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(1)

* ᯙᱽݡ⦺Ʊ ⪹ĞŖ⦺ŝ ၶᔍŝᱶ ([email protected])

Received January 27 2013, Revised March 7 2013, Accepted April 4 2013

Copyright ⵑ 2013 by the Korean Society of Civil Engineers

This is an Open Access article distributed under the terms of the Creative Commons Attribution Non-Commercial License (http://creativecommons.org/licenses/by-nc/3.0)

 ǣŠ––’ǣȀȀ†šǤ†‘‹Ǥ‘”‰ȀͳͲǤͳʹ͸ͷʹȀ•…‡ǤʹͲͳ͵Ǥ͵͵Ǥ͵Ǥͻͻ͹ ™™™Ǥ•…‡Œ‘—”ƒŽǤ‘”Ǥ”

5㇦Ⲏ#⌾ⷓ἖#⁦㯓ⴂ#ⴲⱧ㬚#ᨒ㐖ⴖ#⟖Ὢ㡷⛯#⍂⛛

֜ઽผ ȵ৉ఢֽ ȵ׌ઽܑ ȵছଵ଀

Ku, Young Hun*, Song, Chang Geun**, Kim, Young Do***, Seo, Il Won****

Analysis of Hydraulic Characteristics of Flood Plain Using Two-Dimensional Unsteady Model

ABSTRACT

Since the cross-sectional shape of the Nakdong river is compound type, the water stage rises up to the top of the flood plane, as the flow discharge increases during the extreme rain storm in summer. The recent increase of rainfall intensity and flood frequency results in the immersions of parks and hydrophilic facilities located in the flood plain. Therefore it is necessary to analyze the hydraulic characteristics evolved by the extreme rain storm in the flood plain. The study reach ranging from the Gangjeong Goryeong Weir and the Dalseong Weir, where several hydraulic facilities are located along the channel, was selected and numerical simulations were conducted for 42 hours including the peak flood of the typhoon Sanba. The 2-D transient model, FaSTMECH was employed and the accuracy of the model was assessed by comparing the water level between the simulation results and the measured ones at a gauging station. It showed a high correlation with R2 of 0.990, AME of 0.195, and RMSE of 0.252. In addition, the inundation time, the inundation depth, the inundation velocity, and the shear stress variation in the flood plain facilities were analyzed.

Key words : Compound channel, Extreme rain storm, Flood plain, FaSTMECH

Ⅹಾ

Ӻ࠺v᮹⬂݉໕ᮡᅖ݉໕⩶┽ෝ஥Łᯩᮝအಽ, ᩍ෥℁Ḳᵲ⪙ᬑᨱ᮹⧕ᕽ⦹⃽ᮁపᯕ᷾a⦹໕ࢵ⊹ᔢᇡʭḡ⦹⃽ᙹ᭥aᔢ᜚⦹۵✚Ḷᯕ

ᯩ݅. ੱ⦽↽ɝvᬑvࠥၰ⪮ᙹኩࠥ᮹᷾aಽᯙ⧕šಉ⦝⧕aɪ᷾⦹Łᯩᮝ໑, ᯕ۵⪮ᙹ░ᨱᖅ⊹ࡽŖᬱŝzᮡ⊽ᙹ᜽ᖅॅ᮹⋉ᙹ⦝⧕

᪡Ḣᱲᱢᮝಽᩑšࡹအಽ, ɚ⦽vᬑ᜽ࢵ⊹ᨱᕽ᮹ᙹญ⦺ᱢᩢ⨆ᇥᕾᯕ⦥᫵⦹݅Ł❱݉ࡽ݅. ᅙᩑǍᨱᕽ۵݅᧲⦽⊽ᙹ᜽ᖅॅᯕ᳑ᖒࡹᨕ

ᯩ۵vᱶŁಚᅕ᪡ݍᖒᅕᔍᯕෝ༉᮹Ǎeᮝಽᖁᱶ⦹ᩍ┽⣮ᔑၵᨱ᮹⧕℉ࢱ⪮ᙹపᯕၽᔾ⦽᜽ᱱᮥᱥ⬥ಽⅾ42᜽eᨱÙ⊽ᙹ⊹༉᮹ෝ

ᝅ᜽⦹ᩡ݅. 2₉ᬱᇡᱶඹ༉⩶ᯙFaSTMECH ༉᮹đŝ᪡ᙹ᭥š⊂ᗭᨱᕽᝅ⊂ࡽᝅ⊂ᙹ᭥᪡እƱ⦹ᩍ༉⩶᮹ᱢᬊᖒᮥá☁⦽đŝR2۵

0.990, AME۵0.195, RMSE۵0.252ಽ׳ᮡᔢššĥෝᅕᩡ݅. əญŁá᷾ࡽFaSTMECH ༉⩶ᮥᯕᬊ⦹ᩍ┽⣮ᔍᔢ᜽⪮ᙹ░ԕᨱ᭥

⊹⧕ᯩ۵⌁⦲ᰆŝᔾ┽Ŗᬱ॒ŝzᮡ⊽ᙹ᜽ᖅᯕ⋉ᙹࡹ۵᜽eၰ⋉ᙹᝍ, ⋉ᙹᮁᗮၰᱥ݉ಆ॒ᮥᇥᕾ⦹ᩡ݅.

áᔪᨕ ᅖ݉໕, Ḳᵲ⪙ᬑ, ࢵ⊹, FaSTMECH

ƒ–‡”‰‹‡‡”‹‰ սėॡ

(2)

1. ᕽು

↽ɝvᬑvࠥ᮹᷾aಽ⪮ᙹ᮹ၽᔾኩࠥ᪡⪮ᙹపᯕ᷾a⦹Ł

ᯩᮝ໑, ᩍ෥℁ ┽⣮ᨱ ᮹⦽ Ḳᵲ⪙ᬑಽ ⦹⃽᮹ ࢵ⊹ᨱ ᖅ⊹ࡽ

⊽ᙹ᜽ᖅ᮹ ⋉ᙹ⦝⧕ a܆ᖒᯕ ׳ᦥḡŁ ᯩ݅. ੱ⦽ 2000֥ݡ

⬥ၹᯕ௹ಽ⦹⃽᮹ࢵ⊹ෝ⪽ᬊ⦹ᩍᔾ┽Ŗᬱᯕӹℕᮂ᜽ᖅ॒ŝ

zᮡ݅᧲⦽⊽ᙹ᜽ᖅॅᯕ᳑ᖒࡹᨩᮝӹ, ᩍ෥℁Ḳᵲvᬑᨱ᮹⦽

⦹⃽᮹⪮ᙹ᭥ᔢ᜚ᮡᯕ్⦽⊽ᙹ᜽ᖅ᮹⋉᜾ŝ♕ᱢ॒ŝzᮡ

⋉ᙹ⦝⧕ෝ aᵲ᜽┅۵ ᬱᯙᯕ ࡹʑࠥ ⦽݅. ঑௝ᕽ ᯕ᪡ zᮡ

⪮ᙹ⦝⧕ෝᩩ⊂⦹ʑ᭥⧕ᕽ۵ࢵ⊹ෝ⡍⧉⦽ᅖ݉໕ᨱᕽ᮹⮱෥

⧕ᕾᮥ☖⦽ᙹญ⦺ᱢᩢ⨆ᇥᕾᯕ⦥᫵⦹݅. ࢵ⊹ᨱᕽ᮹⮱෥᧲ᔢ

ᮡᅙඹᨱእ⦹ᩍᙹᝍᯕ᯲Ł⮱෥ᨱݡ⦽ᱡ⧎ᯕ⍅ᕽᅙඹ᮹

⮱෥ŝ۵ฯᮡ₉ᯕaᯩᮝအಽ2₉ᬱᙹ⊹⧕ᕾᯕၵ௭Ḣ⦽äᮝಽ

ᱽᦩࡹŁ ᯩ݅(Sato et al., 1989).

