Subsurface Characterization of the Al-Hassa National Park, Eastern Saudi Arabia, Using Multi-Geophysical Methods

被引:0
作者
Khogali, Abid [1 ]
Chavanidis, Konstantinos [1 ]
Kirmizakis, Panagiotis [2 ]
Stampolidis, Alexandros [3 ]
Ashadi, Abdul Latif [1 ,4 ]
Hanstein, Tilman [5 ]
Candansayar, Emin [6 ]
Soupios, Pantelis [1 ]
机构
[1] King Fahd Univ Petr & Minerals, Coll Petr Engn & Geosci, Dept Geosci, Dhahran 31261, Saudi Arabia
[2] King Fahd Univ Petr & Minerals, Coll Petr Engn & Geosci, Ctr Integrat Petr Res, Dhahran 31261, Saudi Arabia
[3] Aristotle Univ Thessaloniki, Sch Geol, Thessaloniki 54124, Greece
[4] Univ Cologne, Inst Geophys & Meteorol, D-50923 Cologne, Germany
[5] KMS Technol KJT Enterprises Inc, Houston, TX 77079 USA
[6] Ankara Univ, Dept Geophys Engn, TR-06830 Golbasi, Turkiye
关键词
Magnetotelluric; Transient electromagnetic; Gravity; 3D modeling; Geophysical data integration; Subsurface characterization; Geophysical modeling; 2-DIMENSIONAL JOINT INVERSION; DIRECT-CURRENT RESISTIVITY; ER-RADHUMA AQUIFER; ELECTROMAGNETIC METHODS; CRUSTAL STRUCTURE; GROUNDWATER; FIELD; TEM; INTRUSION; SYSTEM;
D O I
10.1007/s13369-024-09584-4
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
Al-Hassa, located in eastern Saudi Arabia, hosts the world's largest oasis and naturally irrigated land. Historically, 280 natural springs irrigated farms, with varying water quality suggesting a complex subsurface regime. To explore this, a multi-geophysical approach was applied in a remote part of the Al-Hassa National Park, where minimum cultural noise from agricultural and industrial activities is present. Five geophysical methods-210 gravity stations, a 3.6 km magnetic profile, 46 magnetotelluric (MT), six audio-magnetotelluric (AMT), and 35 transient electromagnetic (TEM) stations-were acquired to reconstruct a 3D subsurface model. Processing and integration of gravity and electromagnetic data revealed a complex underground structure with lateral resistivity (pr) discontinuities, a possible salt dome structure, and fracture zones affecting groundwater flow. Key findings include low-resistivity anomalies indicating potential basins filled with low-density (pd) sediments and high-resistivity zones suggesting basement rocks. The MT model reaches 4.5 km depth (z), while the 2D gravity model extends to 1.8 km. Low-resistivity zones in the MT data correlate with high-potential aquifers. The comparison of the gravity, TEM, and MT data showed good agreement, confirming the subsurface features. These results indicate significant hydrogeological complexity, impacting groundwater management and resource exploration. This comprehensive modeling approach provides insights into the qualitative hydrogeological characteristics and deeper subsurface conditions, potentially impacting the world's largest conventional oilfield, Ghawar, located in the vicinity of the study area (A).
引用
收藏
页码:433 / 452
页数:20
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