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	<title>APLIKASI METODE GEOLISTRIK RESISTIVITAS UNTUK ANALISIS BIDANG GELINCIR DAN STUDI KARAKTERISTIK LONGSORAN DI JALAN RAYA SUBAN BANDAR LAMPUNG | Mulyasari | Jurnal Geofisika Eksplorasi</title>
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			<meta name="keywords" content="slip surface; landslide; resistivity" />
	
	
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	<meta name="DC.Contributor.Sponsor" xml:lang="en" content=""/>
	<meta name="DC.Creator.PersonalName" content="Rahmi Mulyasari"/>
	<meta name="DC.Creator.PersonalName" content="IG Boy Darmawan"/>
	<meta name="DC.Creator.PersonalName" content="Dersan Surya Effendi"/>
	<meta name="DC.Creator.PersonalName" content="Sugeng Purwo Saputro"/>
	<meta name="DC.Creator.PersonalName" content="Hesti Hesti"/>
	<meta name="DC.Creator.PersonalName" content="Akroma Hidayatika"/>
	<meta name="DC.Creator.PersonalName" content="Nandi Haerudin"/>
	<meta name="DC.Date.created" scheme="ISO8601" content="2020-03-18"/>
	<meta name="DC.Date.dateSubmitted" scheme="ISO8601" content="2020-02-06"/>
	<meta name="DC.Date.issued" scheme="ISO8601" content="2020-03-18"/>
	<meta name="DC.Date.modified" scheme="ISO8601" content="2020-03-18"/>
	<meta name="DC.Description" xml:lang="en" content=" 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. "/>
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	<meta name="DC.Identifier" content="61"/>
	<meta name="DC.Identifier.pageNumber" content="66-76"/>
							<meta name="DC.Identifier.DOI" content="10.23960/jge.v6i1.61"/>
		<meta name="DC.Identifier.URI" content="https://jge.eng.unila.ac.id/index.php/geoph/article/view/61"/>
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	<meta name="DC.Source" content="Jurnal Geofisika Eksplorasi"/>
	<meta name="DC.Source.ISSN" content="2685-6182"/>
	<meta name="DC.Source.Issue" content="1"/>	<meta name="DC.Source.URI" content="https://jge.eng.unila.ac.id/index.php/geoph"/>
	<meta name="DC.Source.Volume" content="6"/>						<meta name="DC.Subject" xml:lang="en" content="slip surface"/>
								<meta name="DC.Subject" xml:lang="en" content="landslide"/>
								<meta name="DC.Subject" xml:lang="en" content="resistivity"/>
				<meta name="DC.Title" content="APLIKASI METODE GEOLISTRIK RESISTIVITAS UNTUK ANALISIS BIDANG GELINCIR DAN STUDI KARAKTERISTIK LONGSORAN DI JALAN RAYA SUBAN BANDAR LAMPUNG"/>
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	<meta name="citation_journal_title" content="Jurnal Geofisika Eksplorasi"/>
	<meta name="citation_issn" content="2685-6182"/>
        <meta name="citation_author" content="Rahmi Mulyasari"/>
        <meta name="citation_author_institution" content="Jurusan T. Geofisika, Universitas Lampung"/>
        <meta name="citation_author" content="IG Boy Darmawan"/>
        <meta name="citation_author_institution" content="Jurusan T. Geofisika, Universitas Lampung"/>
        <meta name="citation_author" content="Dersan Surya Effendi"/>
        <meta name="citation_author_institution" content="Jurusan T. Geofisika, Universitas Lampung"/>
        <meta name="citation_author" content="Sugeng Purwo Saputro"/>
        <meta name="citation_author_institution" content="LIPI Kebumen"/>
        <meta name="citation_author" content="Hesti Hesti"/>
        <meta name="citation_author_institution" content="Jurusan T. Geofisika, Universitas Lampung"/>
        <meta name="citation_author" content="Akroma Hidayatika"/>
        <meta name="citation_author_institution" content="Jurusan T. Geofisika, Universitas Lampung"/>
        <meta name="citation_author" content="Nandi Haerudin"/>
        <meta name="citation_author_institution" content="Jurusan T. Geofisika, Universitas Lampung"/>
<meta name="citation_title" content="APLIKASI METODE GEOLISTRIK RESISTIVITAS UNTUK ANALISIS BIDANG GELINCIR DAN STUDI KARAKTERISTIK LONGSORAN DI JALAN RAYA SUBAN BANDAR LAMPUNG"/>

				<meta name="citation_date" content="2020/03/18"/>
	
	<meta name="citation_volume" content="6"/>
	<meta name="citation_issue" content="1"/>

