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  1. NTU Theses and Dissertations Repository
  2. 工學院
  3. 工程科學及海洋工程學系
請用此 Handle URI 來引用此文件: http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/39425
完整後設資料紀錄
DC 欄位值語言
dc.contributor.advisor陳琪芳(Chi-Fang Chen)
dc.contributor.authorYen-Hsun Chenen
dc.contributor.author陳彥勳zh_TW
dc.date.accessioned2021-06-13T17:28:14Z-
dc.date.available2004-11-11
dc.date.copyright2004-11-11
dc.date.issued2004
dc.date.submitted2004-10-26
dc.identifier.citation[1]F.D.Tappert, “The parabolic approximation method”, In Wave Propagation and Underwater Acoustic, edited by J.B.Keller and J. S. Papadakis, Lecture Notes in Physics, 70.Springer,1977
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[4]陳屏先,“海洋聲學傳播模組分析”, 國立台灣大學造船暨海洋工程研究所碩士論文,1998
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[7]E.C.Shang and Y.Y.Wang, “Acoustic Travel Time Computation Based on PE Solution”, J.of Computational Acoustics, Vol.1, No.1,pp. 91-100, 1991
[8]Timothy F. Duda ,James F. Lynch, Arthur E. Newhall, Wu Lixin, C. –S. Chiu, “Fluctuation of 400Hz Sound Intensity in the 2001 ASIAEX Sound China Sea Experiment”, IEEE J.Oceanic Eng, to be published, 2004
[9] Timothy F. Duda , James C. Preisig,“Coupled Acoustic Mode Propagation Through Continental-Shelf Internal Solitary Waves”, IEEE J.Oceanic Eng,1997
[10] A.C.Warn-Varnas ,“Modeling the Effects of Solitons on Acoustics”IOS/WHOI/ONR Internal Solitary Wave Workshop Papers,6 edition,1999
[11]C. –S. Chiu, S.R.Ramp, C.W.Miller, J.F.Lynch, T.F.Duta, T.Y. Tang , ”Acoustic intensity fluctuations by South China Sea internal tides and solitons”, IEEE J.Oceanic Eng, to be published, 2004
[12]Y.J.Yang, T.Y.Tang, M.H.Chuang, A.K.Liu, M.-K.Hsu, S.R.Ramp, “Soliton Northeast of Tung-Shang Island Pilot Study of ASIAEX”, IEEE J.Oceanic Eng, to be published ,2004
[13]Edwin L. Hamilton, “Geoacoustic modeling of the sea floor”, J. Acoust. Soc. Am.,Vol.68,No.5,pp. 1313-1340,1980
[14]E. L. Hamilton, “Compressional Wave Attenuation in Marine Sediments”, Geophysics 37,pp. 620-646,1972
[15]E. L. Hamilton, “Sound attenuation as a fuction of depth in the sea floor”, J. Acoust. Soc. Am., Vol.59, No.3,pp. 528-535,1976
[16] Edwin L.Hamilton, ”Sound velocity-density relations in sea-floor sediments and rocks”,J. Acoust. Soc. Am., Vol.63, No.2,pp. 1366-1377,1978
[17] E. L.Hamilton, “Sound velocity gradient in marine sediments”, J. Acoust. Soc. Am., Vol.65,No.4,pp. 909-922(1979)
[18]E.L.Hamilton, “ and Poisson’s Ratios in Marine Sediments and Rocks”, J. Acoust. Soc. Am., Vol.66,pp. 1093-1101,1979
[19]E.L.Hamilton, “Shear-Wave Velocity Versus Depth in Marine Sediments: A Review”,Geophysics.,Vol.41,No.5,pp. 985-996,1976
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[21]E.L.Hamilton, “Prediction of in-situ Acoustic and Elastic Properties of Marine Sediments”,Geophysics., Vol.36,No.2,pp. 266-284,1971
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[23]Arthur Newhall et al., ”Preliminary Acoustic and Oceanographic Observations from the ASIAEX 2001 South China Sea Experiment”, Woods Hole Oceanographic Institution Technical Report WHOI-2001-12, September,2001
[24]Antony K. Liu, Yunhe Zhao, T.Y. Tang, M.K.Hsu, ”Nonlinear Internal Wave Study during ASIAEX”, IEEE J.Oceanic Eng, to be published,2004
[25]Ying Tsong Lin, ” Acoustic Inversions from an Explosive Source in the ASIAEX-SCS Experiment”,Department of Engineering Science and Ocean Engineering , National Taiwan University ,Ph.D. thesis, Jan. ,2004
[26]S. Schock, “A method for estimating the physical and acoustical properties of the seabed using chirp sonar data,” Submitted to IEEE J. Oceanic Eng, Special Issue on the Asian Marginal Seas,2003
[27]Y.-S.Chiu, Y.-S. Chen, Y.-T. Lin, C-F Chen, “J-15 CW Transmission Data Analysis and Comparison with Simulation Results”, Underwater Technology 2004, conference paper,2004
[28]陳儀清、陳民本,”台灣西南海域海床表層沈積構造與聲學特性圖集”,國科會國防科技學術合作協調小組委託計畫研究成果報告,1997
