed et al. 2020a, b) as well as
statistical techniques (Ahmed et al. 2020a). Therefore, this
study aims at identifying the groundwater quality close to
the newly constructed power plant in New Damietta coastal
area and evaluate the underneath coastal aquifer (...truncated)