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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 | 孫志鴻(Chih-Hong Sun) | |
dc.contributor.author | Yu-Hung Chen | en |
dc.contributor.author | 陳育宏 | zh_TW |
dc.date.accessioned | 2021-06-17T06:01:06Z | - |
dc.date.available | 2019-02-15 | |
dc.date.copyright | 2019-02-15 | |
dc.date.issued | 2019 | |
dc.date.submitted | 2019-02-11 | |
dc.identifier.citation | Aboud, E., Saud, R., Asch, T., Aldamegh, K., & Mogren, S. (2014). Water exploration using Magnetotelluric and gravity data analysis; Wadi Nisah, Riyadh, Saudi Arabia. NRIAG Journal of Astronomy and Geophysics, 3(2), 184-191.
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dc.identifier.uri | http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/71458 | - |
dc.description.abstract | 台灣年平均降雨量約 2510 mm,為世界平均值的2.5倍,但降雨時空分布不均,南部區域豐枯比達9:1為甚,又因山高流短使得水源儲存不易,以致於枯水期河川逕流量大幅減少,為能穩定南部地區水資源之供應,伏流水(hyporheic flow)的開發具有其必要性。然而,伏流水的研究大多侷限於生物以及生態領域,研究焦點為伏流水帶(hyporheic zone)與生態環境之間的相互關係,對於伏流水帶擷取利用的評估相對缺乏。再者,實務工程上,同樣缺乏掌握伏流水帶邊界的有效分析方法,也難以做到伏流水開發的精準評估。
為解決以上問題,本研究目的為伏流水帶的劃分、評估與結果驗證。本研究透過SYT及DGT特低頻電磁波物性探勘儀(SYT/DGT ultra low frequency remote sensing techniques ),進行伏流水帶探測工作,參照研究區的水文、地質與岩芯等地真資料(ground truth)建立水文地質概念模型,並透過三階段判識率定各岩層電阻率(resistivity)的值閾,進而劃分伏流水帶邊界並評估最佳取水目標區。本研究亦在高屏堰上分別於乾、溼季施測,以勾勒出豐、枯水期伏流水之變化情形。 依照本研究結果,水文地質概念模型與電性響應一致,推估伏流水帶介於河床底部至第一阻水層之間(約為-4m~-38m),並以第一含水層中之礫石層(約為-24m~-34m)為最佳取水目標區。乾、旱季之測量則呈現明顯季節性差異,兩者有相同的電阻率轉換深度,惟電阻率變化趨勢不同,呈現溼季時表層相較「富水」、底層相較「乾涸」,乾季時則表層相較「乾涸」、底層相較「富水」。 根據以上所述的特低頻電磁波遙測法,希望以此探勘方法增加現今伏流水帶分析的快速性與準確性,以達到更完善的伏流水資源利用。 | zh_TW |
dc.description.abstract | With growing instability of spatial and temporal precipitation variability and water supply in Taiwan, utilizing alternative water sources is one of the important trends in water resources development. Understanding that hyporheic water is one of the resources that has the characteristics of slow flow velocity, low turbidity, high water quality and low ecological impact, it has a great potential to be utilized. However, the researches about hyporheic water are mainly focused on the interrelationships between the hyporheic zone and its biological ecosystem. The researches about utilizing hyporheic water are relatively insufficient and the potential water content can’t be effectively estimated.
