Identification of Landfill Using Refraction Seismic Method in LIPI Area - Bandung

Research has been carried out using seismic refraction in the LIPI area - Bandung, which aims to determine the land of embankment in the area. Retrieval of field data was carried out using geometric  Es-3000 tool along 46 meters with a spacing of 2 meters and a 7 shoot punch consisting of 2 phantom...

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Main Authors: Resi Wasilatus Syifa, Nur Ichsan Sumardani, Nur Amalia Dewi, Teti Febrianti, Jauhari Arifin, Bebeh Wahid Nuryadin
Format: Article
Language:English
Published: Kelompok Peneliti Muda Universitas Negeri Jakarta 2020-04-01
Series:Risenologi
Subjects:
Online Access:https://ejurnal.kpmunj.org/index.php/risenologi/article/view/76
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spelling doaj-bb426dbe3898458ba49d501ddb3290642021-07-12T19:26:45ZengKelompok Peneliti Muda Universitas Negeri JakartaRisenologi2502-56432720-95712020-04-0151263710.47028/j.risenologi.2020.51.7650Identification of Landfill Using Refraction Seismic Method in LIPI Area - BandungResi Wasilatus Syifa0Nur Ichsan Sumardani1https://orcid.org/0000-0002-6355-724XNur Amalia Dewi2Teti Febrianti3Jauhari Arifin4Bebeh Wahid Nuryadin5https://orcid.org/0000-0002-6653-4174Universitas Islam Negeri BandungUniversitas Islam Negeri BandungUniversitas Islam Negeri BandungUniversitas Islam Negeri BandungPuslit Geoteknologi, LIPI BandungUniversitas Islam Negeri BandungResearch has been carried out using seismic refraction in the LIPI area - Bandung, which aims to determine the land of embankment in the area. Retrieval of field data was carried out using geometric  Es-3000 tool along 46 meters with a spacing of 2 meters and a 7 shoot punch consisting of 2 phantom shoots beginning and ending. Data processing is done by the first step, namely by geometric editing so that data can be read by the computer. The inversion process is done by seismimager software which consists of pickwin to extract data and plotera for modeling the subsurface layer. The results of the data interpretation show the P wave velocity from 315 - 435 m / s. layer grouping based on P wave velocity is at the first color layer having a wave velocity of about 315 - 342 m / s, the second color layer has a wave speed of 355-382 m / s, and the third color layer has a speed of 359 - 422 m / s and thick layer more than 435. Based on the lithological classification of subsurface rock layers, this study area tends to have a layer of soil type with a depth of 5 meters, and can be said to be a layer of soil deposits because of the formation of soil structures that tend to be newhttps://ejurnal.kpmunj.org/index.php/risenologi/article/view/76seismic refraction, geometric es – 3000, seisimager, groundfill
collection DOAJ
language English
format Article
sources DOAJ
author Resi Wasilatus Syifa
Nur Ichsan Sumardani
Nur Amalia Dewi
Teti Febrianti
Jauhari Arifin
Bebeh Wahid Nuryadin
spellingShingle Resi Wasilatus Syifa
Nur Ichsan Sumardani
Nur Amalia Dewi
Teti Febrianti
Jauhari Arifin
Bebeh Wahid Nuryadin
Identification of Landfill Using Refraction Seismic Method in LIPI Area - Bandung
Risenologi
seismic refraction, geometric es – 3000, seisimager, groundfill
author_facet Resi Wasilatus Syifa
Nur Ichsan Sumardani
Nur Amalia Dewi
Teti Febrianti
Jauhari Arifin
Bebeh Wahid Nuryadin
author_sort Resi Wasilatus Syifa
title Identification of Landfill Using Refraction Seismic Method in LIPI Area - Bandung
title_short Identification of Landfill Using Refraction Seismic Method in LIPI Area - Bandung
title_full Identification of Landfill Using Refraction Seismic Method in LIPI Area - Bandung
title_fullStr Identification of Landfill Using Refraction Seismic Method in LIPI Area - Bandung
title_full_unstemmed Identification of Landfill Using Refraction Seismic Method in LIPI Area - Bandung
title_sort identification of landfill using refraction seismic method in lipi area - bandung
publisher Kelompok Peneliti Muda Universitas Negeri Jakarta
series Risenologi
issn 2502-5643
2720-9571
publishDate 2020-04-01
description Research has been carried out using seismic refraction in the LIPI area - Bandung, which aims to determine the land of embankment in the area. Retrieval of field data was carried out using geometric  Es-3000 tool along 46 meters with a spacing of 2 meters and a 7 shoot punch consisting of 2 phantom shoots beginning and ending. Data processing is done by the first step, namely by geometric editing so that data can be read by the computer. The inversion process is done by seismimager software which consists of pickwin to extract data and plotera for modeling the subsurface layer. The results of the data interpretation show the P wave velocity from 315 - 435 m / s. layer grouping based on P wave velocity is at the first color layer having a wave velocity of about 315 - 342 m / s, the second color layer has a wave speed of 355-382 m / s, and the third color layer has a speed of 359 - 422 m / s and thick layer more than 435. Based on the lithological classification of subsurface rock layers, this study area tends to have a layer of soil type with a depth of 5 meters, and can be said to be a layer of soil deposits because of the formation of soil structures that tend to be new
topic seismic refraction, geometric es – 3000, seisimager, groundfill
url https://ejurnal.kpmunj.org/index.php/risenologi/article/view/76
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