ǎԕᨱᕽ 2₉ᬱ ᙹ⊹༉⩶᮹ ᱢᬊᨱ š⦽ ᩑǍಽ۵ ݡᇡᇥᯕ

RMA-2ӹRiver2D ၰCCHE-2D᪡zᮡ᪅௽ʑe࠺ᦩᱢᬊᖒᯕ

á᷾ࡽᔢᬊ༉⩶᮹ᱢᬊᯕᵝෝᯕ൉Łᯩᮝ໑༉⩶ᮥ}ၽ⦹ᩍ

݅᧲⦽ᝅ⨹ᙹಽၰᯱᩑ⦹⃽ᨱᱢᬊ⦽ᩑǍࠥᯩ݅. Yoon (1982) ᯕ bb⧎อԕ ☁ᔍᯕ࠺ ᩩ⊂ŝ݉໕ ɪ⪶ݡᨱ ᮹⦽⮱෥ᩢ⨆

ᮥᇥᕾ⦹ʑ᭥⧕ᱢᬊ⦹ᩡŁ, Lee et al. (1996)ᮡᮁ⦽ℕᱢჶᮥ

ᯕᬊ⦹ᩍ}ᙹಽ⇶ᗭᇡ᮹ᙹญ✚ᖒᮥᩑǍ⦹ᩡŁ, Kim (2002)ᮡ

⦽v⦹ඹᇡ᮹᳑ᕾ᮹ᩢ⨆ᮥၼ۵ᝁłᙹᵲᅕᔢ⦹ඹḡᩎᮥᵲᝍ ᮝಽ⩥ᰆ᳑ᔍ᪡ᙹ⊹⧕ᕾᮥᯕᬊ⦹ᩍḡᩎ᮹ᙹญ✚ᖒᮥá☁⦹

ᩡᮝ໑, Yong (2003)ᮡRMA-2 ༉⩶ᮥᯕᬊ⦹ᩍᅖᰂ⦽ᯱᩑḡ⩶

ᯕӹ⮱෥ᯕɪᄡ⦹۵ḡᩎᨱᕽ᮹⮱෥᧲ᔢᮥǍℕᱢᮝಽ⢽⩥⦹

ᩡ݅. ੱ⦽, Kim et al. (2009)ᮡᯱᩑ⦹⃽ᨱᕽษ෥/ᱷᮭᮥ⃹ญෝ

᭥⦽ᮁ⦽᫵ᗭʑၹ᮹ĊᯱᰍǍᖒʑჶᮥ}ၽ⦹ᩍᱢᬊ⦹ᩡᮝ໑, Ahn et al. (2009)ᮡ⦽v⦹Ǎḡᩎ᮹Ǎ᳑ྜྷᖅ⊹ᨱ᮹⦽ᙹญ✚ᖒ

ᮥ ᇥᕾ⦽ ၵ ᯩ݅(Choi et al., 2011). Seo᪡ Song (2010)ᮡ

GalerkinჶᨱɝÑ⦽⃽ᙹ⮱෥⧕ᕾ༉⩶ᮥ}ၽ⦹ᩍ, ᝅ⨹ᝅᔍ⧪

ᙹಽ᮹อłᇡᙹ⊹༉᮹᪡12}᮹ᱱᄡ⪵ඹᙹ໕łᖁ༉᮹ᨱᱢᬊ

⦽ၵᯩᮝ໑, Seo᪡Song (2010)ᮡ⃽ᙹ⮱෥ᙹ⊹༉᮹᮹ᔢඹ݉

Ğĥ᳑Õᮝಽᇡᩍࡹ۵ᮁ᯦ᮁᗮ ⩶ᔢᮥᄁ┡ᇥ⡍॒ᮥᯕᬊ⧕

݅᧲⦹í᯦ಆ⧁ᙹᯩ۵ႊჶᮥᱽᦩ⦹ᩡŁ, SongŝSeo (2012)ᮡ

SU/PG ʑჶᮥᯕᬊ⧕ᯕᘂᯕḡ႑ᱢᯙ⃽ᯕඹၰFr=2.7 ᯕᔢ᮹

ᔍඹ⮱෥ᮥᙹ⊹༉᮹⦽ၵᯩ݅. ੱ⦽Song ॒(2012)ᮡᇥᔑ᮲ಆ

}ֱᮥ᯦ࠥ⦹ᩍᯱᩑ⦹⃽อłᇡᨱᕽၽᔾ⦹۵ᯕ₉ඹ᮹3₉ᬱᱢ

ᮁᗮǍ᳑ෝ2₉ᬱ࠺ᙹᩎ⦺ᙹ⊹༉᮹ᨱၹᩢ⦹ᩍԉvݱ⦹ඹᇡᨱ

ᱢᬊ⦽ᔍಡaᯩᮝ໑, Seo᪡Song (2012)ᮡᙹ⠪2₉ᬱ⮱෥༉᮹

᜽ԕᇡĞĥ᳑Õᨱ঑ෙǍ᳑ྜྷᵝᄡᨱᕽ᮹᪡ࠥ, ᮁᗮၰᙹᝍ

ᇥ⡍ෝ እƱ⦽ ᩑǍෝ ᙹ⧪⦹ᩡ݅.

ǎ᫙ᨱᕽ۵ Adeff᪡ Wang (1985)ᯕ ⦹ࠥ฾ ⧕ᕾᮥ ᭥⧕ᕽ

qᙁ⩶ᮁ⦽᫵ᗭʑჶᮥᯕᬊ⦹ᩍ⧕ᕾ⦹ᩡᮝ໑, Ali᪡Ben (1981)

ᮡ₉ᇥႊᱶ᜾ᮥᯕᬊ⦽༉ߙಽ៉⦹⃽᮹⮱෥ᯕᔢඹ⮱෥ᔢ┽ᨱ ᕽ⧊ඹᱱᯕḡඹᨱၙ⊹۵ᩢ⨆ᨱݡ⦹ᩍᩑǍ⦹ᩡŁ, Vreugdenhul ŝWijbenga (1982)۵ADI(Alternating-Direction-Implicit)ʑ ჶᮥᮁ⦽₉ᇥ⧕ᕾჶᨱᱢᬊ⦹ᩍ⪮ᙹ᜽⦹⃽᮹2₉ᬱ⮱෥⧕ᕾᮥ

ᝅ᜽⦹ᩡŁ, Choi (1991)۵⦹⃽ᨱᕽ⧊ඹᱱᨱᕽ᮹⮱෥ᄡ⪵ෝ

ᩑǍ⦽ၵᯩ݅. ᯕ్⦽2₉ᬱᙹ⊹⧕ᕾᮡᵝಽᅙඹ᮹⮱෥⧕ᕾᨱ

ݡ⦽ ᩑǍa ᯕ൉ᨕ Ჭᮥ ᐱ ࢵ⊹ᨱᕽ᮹ ᙹญ⦺ᱢ ᩢ⨆ᇥᕾᨱ

ݡ⦽ ᩑǍ۵ ၙḥ⦽ ᝅᱶᯕ݅.

