Vertical electrical sounding for revealing the groundwater resources in the geothermal spring of Jaboi volcano

Yanis, Muhammad; Zaini, Nasrullah; Abdullah, Faisal; Isa, Muhammad; Marwan, Marwan; Idris, Syafrizal; Paembonan, Andri Yadi; Ananda, Riski; Zainal, Muzakir; Ghani, Azman Abdul; Saputra, Deni

doi:10.1007/s11600-023-01164-8

Artykuł - szczegóły

Tytuł artykułu

Vertical electrical sounding for revealing the groundwater resources in the geothermal spring of Jaboi volcano

Autorzy

Yanis Muhammad , Zaini Nasrullah , Abdullah Faisal , Isa Muhammad , Marwan Marwan , Idris Syafrizal , Paembonan Andri Yadi , Ananda Riski , Zainal Muzakir , Ghani Azman Abdul , Saputra Deni

Wybrane pełne teksty z tego czasopisma

https://www.springer.com/journal/11600

Identyfikatory

DOI

10.1007/s11600-023-01164-8

Warianty tytułu

Języki publikacji

Abstrakty

Geothermal energy is considered renewable energy that is environmentally friendly and sustainable compared to the conventional energy from fossil fuels. However, uncontrolled geothermal exploitation can cause a decrease in the groundwater table and reservoir temperature, such as in the Jaboi volcano on Weh Island, where a power plant has been built to generate electrical energy with an estimated power of 50 MWe but still has not been operated. A geophysical survey is needed to determine the local hydrothermal system, including groundwater reserves under the surface which can be used to refill the hydrothermal wells during exploitation. This study measured vertical electrical sounding (VES) data at 15 points near the crater and geothermal power plant. In addition, very-low-frequency (VLF) data that pass through the crater were also collected to determine the presence of other hydrothermal resources such as fractures and faults. The results of the 1D least-square inversion show three subsurface models where groundwater resources with low resistivity (< 1.5 Qm) are found at a depth of 50-100 m. The same results are also obtained from the 2D cross-section model that impermeable resistive anomalies in alluvial and tuff rocks dominate the near-surface area. The layer after groundwater is an impermeable rock in the form of breccia. The results of 2D VES and VLF modeling also show the presence of the Ceunohot and Leumomate faults, which are beneficial as fluid access to the surface. Based on the data analysis, the combination of VES and VLF data can be used to image shallow hydrothermal systems such as groundwater resources and faults in the Jaboi volcano.

Słowa kluczowe

VES groundwater resources geothermal energy Jaboi volcano

VES zasoby wód podziemnych geotermia wulkan Jaboi

Wydawca

Instytut Geofizyki PAN
Springer

Czasopismo

Acta Geophysica

Rocznik

2024

Tom

Vol. 72, no. 3

Strony

1617--1635

Opis fizyczny

Bibliogr. 36 poz.

Twórcy

autor

Yanis Muhammad

yanis@usk.ac.id

Geophysical Engineering Department, Universitas Syiah Kuala, Darussalam-Banda Aceh 23111, Indonesia

https://orcid.org/0000-0002-5773-6487

autor

Zaini Nasrullah

Geophysical Engineering Department, Universitas Syiah Kuala, Darussalam-Banda Aceh 23111, Indonesia
Physics Department, Universitas Syiah Kuala, Darussalam-Banda Aceh 23111, Indonesia

autor

Abdullah Faisal

Geophysical Engineering Department, Universitas Syiah Kuala, Darussalam-Banda Aceh 23111, Indonesia
Physics Department, Universitas Syiah Kuala, Darussalam-Banda Aceh 23111, Indonesia

autor

Isa Muhammad

Geophysical Engineering Department, Universitas Syiah Kuala, Darussalam-Banda Aceh 23111, Indonesia
Physics Department, Universitas Syiah Kuala, Darussalam-Banda Aceh 23111, Indonesia

autor

Marwan Marwan

Geophysical Engineering Department, Universitas Syiah Kuala, Darussalam-Banda Aceh 23111, Indonesia
Physics Department, Universitas Syiah Kuala, Darussalam-Banda Aceh 23111, Indonesia

autor

Idris Syafrizal

Physics Department, Universitas Malikussaleh, Lhokseumawe 24351, Indonesia

autor

Paembonan Andri Yadi

Geophysical Engineering Department, Institut Teknologi Sumatera, Lampung Selatan, Lampung, Indonesia

autor

Ananda Riski

Department of Geophysical Engineering, Faculty of Mining and Petroleum, Bandung Institute of Technology, Bandung 40132, Indonesia

autor

Zainal Muzakir

Geophysical Engineering Department, Universitas Syiah Kuala, Darussalam-Banda Aceh 23111, Indonesia

autor

Ghani Azman Abdul

Department of Geology, Faculty of Science, University of Malaya, 50603 Kuala Lumpur, Malaysia

autor

Saputra Deni

PT. Elnusa Tbk, Simatupang, Graha Elnusa, Jakarta Selatan 12560, Indonesia

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Typ dokumentu

Bibliografia

Identyfikator YADDA

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