Experimental study on bottom boundary layer beneath solitary wave

A tsunami as long wave and an oscillatory wave moves into shoaling water have behavior similar to solitary wave and therefore comprehension on its bottom boundary layer characteristics come to be essential key on near-shore sediment transport modeling. In the present study, the hydraulics...

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Main Authors: Winarta, Bambang, Nadiatul Adilah, Ahmad Abdul Ghani, Tanaka, Hitoshi, Yamaji, Hiroto, Mohammad Fadhli, Ahmad
Format: Article
Language:English
Published: Asian Research Publishing Network (ARPN) 2016
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Online Access:http://umpir.ump.edu.my/id/eprint/21732/1/Experimental%20study%20on%20bottom%20boundary.pdf
http://umpir.ump.edu.my/id/eprint/21732/
http://www.arpnjournals.org/jeas/research_papers/rp_2016/jeas_0416_4119.pdf
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Institution: Universiti Malaysia Pahang
Language: English
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spelling my.ump.umpir.217322018-07-24T01:34:18Z http://umpir.ump.edu.my/id/eprint/21732/ Experimental study on bottom boundary layer beneath solitary wave Winarta, Bambang Nadiatul Adilah, Ahmad Abdul Ghani Tanaka, Hitoshi Yamaji, Hiroto Mohammad Fadhli, Ahmad TA Engineering (General). Civil engineering (General) A tsunami as long wave and an oscillatory wave moves into shoaling water have behavior similar to solitary wave and therefore comprehension on its bottom boundary layer characteristics come to be essential key on near-shore sediment transport modeling. In the present study, the hydraulics phenomena of solitary wave are studied in deep through experiments utilizing a closed conduit generation system. This result was examined by analytical and numerical laminar solution. Moreover, wave friction factor is discussed based on the present laboratory experiment and previous studies of (Sumer et al., 2010); (Vittory and Blondeaux, 2011, 2012). As conclusions, in-consistent critical Reynolds number was found for solitary wave case. This observable fact is distinct difference with sinusoidal wave case which has consistency in critical Reynolds number. As a main conclusion that a new generation system proposed in the present study will be able and applicable to shore up an experiment on sediment transport induced by solitary wave. Asian Research Publishing Network (ARPN) 2016 Article PeerReviewed pdf en http://umpir.ump.edu.my/id/eprint/21732/1/Experimental%20study%20on%20bottom%20boundary.pdf Winarta, Bambang and Nadiatul Adilah, Ahmad Abdul Ghani and Tanaka, Hitoshi and Yamaji, Hiroto and Mohammad Fadhli, Ahmad (2016) Experimental study on bottom boundary layer beneath solitary wave. ARPN Journal of Engineering and Applied Sciences, 11 (8). pp. 5358-5364. ISSN 1819-6608 http://www.arpnjournals.org/jeas/research_papers/rp_2016/jeas_0416_4119.pdf
institution Universiti Malaysia Pahang
building UMP Library
collection Institutional Repository
continent Asia
country Malaysia
content_provider Universiti Malaysia Pahang
content_source UMP Institutional Repository
url_provider http://umpir.ump.edu.my/
language English
topic TA Engineering (General). Civil engineering (General)
spellingShingle TA Engineering (General). Civil engineering (General)
Winarta, Bambang
Nadiatul Adilah, Ahmad Abdul Ghani
Tanaka, Hitoshi
Yamaji, Hiroto
Mohammad Fadhli, Ahmad
Experimental study on bottom boundary layer beneath solitary wave
description A tsunami as long wave and an oscillatory wave moves into shoaling water have behavior similar to solitary wave and therefore comprehension on its bottom boundary layer characteristics come to be essential key on near-shore sediment transport modeling. In the present study, the hydraulics phenomena of solitary wave are studied in deep through experiments utilizing a closed conduit generation system. This result was examined by analytical and numerical laminar solution. Moreover, wave friction factor is discussed based on the present laboratory experiment and previous studies of (Sumer et al., 2010); (Vittory and Blondeaux, 2011, 2012). As conclusions, in-consistent critical Reynolds number was found for solitary wave case. This observable fact is distinct difference with sinusoidal wave case which has consistency in critical Reynolds number. As a main conclusion that a new generation system proposed in the present study will be able and applicable to shore up an experiment on sediment transport induced by solitary wave.
format Article
author Winarta, Bambang
Nadiatul Adilah, Ahmad Abdul Ghani
Tanaka, Hitoshi
Yamaji, Hiroto
Mohammad Fadhli, Ahmad
author_facet Winarta, Bambang
Nadiatul Adilah, Ahmad Abdul Ghani
Tanaka, Hitoshi
Yamaji, Hiroto
Mohammad Fadhli, Ahmad
author_sort Winarta, Bambang
title Experimental study on bottom boundary layer beneath solitary wave
title_short Experimental study on bottom boundary layer beneath solitary wave
title_full Experimental study on bottom boundary layer beneath solitary wave
title_fullStr Experimental study on bottom boundary layer beneath solitary wave
title_full_unstemmed Experimental study on bottom boundary layer beneath solitary wave
title_sort experimental study on bottom boundary layer beneath solitary wave
publisher Asian Research Publishing Network (ARPN)
publishDate 2016
url http://umpir.ump.edu.my/id/eprint/21732/1/Experimental%20study%20on%20bottom%20boundary.pdf
http://umpir.ump.edu.my/id/eprint/21732/
http://www.arpnjournals.org/jeas/research_papers/rp_2016/jeas_0416_4119.pdf
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