ᅙᩑǍᨱᕽ۵ၙǎ᮹USGS(ၙǎḡḩ᳑ᔍǎ)᪡ᯝᅙ᮹RIC (⬸⋕ᯕࠥ ⦹⃽ ႊᰍᖝ░)ᨱᕽ Ŗ࠺ }ၽ⦽ iRIC ԕᨱ ┲ᰍࡽ

ษ෥/ᱷᮭ⃹ญaa܆⦽2₉ᬱᇡᱶඹ⮱෥⧕ᕾ༉⩶ᯙFaSTMECH

ෝᯕᬊ⦹ᩍ⪮ᙹ░ᨱᕽ᮹ᙹญ⦺ᱢᩢ⨆ᮥᇥᕾ⦹ᩡ݅. ݅᧲⦽

⊽ᙹ᜽ᖅॅᯕ᳑ᖒࡹᨕᯩ۵vᱶŁಚᅕ᪡ݍᖒᅕᔍᯕෝ༉᮹Ǎ eᮝಽᖁᱶ⦹ᩍ┽⣮ᔑၵᨱ᮹⧕℉ࢱ⪮ᙹపᯕၽᔾ⦽᜽ᱱᮥ

ᱥ⬥ಽⅾ42᜽eᨱÙ⊽ᙹ⊹༉᮹ෝᝅ᜽⦹ᩡ݅. ᯕෝ☖⧕⪮ᙹ᜽

ࢵ⊹ԕᨱ᭥⊹⦽⊽ᙹ᜽ᖅᯕ⋉ᙹࡹ۵᜽eၰ⋉ᙹᝍ, əญŁ

ᯕᨱ ঑ෙ ᮁᗮ ၰ ᱥ݉ಆ ॒ᮥ ᇥᕾ⦹ᩡ݅.

2. FaSTMECH༉⩶}᫵

FaSTMECH(Flow and Sediment Transport with Mechanical Evolution of Channels) ༉⩶ᮡၙǎ᮹USGS᪡ᯝᅙ᮹RICᨱᕽ

Ŗ࠺}ၽ⦽iRIC ԕᨱ┲ᰍࡽ2₉ᬱ⮱෥⧕ᕾ༉⩶ᮝಽᇡᱶඹ

⧕ᕾŝษ෥/ᱷᮭ⃹ญaa܆⦹݅. ᮁᔍᯕᘂŝ⦹ᔢᄡ࠺ᖒᇥᮥ

☖⧊⦹۵༉ऩłᖁ᳭⢽ĥs, n, əญŁz᮹ႊ⨆ᨱݡ⦽ḡ႑ႊᱶ᜾

ᮡ ݅ᮭŝ z݅(Nelson and McDonald, 1996).

ćÎ à §Î

ćŞƓ à ćŞƑ ÞÎ à§ß«Ɣ

â ćŞƌŞƔ â ćŞƕ áתƘ (1)

ćÎà §Ɠ

ćŞƓ âƔŞƑ ćŞƌŞƓ âƕćŞƘŞƓ àćÞÎà §ß«ƓƔ á ćÎà §

à ƅ 檞 âŞƑ ćŇÎ ƙ Ɯƚć

Îà §Î ćŞƑ

ŞʼnƑƑ â ćŞƌ

ŞʼnƌƑ â ćŞƘ

ŞʼnƘƑ

à ÏćÞÎà §ß«

ʼnƌƑ ƛ Ɲƞ

(2)

ćÎ à §Ɠ

ćŞƑŞƔ âƔćŞƌŞƓ âƕćŞƘŞƔ à ćÞÎ à §ß«ƓÏ á à ƅ檞 â ćŞƌ ŇÎ ƙ

Ɯƚć

Î à §Î ćŞƑ

ŞʼnƌƑ

â ćŞƌ Şʼnƌƌ

â ćŞƘ ŞʼnƘƌ

â ćÞÎ à§ß«

ʼnƑƑà ʼnƌƌƛ Ɲƞ

(3)

× á ćŇÎ

ćŞƘŞƎ àƅ (4)

(3)

Fig. 1. Study Reach (HEC-RAS)

Fig. 2. Photographs of Region A and B in Fig. 1(after Typhoon Sanba; Sep. 19, 2012) ᩍʑᕽ, u, v, w۵bb⦹ඹႊ⨆, ⬂ႊ⨆, əญŁᩑḢႊ⨆ᖒ

ᇥᯕ݅. E۵ ᙹ໕׳ᯕᯕŁ, Rᮡ ᙹಽ ᵲᝍᖁ᮹ łශၹĞᯕ݅.

Î à § á Î à ƌî« (Nelson et al., 2006)ᮡłᖁ᳭⢽ĥಽ᳑⧊ࡽ

⦹ඹᇡÑญᯕ݅.ʼnƑƑ,ʼnƌƑ,ʼnƘƑ,ʼnƌƌ,ʼnƘƌ,ʼnƘƘᮡbb⠙⨆᮲ಆ▱ᕽ (deviatoric stress tensors)᮹᫵ᗭᖒᇥᯕ݅. ᜾(5)ᨱӹ┡ԙၵ᪡

zᯕᯱᩑ⦹⃽ᨱᕽ᮹ᱱᖒ᮲ಆᮡ౩ᯕסᷩ᮲ಆŝእƱ⦹ᩍᯝၹ ᱢᮝಽ ᩢ⨆ᯕ ᱢᮝ໑ ྕ᜽⧁ ᙹ ᯩ݅(Nelson et al., 2003).

ʼnƑƑá ÏҤ

Þ

ćÎ à §Î

ćŞƑŞ àćÞÎ à§ß«Ɣ

ß

, ʼnƌƌá ÏҤ

Þ

ćŞƌŞƔ

ß

,

ʼnƘƑá Ҥ

Þ

ćÎ à §Î

ćŞƕ â ćŞƑ ŞƓŞƘ

ß

ʼnƘƘá ÏҤ

Þ

ćŞƕŞƘ

ß

, ʼnƘƌá Ҥ

Þ

ćŞƕ â ćŞƖ ŞƘŞƔ

ß

,

ʼnƌƑá Ҥ

Þ

ćÎ à §Î

ćŞƑŞƔ âćÞÎ à §ß«Ɠ

â ćŞƌŞƓ

ß

(5)