[29] G.V.Frisk, ”Ocean and Seabed Acoustics”, A Theory of Wave Propagation, Prentice Hall, New Jersey,1994
[30]Shephard, F.P.(1961)Deep-Sea Sand: Internat. Geol. Con. 21 st, Nordon, Repts. , 23,pp. 26-42
[31] E.L.Hamilton, “Low sound velocities in high-porosity sediments”, J. Acoust. Soc. Am., Vol.28,pp. 16-19,1956
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dc.identifier.urihttp://tdr.lib.ntu.edu.tw/jspui/handle/123456789/39425-
dc.description.abstract本文目的為比較ASIAEX南海實驗音傳損耗(Transmission Loss)的資料與數值模擬結果,並探討水文及底質特性對淺海聲音傳播的影響。文中主要探討在ASIAEX南海實驗中,J-15-3第二條拖曳路徑中(5月5日23:31到5月6日00:23之間) CW訊號在140Hz時的音傳損耗,並將其理論計算與實際資料相比,發現數值模擬可因水文(內波)及底質參數之輸入調整,而與資料結果相仿,因此探討水文及底質特性問題。底質算例結果顯示底層聲速越高其音傳損耗越小,由聲源頻率50∼300Hz的結果發現,聲源頻率越低底層有效深度越深,而聲源頻率增加其有效深度則減少。水文算例結果顯示由內波所產生的音傳擾動會更加紊亂,因而在實際水文環境中,找出內波切確位置及速度就極為重要。zh_TW
dc.description.abstractThe comparison between the data of the transmission loss in the ASIAEX SCS experiment and the result of the numerical simulations is presented in this paper. In addition, we try to discuss the effect of water column and sediment property on the acoustic propagation in the ocean. In this paper, we mainly discuss the transmission loss of CW tones transmitted in 140 Hz during a segment of J-15-3 RUN2 which started at 05/05 23:31 and ended in 05/06 00:23. Furthermore, according to the comparison between theoretical calculations and practical data, we found the result of the numerical simulations would be similar to the practical data if the parameter of water column (internal wave) and sediments are corrected. Therefore, it is necessary to consider water column as well as sediment property further. The result of the calculation of the sediment shows the transmission loss would get lower as the sound speed gets higher and in 50-300Hz range, the effect depth of the sediment is an inverse proportion to the source frequency. The results of water column case show that due to internal waves, the fluctuation in sound propagation becomes severer. Therefore it is very important to find out the exact locations and speed of internal waves in the real ocean environment.en
dc.description.provenanceMade available in DSpace on 2021-06-13T17:28:14Z (GMT). No. of bitstreams: 1
ntu-93-R91525019-1.pdf: 13920665 bytes, checksum: 994ed5b162495748d5d64f6be3b008ab (MD5)
Previous issue date: 2004
en
dc.description.tableofcontents致謝及感言 ……………………............I
中文摘要…………………………………………………II
Abstract…………………………………………………III
目錄………………………………………………………IV
圖表目錄…………………………………………………VI
第一章 緒論……………………………………………1
1.1 背景介紹…………………………………………1
1.2 研究動機與目的…………………………………1
1.3 文獻蒐集…………………………………………5
1.4 研究方法…………………………………………7
1.4.1 PE拋物線方程式…………………………7
1.4.2 Normal Modes……………………………10
1.4.3 MOS3DPEF……………………………………….14
1.5 論文架構………………………………………….16
第二章 ASIAEX J-15-3 RUN2實驗分析及數值模擬……17
2.1 ASIAEX J-15-3 實驗簡介………………………18
2.1.1 實驗配置及步驟………………………………19
2.1.2 實驗區域海洋環境簡介………………………21
2.2 實驗訊號處理……………………………………28
2.3 數值模擬…………………………………………31
2.3.1 海洋音響環境建立……………………………31
2.4 結果與討論……………………………………………35
2.4.1實驗數據及數值模擬結果比較………………..35
2.4.2相關問題延伸…………………………………..42
第三章 淺海環境中底質特性對音傳之影響……………44
3.1 淺海底質對聲學性質之影響…………………………45
3.2 Hamilton之地音模型建立………………………….47
3.3 底質特性對音傳損耗的影響…………………………56
3.4 底質特性對音傳模組之影響…………………………65
3.4.1 不同底質的有效深度…………………………66
3.4.2 底層計算深度結果……………………………71
第四章 淺海環境水文對音傳影響…………………………79
4.1 內波對音傳損耗之影響………………………………79
4.1.1不同位置之內波對音傳之影響………………82
4.2 內波對模組之音傳影響…..……………………88
第五章 結論及未來研究方向…………………………100
參考文獻…………………………………………………104
dc.language.isozh-TW
dc.title淺海環境水文及底質對音傳特性之影響zh_TW
dc.titleEnvironmental Effects on Sound Propagation in Shallow Watersen
dc.typeThesis
dc.date.schoolyear93-1
dc.description.degree碩士
dc.contributor.oralexamcommittee王崇武(Chung-Wu Wang),楊穎堅,宋家驥,林穎聰(Ying-Tsong Lin)
dc.subject.keyword淺海環境,音傳特性,zh_TW
dc.subject.keywordShallow Waters,Sound Propagation,en
dc.relation.page106
dc.rights.note有償授權
dc.date.accepted2004-10-27
dc.contributor.author-college工學院zh_TW
dc.contributor.author-dept工程科學及海洋工程學研究所zh_TW
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