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完整後設資料紀錄
DC 欄位 | 值 | 語言 |
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dc.contributor.advisor | 游景雲(Gene Jiing-Yun You) | |
dc.contributor.author | Chia-Chi Liao | en |
dc.contributor.author | 廖家祺 | zh_TW |
dc.date.accessioned | 2023-03-19T22:26:31Z | - |
dc.date.copyright | 2022-09-06 | |
dc.date.issued | 2022 | |
dc.date.submitted | 2022-08-30 | |
dc.identifier.citation | 1. Muthusamy, M., Casado, M. R., Butler, D., & Leinster, P. (2021). Understanding the effects of Digital Elevation Model resolution in urban fluvial flood modelling. Journal of Hydrology, 596, 126088. 2. Muthusamy, M., Casado, M. R., Butler, D., & Leinster, P. (2021). Understanding the effects of Digital Elevation Model resolution in urban fluvial flood modelling. Journal of Hydrology, 596, 126088. 3. O'Callaghan, J. F., & Mark, D. M. (1984). The extraction of drainage networks from digital elevation data. Computer vision, graphics, and image processing, 28(3), 323-344 4. Quinn, P. F. B. J., Beven, K., Chevallier, P., & Planchon, O. (1991). The prediction of hillslope flow paths for distributed hydrological modelling using digital terrain models. Hydrological processes, 5(1), 59-79. 5. Costa‐Cabral, M. C., & Burges, S. J. (1994). Digital elevation model networks (DEMON): A model of flow over hillslopes for computation of contributing and dispersal areas. Water resources research, 30(6), 1681-1692. 6. Tarboton, D. G. (1997). A new method for the determination of flow directions and upslope areas in grid digital elevation models. Water resources research, 33(2), 309-319. 7. Deltares. (2019). SOBEK: Hydrodynamics, Rainfall and Real-Time Control User Manual. 8. Terstriep, M. L., & Stall, J. B. (1974). The Illinois urban drainage area simulator, ILLUDAS. Bulletin (Illinois State Water Survey) no. 58. 9. Sevuk, A. S., Yen, B. C., & Peterson, G. E. (1973). Illinois storm sewer system simulation model: user’s manual. 10. Sidek, L. M., Jaafar, A. S., Majid, W. H. A. W. A., Basri, H., Marufuzzaman, M., Fared, M. M., & Moon, W. C. (2021). High-resolution hydrological-hydraulic modeling of urban floods using InfoWorks ICM. Sustainability, 13(18), 10259. 11. Kuok, K. K., Chen, E., & Chiu, P. C. (2020). Integration of IR4. 0 with Geospacial SuperMap GIS and InfoWorks ICM. Solid State Technol, 63, 21651-21662. 12. Luan, Q., Zhang, K., Liu, J., Wang, D., & Ma, J. (2018). The application of Mike Urban model in drainage and waterlogging in Lincheng county, China. Proceedings of the International Association of Hydrological Sciences, 379, 381-386. 13. Rossman, L. (2015). Storm Water Management Model User’s Manual Version 5.1—Manual. US EPA Office of Research and Development, EPA: Washington, DC, USA. 14. Rossman, L. A., & Supply, W. (2006). Storm water management model, quality assurance report: dynamic wave flow routing. US Environmental Protection Agency, Office of Research and Development, National Research Management Research Laboratory. 15. 下水道誌. (民國100年). 內政部營建署. 16. 林子平,2002年,都市水循環之研究-地表不透水率之調查及逕流量實测解析,成大建築系博士論文 17. 出流管制計畫書與規劃書檢核基準及洪峰流量計算方法,2019年,經濟部水利署 18. 複合型都市排水系統模式建置教學手冊(109.11),內政部營建署 19. 市區道路附屬工程設計規範(111 02修正版),內政部營建署 | |