3. ༉⩶᮹ᱢᬊ

3.1 ۩ঃ֜ԩ෮จ

┽⣮ᔍᔢ᜽ࢵ⊹᮹ᙹญ⦺ᱢᩢ⨆ᮥᇥᕾ⦹ʑᨱᦿᕽᅙᩑǍᨱ ᕽ ༉᮹ෝ ᭥⧕ ᖁᱶ⦽ FaSTMECH ༉⩶ŝ 1₉ᬱ HEC-RAS

༉⩶ᮥᝅᱽᮁᩎᨱݡ⦹ᩍᙹ⊹༉᮹ෝᙹ⧪⦹Ł, ⪮ᙹ᜽ᙹ᭥ᄡ⪵

ᨱ ݡ⦽ ᝅ⊂⊹᪡ እƱ⧉ᮝಽ៉ FaSTMECH ༉⩶᮹ ᱢᬊᖒᮥ

á☁⦹Łᯱ⦹ᩡ݅. ᅙᩑǍᨱᕽᙹ⊹༉⩶᮹á᷾ᮥ᭥⧕ᖁᱶ⦽

ݡᔢᮁᩎᮡݡǍݍᖒǑ⪵ᬱᮮᨱ᭥⊹⦽⪵ᬱᙹ᭥š⊂ᗭᇡ░ݡ ǍݍᖒǑ⩥⣮໕ᨱ᭥⊹⦽⩥⣮ᙹ᭥š⊂ᗭʭḡ᧞18 kmᨱᯕ෕

۵Ǎeᯕ݅. Fig. 1ᨱ༉᮹Ǎe᮹⠪໕ࠥ᪡Ӻ࠺v⦹⃽ᱶእʑᅙĥ

⫮᮹⊂పᯱഭෝᯕᬊ⦹ᩍǍ⇶⦽HEC-RAS᮹ḡ⩶ᮥӹ┡ԕᨩ ᮝ໑, ༉᮹Ǎeԕᨱ۵⌁⦲ᰆ, ᙹᄡߑⓍ, ᯙŖ᜖ḡəญŁŖᬱŝ

zᮡ݅᧲⦽⊽ᙹ᜽ᖅॅᯕ᭥⊹⦹Łᯩ۵äᮥ᦭ᙹᯩ݅. á᷾ᮥ

᭥⦽ᱢᬊ ᔍᔢᮝಽ ┽⣮‘ᔑၵ’ ԕ᜖᜽᮹ ⪮ᙹෝ ᖁᱶ⦹ᩡ݅.

┽⣮ᔑၵ۵2012֥9ᬵ11ᯝ᪅ᱥ9᜽ᨱ⦥ญ⦡ษܱ௝࠺ԉ࠺἞

1,530 km ⧕ᔢᨱᕽၽᔾ⦹ᩡᮝ໑┽⣮ᔢයᱥ⬥ಽḲᵲ⪙ᬑa

࠺ၹࡹᨕ ⓑ ⦝⧕a ၽᔾ⧩݅. Fig. 2۵ Fig. 1ᨱ ⢽᜽⦽ A᪡

Bḡᱱᨱᕽ┽⣮ᔑၵᯕ⬥ݍᖒᅕᨱ᭥⊹⦽Ŗᬱŝ⪙ᦩᨱᕽ᮹

⩥ᰆᔍḥᮥӹ┡ԙäᮝಽ┽⣮ᨱ᮹⧕ ⪙ᦩᮁᝅŝŖᬱᨱᕽ᮹

☁ᔍ♕ᱢᯕ ၽᔾࡽ äᮥ ᦭ ᙹ ᯩ݅.

3.2 ࡦଭէրଭՑஹ

ᙹ⊹༉⩶᮹á᷾ᮥ᭥⦹ᩍ2012֥9ᬵ17ᯝ11᜽ᨱᕽ2012֥

9ᬵ19ᯝ05᜽ʭḡ℉ࢱ⪮ᙹపᯕၽᔾ⦽ᱥ⬥ಽ⦹ᩍⅾ42᜽eᨱ

Ùℱ HEC-RAS ᇡᱶඹ༉᮹ෝ ᝅ᜽⦹ᩡ݅. ᔢඹ݉ Ğĥ᳑Õᮡ

Ӻ࠺v⪮ᙹ☖ᱽᗭᨱᕽᱽŖ⦹۵⪵ᬱᙹ᭥š⊂ᗭḡᱱ᮹ᮁపs

(Ӻ࠺vᙹĥᅙඹᮁప⊂ᱶ᳑ᔍᅕŁᕽ(2003)ᨱᕽᱽ᜽ࡽᙹ᭥ᮁ

పšĥłᖁ᜾ª á ÎÔ×ÓíÒÒÒÑ¡×íÒÕÓÔᨱ᮹⧕ᔑᱶࡽs)ᮥᯕᬊ⦹

(4)

Table 1. Parameters Used in HEC-RAS Simulation

Parameter Value

Manning’s n Values

LOB 0.023

Channel 0.023

ROB 0.023

Coefficients Contraction 0.1 Expansion 0.3

Fig. 3. Boundary Condition for HEC-RAS (Sep. 17, 2012 ~ Sep. 19, 2012)

Fig. 4. Verification of WSE at Goryeong Bridge (HEC-RAS)

Fig. 5. Study Reach and Finite Element (FaSTMECH)

Table 2. Parameters Used in FaSTMECH Simulation

Parameter Value

Constant Roughness Value 0.023 Lateral Eddy Viscosity 0.45

Fig. 6. Boundary Condition for FaSTMECH (Sep. 17, 2012 ~ Sep. 19, 2012)

ᩡᮝ໑, ⦹ඹ݉Ğĥ᳑Õᮡ⩥⣮ᙹ᭥š⊂ᗭ᮹ᝅ⊂ᙹ᭥sᮥᯕ ᬊ⦹ᩡ݅. ⦹⃽ʑᅙĥ⫮᮹݉໕ᯱഭෝ☖⧕ݍᖒᅕǍ᳑ྜྷᮥၹᩢ

⦹ᩡᮝ໑, ༉᮹ʑe࠺ᦩa࠺ᅕෝ☖⦽ᬵඹaĥᗮḥ⧪ࡽ݅۵

aᱶ⦹ᨱ༉᮹ෝᙹ⧪⦹ᩡ݅. ᳑ࠥĥᙹ۵Ӻ࠺v⦹⃽ᱶእʑᅙĥ

⫮ᕽᨱᕽᱽ᜽ࡽ0.023ᮥᔢᙹಽ᯦ಆ⦹ᩡ݅. Table 1ᨱHEC- RAS ༉᮹ᨱ ᯕᬊ⦽ ᵝ᫵ ๅ}ᄡᙹෝ ӹ┡ԕᨩᮝ໑, Fig. 3ᮡ

ᅙ ᙹ⊹༉᮹ᨱ ᔍᬊࡽ Ğĥ᳑Õᮥ ӹ┡ԕᨩ݅.

Fig. 4۵ŁಚƱᙹ᭥š⊂ᗭ᮹ᝅ⊂ᙹ᭥sŝHEC-RAS ༉⩶

᮹༉᮹đŝෝእƱ⦽äᯕ݅. HEC-RAS ༉᮹ᙹ⧪ᮥ᭥⦽ĥᔑ᜽

eeĊᮡ10ᇥ, ⅾ༉᮹᜽eᮡ42᜽eᮝಽ⦹ᩡᮝ໑, ༉⩶᮹ᱶ

⪶ᖒᮥ ⠪a⦹ʑ ᭥⦽ ☖ĥḡ⢽ಽ đᱶĥᙹ(R2), ᱩݡ⠪Ɂ᪅₉ (AME), ⠪ɁᱽŒ᪅₉᮹ ⠪ႊɝ(RMSE), ᮁ᮹⪶ශ(P-value)ෝ

ᔍᬊ⦹ᩡ݅. ᝅ⊂sŝ š⊂s᮹ እƱđŝ R2۵ 0.988, AME۵

0.208, RMSE۵ 0.239᮹ ᔢššĥෝ aḡŁ ᯩᨩᮝ໑, ᮁ᮹ᙹ ᵡ0.01ᅕ݅P-value᮹sᯕԏíӹ┡ӹȡྕaᖅᮥʑb⦹í

ࡹအಽ, ☖ĥᱢᮝಽᔢššĥaᯩ݅Łӹ┡ԍ݅. ᯕෝၵ┶ᮝಽ

HEC-RAS᮹༉᮹đŝෝࢵ⊹ᨱᕽ᮹ᙹญ⦺ᱢᩢ⨆ᇥᕾᮥ᭥⦽

2₉ᬱ⮱෥༉⩶᮹⦹ඹ݉Ğĥ᳑Õᮝಽᔍᬊ⦹ʑᨱᱢ⧊⦹݅Ł

❱݉⦹ᩡ݅.

