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請用此 Handle URI 來引用此文件: http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/71036
完整後設資料紀錄
DC 欄位值語言
dc.contributor.advisor卡艾瑋(Herve Capart)
dc.contributor.authorYu-Ching Huangen
dc.contributor.author黃郁晴zh_TW
dc.date.accessioned2021-06-17T04:49:43Z-
dc.date.available2021-08-14
dc.date.copyright2018-08-14
dc.date.issued2018
dc.date.submitted2018-07-31
dc.identifier.citationAdams, E. W., W. Schlager, and F. S. Anselmetti (2001). Morphology and curvature of delta slopes in Swiss lakes: lessons for the interpretation of clinoforms in seismic data. Sedimentology, 48, 661-679.
Ashmore, P. E. (1982). Laboratory modelling of gravel braided stream morphology. Earth Surf. Processes Landforms, 7(3), 201–225.
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Capart, H., Young, D. L., Zech, Y. (2002). Voronoi imaging methods for the measurement of granular flows. Experiments in Fluids, 32, 121–135.
Chang, J. Y. (2017). Hyperpycnal delta morphodynamics in finite length valleys: theoretical, experimental and field study, M. S. thesis, Graduate Institute of Civil Engineering. National Taiwan University, Taiwan.
Edmonds, D. A. and Slingerland, R. L. (2007). Mechanics of river mouth bar formation: Implications for the morphodynamics of delta distributary networks. Journal of Geophysical Research, 112, F02034.
Egozi, R. and Ashmore, P. (2009). Experimental analysis of braided channel pattern response to increased discharge. Journal of Geophysical Research, 114, F02012.
Froude, M. J., Alexander, J., Barclay, J. and Cole, P. (2017). Interpreting flash flood palaeoflow parameters from antidunes and gravel lenses: An example from Montserrat, West Indies. Sedimentology, 64, 1817–1845.
Foreman, B. Z., Lai, S. Y. J., Komatsu, Y., and Paola, C. (2015) Braiding of submarine channels controlled by aspect ratio similar to rivers. Nature Geoscience, 8, 700-703.
Gamberi, F., Rovere, M., Mercorella, A., Leidi, E. and Valle, G. D. (2014). Geomorphology of the NE Sicily continental shelf controlled by tidal currents, canyon head incision and river-derived sediments. Geomorphology, 217, 106–121.
Gilbert. G. K. (1885). The topographic features of lake shores. Ann. Rep. U. S. Geol. Surv.,5, 69-23.
Huang, M. Y. F., Huang, A. Y. L. and Capart, H. (2010). Joint mapping of bed elevation and flow depth in microscale morphodynamics experiments. Experiments in Fluids, 49, 1121–1134.
Ke, W. T. and Capart, H. (2015). Theory for the curvature dependence of delta front progradation. Geophysical Research Letters, 42(24).
Ke, W. T. (2005). Formation of symmetrically palmated deltas: shallow flow computations and experimental study, M. S. thesis, Graduate Institute of Civil Engineering. National Taiwan University, Taiwan.
Ke, W. T. (2016). Delta progradation, reservoir infill, and deposit removal in idealized and field reservoir, Ph. D. thesis, Graduate Institute of Civil Engineering. National Taiwan University, Taiwan.
Kenyon, P. M. and Turcotte, D. L. (1985). Morphology of a delta prograding by bulk sediment transport. Geological Society of America Bulletin, 90(11), 1457-1465.
Kim, W., Dai, A., Muto, T. and Parker, G. (2007). Delta progradation driven by an advancing sediment source: Coupled theory and experiment describing the evolution of elongated deltas. Water Resour. Res., 45, W06428.
Kostic, S. and Parker G. (2003). Progradational sand-mud deltas in lakes and reservoirs. Part 2. Experiment and numerical simulation. Journal of Hydraulic Research, 41(2), 141-152.
Lai, S. Y. J. (2010). Morphodynamics of coevolving fluvial and hyperpycnal valleys, Ph. D. thesis, Graduate Institute of Civil Engineering. National Taiwan University, Taiwan.
Lai, S. Y. J., Hung, S. S. C., Foreman, B. Z., Limaye, A. B., Grimaud, J. L., and Paola, C. (2017). Stream power controls the braiding intensity of submarine channels similarly to rivers. Geophysical Research Letters, 44, 5062–5070.
Lai, S. Y. J., Hsiao, Y. T. and Wu, F. C. (2017). Asymmetric Effects of Subaerial and Subaqueous Basement Slopes on Self-Similar Morphology of Prograding Deltas. Journal of Geophysical Research: Earth Surface, 122, 2506-2526.
Lee, H. Y. and Yu, W. S. (1997). Experimental study of reservoir turbidity current. Journal of Hydraulic Engineering, 123(6), 520-528.