dc.identifier.uri | http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/84804 | - |
dc.description.abstract | 都市集水區劃分通常是由建模者根據研究區域資料,決定子集水區數量、大小以及匯流位置,此種劃分方式會因不同建模者而有不同劃分結果,進而對下水道出流產生影響。所以本研究欲探討都市集水區劃分對於下水道出流之影響,首先利用SWMM(Storm Water Management Model)建置數值試驗模式,分別模擬在不同降雨條件下,改變單一子集水區匯流方向以及將所有子集水區往前一段管長之人孔點匯流兩部分情境。透過比較出流歷線、洪峰時間誤差以及洪峰流量誤差,以了解兩部分情境對下水道出流之影響。模擬結果洪峰時間誤差大於5%的降雨條件有降雨延時為10分鐘,最大降雨強度為60mm/hr、120mm/hr、240mm/hr以及降雨延時為30分鐘,最大降雨強度為60mm/hr,洪峰流量誤差大於5%的降雨條件有降雨延時為10分鐘,最大降雨強度為60mm/hr、120mm/hr、240mm/hr。說明在短延時的降雨條件下,集水區的劃分方式對系統的影響較大。 最後以撫遠抽水站集水區為例,用三種劃分方式建置依街道輪廓劃分、子集水區匯流點為角落之人孔點、依流向劃分之三種情境,分別模擬6小時延時定量降水350毫米、24小時延時定量降水650毫米、歷史延時7小時之豪雨事件、歷史延時11小時之大雨事件以及歷史延時1小時之降雨事件,比較不同情境間之出流,洪峰時間誤差和洪峰流量誤差皆小於5%,符合數值試驗模式之結果,說明在降雨延時較長的情況下,都市集水區劃分對於下水道出流之影響可被接受。 關鍵字:下水道系統都市集水區、劃分方式、洪峰時間誤差、洪峰流量誤差、流量歷線、SWMM | zh_TW |
dc.description.abstract | The sewershed delineation is usually done by the modeler based on the study area data to determine the number, area size, and flow direction of subcatchments. The delineation method will have distinct results due to different modelers, which will have an influence on the sewershed runoff estimation. The purpose of this study was to examine the influence of sewershed delineation on runoff. Firstly, use SWMM to construct two scenario numerical test models to simulate changing the flow direction of a single subcatchment, and all subcatchments outlet junctions move forward a pipe length under different rainfall conditions. By comparing the discharge hydrograph,the error of peak discharge, and the error of time to peak, it can help to understand the influence of the two scenarios on outflow. The results show that the error of time to peak or the error of peak discharge is more than 5%, mainly arise in the rainfall duration is 10 minutes, the maximum rainfall intensity is 60mm/hr, 120mm/hr, and 240mm/hr. The results demonstrate that the delineation of sewershed has a greater impact on the outflow under short-duration rainfall condition. Finally, constructing three scenarios with three methods of delineation in a case study on the watershed of FUYUAN: the subcatchments are delineated according to the outline of the street, the outlet junction of the subcatchment is the corner manhole, and the subcatchments are delineated according to the flow direction. For the three scenarios, simulate 6-hour duration quantitative precipitation of 350 