2₉ᬱ༉⩶᮹á᷾ᮥ᭥⧕vᱶŁಚᅕ⦹ඹᨱ᭥⊹⦽⪵ᬱᙹ

᭥š⊂ᗭᨱᕽᇡ░ݍᖒᅕḢᔢඹǍeʭḡ᧞15 kmෝᖁᱶ⦹ᩡ

݅. Fig. 5ᨱᱢᬊݡᔢᮁᩎ᮹⠪໕ࠥ᪡ᙹ⊹ḡ⩶ࠥ᮹⊂పᯱഭෝ

ᯕᬊ⦹ᩍǍᖒ⦽2₉ᬱᮁ⦽᫵ᗭ฾ᮥӹ┡ԕᨩ݅. FaSTMECH

༉⩶ᮡᔍbĊᯱ฾ᮝಽอ༉᮹aa܆⦹ʑভྙᨱᮁ⦽᫵ᗭ฾ᮡ

ⅾ 23,550}᮹ ᔍbĊᯱಽ Ǎᖒ⦹ᩡ݅.

༉⩶᮹ᔢඹ݉Ğĥ᳑Õᮡᦿᖁ༉᮹᪡࠺ᯝ⦽᜽eݡᨱӺ࠺

v⪮ᙹ☖ᱽᗭᨱᕽᱽŖ⦹۵⪵ᬱᙹ᭥š⊂ᗭḡᱱ᮹ ᮁపsᮥ

ᯕᬊ⦹ᩡ݅. ⦹ḡอ⦹ඹ݉Ğĥ᳑Õᖁᱶᮥ᭥⦽ᝅ⊂sᯕ᳕ᰍ

⦹ḡᦫʑভྙᨱá᷾ࡽHEC-RAS᮹ᙹ᭥đŝෝ⦹ඹ݉Ğĥ᳑

(5)

(a) Sep. 17 (11:00) (b) Sep. 17 (18:00) (c) Sep. 18 (01:00)

(d) Sep. 18 (08:00) (e) Sep. 18 (15:00) (f) Sep. 18 (22:00) Fig. 8. Variation of Water Surface Elevation During Typhoon Sanba

Fig. 7. Verification of WSE at Goryeong Bridge (FaSTMECH) Õᮝಽᔍᬊ⦹ᩡ݅. FastMECH ༉⩶ᨱᕽ۵ᇡᱶඹ༉᮹ෝᙹ⧪

⧉ᨱᯩᨕᕽᯝᱶ᜽eษ݅ᱶᔢᔢ┽ෝaᱶ⦹ᩍᙹ⊹⧕ෝᙹಕ᜽

┅໑, ᅙᩑǍᨱᕽ۵3᜽e30ᇥษ݅ᵡᇡᱶඹ༉᮹ෝᙹ⧪⦹ᩍ

ⅾ42᜽eᮥ༉᮹⦹ᩡ݅. ੱ⦽, ᳑ࠥĥᙹ۵Ӻ࠺v⦹⃽ʑᅙĥ⫮ᨱ ᕽᱽ᜽ࡽ0.023ᮥᔢᙹಽ᯦ಆ⦹ᩡ݅(MLTM, 2009). Table 2ᨱ

FaSTMECHᨱݡ⦽ᵝ᫵ๅ}ᄡᙹෝᙹಾ⦹ᩡŁ, Fig. 6ᨱ2₉ᬱ

༉⩶᮹ Ğĥ᳑Õᮥ ࠥ᜽⦹ᩡ݅.

2₉ᬱ ༉⩶᮹ ༉᮹ ᙹ⧪đŝෝ á᷾⦹ʑ ᭥⧕ ݡᔢǍeԕ᮹

ŁಚƱᙹ᭥š⊂ᗭ᮹ᝅ⊂ᙹ᭥ෝᯕᬊ⦹ᩍá᷾ᮥᝅ᜽⦹ᩡ݅.

Fig. 7ᨱ༉ߙ᮹᜽eᨱ঑ෙᙹ᭥đŝ᪡ᝅ⊂sᮥӹ┡ԕᨩ݅.

ᙹ⊹ ༉᮹đŝ᪡ ŁಚƱᨱᕽ᮹ ᝅ⊂ ᙹ᭥s᮹ እƱđŝ R2۵

0.990, AME۵0.195, RMSE۵0.252᮹ᔢššĥෝᅕᩡᮝ໑,

ᮁ᮹ᙹᵡ0.01ᅕ݅P-value᮹sᯕԏíӹ┡ӹȡྕaᖅᮥʑb⦹

íࡹအಽ, ☖ĥᱢᮝಽᔢššĥaᯩ݅Łӹ┡ԍ݅. ঑௝ᕽ༉᮹Ǎ eᨱ ݡ⦽ FaSTMECH ༉⩶᮹ ᱢᬊᖒᯕ ׳݅Ł ❱݉ࡹᨩ݅.

4. vᬑᨱ᮹⦽ࢵ⊹⊽ᙹ᜽ᖅ᮹ᙹญ⦺ᱢᩢ⨆

á᷾ࡽ2₉ᬱᙹ⊹༉⩶ᮥᯕᬊ⦹ᩍ┽⣮ᔍᔢ᜽vᱶŁಚᅕ

⦹ඹᨱᕽݍᖒᅕḢᔢඹǍeʭḡᇡᱶඹ༉᮹ෝᝅ᜽⦹ᩡ݅. ᜽e ᨱ঑ෙ॒ᙹ᭥ࠥᄡ⪵ෝӹ┡ԙFig. 8ಽᇡ░ษ෥/ᱷᮭᯕᱢᱩ⦹

í༉᮹ࡹŁᯩᮝ໑, ℉ࢱ⪮ᙹపᯕၽᔾ⦽᜽ʑᨱݡᇡᇥ᮹ࢵ⊹ᨱ ᕽ ⋉ᙹa ၽᔾ⦽ äᮥ ᦭ ᙹ ᯩ݅.

(6)

(a) Sep. 17 (11:00) (b) Sep. 17 (18:00) (c) Sep. 18 (01:00)

(d) Sep. 18 (08:00) (e) Sep. 18 (15:00) (f) Sep. 18 (22:00) Fig. 10. Velocity Vector at Two Points During Typhoon Sanba

Fig. 9. Analysis Points

༉᮹ࡽđŝෝᯕᬊ⦹ᩍFig. 9᪡zᯕࢵ⊹ᨱᕽ᮹ᙹญ⦺ᱢ

ᩢ⨆ᮥᇥᕾ⦹ʑ᭥⧕༉᮹Ǎeᔢඹᬑᦩᨱ᭥⊹⦽ᮡ⧪ӹྕ⌁⦲

ᰆŝݍᖒᅕᔢඹ᳭ᦩᨱ᭥⊹⦽Ŗᬱᮥᖁᱶ⦹ᩍ, ࢱḡᱱᨱᕽ᮹

┽⣮ ᔍᔢ᜽ ᜽eᨱ ঑ෙ ᙹ᭥ᄡ⪵᪡ ᮁᗮᄡ⪵ ၰ ᱥ݉᮲ಆᮥ

ᇥᕾ⦹ᩡ݅.

