Identifying the subsurface layer structure and the temperature distribution of geothermal areas in Mantikole village

Main Authors: Suryadi, Yantri, Efendi, Rustan, Sandra, Sandra
Format: Article info application/pdf eJournal
Bahasa: eng
Terbitan: Gravitasi , 2015
Online Access: http://jurnal.untad.ac.id/jurnal/index.php/GravitasiFisika/article/view/4433
http://jurnal.untad.ac.id/jurnal/index.php/GravitasiFisika/article/view/4433/3305
ctrlnum article-4433
fullrecord <?xml version="1.0"?> <dc schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd"><title lang="en-US">Identifying the subsurface layer structure and the temperature distribution of geothermal areas in Mantikole village</title><creator>Suryadi, Yantri</creator><creator>Efendi, Rustan</creator><creator>Sandra, Sandra</creator><description lang="en-US">Research on identifying the subsurface layer structure and the temperaturedistribution of geothermal areas in Mantikolevillage. Dolodistrict, Sigiregency has been conducted. Measurements were performed on3 tracks around geothermal sources by using the geoelectric resistivity of wenner configuration that was subsequently processed using EarthImager2D software. Based on the results of dataprocessing, the subsurface layer structures in study area were surface water, clay, and igneous rock of granite with resistivity values ranging between 75 &#x3A9;m-1585 &#x3A9;m.Subsequently, the obtainedresistivity values were converted to a temperature distribution using anequation that is derived from Archie formula and further modelled usingRockwork software. Considering this temperature distribution, it is known that the temperature values ranged between 38oC-57oC with the highest temperature at the second track. Keywords: Geolistrik resistivity, geothermal, temperature distribution.</description><publisher lang="en-US">Gravitasi</publisher><contributor lang="en-US"/><date>2015-06-30</date><type>Journal:Article</type><type>Other:info:eu-repo/semantics/publishedVersion</type><type>Journal:Article</type><type>File:application/pdf</type><identifier>http://jurnal.untad.ac.id/jurnal/index.php/GravitasiFisika/article/view/4433</identifier><source lang="en-US">Gravitasi; Vol 14, No 1 (2015)</source><language>eng</language><relation>http://jurnal.untad.ac.id/jurnal/index.php/GravitasiFisika/article/view/4433/3305</relation><recordID>article-4433</recordID></dc>
language eng
format Journal:Article
Journal
Other:info:eu-repo/semantics/publishedVersion
Other
File:application/pdf
File
Journal:eJournal
author Suryadi, Yantri
Efendi, Rustan
Sandra, Sandra
title Identifying the subsurface layer structure and the temperature distribution of geothermal areas in Mantikole village
publisher Gravitasi
publishDate 2015
url http://jurnal.untad.ac.id/jurnal/index.php/GravitasiFisika/article/view/4433
http://jurnal.untad.ac.id/jurnal/index.php/GravitasiFisika/article/view/4433/3305
contents Research on identifying the subsurface layer structure and the temperaturedistribution of geothermal areas in Mantikolevillage. Dolodistrict, Sigiregency has been conducted. Measurements were performed on3 tracks around geothermal sources by using the geoelectric resistivity of wenner configuration that was subsequently processed using EarthImager2D software. Based on the results of dataprocessing, the subsurface layer structures in study area were surface water, clay, and igneous rock of granite with resistivity values ranging between 75 Ωm-1585 Ωm.Subsequently, the obtainedresistivity values were converted to a temperature distribution using anequation that is derived from Archie formula and further modelled usingRockwork software. Considering this temperature distribution, it is known that the temperature values ranged between 38oC-57oC with the highest temperature at the second track. Keywords: Geolistrik resistivity, geothermal, temperature distribution.
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institution Universitas Tadulako
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repoId IOS1036
first_indexed 2016-09-16T19:02:31Z
last_indexed 2016-09-22T21:32:30Z
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