Investigate the Effectiveness of Seawall Construction using CADMAS Surf 2D

Tsunami that hit Japan in 2011 shocked the world. The earthquake at the coast of the Pacific Ocean was 9.0 on Richter scale leading to 10 meters of wave. The epicentre was reported to be off the coast of Oshika Peninsula, at the east coast of Tohoku, at a depth of 244 kilometres. The earthquake and...

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Main Authors: Usman Fadly, Effendi Rahim Supli
Format: Article
Language:English
Published: EDP Sciences 2017-01-01
Series:MATEC Web of Conferences
Online Access:https://doi.org/10.1051/matecconf/20179701065
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spelling doaj-5f08bc67d6504885b0491b0f8a23dd142021-02-02T02:46:58ZengEDP SciencesMATEC Web of Conferences2261-236X2017-01-01970106510.1051/matecconf/20179701065matecconf_etic2017_01065Investigate the Effectiveness of Seawall Construction using CADMAS Surf 2DUsman Fadly0Effendi Rahim Supli1Department of Urban and Regional Planning, Faculty of Engineering, University of BrawijayaAgrotechnology Department, Agriculture Faculty, University of Palembang (UNPAL)Tsunami that hit Japan in 2011 shocked the world. The earthquake at the coast of the Pacific Ocean was 9.0 on Richter scale leading to 10 meters of wave. The epicentre was reported to be off the coast of Oshika Peninsula, at the east coast of Tohoku, at a depth of 244 kilometres. The earthquake and tsunami caused more than 20,000 victims in six prefectures. In an effort to anticipate to the tsunami, Japan has long build walls around the beach directly face the Pacific Ocean—the walls are known as seawall. In this paper, facts show that the effectiveness of seawall in reducing the energy of tsunami is accompanied by tremendous destructive energy. Analysis in this research was done using a software named CADMAS Surf 2D with numerical analysis method. Observations were made using two variants of heights of seawall, two meters and three meters. Both are observed based on the heights of the wave coming from the Ocean, after passing through the seawall, and at some points of observation. The level of damage caused by the seawall was due to turbulence just behind the construction that resulted in crushing, scouring, and or destructive energy, the energy was even bigger after passing the seawall. Nevertheless, tsunami wave height and velocity decreased significantly after the seawall.https://doi.org/10.1051/matecconf/20179701065
collection DOAJ
language English
format Article
sources DOAJ
author Usman Fadly
Effendi Rahim Supli
spellingShingle Usman Fadly
Effendi Rahim Supli
Investigate the Effectiveness of Seawall Construction using CADMAS Surf 2D
MATEC Web of Conferences
author_facet Usman Fadly
Effendi Rahim Supli
author_sort Usman Fadly
title Investigate the Effectiveness of Seawall Construction using CADMAS Surf 2D
title_short Investigate the Effectiveness of Seawall Construction using CADMAS Surf 2D
title_full Investigate the Effectiveness of Seawall Construction using CADMAS Surf 2D
title_fullStr Investigate the Effectiveness of Seawall Construction using CADMAS Surf 2D
title_full_unstemmed Investigate the Effectiveness of Seawall Construction using CADMAS Surf 2D
title_sort investigate the effectiveness of seawall construction using cadmas surf 2d
publisher EDP Sciences
series MATEC Web of Conferences
issn 2261-236X
publishDate 2017-01-01
description Tsunami that hit Japan in 2011 shocked the world. The earthquake at the coast of the Pacific Ocean was 9.0 on Richter scale leading to 10 meters of wave. The epicentre was reported to be off the coast of Oshika Peninsula, at the east coast of Tohoku, at a depth of 244 kilometres. The earthquake and tsunami caused more than 20,000 victims in six prefectures. In an effort to anticipate to the tsunami, Japan has long build walls around the beach directly face the Pacific Ocean—the walls are known as seawall. In this paper, facts show that the effectiveness of seawall in reducing the energy of tsunami is accompanied by tremendous destructive energy. Analysis in this research was done using a software named CADMAS Surf 2D with numerical analysis method. Observations were made using two variants of heights of seawall, two meters and three meters. Both are observed based on the heights of the wave coming from the Ocean, after passing through the seawall, and at some points of observation. The level of damage caused by the seawall was due to turbulence just behind the construction that resulted in crushing, scouring, and or destructive energy, the energy was even bigger after passing the seawall. Nevertheless, tsunami wave height and velocity decreased significantly after the seawall.
url https://doi.org/10.1051/matecconf/20179701065
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