Fig. 10ᮡࢱḡᱱᇡɝᨱᕽ᮹᜽eᨱ঑ෙᮁᗮᄂ░ෝӹ┡ԙ

əฝᯕ݅. ᵝᙹಽԕ᮹⮱෥ᯕࢵ⊹ʭḡ₉᪍௝⋉ᙹaࡹŁᯕᨱ

঑ෙ ⋉ᙹ ᮁᗮᯕ ၽᔾ⦹۵ äᮥ Fig. 10(c)᪡ (d)ᨱᕽ ⪶ᯙ⧁

ᙹᯩᮝ໑, ᯕ⬥əฝᨱᕽ۵⋉ᙹᝍᯕqᗭ⧉ᮥ⪶ᯙ⧁ᙹᯩ݅.

ࢵ⊹ᨱᕽ᮹↽ݡᮁᗮᮡ0.4 m/s ԕ᫙ᯕŁ⋉ᙹࡽݡᇡᇥ᮹ḡᱱᨱ ᕽ۵ᯕᅕ݅⭉ᦍԏᮡᮁᗮᯕšₑࡹအಽ, ࢱḡᱱᨱᕽ⋉᜾ᅕ݅۵

☁ᔍ♕ᱢ᮹ ၽᔾᯕ ޵ᬒ ྙᱽa ࢁ ᙹ ᯩ݅Ł ❱݉ࡽ݅.

Fig. 11ᮡࢱḡᱱᨱᕽ᮹᜽eᨱ঑ෙᙹ᭥ᄡ⪵ෝӹ┡ԙəฝᯕ

݅. ᇪᮡᖁᮡb ḡᱱᨱᕽ᮹ḡ⩶ၵ݆᮹⢽Łෝ ӹ┡ԙäᮝಽ, ၵ݆᮹⢽Łᅕ݅ ᙹ᭥a ׳ᮥভ b ḡᱱᨱᕽ⋉ᙹa ၽᔾ⦹í

ࡽ݅. ݡఖ17ᯝ11᜽30ᇥᇡ░⋉ᙹaࡹᨕ18ᯝ01᜽ᨱaᰆ

(7)

(a) Point 1 (b) Point 2 Fig. 11. Change of Water Surface Elevation on Flood Plain (Sep. 17, 2012 ~ Sep. 19, 2012) Table 3. Time Variation of Inundation Depth, Velocity and Shear Stress

Time Point 1 Point 2

Inundation (m) Velocity (m/s) Shear Stress (N/m2) Inundation (m) Velocity (m/s) Shear Stress (N/m2)

11:00 - - - - - -

14:30 0.049 0.001 0.000 - - -

18:00 1.612 0.041 0.008 0.834 0.159 0.283

21:30 2.874 0.339 0.440 2.283 0.372 1.143

01:00 3.249 0.402 0.594 2.714 0.423 1.369

04:30 3.157 0.383 0.546 2.624 0.408 1.294

08:00 2.803 0.321 0.400 2.247 0.358 1.067

11:30 2.162 0.163 0.114 1.543 0.272 0.736

15:00 1.437 0.051 0.013 0.739 0.185 0.357

18:30 0.697 0.033 0.008 - - -

22:00 - - - - - -

01:30 - - - - - -

05:00 - - - - - -

(a) Point 1 (b) Point 2

Fig. 12. Changes of Velocity and Inundation on Flood Plain (Sep. 17, 2012 ~ Sep. 19, 2012)

׳ᮡᙹ᭥ෝᅕᩡ݅. Point 1ᨱᕽ۵18ᯝ22᜽ᯕ⬥ᇡ░۵ᙹ᭥a

ḡ⩶ᅕ݅ԏᦥᲭᮝ໑, Point 2ᨱᕽ۵18ᯝ18᜽ᯕ⬥ᨱᙹ᭥a

ԏᦥḥäᮝಽӹ┡ӹࢱḡᱱ༉ࢱ┽⣮ᔑၵভ24᜽eᯕᔢ

⋉ᙹࡽ äᮥ ᦭ ᙹ ᯩ݅.

Table 3ᨱ ᜽eᨱ ঑ෙ ⋉ᙹᝍŝ ᮁᗮ ၰ ᱥ݉᮲ಆ đŝෝ

ӹ┡ԕᨩŁ, Fig. 12ᮡ᜽eᨱ঑ෙ⋉ᙹᝍŝᮁᗮ᮹ᄡ⪵ෝӹ┡ԙ

݅. Point 1ᨱᕽ᮹ ⋉ᙹᝍŝ ᮁᗮᮡ 18ᯝ 1᜽ᨱ aᰆ ׳ᮡ 3.2 m᪡ 0.40 m/sෝ ᅕᩡᮝ໑, Point 2ᨱࠥ ษ₍aḡಽ zᮡ ᜽e

(8)

(a) Point 1 (b) Point 2 Fig. 13. Changes of Velocity and Shear Stress on Flood Plain (Sep. 17, 2012 ~ Sep. 19, 2012)

aᰆ׳ᮡ2.6 m᪡0.42 m/sಽӹ┡ԍ݅. ࢱḡᱱ༉ࢱ⋉ᙹᝍ᮹

᷾aᨱ঑௝ᮁᗮᯕ᷾a⧩ᮝ໑, ⦹ඹǍeᯙPoint 2ᨱᕽ᮹⋉ᙹᝍ ᨱ ঑ෙ ᮁᗮᯕ Point 1ᅕ݅ ݅ᗭ ׳ᮡ äᮝಽ ӹ┡ԍ݅.

Fig. 13ᨱ᜽eᨱ঑ෙ⋉ᙹᝍŝᱥ݉᮲ಆ᮹ᄡ⪵ෝӹ┡ԕᨩ

݅. FaSTMECH ༉⩶ᮡ ๅ ĥᔑ ᜽eษ݅ Ċᯱᄥಽ ᱥ݉ಆᮥ

ʼn›á ҜƂÞƓÏâƔÏß ᜾ᨱ᮹⧕ĥᔑ⦹ᩍ⇽ಆ⦹အಽᅙᩑǍᨱᕽ۵

ᯕsᮥᯕᬊ⦹ᩡ݅. Point 1ŝPoint 2ᨱᕽaᰆ׳ᮡ⋉ᙹᝍᯕ

ӹ┡ԁভ, ᱥ݉᮲ಆᮡbb0.59 N/m2, 1.37 N/m2ಽӹ┡ԍᮝ໑, ࢱ ḡᱱ ༉ࢱ ⋉ᙹᝍᯕ ᷾a⧉ᨱ ঑௝ ᱥ݉᮲ಆᯕ ᷾a⦹ᩡ݅.

