Subsurface complexity controls the aquifer heterogeneity: A case study from the Al-Hassa oasis, Eastern Saudi Arabia

被引:0
|
作者
Khogali, Abid [1 ]
Chavanidis, Konstantinos [1 ]
Stampolidis, Alexandros [2 ]
Kirmizakis, Panagiotis [3 ]
Yassin, Mohamed [4 ]
Abu-Mahfouz, Israa S. [1 ]
Al-Shaibani, Abdulaziz [5 ]
Tawabini, Bassam [1 ]
Soupios, Pantelis
机构
[1] King Fahd Univ Petr & Minerals, Coll Petr Engn & Geosci, Dept Geosci, Dhahran 31261, Saudi Arabia
[2] Aristotle Univ Thessaloniki, Dept Geophys, Thessaloniki 54124, Greece
[3] King Fahd Univ Petr & Minerals, Coll Petr Engn & Geosci, Ctr Integrat Petr Res, Dhahran 31261, Saudi Arabia
[4] King Fahd Univ Petr & Minerals, Interdisciplinary Res Ctr Membranes & Water Secur, Dhahran 31261, Saudi Arabia
[5] Minist Environm Water & Agr, Riyadh 11195, Saudi Arabia
关键词
Groundwater chemistry; Subsurface heterogeneity; Gravity survey; Geological controls; Al-Hassa oasis; GROUNDWATER SALINITY; GRAVITY; BASIN; LANDSCAPE; AREA;
D O I
10.1016/j.gsd.2024.101322
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Al-Hassa region in the eastern part of Saudi Arabia is well-known for its geological and hydrogeological importance since it has historically hosted over 280 natural springs, which were used to irrigate the largest oasis in the world. Al-Hassa is located near the renowned Ghawar oil field, the largest conventional oil field globally, which represents a potential pollution source. This study utilizes and integrate hydrochemical investigations and geophysical gravity surveys to understand and reconstruct the subsurface heterogeneity in the Al-Hassa area. The dataset encompasses 113 groundwater wells distributed across the Al-Hassa Oasis which have been analyzed for salinity major ions, and isotopic (oxygen and hydrogen) compositions. A total of 571 gravity stations covering the broader oasis area (approximately 350 km2) 2 ) are collected, processed, and modeled. The combined hydro- chemical and geophysical results show a good agreement between groundwater quality and density (gravity anomalies) distribution within the study area. The southeastern part of the study area exhibits distinctive positive gravity anomalies, indicating denser rock formations alongside high total dissolved solids (TDS) in groundwater, reflecting poor water quality. Conversely, the southwest displays significant negative gravity anomalies, suggesting basins filled with loose sediments and low TDS values, signifying good water quality. Furthermore, the study reveals a certain pattern in groundwater temperature distribution, with cooler waters in the areas characterized by negative gravity anomalies (basins), and hotter waters emerging from areas with positive gravity anomalies. These findings suggest that groundwater quality differences may stem from varying sub-basins and interactions with distinct geological substrates. Temperature variations may also be attributed to differing subsurface flow pathways. This study attempts to explain the controlling factors for groundwater heterogeneity in the Al-Hassa Oasis area, emphasizing the role of geological, tectonic, and hydrogeological elements in shaping the Oasis's hydrological and hydrochemical pattern.
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页数:16
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