Mulyasari, Rahmi and Darmawan, I Gede Boy and Efendi, Dersan Surya and Hesti, Hesti and Hidayatika, Akroma and Nandi Haerudin, NH IDENTIFICATION OF SLIP SURFACE USING 2D RESISTIVITY METHOD, CASE STUDY IN PIDADA, BANDAR LAMPUNG. In: SIMTEK 2019, 12-13 Nov 2019, Bandar Lampung, Indonesia. (Submitted)

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Landslide is a disaster that occurs influenced by morphology, lithology, geological structure, hydrogeology and land use factors. Pidada Urban Village, Panjang District, Bandar Lampung is an area with morphological conditions in the form of hills with steep slopes. Based on data from the Center for Volcanology and Disaster Mitigation (PVMBG) in January-October 2019, the research area in Panjang District has the potential for medium-high mass movement. Criteria for the occurrence of landslides are steep slopes, the presence of slip surface below the surface of water saturated soil and the amount of water content that comes from rain water that seeps into the ground. One of the geophysical methods that can detect skid fields is the 2D Resistivity Method of Wenner-Schlumberger Configuration. Through this method it is known that areas that have high water content are indicated by low resistivity values. In this study, measurements were carried out on the slip area in a landslide prone area. After measuring the 2 lines, depth of the slip area of the study area was obtained.

Item Type: Conference or Workshop Item (Speech)
Subjects: Q Science > QE Geology
Divisions: Fakultas Teknik (FT) > Prodi Teknik Geofisika
Depositing User: Rahmi Mulyasari
Date Deposited: 14 Nov 2019 10:57
Last Modified: 14 Nov 2019 10:57

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