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| DC 欄位 | 值 | 語言 |
|---|---|---|
| dc.contributor.advisor | 施上粟 | zh_TW |
| dc.contributor.advisor | Shang-Shu Shih | en |
| dc.contributor.author | 王丰聖 | zh_TW |
| dc.contributor.author | Feng-Sheng Wang | en |
| dc.date.accessioned | 2023-08-09T16:18:57Z | - |
| dc.date.available | 2023-11-09 | - |
| dc.date.copyright | 2023-08-09 | - |
| dc.date.issued | 2023 | - |
| dc.date.submitted | 2023-07-24 | - |
| dc.identifier.citation | 1. Al-Rubaei, A., Engström, M., Viklander, M., & Blecken, G. (2014). Long-Term Treatment Efficiency of a Constructed Stormwater Wetland: Preliminary Results.
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| dc.identifier.uri | http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/88273 | - |
| dc.description.abstract | 因溫室氣體濃度上升導致的氣候變遷在全球各地造成不同程度與類型的災害事件，紅樹林生態系除了具備吸碳、固碳、底床土壤累積碳含量等優異碳匯能力外，紅樹林濕地的地形抬昇特性有機會對抗海平面上升帶來的衝擊，包括海岸線退縮。本研究區域位於桃園市新屋溪河口，屬於紅樹林與藻礁生態複合共生系統，本研究假設紅樹林生態系統具備囚砂能力，是作為國土保育的重要生態工程策略，並可藉此降低排入下游藻礁生態系統的砂量及懸浮泥砂濃度，呼應近年國際間大力倡議之自然解方精神(nature-based solution, NbS)。
本研究進行地形、水位、流速等現地調查，包括UAV、壓力式水位計、都普勒流速剖面儀等，並收集水文、泥砂、空照圖資等歷史資料以建立數值模式並進行模式驗證；結果顯示，本研究建立的模式在常時水位驗證下具有非常良好的品質(NSE=0.9821)具備可信度，同時在高流量測試下所設置之結構物功能可在不影響模式水流分布下達成預設的阻力，而模式選用之適當輸砂公式透過模式建議之採用公式、歷年正射影像資料以及輸砂公式原理選定。另外，本研究進行9種情境之模擬分析：3種「25年重現期入流泥砂濃度」搭配3種「下游河口水位」條件；情境模擬結果顯示，入流泥砂濃度是影響濕地沖淤深度及範圍最大的因子，入流濃度提升淤積越多越廣，至於下游水位上升的影響程度相對而言屬較次要因子，研究也發現入流泥砂濃度提升至兩倍後對灘地整體高程變化為0.27 mm/yr，因未考量到紅樹林本身的生物堆積作用，故尚不足以達到平均海平面上升速率(2.35mm/yr)，但紅樹林確實提供近岸藻礁生態系自然囚砂機制，而此固砂效益也展現其作為延緩國土流失自然解方的潛力。 | zh_TW |
| dc.description.abstract | Climate change caused by increased greenhouse gas concentrations has resulted in varying degrees and types of disasters worldwide. The mangrove ecosystem, in addition to its excellent carbon sequestration capacity, such as carbon absorption, fixation, and accumulation in the sediment, has been able to counteract the impacts of rising sea levels, including coastal erosion.
