Mapping of rock resistivity value using geoelectrical method Schlumberger configuration in Solok Regency, West Sumatera
Mapping of rock resistivity value is useful for knowing the potential of the natural wealth contained in the earth. Investigation of resistivity value in Solok Regency is using 3 lines. The first line is at S 00055'0.7 "and E 100040'56.8" coordinates, the second line is located a...
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| Format: | Article |
| Language: | English |
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Universitas Sebelas Maret
2019-03-01
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| Series: | Journal of Physics: Theories and Applications |
| Subjects: | |
| Online Access: | https://jurnal.uns.ac.id/jphystheor-appl/article/view/38134 |
| _version_ | 1811237759391629312 |
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| author | Elsi Ariani Akmam Akmam |
| author_facet | Elsi Ariani Akmam Akmam |
| author_sort | Elsi Ariani |
| collection | DOAJ |
| description | Mapping of rock resistivity value is useful for knowing the potential of the natural wealth contained in the earth. Investigation of resistivity value in Solok Regency is using 3 lines. The first line is at S 00055'0.7 "and E 100040'56.8" coordinates, the second line is located at S 00054'53.2 "and E 100041'00.9" coordinates, and the third line is coordinated by S 00055'20.5 "and E 100041'01.8". The method of mapping is using the Geoelectric method with Schlumberger Configuration and the Ares (Apparent Resistivity) tool. The data obtained is processed by using Res2Dinv software to be analyzed and interpreted. The results obtained on the first line have resistivity value of 3.95-641 Ωm which is interpreted by having a rock structure consisting of Groundwater, Clay, Dry Clay, Basalt and Andesite. Next on the second line, the resistivity values of 2.53-1560.5 Ωm are obtained consisting of layers of rock Groundwater, Clay, Dry Clay, Basalt, and Andesite. Finally on the third line have resistivity value about 6.85-113.5 Ωm having a Groundwater, Tuff, Sandstone, Clay, Dry Clay, Basalt, Andesite, and Lava rock structure. The Tuff rock layer is estimated as a geothermal reservoir because its resistivity value is 20.8-23.6 Ωm surrounded by more contrasting rock layers and is located between two solid rock layers. |
| first_indexed | 2024-04-12T12:29:55Z |
| format | Article |
| id | doaj.art-914b7ec692784620b8fc84728d8856b8 |
| institution | Directory Open Access Journal |
| issn | 2549-7316 2549-7324 |
| language | English |
| last_indexed | 2024-04-12T12:29:55Z |
| publishDate | 2019-03-01 |
| publisher | Universitas Sebelas Maret |
| record_format | Article |
| series | Journal of Physics: Theories and Applications |
| spelling | doaj.art-914b7ec692784620b8fc84728d8856b82022-12-22T03:33:04ZengUniversitas Sebelas MaretJournal of Physics: Theories and Applications2549-73162549-73242019-03-0131273510.20961/jphystheor-appl.v3i1.3813425681Mapping of rock resistivity value using geoelectrical method Schlumberger configuration in Solok Regency, West SumateraElsi Ariani0Akmam Akmam1State Islamic University Sultan Maulana Hasanuddin BantenPadang State UniversityMapping of rock resistivity value is useful for knowing the potential of the natural wealth contained in the earth. Investigation of resistivity value in Solok Regency is using 3 lines. The first line is at S 00055'0.7 "and E 100040'56.8" coordinates, the second line is located at S 00054'53.2 "and E 100041'00.9" coordinates, and the third line is coordinated by S 00055'20.5 "and E 100041'01.8". The method of mapping is using the Geoelectric method with Schlumberger Configuration and the Ares (Apparent Resistivity) tool. The data obtained is processed by using Res2Dinv software to be analyzed and interpreted. The results obtained on the first line have resistivity value of 3.95-641 Ωm which is interpreted by having a rock structure consisting of Groundwater, Clay, Dry Clay, Basalt and Andesite. Next on the second line, the resistivity values of 2.53-1560.5 Ωm are obtained consisting of layers of rock Groundwater, Clay, Dry Clay, Basalt, and Andesite. Finally on the third line have resistivity value about 6.85-113.5 Ωm having a Groundwater, Tuff, Sandstone, Clay, Dry Clay, Basalt, Andesite, and Lava rock structure. The Tuff rock layer is estimated as a geothermal reservoir because its resistivity value is 20.8-23.6 Ωm surrounded by more contrasting rock layers and is located between two solid rock layers.https://jurnal.uns.ac.id/jphystheor-appl/article/view/38134resistivity, geoelectrical method, schlumberger configuration |
| spellingShingle | Elsi Ariani Akmam Akmam Mapping of rock resistivity value using geoelectrical method Schlumberger configuration in Solok Regency, West Sumatera Journal of Physics: Theories and Applications resistivity, geoelectrical method, schlumberger configuration |
| title | Mapping of rock resistivity value using geoelectrical method Schlumberger configuration in Solok Regency, West Sumatera |
| title_full | Mapping of rock resistivity value using geoelectrical method Schlumberger configuration in Solok Regency, West Sumatera |
| title_fullStr | Mapping of rock resistivity value using geoelectrical method Schlumberger configuration in Solok Regency, West Sumatera |
| title_full_unstemmed | Mapping of rock resistivity value using geoelectrical method Schlumberger configuration in Solok Regency, West Sumatera |
| title_short | Mapping of rock resistivity value using geoelectrical method Schlumberger configuration in Solok Regency, West Sumatera |
| title_sort | mapping of rock resistivity value using geoelectrical method schlumberger configuration in solok regency west sumatera |
| topic | resistivity, geoelectrical method, schlumberger configuration |
| url | https://jurnal.uns.ac.id/jphystheor-appl/article/view/38134 |
| work_keys_str_mv | AT elsiariani mappingofrockresistivityvalueusinggeoelectricalmethodschlumbergerconfigurationinsolokregencywestsumatera AT akmamakmam mappingofrockresistivityvalueusinggeoelectricalmethodschlumbergerconfigurationinsolokregencywestsumatera |