Investigating the Structure of a Coastal Karstic Aquifer through the Hydrogeological Characterization of Springs Using Geophysical Methods and Field Investigation, Gökova Bay, SW Turkey

Water

卷:12

Pantelis Soupios¹  Korhan Ayrancı¹  SanLinnI. Kaka¹  Moumtaz Razack²  MustafaCan Canoğlu³  Erkan Düztaş⁴  Çağdaş Sağır⁴  Günseli Erdem⁴  Bedri Kurtuluş⁴  MuratErsen Aksoy⁴  Özgür Avşar⁴  Emrah Pekkan⁵ 

[1] College of Petroleum Engineering & Geosciences, King Fahd University of Petroleum and Minerals, Dhahran 31261, Saudi Arabia;

[2] Department of Hydrogeology, University of Poitiers, UMR CNRS 7285, 5 rue Albert Turpain, 86073 Poitiers, France;

[3] Environmental Engineering Department, Sinop University, 57002 Sinop, Turkey;

[4] Geological Engineering Department, Muğla Sıtkı Koçman University, Menteşe, 48000 Muğla, Turkey;

[5] Institute of Earth and Space Sciences, Eskişehir Technical University, 26555 Eskişehir, Turkey;

关键词: electrical resistivity tomography;    induced polarization;    3D imaging;    karstic aquifer;   

DOI  :  10.3390/w12123343

来源: DOAJ

【 摘 要 】

The electrical resistivity tomography method has been widely used in geophysics for many purposes such as determining geological structures, water movement, saltwater intrusion, and tectonic regime modeling. Karstic springs are important for water basin management since the karst systems are highly complex and vulnerable to exploitation and contamination. An accurate geophysical model of the subsurface is needed to reveal the spring structure. In this study, several karst springs in the Gökova Bay (SW, Turkey) were investigated to create a 3D subsurface model of the nearby karstic cavities utilizing electrical resistivity measurements. For this approach, 2D resistivity profiles were acquired and interpreted. Stratigraphically, colluvium, conglomerate, and dolomitic-limestone units were located in the field. The resistivity values of these formations were determined considering both the literature and field survey. Then, 2D profiles were interpolated to create a 3D resistivity model of the study area. Medium-large sized cavities were identified as well as their locations relative to the springs. The measured resistivities were also correlated with the corresponding geological units. The results were then used to construct a 3D model that aids to reveal the cavity geometry in the subsurface. Additionally, several faults are detected and their effect on the cavities is interpreted.

【 授权许可】

Unknown