Studi Kasus Penyebaran Panas Bumi Non Vulkanik Sekitar Sumber Air Panas Hantakan, Kalimantan Selatan

The measurement had been conducted about an identification of geothermal fluid in heated pool tourist territory Murung B village, Hantakan subdistrict, Hulu Sungai Tengah regency. This research aims to find out litolhogy soil/rock in the area around the hot water pool, knowing the value detainees so...

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Main Authors: Simon Sadok Siregar, Sri Cahyo Wahyono, Nurlina Nurlina
Format: Article
Language:English
Published: Lambung Mangkurat University Press 2017-03-01
Series:Jurnal Fisika Flux
Subjects:
Online Access:http://ppjp.unlam.ac.id/journal/index.php/f/article/view/3108
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spelling doaj-331f10e625cc409997d89b4fe8bd88ff2020-11-25T01:24:19ZengLambung Mangkurat University PressJurnal Fisika Flux1829-796X2541-17132017-03-018175842834Studi Kasus Penyebaran Panas Bumi Non Vulkanik Sekitar Sumber Air Panas Hantakan, Kalimantan SelatanSimon Sadok Siregar0Sri Cahyo Wahyono1Nurlina Nurlina2Staf Pengajar Program Studi Fisika FMIPA, Universitas Lambung Mangkurat, BanjarbaruStaf Pengajar Program Studi Fisika FMIPA, Universitas Lambung Mangkurat, BanjarbaruStaf Pengajar Program Studi Fisika FMIPA, Universitas Lambung Mangkurat, BanjarbaruThe measurement had been conducted about an identification of geothermal fluid in heated pool tourist territory Murung B village, Hantakan subdistrict, Hulu Sungai Tengah regency. This research aims to find out litolhogy soil/rock in the area around the hot water pool, knowing the value detainees soil type/rock containing geothermal fluid and determine the distribution methods of arrest. Electrode configuration used method Schlumberger (1D) and pole-pole (3D). Referring to the results of the processing of Progress program can be made two-dimensional crosssection to find out manually litolhogy coating model soil / rock which then correlated with ploting 3D models of Res3Dinv program. Geoelectric research results indicate that the geothermal fluid in the surrounding in heated pool tourist territory, Hantakan subdistrict, Hulu Sungai Tengah regency has a range of resistance values between 108 - 663.60 Ωm, in the depths of 14.67 - 90.2 m from the point G-3 - G-1. Geothermal fluid distribution direction at the research area is spread laterally from the point G-3 - G-1 where a layer of sand mixed with clay and granite rock fragments as an area of conductive layers and clay as cover.http://ppjp.unlam.ac.id/journal/index.php/f/article/view/3108heated pool, resistance, geothermal
collection DOAJ
language English
format Article
sources DOAJ
author Simon Sadok Siregar
Sri Cahyo Wahyono
Nurlina Nurlina
spellingShingle Simon Sadok Siregar
Sri Cahyo Wahyono
Nurlina Nurlina
Studi Kasus Penyebaran Panas Bumi Non Vulkanik Sekitar Sumber Air Panas Hantakan, Kalimantan Selatan
Jurnal Fisika Flux
heated pool, resistance, geothermal
author_facet Simon Sadok Siregar
Sri Cahyo Wahyono
Nurlina Nurlina
author_sort Simon Sadok Siregar
title Studi Kasus Penyebaran Panas Bumi Non Vulkanik Sekitar Sumber Air Panas Hantakan, Kalimantan Selatan
title_short Studi Kasus Penyebaran Panas Bumi Non Vulkanik Sekitar Sumber Air Panas Hantakan, Kalimantan Selatan
title_full Studi Kasus Penyebaran Panas Bumi Non Vulkanik Sekitar Sumber Air Panas Hantakan, Kalimantan Selatan
title_fullStr Studi Kasus Penyebaran Panas Bumi Non Vulkanik Sekitar Sumber Air Panas Hantakan, Kalimantan Selatan
title_full_unstemmed Studi Kasus Penyebaran Panas Bumi Non Vulkanik Sekitar Sumber Air Panas Hantakan, Kalimantan Selatan
title_sort studi kasus penyebaran panas bumi non vulkanik sekitar sumber air panas hantakan, kalimantan selatan
publisher Lambung Mangkurat University Press
series Jurnal Fisika Flux
issn 1829-796X
2541-1713
publishDate 2017-03-01
description The measurement had been conducted about an identification of geothermal fluid in heated pool tourist territory Murung B village, Hantakan subdistrict, Hulu Sungai Tengah regency. This research aims to find out litolhogy soil/rock in the area around the hot water pool, knowing the value detainees soil type/rock containing geothermal fluid and determine the distribution methods of arrest. Electrode configuration used method Schlumberger (1D) and pole-pole (3D). Referring to the results of the processing of Progress program can be made two-dimensional crosssection to find out manually litolhogy coating model soil / rock which then correlated with ploting 3D models of Res3Dinv program. Geoelectric research results indicate that the geothermal fluid in the surrounding in heated pool tourist territory, Hantakan subdistrict, Hulu Sungai Tengah regency has a range of resistance values between 108 - 663.60 Ωm, in the depths of 14.67 - 90.2 m from the point G-3 - G-1. Geothermal fluid distribution direction at the research area is spread laterally from the point G-3 - G-1 where a layer of sand mixed with clay and granite rock fragments as an area of conductive layers and clay as cover.
topic heated pool, resistance, geothermal
url http://ppjp.unlam.ac.id/journal/index.php/f/article/view/3108
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AT nurlinanurlina studikasuspenyebaranpanasbuminonvulkaniksekitarsumberairpanashantakankalimantanselatan
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