Geochemistry Exploration and Geothermometry Application in the North Zone of Seulawah Agam, Aceh Besar District, Indonesia

A geochemistry study has been done in four geothermal manifestations&#8212;<i>Ie-Seu&#8217;um</i>, <i>Ie-Br&#244;uk</i>, <i>Ie-Jue</i> and the Van-Heutz crater&#8212;located in the north zone of Seulawah Agam mountain (Aceh Besar District, Indonesi...

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Main Authors: Rinaldi Idroes, Muhammad Yusuf, Saiful Saiful, Muksin Alatas, Subhan Subhan, Andi Lala, Muslem Muslem, Rivansyah Suhendra, Ghazi Mauer Idroes, Marwan Marwan, Teuku Meurah Indra Mahlia
Format: Article
Language:English
Published: MDPI AG 2019-11-01
Series:Energies
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Online Access:https://www.mdpi.com/1996-1073/12/23/4442
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author Rinaldi Idroes
Muhammad Yusuf
Saiful Saiful
Muksin Alatas
Subhan Subhan
Andi Lala
Muslem Muslem
Rivansyah Suhendra
Ghazi Mauer Idroes
Marwan Marwan
Teuku Meurah Indra Mahlia
author_facet Rinaldi Idroes
Muhammad Yusuf
Saiful Saiful
Muksin Alatas
Subhan Subhan
Andi Lala
Muslem Muslem
Rivansyah Suhendra
Ghazi Mauer Idroes
Marwan Marwan
Teuku Meurah Indra Mahlia
author_sort Rinaldi Idroes
collection DOAJ
description A geochemistry study has been done in four geothermal manifestations&#8212;<i>Ie-Seu&#8217;um</i>, <i>Ie-Br&#244;uk</i>, <i>Ie-Jue</i> and the Van-Heutz crater&#8212;located in the north zone of Seulawah Agam mountain (Aceh Besar District, Indonesia). The study was performed through water and gas analysis. Water analysis were done for all geothermal manifestations, but gas analysis was only done for the <i>Ie-Jue</i> manifestation that has fumaroles. Cation and anion contents were analyzed by ion chromatography, ICP-OES, alkalimetry titrations, and spectrophotometry, meanwhile isotopes were measured by a Liquid Water Isotope Analyzer. The resulting data were used for fluid and gas geothermometry calculations, and plotted in a FT-CO<sub>2</sub> Cross-Plot and a CH<sub>4</sub>-CO<sub>2</sub>-H<sub>2</sub>S triangle diagram to obtain reservoir temperatures. The data were also plotted by a Cl-HCO<sub>3</sub>-SO<sub>4</sub> triangle and Piper diagram to obtain the water type and dominant chemical composition, a Na-K-Mg triangle diagram to obtain fluid equilibria, the isotope ratio in the stable isotope plot to obtain the origin of water, and a N<sub>2</sub>-He-Ar triangle diagram to establish the origin of fumaroles. The water analysis results showed that (1) <i>Ie-Seu&#8217;um</i> has an average reservoir temperature of 241.9 &#177; 0.3 &#176;C, a chloride water type, a dominant Na-K-Cl chemical composition, a mature water fluid equilibrium, and water of meteoric origin; (2) <i>Ie-Br&#244;uk</i> has an average reservoir temperature of 321.95 &#177; 13.4 &#176;C, a bicarbonate water type, a dominant Na-Ca-HCO<sub>3</sub>chemical composition, an immature water fluid equilibrium, and water of meteoric origin; (3) <i>Ie-Jue</i> has an average reservoir temperature of 472.4 &#177; 91.4 &#176;C, a sulphate water type, a dominant Ca-SO<sub>4</sub> chemical composition, an immature water fluid equilibrium and water of meteoric origin; and (4) the Van-Heutz crater has an average reservoir temperature of 439.3 &#177; 95.3 &#176;C, a sulphate water type, a dominant Ca-SO<sub>4</sub> chemical composition, an immature water fluid equilibrium and water of magmatic origin. The results of our gas analysis showed that <i>Ie-Jue</i> has an average reservoir temperature of 258.85 &#176;C, and water of meteoric origin. Based on the reservoir temperatures, the geothermal manifestation of the north zone of Seulawah Agam mountain is considered as a high-temperature geothermal system suitable for power plant development.