			<meta name="citation_firstpage" content="66"/>
				<meta name="citation_lastpage" content="76"/>
								<meta name="citation_doi" content="10.23960/jge.v6i1.61"/>
		<meta name="citation_abstract_html_url" content="https://jge.eng.unila.ac.id/index.php/geoph/article/view/61"/>
	<meta name="citation_language" content="en"/>
						<meta name="citation_keywords" xml:lang="en" content="slip surface"/>
								<meta name="citation_keywords" xml:lang="en" content="landslide"/>
								<meta name="citation_keywords" xml:lang="en" content="resistivity"/>
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		<em>Rahmi Mulyasari</em>
								<br />Jurusan T. Geofisika, Universitas Lampung		<br />Indonesia	</p>

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		<em>IG Boy Darmawan</em>
								<br />Jurusan T. Geofisika, Universitas Lampung		<br />Indonesia	</p>

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		<em>Dersan Surya Effendi</em>
								<br />Jurusan T. Geofisika, Universitas Lampung		<br />Indonesia	</p>

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		<em>Sugeng Purwo Saputro</em>
								<br />LIPI Kebumen		<br />Indonesia	</p>

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		<em>Hesti Hesti</em>
								<br />Jurusan T. Geofisika, Universitas Lampung		<br />Indonesia	</p>

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		<em>Akroma Hidayatika</em>
								<br />Jurusan T. Geofisika, Universitas Lampung		<br />Indonesia	</p>

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		<em>Nandi Haerudin</em>
								<br />Jurusan T. Geofisika, Universitas Lampung		<br />Indonesia	</p>

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	<a href="https://jge.eng.unila.ac.id/index.php/geoph/issue/view/7" target="_parent">Vol 6, No 1 (2020)</a> &gt;	<a href="https://jge.eng.unila.ac.id/index.php/geoph/article/view/61/0" class="current" target="_parent">Mulyasari</a>
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	<div id="articleTitle"><h3>APLIKASI METODE GEOLISTRIK RESISTIVITAS UNTUK ANALISIS BIDANG GELINCIR DAN STUDI KARAKTERISTIK LONGSORAN DI JALAN RAYA SUBAN BANDAR LAMPUNG</h3></div>
	<div id="authorString"><em>Rahmi Mulyasari, IG Boy Darmawan, Dersan Surya Effendi, Sugeng Purwo Saputro, Hesti Hesti, Akroma Hidayatika, Nandi Haerudin</em></div>
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		<h4>Abstract</h4>
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		<div><p>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.</p></div>
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		<h4>Keywords</h4>
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		<div>slip surface; landslide; resistivity</div>
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		<h4>References</h4>
		<br />
		<div>
							<p>Bukhari, Saputra, A. D., Pratama, A. H., Abdullah, F., Yanis, M. dan Ismail, N., 2017, Identifikasi struktur berpotensi longsor berdasarkan model resistivitas listrik 2D, Prosiding Semirata 2017 Bidang MIPA BKS-PTN Wilayah Barat, ISBN: 978-602-50593-0-8, 942-953.</p>
							<p>Harian Lampung, 2019, Babinsa Koramil 0410-01 Panjang Bersama Masyarakat Gotong Royong Bersihkan Banjir dan Longsor, http://www.harianlampung.com/index.php?k=Politik&amp;i=49735, diakses tanggal 20 November 2019.</p>
							<p>Karnawati, D., 2005, Gerakan Massa Tanah di Indonesia dan Upaya Penanggulangannya, Jurusan Teknik Geologi Fakultas Teknik Universitas Gadjah Mada, Yogyakarta.</p>
							<p>Mulyasari, R., Utama, H.W., dan Haerudin, N., 2019, Geomorphology study on the Bandar Lampung Capital City for recommendation of development area, IOP Conf. Series: Earth and Environmental Science 279 (2019) 012026.</p>
							<p>Paimin, Sukresno dan Pramono. I. P., 2009, Teknik Mitigasi Banjir dan Tanah Longsor, Tropenbos International Indonesia Programme, Balikpapan.</p>
							<p>Pusat Vulkanologi dan Mitigasi Bencana Geologi (PVMBG), 2019, Wilayah Potensi Gerakan Tanah di Lampung, http://www.vsi.esdm.go.id/, diakses tanggal 17 Oktober 2019.</p>
							<p>Sugito, Irayani, Z. dan Jati, I.P., 2010, Investigasi bidang gelincir tanah longsor menggunakan metode geolistrik tahanan jenis di Desa Kebarongan Kec. Kemranjen Kab. Banyumas, Berkala Fisika, ISSN: 1410 – 9662, Vol 13, Ed. 2.</p>
							<p>Telford, W. M, Geldard, L.P, Sherrif, R.E., dan Keys, D. A., 1990, Applied Geophysics, Cambridge University Press, London.</p>
							<p>Utiya, J., As’ari dan Tongkukut, HJ., 2015, Metode geolistrik resistivitas konfigurasi Wenner-Schlumberger dan konfigurasi Dipole-Dipole untuk Identifikasi patahan Manado di Kecamatan Paaldua Kota Manado, Jurnal Ilmiah Sains, Vol 15, No 2</p>
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		DOI: <a id="pub-id::doi" href="https://doi.org/10.23960/jge.v6i1.61">https://doi.org/10.23960/jge.v6i1.61</a>																				

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