This study hypothesizes that the mangrove ecosystem has sediment-trapping capability, making it an essential ecological engineering strategy for land conservation. Reducing the sediment load and suspended sediment concentration entering the downstream algal reef ecosystem aligns with the spirit of nature-based solutions (NbS), which has been strongly advocated internationally in recent years. The study area is located at the mouth of Xinwu River in Taoyuan City, with a complex symbiotic system of mangroves and algal reefs. We conducted field surveys on topography, water levels, and flow velocities using UAVs, pressure transducers, and ADCP. Historical data on hydrology, sediment, and aerial photographs were also collected and incorporated with the filed investigation to establish a numerical model and the relevant model validation. The results showed that the model developed in this study exhibited excellent quality (NSE=0.982) and reliability when validated against steady-state water levels. The structural elements installed for high-flow testing achieved the intended resistance without affecting the water flow distribution. The appropriate sediment transport formulas were selected based on the literature recommendations, historical orthophotos, and principles of sediment transport formulas. Furthermore, the study conducted simulations for nine scenarios involving the 25y-return-period inflow sediment concentration combined with downstream water levels. The simulation results indicated that inflow sediment concentration was the most influential factor affecting wetland siltation depth and extent. As the inflow concentration increased, siltation became more extensive. The impact of downstream water level rise was relatively minor. The study also found that doubling the inflow sediment concentration resulted in an overall elevation change of 0.27 mm/yr in the intertidal zone. Although it is insufficient to meet the average rate of sea-level rise (2.35 mm/yr), the mangrove forest provides a natural sediment-trapping mechanism for nearshore algal reef ecosystems. The sediment retention benefits demonstrated its potential as a nature-based solution to mitigate the land loss caused by the increased inundation under rising sea levels. | en |
| dc.description.provenance | Submitted by admin ntu (admin@lib.ntu.edu.tw) on 2023-08-09T16:18:57Z No. of bitstreams: 0 | en |
| dc.description.provenance | Made available in DSpace on 2023-08-09T16:18:57Z (GMT). No. of bitstreams: 0 | en |
| dc.description.tableofcontents | 論文口試委員審定書 i
誌謝 ii 摘要 iii Abstract iv 目錄 vi 圖目錄 ix 表目錄 xi 第一章 緒論 1 1.1 研究背景 1 1.2 研究假說與目的 4 1.3 論文架構 4 第二章 文獻回顧 5 2.1 紅樹林介紹 5 2.2 紅樹林的固砂及對抗海平面上升潛力 6 2.3 紅樹林的碳匯及固碳能力 7 2.4 藻礁生態系統 8 2.5 自然解方 9 第三章 現地調查方法 11 3.1 地形調查 12 3.2 水文調查 15 3.3 河道與灘地底床調查 17 第四章 模式理論與設定 18 4.1 SRH-2D模式理論 19 4.1.1 水理相關方程式 19 4.1.2 結構物阻力計算 21 4.1.3 輸砂原理與相關方程式 22 4.2 SRH-2D模式設定 24 4.2.1 網格建置 24 4.2.2 底床參數設定 25 4.2.3 結構物設置 29 4.2.4 入出流邊界及土層厚度 30 4.2.5 輸砂公式選擇 30 第五章 結果與討論 32 5.1 現地調查成果 32 5.1.1 地形調查結果 32 5.1.2 水文調查結果 35 5.1.3 灘地調查成果 39 5.2 模式建立 40 5.2.1 模式條件設定 40 5.2.2 參數調整及模式驗證 45 第六章 情境設定與模擬分析 55 6.1 情境假設與邊界條件設定 55 6.1.1 25年重現期上游流量與泥砂濃度條件 55 6.1.2 下游水位條件 59 6.1.3 模式模擬最終參數設定 61 6.2 情境模擬成果 62 6.2.1 研究區域在原始條件下的模擬成果 62 6.2.2 九種情境模擬的參數統整與分析 71 6.3 討論 72 第七章 結論與建議 77 7.1 結論 77 7.2 建議 78 參考文獻 79 附件1 85 附件2 88 附件3 91 附件4 93 | - |
| dc.language.iso | zh_TW | - |
| dc.subject | 自然解方 | zh_TW |
| dc.subject | 藻礁 | zh_TW |
| dc.subject | 國土保育 | zh_TW |
| dc.subject | 紅樹林 | zh_TW |
| dc.subject | 固砂 | zh_TW |
| dc.subject | 海平面上升 | zh_TW |
| dc.subject | Algal reef | en |
| dc.subject | Land conservation | en |
| dc.subject | Sea level rise | en |
| dc.subject | Sediment trap | en |
| dc.subject | Mangrove | en |
| dc.subject | Nature-based solution | en |
| dc.title | 紅樹林作為國土保育自然解方之潛力評估 | zh_TW |
| dc.title | Mangrove ecosystems as potential nature-based solutions in enhancing sediment trap efficiency against coastal erosion | en |
| dc.type | Thesis | - |
| dc.date.schoolyear | 111-2 | - |
| dc.description.degree | 碩士 | - |
| dc.contributor.oralexamcommittee | 游景雲;胡明哲 | zh_TW |
| dc.contributor.oralexamcommittee | JIING-YUN YOU;MING-CHE HU | en |
| dc.subject.keyword | 紅樹林,固砂,國土保育,海平面上升,藻礁,自然解方, | zh_TW |
| dc.subject.keyword | Mangrove,Algal reef,Sediment trap,Land conservation,Sea level rise,Nature-based solution, | en |
| dc.relation.page | 97 | - |
| dc.identifier.doi | 10.6342/NTU202301947 | - |
| dc.rights.note | 同意授權(全球公開) | - |
| dc.date.accepted | 2023-07-25 | - |
| dc.contributor.author-college | 工學院 | - |
| dc.contributor.author-dept | 土木工程學系 | - |
| 顯示於系所單位： | 土木工程學系 | |
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