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Sosialisasi Metode Geolistrik Untuk Eksplorasi Air Tanah Bagi Siswa SMK Negeri 9 Energi dan Pertambangan Jayapura

JURNAL PENGABDIAN PAPUA · Vol. 9 No. 2 (2025) · pp. 114–120

DOI
10.31957/jpp.v9i2.3776
ISSN
2579-9592, 2550-0082
Published
2025-07-07
Publisher
LPPM Uncen
Language
eng
License
creativecommons.org/licenses/by-nc-sa/4.0

Abstract

The purpose of the activity is to provide experience and train participants to understand geoelectric theory, data collection and processing and analysis packaged in the form of reports, and specifically to obtain real input for curriculum development in universities to be more relevant to development needs. Based on the problems experienced by students of SMK Negeri 9 Energy and Mining Jayapura, a service activity was carried out that intends to explain geophysical methods related to groundwater utilization for agriculture. Students will receive material with a ratio of 50% theory and 50% practice. Through this activity, participants will better understand the concepts in searching for groundwater and be able to develop skills, especially in the development of geophysical tools and be able to interpret the measurement results and resistivity values accurately, measurably and integrated. The results of geoelectric data processing of VES 1-3 points show that VES.1 has a relatively larger specific resistance value when compared to the two measurement points VES.2 and VES.3. This difference is due to the structure of VES.1 in the form of hard rock part of the Ultramafic formation which is composed of rock types such as marl, fine sandstone, tuff, and tuff. The results of geoelectric data processing from the four measurement points show that the measurement points VES. 4, VES. 6 and VES. 7 have relatively low specific gravity values, in contrast to the relatively high value of VES. 5 which is relatively high. The difference in specific gravity values is very influential on the presence of aquifers at each measuring point. Based on the distribution of specific gravity values, the vertical lithology of the four measuring points is arranged by rock types, namely surface rocks, breccias, tuffs, clay stones, and siltstones.

Collaboration network of the authors

40 authors · 94 co-authorship links · showing the 40 most connected

Hover or tap a name to highlight its co-authors. Double-click to open the author's page.

  • Cenderawasih University
  • Affiliation unknown
  • Different organisations
  • Same organisation
  • Affiliation unknown
  • Thicker line = more joint articles · bigger circle = more articles
Show as table
Co-authorOrganisationJoint articles
Albert LumbuCenderawasih University7
Triwiyono TriwiyonoCenderawasih University5
Bonefasius Yanwar BoyCenderawasih University4
Muhammad AkbarCenderawasih University3
Johnson SiallaganCenderawasih University2
Catur Fathonah DjarwoCenderawasih University2
Agnes AryesamCenderawasih University2
Meylani Aljeinie TijowCenderawasih University2
Nofriana TajoCenderawasih University2
Basa T. RumahorboCenderawasih University1
Indah SetyowatiAffiliation unknown1
Novita MedyatiCenderawasih University1
Tanta TantaCenderawasih University1
Dolfina Costansah KoirewoaCenderawasih University1
Diana SetyaningsihCenderawasih University1
Erna OluaCenderawasih University1
Siti R. AyubCenderawasih University1
Yalince YikwaCenderawasih University1
Maklon WarpurCenderawasih University1
Roy SalindingCenderawasih University1
Janviter ManaluCenderawasih University1
Yulius MataputunCenderawasih University1
Leni Tri YulianingsihCenderawasih University1
Eva FebyantiCenderawasih University1
Ferdinanda RumbinoCenderawasih University1
Hana SuryanaCenderawasih University1
Mega FatmawatiCenderawasih University1
sunardi sunardiCenderawasih University1
. FitriAffiliation unknown1
Eka Suci LestariCenderawasih University1
Ebriani AntonCenderawasih University1
Trieana S TuhusulaCenderawasih University1
Siti Marwah SyukurCenderawasih University1
Siti HajarCenderawasih University1
Adeline SilabanCenderawasih University1

Affiliations come from OpenAlex; journal OAI-PMH metadata carries none. Authors without an OpenAlex ID are matched by name, which can merge or split people.

Metadata source: OAI-PMH (metadata jurnal) https://ejournal.uncen.ac.id/index.php/JP/oai, first harvested 1 Nov 2026, last seen 8 Nov 2026.
Original metadata (oai_dc)
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	<dc:title xml:lang="en-US">Sosialisasi Metode Geolistrik Untuk Eksplorasi Air Tanah Bagi Siswa SMK Negeri 9 Energi dan Pertambangan Jayapura </dc:title>
	<dc:creator>Panda, Florentina M.</dc:creator>
	<dc:creator>Lasmono, Paulus G.  D.</dc:creator>
	<dc:creator>Walukow, Auldry F.</dc:creator>
	<dc:creator>Virman</dc:creator>
	<dc:creator>Inghondem, Yosfince</dc:creator>
	<dc:description xml:lang="en-US">The purpose of the activity is to provide experience and train participants to understand geoelectric theory, data collection and processing and analysis packaged in the form of reports, and specifically to obtain real input for curriculum development in universities to be more relevant to development needs. Based on the problems experienced by students of SMK Negeri 9 Energy and Mining Jayapura, a service activity was carried out that intends to explain geophysical methods related to groundwater utilization for agriculture. Students will receive material with a ratio of 50% theory and 50% practice. Through this activity, participants will better understand the concepts in searching for groundwater and be able to develop skills, especially in the development of geophysical tools and be able to interpret the measurement results and resistivity values accurately, measurably and integrated. The results of geoelectric data processing of VES 1-3 points show that VES.1 has a relatively larger specific resistance value when compared to the two measurement points VES.2 and VES.3. This difference is due to the structure of VES.1 in the form of hard rock part of the Ultramafic formation which is composed of rock types such as marl, fine sandstone, tuff, and tuff. The results of geoelectric data processing from the four measurement points show that the measurement points VES. 4, VES. 6 and VES. 7 have relatively low specific gravity values, in contrast to the relatively high value of VES. 5 which is relatively high. The difference in specific gravity values is very influential on the presence of aquifers at each measuring point. Based on the distribution of specific gravity values, the vertical lithology of the four measuring points is arranged by rock types, namely surface rocks, breccias, tuffs, clay stones, and siltstones. </dc:description>
	<dc:publisher xml:lang="en-US">LPPM Uncen</dc:publisher>
	<dc:date>2025-07-07</dc:date>
	<dc:type>info:eu-repo/semantics/article</dc:type>
	<dc:type>info:eu-repo/semantics/publishedVersion</dc:type>
	<dc:type xml:lang="en-US">Peer-reviewed Article</dc:type>
	<dc:format>application/pdf</dc:format>
	<dc:identifier>https://ejournal.uncen.ac.id/index.php/JP/article/view/3776</dc:identifier>
	<dc:identifier>10.31957/jpp.v9i2.3776</dc:identifier>
	<dc:source xml:lang="en-US">JURNAL PENGABDIAN PAPUA; Vol. 9 No. 2 (2025); 114-120</dc:source>
	<dc:source xml:lang="id-ID">JURNAL PENGABDIAN PAPUA; Vol 9 No 2 (2025); 114-120</dc:source>
	<dc:source>2579-9592</dc:source>
	<dc:source>2550-0082</dc:source>
	<dc:language>eng</dc:language>
	<dc:relation>https://ejournal.uncen.ac.id/index.php/JP/article/view/3776/3257</dc:relation>
	<dc:rights xml:lang="en-US">https://creativecommons.org/licenses/by-nc-sa/4.0</dc:rights>
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