APLIKASI METODE GEOLISTRIK RESISTIVITAS UNTUK ANALISIS BIDANG GELINCIR DAN STUDI KARAKTERISTIK LONGSORAN DI JALAN RAYA SUBAN BANDAR LAMPUNG
Pidada Urban Village, Panjang District, Bandar Lampung is an area that has medium to high landslide potential. One of landslides prone area triggered by rain located on Jalan Raya Suban. The slip surface areas under water-saturated soil is one of causes of landslides triggered by rain. Geophysical m...
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| Format: | Article |
| Language: | English |
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Jurusan Teknik Geofisika Fakultas Teknik Universitas Lampung
2020-03-01
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| Series: | JGE |
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| Online Access: | https://jge.eng.unila.ac.id/index.php/geoph/article/view/61 |
| _version_ | 1819073193564962816 |
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| author | Rahmi Mulyasari IG Boy Darmawan Dersan Surya Effendi Sugeng Purwo Saputro Hesti Hesti Akroma Hidayatika Nandi Haerudin |
| author_facet | Rahmi Mulyasari IG Boy Darmawan Dersan Surya Effendi Sugeng Purwo Saputro Hesti Hesti Akroma Hidayatika Nandi Haerudin |
| author_sort | Rahmi Mulyasari |
| collection | DOAJ |
| description | Pidada Urban Village, Panjang District, Bandar Lampung is an area that has medium to high landslide potential. One of landslides prone area triggered by rain located on Jalan Raya Suban. The slip surface areas under water-saturated soil is one of causes of landslides triggered by rain. Geophysical method used to detect slip surface is 2D Resistivity Method of Wenner-Schlumberger Configuration. In this study, an analysis of the slip surface has been carried out with the 2D resistivity method of the Wenner-Schlumberger Configuration and determination characteristic of landslide on Jalan Raya Suban. Based on the results of study indicated that the subsurface lithology consists of layers of tuff sediment, sandy clay and breccia. The slip surface is estimated at the boundary the layers of tuff sediment layer and sandy clay with depth (5-15) meters from the ground surface. The results of analysis and observation showed that type of landslide is translational fine-grained soil. Types of slope reinforcement that can be applied are civil and vegetative techniques. |
| first_indexed | 2024-12-21T17:49:44Z |
| format | Article |
| id | doaj.art-5314c910d6b94963b8ce54a2d3d11d61 |
| institution | Directory Open Access Journal |
| issn | 2356-1599 2685-6182 |
| language | English |
| last_indexed | 2024-12-21T17:49:44Z |
| publishDate | 2020-03-01 |
| publisher | Jurusan Teknik Geofisika Fakultas Teknik Universitas Lampung |
| record_format | Article |
| series | JGE |
| spelling | doaj.art-5314c910d6b94963b8ce54a2d3d11d612022-12-21T18:55:23ZengJurusan Teknik Geofisika Fakultas Teknik Universitas LampungJGE2356-15992685-61822020-03-0161667610.23960/jge.v6i1.6161APLIKASI METODE GEOLISTRIK RESISTIVITAS UNTUK ANALISIS BIDANG GELINCIR DAN STUDI KARAKTERISTIK LONGSORAN DI JALAN RAYA SUBAN BANDAR LAMPUNGRahmi Mulyasari0IG Boy Darmawan1Dersan Surya Effendi2Sugeng Purwo Saputro3Hesti Hesti4Akroma Hidayatika5Nandi Haerudin6Jurusan T. Geofisika, Universitas LampungJurusan T. Geofisika, Universitas LampungJurusan T. Geofisika, Universitas LampungLIPI KebumenJurusan T. Geofisika, Universitas LampungJurusan T. Geofisika, Universitas LampungJurusan T. Geofisika, Universitas LampungPidada Urban Village, Panjang District, Bandar Lampung is an area that has medium to high landslide potential. One of landslides prone area triggered by rain located on Jalan Raya Suban. The slip surface areas under water-saturated soil is one of causes of landslides triggered by rain. Geophysical method used to detect slip surface is 2D Resistivity Method of Wenner-Schlumberger Configuration. In this study, an analysis of the slip surface has been carried out with the 2D resistivity method of the Wenner-Schlumberger Configuration and determination characteristic of landslide on Jalan Raya Suban. Based on the results of study indicated that the subsurface lithology consists of layers of tuff sediment, sandy clay and breccia. The slip surface is estimated at the boundary the layers of tuff sediment layer and sandy clay with depth (5-15) meters from the ground surface. The results of analysis and observation showed that type of landslide is translational fine-grained soil. Types of slope reinforcement that can be applied are civil and vegetative techniques.https://jge.eng.unila.ac.id/index.php/geoph/article/view/61slip surfacelandslideresistivity |
| spellingShingle | Rahmi Mulyasari IG Boy Darmawan Dersan Surya Effendi Sugeng Purwo Saputro Hesti Hesti Akroma Hidayatika Nandi Haerudin APLIKASI METODE GEOLISTRIK RESISTIVITAS UNTUK ANALISIS BIDANG GELINCIR DAN STUDI KARAKTERISTIK LONGSORAN DI JALAN RAYA SUBAN BANDAR LAMPUNG JGE slip surface landslide resistivity |
| title | APLIKASI METODE GEOLISTRIK RESISTIVITAS UNTUK ANALISIS BIDANG GELINCIR DAN STUDI KARAKTERISTIK LONGSORAN DI JALAN RAYA SUBAN BANDAR LAMPUNG |
| title_full | APLIKASI METODE GEOLISTRIK RESISTIVITAS UNTUK ANALISIS BIDANG GELINCIR DAN STUDI KARAKTERISTIK LONGSORAN DI JALAN RAYA SUBAN BANDAR LAMPUNG |
| title_fullStr | APLIKASI METODE GEOLISTRIK RESISTIVITAS UNTUK ANALISIS BIDANG GELINCIR DAN STUDI KARAKTERISTIK LONGSORAN DI JALAN RAYA SUBAN BANDAR LAMPUNG |
| title_full_unstemmed | APLIKASI METODE GEOLISTRIK RESISTIVITAS UNTUK ANALISIS BIDANG GELINCIR DAN STUDI KARAKTERISTIK LONGSORAN DI JALAN RAYA SUBAN BANDAR LAMPUNG |
| title_short | APLIKASI METODE GEOLISTRIK RESISTIVITAS UNTUK ANALISIS BIDANG GELINCIR DAN STUDI KARAKTERISTIK LONGSORAN DI JALAN RAYA SUBAN BANDAR LAMPUNG |
| title_sort | aplikasi metode geolistrik resistivitas untuk analisis bidang gelincir dan studi karakteristik longsoran di jalan raya suban bandar lampung |
| topic | slip surface landslide resistivity |
| url | https://jge.eng.unila.ac.id/index.php/geoph/article/view/61 |
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