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spelling doaj.art-2f934e85a9c0402ca3af45731665a0812022-12-22T04:03:49ZengMDPI AGEnergies1996-10732019-11-011223444210.3390/en12234442en12234442Geochemistry Exploration and Geothermometry Application in the North Zone of Seulawah Agam, Aceh Besar District, IndonesiaRinaldi Idroes0Muhammad Yusuf1Saiful Saiful2Muksin Alatas3Subhan Subhan4Andi Lala5Muslem Muslem6Rivansyah Suhendra7Ghazi Mauer Idroes8Marwan Marwan9Teuku Meurah Indra Mahlia10Department of Chemistry, Faculty of Mathematics and Natural Sciences, Universitas Syiah Kuala, Banda Aceh 23111, IndonesiaDepartment of Chemistry, Faculty of Mathematics and Natural Sciences, Universitas Syiah Kuala, Banda Aceh 23111, IndonesiaDepartment of Chemistry, Faculty of Mathematics and Natural Sciences, Universitas Syiah Kuala, Banda Aceh 23111, IndonesiaDepartment of Chemistry, Faculty of Mathematics and Natural Sciences, Universitas Syiah Kuala, Banda Aceh 23111, IndonesiaDepartment of Chemistry, Faculty of Mathematics and Natural Sciences, Universitas Syiah Kuala, Banda Aceh 23111, IndonesiaDepartment of Chemistry, Faculty of Mathematics and Natural Sciences, Universitas Syiah Kuala, Banda Aceh 23111, IndonesiaDepartment of Chemistry, Faculty of Mathematics and Natural Sciences, Universitas Syiah Kuala, Banda Aceh 23111, IndonesiaDepartment of Informatics, Faculty of Mathematics and Natural Sciences, Universitas Syiah Kuala, Banda Aceh 23111, IndonesiaDepartment of Chemical Engineering, Faculty of Engineering, Universitas Syiah Kuala, Banda Aceh 23111, IndonesiaDepartment of Geophysic Engineering, Faculty of Engineering, Universitas Syiah Kuala, Banda Aceh 23111, IndonesiaSchool of Information, Systems and Modelling, University of Technology Sydney, Sydney, New South Wales 2007, AustraliaA geochemistry study has been done in four geothermal manifestations&#8212;<i>Ie-Seu&#8217;um</i>, <i>Ie-Br&#244;uk</i>, <i>Ie-Jue</i> and the Van-Heutz crater&#8212;located in the north zone of Seulawah Agam mountain (Aceh Besar District, Indonesia). The study was performed through water and gas analysis. Water analysis were done for all geothermal manifestations, but gas analysis was only done for the <i>Ie-Jue</i> manifestation that has fumaroles. Cation and anion contents were analyzed by ion chromatography, ICP-OES, alkalimetry titrations, and spectrophotometry, meanwhile isotopes were measured by a Liquid Water Isotope Analyzer. The resulting data were used for fluid and gas geothermometry calculations, and plotted in a FT-CO<sub>2</sub> Cross-Plot and a CH<sub>4</sub>-CO<sub>2</sub>-H<sub>2</sub>S triangle diagram to obtain reservoir temperatures. The data were also plotted by a Cl-HCO<sub>3</sub>-SO<sub>4</sub> triangle and Piper diagram to obtain the water type and dominant chemical composition, a Na-K-Mg triangle diagram to obtain fluid equilibria, the isotope ratio in the stable isotope plot to obtain the origin of water, and a N<sub>2</sub>-He-Ar triangle diagram to establish the origin of fumaroles. The water analysis results showed that (1) <i>Ie-Seu&#8217;um</i> has an average reservoir temperature of 241.9 &#177; 0.3 &#176;C, a chloride water type, a dominant Na-K-Cl chemical composition, a mature water fluid equilibrium, and water of meteoric origin; (2) <i>Ie-Br&#244;uk</i> has an average reservoir temperature of 321.95 &#177; 13.4 &#176;C, a bicarbonate water type, a dominant Na-Ca-HCO<sub>3</sub>chemical composition, an immature water fluid equilibrium, and water of meteoric origin; (3) <i>Ie-Jue</i> has an average reservoir temperature of 472.4 &#177; 91.4 &#176;C, a sulphate water type, a dominant Ca-SO<sub>4</sub> chemical composition, an immature water fluid equilibrium and water of meteoric origin; and (4) the Van-Heutz crater has an average reservoir temperature of 439.3 &#177; 95.3 &#176;C, a sulphate water type, a dominant Ca-SO<sub>4</sub> chemical composition, an immature water fluid equilibrium and water of magmatic origin. The results of our gas analysis showed that <i>Ie-Jue</i> has an average reservoir temperature of 258.85 &#176;C, and water of meteoric origin. Based on the reservoir temperatures, the geothermal manifestation of the north zone of Seulawah Agam mountain is considered as a high-temperature geothermal system suitable for power plant development.https://www.mdpi.com/1996-1073/12/23/4442hydro-geothermometrygas-geothermometryisotope analysisseulawah agam mountainindonesia
spellingShingle Rinaldi Idroes
Muhammad Yusuf
Saiful Saiful
Muksin Alatas
Subhan Subhan
Andi Lala
Muslem Muslem
Rivansyah Suhendra
Ghazi Mauer Idroes
Marwan Marwan
Teuku Meurah Indra Mahlia
Geochemistry Exploration and Geothermometry Application in the North Zone of Seulawah Agam, Aceh Besar District, Indonesia
Energies
hydro-geothermometry
gas-geothermometry
isotope analysis
seulawah agam mountain
indonesia
title Geochemistry Exploration and Geothermometry Application in the North Zone of Seulawah Agam, Aceh Besar District, Indonesia
title_full Geochemistry Exploration and Geothermometry Application in the North Zone of Seulawah Agam, Aceh Besar District, Indonesia
title_fullStr Geochemistry Exploration and Geothermometry Application in the North Zone of Seulawah Agam, Aceh Besar District, Indonesia
title_full_unstemmed Geochemistry Exploration and Geothermometry Application in the North Zone of Seulawah Agam, Aceh Besar District, Indonesia
title_short Geochemistry Exploration and Geothermometry Application in the North Zone of Seulawah Agam, Aceh Besar District, Indonesia
title_sort geochemistry exploration and geothermometry application in the north zone of seulawah agam aceh besar district indonesia
topic hydro-geothermometry
gas-geothermometry
isotope analysis
seulawah agam mountain
indonesia
url https://www.mdpi.com/1996-1073/12/23/4442
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