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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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 |
work_keys_str_mv |
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