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Didik Sugiyanto
Universitas Darma Persada
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Journal : Journal of Geoscience, Engineering, Environment, and Technology

 1 
Subsurface Interpretation for Groundwater Potential Mapping Using Electrical Resistivity Tomography (ERT) in Mon Ikeun Village, Aceh Besar, Indonesia Latifa, Adila; Sugiyanto, Didik; Syukri, Muhammad
Journal of Geoscience, Engineering, Environment, and Technology Vol. 10 No. 3 (2025): JGEET Vol 10 No 03 : September (2025)
Publisher : UIR PRESS

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.25299/jgeet.2025.10.3.22580

Abstract

The Mon Ikeun Village area in Aceh Besar is experiencing a clean water crisis due to a prolonged drought, which has significantly impacted human needs and necessitates identifying alternative water sources. This study aims to determine groundwater potential in the area using the Electrical Resistivity Tomography method. Data acquisition was conducted along three survey lines, each 420 m long. The Wenner-Schlumberger configuration was employed, using 22 electrodes with a spacing of 20 m. Data processing was done using ResIPy software to generate 2D resistivity cross-sections representing the subsurface structure. The resistivity sections were interpreted by correlating them with regional geological data and secondary data from wells located near the study area. The results indicate that two different lithologies dominate the subsurface structure of the study area. The first is a conductive zone with resistivity values of ≤316.23 Ω.m, interpreted as alluvium composed of clay, sand, and gravel. The second is a resistive zone with resistivity values of ≥562.34 Ω.m, interpreted as bedrock composed of limestone. Based on the subsurface lithology, zones with groundwater potential are found in conductive areas with resistivity values ranging from 3.16 to 56.23 Ω.m, which are associated with water-saturated alluvial layers, particularly those dominated by clay and sand. From the 2D resistivity cross-sections analysis, line 3 shows the highest potential for groundwater exploration, with water-saturated layers occurring at both shallow and deeper depths, reaching up to 0–40 m. This study provides valuable information for water resource management in Mon Ikeun Village, especially in addressing future clean water shortages.
Subsurface Alteration Characteristics Due to Hydrothermal Influence Using the Geoelectrical Method in the Ie Seu’um Geothermal Area, Aceh Besar Hasana, Nur; Sugiyanto, Didik; Muksin; Syukri, Muhammad
Journal of Geoscience, Engineering, Environment, and Technology Vol. 10 No. 4 (2025): JGEET Vol 10 No 04 : December (2025)
Publisher : UIR PRESS

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.25299/jgeet.2025.10.4.24674

Abstract

Research on subsurface alteration due to hydrothermal fluid influence was conducted in the hydrothermal manifestation area of Mesjid Raya District, Aceh Besar, Aceh. Data was acquired using the electrical resistivity method with a Wenner–Schlumberger configuration along four survey lines. Survey Lines 1 and 2, each 106.5 m long with 1.5 m electrode spacing, represent Zone 1, which is located directly at the hot spring source. Survey Lines 3 and 4, each 210 m long with 3 m electrode spacing, represent Zone 2, located 3.5 km from Zone 1 and 2 unaffected by hot fluid flow. This study aimed to identify the geothermal influence on subsurface characteristics. The results revealed clear differences in the resistivity profiles between Zones 1 and 2, with resistivity variations ranging from 0–600 Ωm and 0–5000 Ω·m, respectively. Interpretation indicates that Zone 1 consists of hydrothermally altered volcanic rocks, while Zone 2 comprises alluvium affected by weathering in the unsaturated (vadose) zone under meteoric water influence. These subsurface alterations provide essential evidence of geothermal impacts on rock characteristics. The findings also support the interpretation that the Ie Seu’um geothermal system is strongly concentrated in Zone 1, whereas surrounding areas show weaker manifestations that do not support the development of an active geothermal system.
Co-Authors -, Nopryandi . Zulfahriza Aep Saeful Uyun Aep Saeful Uyun Aep Saepul Uyun Aep Saipul Uyun Agil Saputro Agus Munandar Aisa Aulia Andriansyah, Septian Anggara, Ardhito Yogie Antasti, Erico As'yari Asyari Asyari Darius Asyari Daryus, Asyari Asyari, Asyari Aulia, Aisa Bagas, Stefanus Besus Dwi Putranto Budhi Susetyo, Ferry Budi Sumartono Daryus, Asy'ari Dewi Dyah Maharani, Maya Djabumir, Sendi Setiawan Dwiki Novandi Dzul Mujahid Jihad Egar Ruli Anmar Erwin Erwin Erwin Erwin Erwin Fahmi Aldi Fandikurnia, Ade Fitriani Fitriani Handayani, Diah Kusuma Handi Hasan Basri hasana, Nur Hernando Christian Herry Susanto Herry Susanto Hidayatullah Hidayatullah Husen Asbanu Ibnu Rusydy Ibrahim, Riki Firmandha Imam Munandar Jamaluddin Purba Joko Mai Kadlina Kadlina, Kadlina Latifa, Adila Lestari, Putri Winda Lono Satrio Maratis, Jerry Muhammad Ikhsan Muhammad Ilham Ramdan Muhammad Isa Muhammad Syahrullah Muhammad Syukri Muksin Mumpuni Ngesti Rahaju, Sri Ngesti Rahaju, Sri Mumpuni Nofendri, Yos Nopryandi Novendri, Yos Noverdo Mayanda Novianto, Bangun Pratama, Juan Rahaju, Sri Mumpuni Ngesti Resma Adi Pangestu Ricky Setiawan Rizky Nugroho Saban, Muhamad Zaki Saputra, Ganang Arya Sholichan, Sholichan Siregar, Rolan Siswanto, Muhamad Helmi Syamsu Marlin Taopik, Angga Trisna Ardi Wiradinata Uci Sulandari Warni Asnita Wicaksono, Enggar Darmawan yefri chan Yendi Esye Yusrizal Zahratun