Liu, H. H. (2010). The influence of water level fluctuation on reservoir delta morphodynamics: experiment and field measurement, M. S. thesis, Graduate Institute of Civil Engineering. National Taiwan University, Taiwan.
Liu, P., Chen, A. Y., Huang Y. N., Han, J. Y., Lai, J. S., Kang, S. C., Wu, T. H., Wen, M. C., and Tsai, M. H. (2014). A review of rotorcraft Unmanned Aerial Vehicle (UAV) developments and applications in civil engineering. Smart Structures and Systems, 13(6), 1065-1094.
Muto, T. (2001). Shoreline autoretreat substantiated in flume experiments. Journal of Sedimentary Research, 71, 245-254.
Ni, W. J. and Capart, H. (2006). Groundwater drainage and recharge by networks of irregular channels. Journal of Geophysical Research: Earth Surface, 111(F2).
Ni, W. J. (2005). Groundwater drainage and recharge by geomorphically active gullies, M. S. thesis, Graduate Institute of Civil Engineering. National Taiwan University, Taiwan.
Remondino, F., Barazzetti, L., Nex, F., Scaioni, M. and Sarazzi, D. (2011). UAV photogrammetry for mapping and 3d modeling–current status and future perspectives. International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences, Vol. 38.
Swenson, J. B. and Muto, T. (2007). Response of coastal plain rivers to falling relative sea-level: allogenic controls on the aggradational phase. Sedimentology, 54, 207–221.
Tinkler, K. J. (1997). Indirect velocity measurement from standing waves in rockbed rivers. Journal of Hydraulic Engineering, 123(10), 918-921.
Wang, C. Y. (2017). Relationship between brinkline sand flux and slip face progradation for three dimensional dunes, M. S. thesis, Graduate Institute of Civil Engineering. National Taiwan University, Taiwan.
台灣電力公司 (2018) 106年度日月潭水庫及霧社水庫淤積測量委託技術服務工作–霧社水庫測量成果報告書。
賴進松、韓仁毓、張文鎰、劉寅春、康仕仲、謝其泰、譚義績、黃振家、李豐佐、林彥廷、林聖峯、張睿宇、溫明璋 (2015) UAV 影像技術應用於河道洪水位及流場之模擬分析。中國土木水利工程學刊,第二十七卷,第三期。
謝承恩、范書睿、林彥廷、黃文正、羅偉 (2016) 無人飛行載具搭載數位相機於地質構造判釋之應用。航測及遙測學刊 第二十一卷,第四期,第257-269頁。
dc.identifier.urihttp://tdr.lib.ntu.edu.tw/jspui/handle/123456789/71036-
dc.description.abstract本研究主要的研究目的是探討三角洲在不同的供砂情形下,如何堆積與對形貌改變之影響。分為兩個部分,第一部分是基於柯文韜博士在2016年所推導的三角洲前進方程式,附加考慮下游的泥沙通量,進而延伸此前進方程式,並已此為基礎,研發一套數值模型來模擬三維三角洲的動態演進過程,再利用三角洲形貌的解析解與實驗成果,對此數值模型進行驗證。第二部分是以現地調查作為啟發,現地調查是以位在台灣中部的霧社水庫作為研究案例,進行縱剖面的測量與無人飛行載具的航照測量,對獲取之現地資料進行觀察,並設計一套實驗,模擬水庫三角洲在定水位時與降低水位後的淤積情形,使用雷射掃描與追蹤粒子進行影像分析,最後將實驗成果與現地現象進行比較。
結果顯示,第一部分的數值模型得以成功模擬三角洲演進之過程,驗證出供砂分佈的多寡影響著三角洲前緣的形狀,此形狀再影響著三角洲在前基層的堆積分佈。第二部分的實驗模擬出霧社水庫現地之現象,包含在一段時間內發生的多變的河道網絡、三角洲演進、三角洲頂基層的形貌改變、水位下降後的沖刷現象等,實驗中,藉由粒子軌跡求得流速分佈,以流速大小代表供砂多寡並驗證其對三角洲淤積情況之影響,實驗的流速亦與現地流速比較得出河寬與流速之關係。
zh_TW
dc.description.abstractThe purpose of the research is to investigate the delta progradation and the influence of morphology with different conditions of sediment supply. We divided into two sections. The first part is based on the theory for the curvature dependence of delta front progradation from Ke (2016). The theory is extended by considering the sediment bypass across the downstream boundary. Moreoever, a numerical model is developed to simulate the dynamic delta progradation in 3D. This numerical model is verified by the experimental results and the analytical solutions. The beginning of the second part is the field survey. Wushe Reservoir in central Taiwan is as our study case. We conducted the traverse survey and aerial photogrammetry by UAV to observe the phenomena in the field. To simulate the delta conditions in the reservoir, the experiment was designed and analyzed with the laser scanning and particle tracking. Finally, the experimental results are compared with the field data.