ੱ⦽, ⦹ඹǍeᯙPoint 2ᨱᕽ᮹⋉ᙹᝍᨱ঑ෙᱥ݉᮲ಆᯕPoint 1ḡᱱᅕ݅݅ᗭ׳ᮡäᮝಽӹ┡ԍᮝ໑, Point 1ᨱᕽ⋉ᙹᝍᯕ

ԏᮡ Ŕᨱᕽ۵ ᱥ݉᮲ಆᯕ Ñ᮹ ӹ┡ӹḡ ᦫᦹ݅.

ᯕᔢᨱᕽ, ɚ⦽vᬑᔍᔢ᜽⪮ᙹ░ԕᨱ᭥⊹⧕ᯩ۵⌁⦲ᰆŝ

ᔾ┽Ŗᬱ॒ŝzᮡ⊽ᙹ᜽ᖅᯕ⋉ᙹࡹ۵᜽eၰ⋉ᙹᝍ, ⋉ᙹ

ᮁᗮၰᱥ݉ಆ॒ᮥ2₉ᬱᇡᱶඹ༉⩶ᮥᯕᬊ⦹ᩍᇥᕾ⦹ᩡᮝ໑, ᯕ۵ ࢵ⊹ᨱᖅ⊹ࡽ ⊽ᙹ᜽ᖅॅ᮹ ⬉ᮉᱢᮁḡ ၰ šญෝ᭥⦽

ᙹญ⦺ᱢ ᯱഭಽ ⪽ᬊࢁ ᙹ ᯩ݅Ł ❱݉ࡽ݅.

5. đು

ᅙᩑǍᨱᕽ۵2₉ᬱ༉⩶᮹ᙹ⊹༉᮹đŝෝᝅ⊂ᙹ᭥᪡እƱ

⦹ᩍ༉⩶᮹ᱢᬊᖒᮥ᯦᷾⦹ᩡᮝ໑, á᷾ࡽ༉⩶ᮥ༉᮹Ǎeᨱ

ᱢᬊ⦹ᩍ┽⣮ᔍᔢ᜽ࢵ⊹ᨱᕽ᮹ᙹญ⦺ᱢᩢ⨆ᮥᇥᕾ⦹ᩡ݅.

ᅙ ᩑǍ᮹ ᩑǍ đŝෝ ᫵᧞⦹໕ ݅ᮭŝ z݅.

(1) ༉᮹Ǎeᨱ ݡ⦽ FaSTMECH ༉⩶᮹ ᱢᬊᨱ ᦿᕽ ༉⩶᮹

⦹ඹ݉Ğĥ᳑Õᮥᇡᩍ⦹ʑ᭥⧕1₉ᬱᔢᬊ༉⩶ᯙHEC- RAS᮹ᙹ᭥đŝෝŁಚƱᙹ᭥š⊂ᗭ᮹ᝅ⊂ᙹ᭥᪡እƱ⦹

ᩡ݅. əđŝR2sᮡ0.988, AME۵0.208, RMSE۵0.239 ᮹ᔢššĥෝᅕᩡᮝ໑, ᮁ᮹ᙹᵡ0.01ᅕ݅P-value᮹sᯕ

ԏíӹ┡ӹȡྕaᖅᮥʑb⦹íࡹအಽ, ☖ĥᱢᮝಽᔢšš

ĥaᯩ݅Łӹ┡ԍ݅. ᯕෝၵ┶ᮝಽHEC-RAS᮹༉᮹đŝ

ෝ2₉ᬱ༉⩶᮹⦹ඹ݉Ğĥ᳑Õᮝಽᔍᬊ⦹ʑᨱᱢ⧊⦹݅Ł

❱݉ࡹᨩ݅.

(2) 2₉ᬱ ༉⩶᮹ á᷾ᮥ ᭥⧕ ┽⣮ ᔑၵᨱ ᮹⧕ ℉ࢱ⪮ᙹపᯕ

ၽᔾ⦽᜽ᱱᮥᱥ⬥ಽ⦹ᩍⅾ42᜽eᨱÙℱᇡᱶඹ༉᮹ෝ

ᝅ᜽⦹ᩡᮝ໑, ⦹ඹ݉Ğĥ᳑Õᮡᦿᕽᔍᬊ⦽HEC-RAS᮹

ᙹ᭥đŝෝᯕᬊ⦹ᩡ݅. ༉᮹đŝෝŁಚƱᙹ᭥š⊂ᗭ᮹ᝅ⊂

ᙹ᭥᪡እƱ⦹ᩡᮝ໑, əđŝR2sᮡ0.990, AME۵0.195, RMSE۵0.252᮹ᔢššĥෝᅕᩡ݅. ੱ⦽, ᮁ᮹ᙹᵡ0.01ᅕ

݅P-value᮹sᯕԏíӹ┡ӹȡྕaᖅᮥʑb⦹íࡹအಽ,

☖ĥᱢᮝಽᔢššĥaᯩ݅Łӹ┡ԍ݅. ঑௝ᕽ, ༉᮹Ǎeᨱ

ݡ⦽ FaSTMECH ༉⩶᮹ ᱢᬊᖒᮥ ᯦᷾⦹ᩡ݅.

(3) ┽⣮ᔍᔢ᜽ࢵ⊹ᨱᕽ᮹ᙹญ⦺ᱢᩢ⨆ᮥᇥᕾ⦹ʑ᭥⧕á᷾

ࡽ2₉ᬱ༉⩶ᮥᱢᬊ⦹ᩡ݅. ༉᮹Ǎeᔢඹᬑᦩᨱ᭥⊹⦽

ᮡ⧪ӹྕ⌁⦲ᰆŝ ݍᖒᅕ ᔢඹ ᳭ᦩᨱ ᭥⊹⦽ Ŗᬱᮥ ᖁᱶ

⦹ᩍ, ࢱḡᱱᨱᕽ᮹᜽eᨱ঑ෙᙹ᭥, ᮁᗮၰᱥ݉᮲ಆ᮹

ᄡ⪵ෝᇥᕾ⦹ᩡ݅. əđŝࢱḡᱱ༉ࢱ┽⣮ᔑၵভ24᜽e

ᯕᔢ ⋉ᙹࡽ äᮥ ᦭ ᙹ ᯩᨩ݅. ੱ⦽, ࢱ ḡᱱ ༉ࢱ zᮡ

᜽eᨱaᰆ׳ᮡ⋉ᙹᝍŝᮁᗮəญŁᱥ݉᮲ಆᮥӹ┡ԕᨩ Ł, ⦹ඹǍeᨱ ᭥⊹⦽ Point 2ᨱᕽ ⋉ᙹᝍᨱ ঑ෙ ᮁᗮŝ

ᱥ݉᮲ಆᯕ Point 1 ᅕ݅ ݅ᗭ ׳ᮡ äᮝಽ ӹ┡ԍ݅.

(4) ࢵ⊹ᨱᕽ᮹↽ݡᮁᗮᮡ0.4 m/s ԕ᫙ᯕŁ⋉ᙹࡽݡᇡᇥ᮹

ḡᱱᨱᕽ۵ᯕᅕ݅⭉ᦍԏᮡᮁᗮᯕšₑࡹအಽ, ࢱḡᱱᨱᕽ

⋉᜾ᅕ݅۵☁ᔍ♕ᱢ᮹ၽᔾᯕ޵ᬒྙᱽaࢁᙹᯩ݅Ł❱݉

ࡽ݅.

