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SIMULASI HIDROTERMAL DAERAH KAWAH DOMAS DENGAN PEMODELAN KONTINU 2-D ANOMALI SELF POTENTIAL (SP)

Journal of Teaching and Learning Physics · Vol. 2 No. 1 (2017) · hlm. 10–16

DOI
10.15575/jotalp.v2i1.5818
ISSN
2580-3107, 2528-5505
Terbit
2017-02-27
Penerbit
UIN Sunan Gunung Djati Bandung
Bahasa
ind

Abstrak

Hydrothermal system research using Self Potential (SP) Method, 2-D DC Resistivity and surface temperature, has been done at Domas Crater (1700 masl). Potential anomaly which is associated with subsurface structure is obtained by SP measurement, whereas temperature measurement is done to get information about surface temperature distribution laterally and resistivity distribution of volcano structures is known by 2-D DC Resistivity measurement. Hydrothermal activities, which cause the existence of SP value, are modeled using this scheme modeling. This schema modeling is validated by comparing the value of SP model with field measurement. The shallow hydrothermal activities at Domas Crater are influenced by meteoric and subsurface water. The velocity of hydrothermal activities are about 10-9 - 10-7 m/s. 16.64% root mean square error is obtained by Comsol modeling, whereas 6.54% root mean square error is obtained by modeling using finite element method.

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13 penulis · 27 tautan kepenulisan bersama · 3 lintas organisasi

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  • Sunan Gunung Djati State Islamic University Bandung
  • Bandung Institute of Technology
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Rekan penulisOrganisasiArtikel bersama
Riki Purnama PutraBandung Institute of Technology4
Yudi DirgantaraSunan Gunung Djati State Islamic University Bandung1
Ivana Sylvi IndrawanSunan Gunung Djati State Islamic University Bandung1
Sri PrihatiniAfiliasi tidak diketahui1
Wahyuni HandayaniAfiliasi tidak diketahui1
Dedi KuntadiAfiliasi tidak diketahui1
Muhammad Ripki RinaldiAfiliasi tidak diketahui1
Ade Yeti NuryantiniAfiliasi tidak diketahui1
Pina PitrianaAfiliasi tidak diketahui1
Seni SusantiAfiliasi tidak diketahui1
Agustinus Bambang SetyadjiAfiliasi tidak diketahui1
Riantini VirtrianaAfiliasi tidak diketahui1

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Sumber metadata: OAI-PMH (metadata jurnal) https://journal.uinsgd.ac.id/index.php/jtlp/oai, pertama di-harvest 7 Nov 2026, terakhir terlihat 8 Nov 2026.
Metadata asli (oai_dc) 
<oai_dc:dc xmlns="http://www.openarchives.org/OAI/2.0/" xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/  http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
	<dc:title xml:lang="en-US">SIMULASI HIDROTERMAL DAERAH KAWAH DOMAS DENGAN PEMODELAN KONTINU 2-D ANOMALI SELF POTENTIAL (SP)</dc:title>
	<dc:creator>Agustina, Rena Denya</dc:creator>
	<dc:subject xml:lang="en-US">hydrothermal</dc:subject>
	<dc:subject xml:lang="en-US">self potential</dc:subject>
	<dc:subject xml:lang="en-US">resistivity</dc:subject>
	<dc:subject xml:lang="en-US">continue modeling</dc:subject>
	<dc:subject xml:lang="en-US">finite element method</dc:subject>
	<dc:subject xml:lang="en-US">Physics</dc:subject>
	<dc:description xml:lang="en-US">Hydrothermal system research using Self Potential (SP) Method, 2-D DC Resistivity and surface temperature, has been done at Domas Crater (1700 masl). Potential anomaly which is associated with subsurface structure is obtained by SP measurement, whereas temperature measurement is done to get information about surface temperature distribution laterally and resistivity distribution of volcano structures is known by 2-D DC Resistivity measurement. Hydrothermal activities, which cause the existence of SP value, are modeled using this scheme modeling. This schema modeling is validated by comparing the value of SP model with field measurement. The shallow hydrothermal activities at Domas Crater are influenced by meteoric and subsurface water. The velocity of hydrothermal activities are about 10-9 - 10-7 m/s. 16.64% root mean square error is obtained by Comsol modeling, whereas 6.54% root mean square error is obtained by modeling using finite element method.</dc:description>
	<dc:publisher xml:lang="en-US">UIN Sunan Gunung Djati Bandung</dc:publisher>
	<dc:date>2017-02-27</dc:date>
	<dc:type>info:eu-repo/semantics/article</dc:type>
	<dc:type>info:eu-repo/semantics/publishedVersion</dc:type>
	<dc:format>application/pdf</dc:format>
	<dc:identifier>https://journal.uinsgd.ac.id/index.php/jtlp/article/view/5818</dc:identifier>
	<dc:identifier>10.15575/jotalp.v2i1.5818</dc:identifier>
	<dc:source xml:lang="en-US">Journal of Teaching and Learning Physics; Vol. 2 No. 1 (2017): Journal of Teaching and Learning Physics (Februari 2017); 10-16</dc:source>
	<dc:source>2580-3107</dc:source>
	<dc:source>2528-5505</dc:source>
	<dc:language>ind</dc:language>
	<dc:relation>https://journal.uinsgd.ac.id/index.php/jtlp/article/view/5818/3322</dc:relation>
</oai_dc:dc>