mm, 24-hour duration quantitative precipitation of 650 mm, 0908 extremely heavy rain, 0525 heavy rain, and 0627 rain event. Comparing the outflow between different scenarios, the error of time to peak and the error of peak discharge are both less than 5%, which fit the results of the numerical test model. It shows that the influence of sewershed delineation on the outflow can be accepted under the long-duration rainfall condition. Key words: sewershed, methods of delineation, the error of peak discharge, the error of time to peak, discharge hydrograph, SWMM | en |
dc.description.provenance | Made available in DSpace on 2023-03-19T22:26:31Z (GMT). No. of bitstreams: 1 U0001-3008202213244800.pdf: 18653128 bytes, checksum: 960c1acf2a2a4f32892e8485fa5615ed (MD5) Previous issue date: 2022 | en |
dc.description.tableofcontents | 目錄 誌謝 i 摘要 ii Abstract iii 圖 目錄 viii 表 目錄 x 第一章 緒論 1 1.1 研究動機 1 1.2 研究目的 2 1.3 研究流程及架構 3 第二章 文獻回顧 5 2.1集水區劃分 5 2.2下水道系統 6 2.3模式分析方法 6 第三章 研究方法 9 3.1 暴雨逕流管理模式(SWMM) 9 3.1.1地表逕流模組(Runoff module) 9 3.1.2 輸水幹線模組(Extran module) 11 第四章 數值試驗模式與研究區域模式建置 16 4.1 數值試驗模式 16 4.2 研究區域概述 20 4.2.1地文條件 20 4.2.2氣候 22 4.3 模式建立 22 4.3.1資料收集 22 4.3.2模擬情境 27 4.3.3輸入資料 29 4.3.4模式驗證 30 第五章 模式模擬與結果分析 36 5.1 數值試驗模式 36 5.1.1 改變各子集水區匯流點對於出流量的影響 36 5.1.2 所有子集水區往前一人孔點匯流對於出流量的影響 43 5.2 實際案例 48 5.2.1 淹水潛勢圖之定量降水 48 5.2.2 歷史降雨事件 55 第六章 結論與建議 61 6.1結論 61 6.2建議 62 參考文獻 63 附錄A數值試驗模式最大降雨強度60mm/hr模擬結果 65 A.1降雨延時10分鐘 65 A.2降雨延時30分鐘 68 A.3降雨延時1小時 71 A.4降雨延時2小時 74 A.5降雨延時4小時 77 附錄B數值試驗模式最大降雨強度120mm/hr模擬結果 80 B.1降雨延時10分鐘 80 B.2降雨延時30分鐘 83 B.3降雨延時1小時 86 B.4降雨延時2小時 89 B.5降雨延時4小時 92 附錄C數值試驗模式最大降雨強度240mm/hr模擬結果 95 C.1降雨延時10分鐘 95 C.2降雨延時30分鐘 98 C.3降雨延時1小時 101 C.4降雨延時2小時 104 C.5降雨延時4小時 107 附錄D數值試驗模式各情境之模擬結果 110 D.1最大降雨強度為60mm/hr 110 D.2最大降雨強度為120mm/hr 112 D.3最大降雨強度為240mm/hr 116 附錄E撫遠模式輸入資料 119 E.1原情境、情境2子集水區資料 119 E.2情境3子集水區資料 123 E.3管線資料 127 E.4人孔資料 134 | |
dc.language.iso | zh-TW | |
dc.title | 下水道系統都市集水區劃分對於出流推估之影響探討 | zh_TW |
dc.title | The examination of the influence of sewershed delineation on runoff estimation | en |
dc.type | Thesis | |
dc.date.schoolyear | 110-2 | |
dc.description.degree | 碩士 | |
dc.contributor.oralexamcommittee | 孫建平(Jian-Ping Suen),張駿暉(Jiun-Huei Jang),陳憲宗(Shien-Tsung Chen),石棟鑫(Dong-Sin Shih) | |
dc.subject.keyword | 下水道系統都市集水區,劃分方式,洪峰時間誤差,洪峰流量誤差,流量歷線,SWMM, | zh_TW |
dc.subject.keyword | sewershed,methods of delineation,the error of peak discharge,the error of time to peak,discharge hydrograph,SWMM, | en |
dc.relation.page | 137 | |
dc.identifier.doi | 10.6342/NTU202202965 | |
dc.rights.note | 同意授權(限校園內公開) | |
dc.date.accepted | 2022-08-31 | |
dc.contributor.author-college | 工學院 | zh_TW |
dc.contributor.author-dept | 土木工程學研究所 | zh_TW |
dc.date.embargo-lift | 2022-09-06 | - |
顯示於系所單位: | 土木工程學系 |
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