In results, the numerical model in the first part can simulate the delta progradation. We verify that the sediment supply distribution influences the shape of shoreline, which affects the deposition on the delta foreset. The experiment in the second part can simulate the phenomena in Wushe Reservoir, including the various channel networks, delta progradation, change of morphology on the topset, and the erosion after water level falling. In the experiment, the flow velocity can be obtained by the particle paths. The velocity represents the amount of sediment supply and influences the deposition on delta. The velocity in the experiment is also compared with the velocity in the field to explore the relationship between the width of channel and the velocity.
en
dc.description.provenanceMade available in DSpace on 2021-06-17T04:49:43Z (GMT). No. of bitstreams: 1
ntu-107-R05521307-1.pdf: 818156854 bytes, checksum: 81f1c3deec34af5a649c182ec4ca876b (MD5)
Previous issue date: 2018
en
dc.description.tableofcontents口試委員會審定書 #
誌謝 i
中文摘要 ii
Abstract iii
Table of Contents iv
List of Figures viii
List of Tables xviii
Chapter 1 Introduction 1
Chapter 2 Delta Progradation and Bypass Model 7
2.1 Theory 7
2.1.1 General case 7
2.1.2 Special case 12
2.1.3 Solution of special case 13
2.2 Numerical model 14
2.2.1 Definition of discrete system 14
2.2.2 The shortest distance decision 18
2.2.3 The deposition area of each different n (n = nearest) 21
Chapter 3 Dry Sand Delta Experiments 23
3.1 Experimental set-up 23
3.2 Experimental procedure 26
3.3 Analysis method 28
3.3.1 Calibration 28
3.3.2 Laser data capture 29
3.3.3 Transformation from 2D image lines to 3D lines 30
Chapter 4 Results and Comparison (Dry Sand) 33
4.1 The steady conditions 33
4.2 The progradation 35
Chapter 5 Field Investigation 43
5.1 Study area 43
5.2 Delta observation in Wushe Reservoir 44
5.3 Field survey method 47
5.3.1 Aerial photogrammetry approach 47
5.3.2 Traverse survey 53
5.3.3 Subaqueous survey by sonar 55
Chapter 6 Field Survey Results 57
6.1 Results by traverse and subaqueous survey 57
6.2 The conception of building 3D model by aerial photogrammetry 57
6.3 Results by aerial photogrammetry 60
6.3.1 Agisoft PhotoScan 61
6.3.2 Pix4Dmapper 66
6.3.3 Pix4Dmapper adjustment 69
6.3.4 Final field result by Pix4Dmapper 80
6.4 Channel network identification 88
Chapter 7 Wet Sand Delta Experiments 91
7.1 Experimental set-up 91
7.2 Experimental procedure 97
7.2.1 Constant water level 98
7.2.2 Sudden water level drop 100
7.3 Analysis method 102
7.3.1 Calibration 103
7.3.2 Laser scanning 104
7.3.3 PTV 104
7.4 Experimental result 105
7.4.1 Morphology 106
7.4.2 Flow velocity 119
Chapter 8 Results and Comparison of Field Observation and Lab 129
8.1 Morphology 129
8.2 Flow velocity 136
Chapter 9 Conclusion 141
References 145
dc.language.isoen
dc.subject三角洲演進zh_TW
dc.subject水工模型試驗zh_TW
dc.subject水位變化zh_TW
dc.subject無人飛行載具zh_TW
dc.subject霧社水庫zh_TW
dc.subject供砂分布zh_TW
dc.subject三角洲形貌zh_TW
dc.subjectlaboratory experimentsen
dc.subjectsediment supply distributionen
dc.subjectdeltaic morphologyen
dc.subjectWushe Reservoiren
dc.subjectUAVen
dc.subjectwater level dropen
dc.subjectdelta progradationen
dc.title三角洲演進與輸砂量分布關係之研究zh_TW
dc.titleRelationship between delta progradation and sediment supply
distribution across the shoreline
en
dc.typeThesis
dc.date.schoolyear106-2
dc.description.degree碩士
dc.contributor.oralexamcommittee周憲德,韓仁毓,賴悅仁,洪啟耀
dc.subject.keyword三角洲演進,供砂分布,三角洲形貌,霧社水庫,無人飛行載具,水位變化,水工模型試驗,zh_TW
dc.subject.keyworddelta progradation,sediment supply distribution,deltaic morphology,Wushe Reservoir,UAV,water level drop,laboratory experiments,en
dc.relation.page149
dc.identifier.doi10.6342/NTU201801812
dc.rights.note有償授權
dc.date.accepted2018-07-31
dc.contributor.author-college工學院zh_TW
dc.contributor.author-dept土木工程學研究所zh_TW
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