Therefore, the purpose of this study is to propose an innovative procedure to investigate distribution of the hyporheic zone and to verify the results by comparing with ground truth data. We also made measurements in wet and dry seasons to see the time series change. The results show that by applying Ultra Low Frequency Electromagnetic Wave Remote Sensing techniques, in most cases the stratigraphic section identified in the study successfully matched the ground true well data and hydrogeological conceptual model. The hyporheic zone lies between riverbed and aquitard 1 (-4m~-38m) and the optimal water intake area lies in gravel layer of aquifer 1 (-24m~-34m). The resistivity profiles of wet and dry seasons show significant difference owing to precipitation variability. In conclusion, this study provides an effective way to evaluate hyporheic zone in southern Taiwan. We hope that this study can contribute to practical hyporheic water resources development project. | en |
dc.description.provenance | Made available in DSpace on 2021-06-17T06:01:06Z (GMT). No. of bitstreams: 1 ntu-108-R03228022-1.pdf: 13746748 bytes, checksum: 8c0a83ae13c43db1c6935af678e7b6e2 (MD5) Previous issue date: 2019 | en |
dc.description.tableofcontents | 摘要 i
Abstract ii 目錄 iii 圖目錄 vi 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 研究步驟與論文架構 2 第二章 文獻回顧 4 2.1 伏流水帶定義 4 2.1.1 生物學觀點的定義方法 4 2.1.2 地球化學的定義方法 5 2.1.3 水力學家的定義方法 5 2.1.4 水文地質的定義方法 6 2.1.5 伏流水帶定義之異同 6 2.2 伏流水帶特性 7 2.2.1 伏流水交換 7 2.2.2 伏流水與地下水 12 2.3 水利署高屏溪傍河取水伏流水模場工程 13 2.4 伏流水帶探測:地球物理探勘 20 2.3.1 地球物理探勘 20 2.3.2 電磁波法 21 2.5 伏流水帶探測:特低頻電磁波遙測法 25 第三章 研究方法 32 3.1 探測儀器驗證 32 3.1.1 地質鑽井驗證規劃 32 3.1.2 人工結構物驗證-管線案例 35 3.2 研究區概述 37 3.3 研究架構 42 3.4 研究流程 43 3.5 測量技術與工具 45 3.6 測量規劃 47 3.6.1 測區邊界 47 3.6.2 測點密度 48 3.6.3 測量深度 49 3.7 資料分析 49 3.7.1 單點電阻率反演計算 49 3.7.2 反距離權重法 50 3.7.3 LoG邊緣偵測 53 3.7.4 電阻率閾值設定 56 3.7.5 伏流水資源評估 58 第四章 研究成果 61 4.1 探測儀器驗證 61 4.1.1地質鑽井驗證 61 4.1.2 人工結構物驗證-管線案例 68 4.2 測線分析 71 4.2.1 資料收集 71 4.2.2 資料反演 73 4.2.3 IDW、邊緣偵測 77 4.2.4 電阻率閾值設定 82 4.2.5 測線分析 94 4.3 伏流水資源評估 106 4.3.1 伏流水帶判識 106 4.3.2 取水目標區分析 110 4.4 結果比對 112 4.5 小結 113 4.5.1 伏流水水帶劃分分析流程建議 113 4.5.2 效益分析 113 第五章 結論與建議 118 5.1 結論 118 5.2 研究貢獻 119 5.3 研究限制與後續研究建議 119 參考文獻 121 附件一:第一次試驗探勘 128 附件二:第二次試驗探勘 131 附件三:Cross Validation Report of F Survey Line 133 | |
dc.language.iso | zh-TW | |
dc.title | 特低頻電磁波遙測技術於伏流水帶劃分之研究-以高屏溪流域為例 | zh_TW |
dc.title | Applying Ultra Low Frequency Remote Sensing Techniques to Hyporheic Zone Delimitation Analysis - A Case Study on Kaoping River, Taiwan | en |
dc.type | Thesis | |
dc.date.schoolyear | 107-1 | |
dc.description.degree | 碩士 | |
dc.contributor.coadvisor | 朱子豪(Tzu-How Chu) | |
dc.contributor.oralexamcommittee | 譚義績(Yih-Chi Tan),黃誌川(Jr-Chuan Huang) | |
dc.subject.keyword | 伏流水帶,特低頻電磁波,SYT物性探測儀,DGT物性探測儀, | zh_TW |
dc.subject.keyword | hyporheic zone,ultra-low frequency electromagnetic wave,SYT detector,DGT detector, | en |
dc.relation.page | 237 | |
dc.identifier.doi | 10.6342/NTU201900399 | |
dc.rights.note | 有償授權 | |
dc.date.accepted | 2019-02-12 | |
dc.contributor.author-college | 理學院 | zh_TW |
dc.contributor.author-dept | 地理環境資源學研究所 | zh_TW |
顯示於系所單位: | 地理環境資源學系 |
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