(5) ᅙᩑǍᨱᕽ۵ɚ⦽vᬑᔍᔢ᜽⪮ᙹ░ԕᨱ᭥⊹⧕ᯩ۵

⌁⦲ᰆŝᔾ┽Ŗᬱ॒ŝzᮡ⊽ᙹ᜽ᖅᯕ⋉ᙹࡹ۵᜽eၰ

⋉ᙹᝍ, ⋉ᙹᮁᗮၰᱥ݉ಆ॒ᮥ2₉ᬱᇡᱶඹ༉⩶ᮥᯕᬊ⦹

ᩍᇥᕾ⦹ᩡᮝ໑, ᯕ۵ࢵ⊹ᨱᖅ⊹ࡽ⊽ᙹ᜽ᖅॅ᮹⬉ᮉᱢ

ᮁḡၰšญෝ᭥⦽ᙹญ⦺ᱢʑⅩᯱഭಽ⪽ᬊࢁᙹᯩ݅Ł

❱݉ࡽ݅.

(9)

qᔍ᮹ɡ

ᅙᩑǍ۵ǎ☁Ʊ☖ᇡÕᖅʑᚁ⩢ᝁᔍᨦ᮹ᩑǍእḡᬱ(11-ʑ ᚁ⩢ᝁ-C06)ᨱ᮹⧕ᙹ⧪ࡹᨩᮝ໑, ᯕ᪡zᮡḡᬱᨱqᔍऽพܩ݅.

References

Adeff, S. E., and Wang, S. S. Y. (1985). “Hydro-dynamic model for river flow in a microcomputer.” Hydraulics and hydrology in small computer age, ASCE, pp. 1017-1023.

Ahn, K. H., Choi, G. W., Jo, H. G., and Jo, S. U. (2009). “Study for influence by installing structures at lower the Han.” Proceedings of 2009 KWRA Spring Meeting, Journal of Korea Water Resources Association, pp. 718-722 (In Korean).

Ali, O. A., and Ben, C. Y. (1981). “Diffusion-wave flood routing in channel networks.” Journal of Hydraulics Division, ASCE, Vol.

107, No. HY6, pp.719-732.

Choi, G. W. (1991). Hydrodynamic network simulation through channel junctions, Ph.D. Dissertation, Colorado State Univer- sity, Ft. Collins, CO.

Choi, S. Y., Nam, K. Y., and Han, K. Y. (2011). “Assessment for characteristics of flow according to installing hydraulic structures by 2-D numerical model.” Journal of Environmental Impact Assessment, Vol. 20, No. 6, pp.797-813 (in Korean).

Jeon, G. S. (1998). “Quasi-two-dimensional model for floodplain flow simulation.” Journal of Korea Water Resources Association, Vol. 31, No. 5, pp. 515-528 (in Korean).

Kim, S. H., Choi, S. Y., Oh, H. W., and Han, K.Y. (2009). “Develop- ment of grid reconstruction method to simulate drying/wetting in natural rivers ( I ) : Model Development and Verification.”

Journal of Korea Water Resources Association, Vol. 42, No. 11, pp. 973-988 (in Korean).

Kim, S. Y. (2002). Analysis of flow characteristics by the Tide Influence in Singok Inline-weir, MSc Thesis, Kyonggi University (in Korean).

Lee, J. H., Kim, K. T., and Shim, M. P. (1996). “Finite volume method for two-dimensional unsteady flow in open channel.” Journal of Korea Water Resources Association, Vol. 29, No. 5, pp. 173-184 (in Korean).

MLTM (Ministry of Land, Transport and Maritime Affairs) (2009).

Nakdong river basin river master plan report (Change), Tech-

nical Report (in Korean).

Nelson, J. M., and McDonald, R. R. (1996). Mechanics and mode- ling of flow and bed evolution in lateral separation eddies, Rep. to Grand Canyon Monitoring and Research Center.

Nelson, J. M., Bennett, J. P., and Wiele, S. M. (2003). Flow and sediment transport modeling tools in fluvial geomorphology, pp. 539-576, Wiley, England.

Nelson, J., Mcdonald, R. R., and Kinzel, P. (2006). “Morphologic evolution in the USGS surface-water modeling system.” Journal of Federal Interagency Sedimentation Conference (8th FISC), pp. 233-240.

Sato, S., Imamura, F., and Shuto, N. (1989). “Numerical simulation of flooding and damage to houses by the Yoshida River due to Typhoon No. 8610.” J. Natura Disaster Science, Vol. 11, No. 2, pp. 1-19 (in Japanese).

Seo, I. W., and Song, C. G. (2010). “Development of 2D finite element model for the analysis of shallow water flow.” Journal of Korean Society of Civil Engineers, Vol. 30, No. 2B, pp. 199- 209 (in Korean).

Seo, I. W., and Song, C. G. (2010). “Specification of wall boundary conditions and transverse velocity profile conditions in finite element modeling.” Journal of Hydrodynamics, Vol. 22, No. 5, pp. 633-638.

Seo, I. W., and Song, C. G. (2012). “Numerical simulation of laminar flow past a circular cylinder with slip conditions.” Interna- tional Journal For Numerical Methods In Fluids, Vol. 68, pp.

1538-1560.

Song, C. G., and Seo, I. W. (2012). “Numerical simulation of convection-dominated flow using SU/PG scheme.” Journal of Korean Society of Civil Engineers, Vol. 32, No. 3B, pp. 175-183 (in Korean).

Song, C. G., Seo, I. W., and Kim, Y. D. (2012) “Analysis of secon- dary current effect in the modeling of shallow flow in open channels.” Advances in Water Resources, Vol. 41, pp. 29-48.

Vreugdenhul, C. B., and Wijbenga, J. H. A. (1982). “Computation of flow patterns in river.” Journal of Hydraulics Division, ASCE, Vol. 108, No. HY11, pp. 1296-130.

Yong, C. J. (2003). Comparison analysis of river flow models and sediment transport models, MSc Thesis, Honam University (in Korean).

Yoon, T. H. (1982) “Sediment transport prediction model in a harbor by finite element method.” Journal of Korean Society of Civil Engineers, Vol. 2, No. 2, pp. 847-587 (in Korean).

수치

Fig. 2. Photographs of Region A and B in Fig. 1(after Typhoon Sanba; Sep. 19, 2012)ᩍʑᕽ, u, v, w۵bb⦹ඹႊ⨆, ⬂ႊ⨆, əญŁᩑḢႊ⨆ᖒ
Table 1. Parameters Used in HEC-RAS Simulation Parameter Value Manning’s n Values LOB 0.023Channel0.023 ROB 0.023 Coefficients Contraction 0.1 Expansion 0.3
Fig. 7. Verification of WSE at Goryeong Bridge (FaSTMECH) Õᮝಽᔍᬊ⦹ᩡ݅. FastMECH ༉⩶ᨱᕽ۵ᇡᱶඹ༉᮹ෝᙹ⧪⧉ᨱᯩᨕᕽᯝᱶ᜽eษ݅ᱶᔢᔢ┽ෝaᱶ⦹ᩍᙹ⊹⧕ෝᙹಕ᜽ ┅໑, ᅙᩑǍᨱᕽ۵3᜽e30ᇥษ݅ᵡᇡᱶඹ༉᮹ෝᙹ⧪⦹ᩍⅾ42᜽eᮥ༉᮹⦹ᩡ݅
Fig. 9. Analysis Points

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