臺灣博碩士論文加值系統

近年來在全球氣候變遷的過程中，因二氧化碳（CO2）長期累積於大氣中而造成地球暖化。其中濕地因具有吸收或排放二氧化碳的功能，其相關碳匯效能之研究更是蓬勃發展，本研究針對位於台南之七股潟湖、虎頭埤與嘉南藥理科技大學人工濕地進行水質分析，二氧化碳(CO2)、甲烷(CH4)及氧化亞氮(N2O)的釋放通量、水中藻類總初級生產量及底泥有機碳密度，進而進行碳吸存及氣體交換通量之分析與測量，以因應國際發展趨勢，發展濕地碳匯管理的技術。
本研究碳收支計算法使用淨生態系統生產量(NEP，Net Ecosystem Production)的觀念結合到碳質量平衡模式中。將濕地的淨初級生產量(NPP，Net primary Productivity)扣除濕地的異營性呼吸量(HR，Heterogeneous Respiration)即可得到淨生態系統生產量（NEP），以濕地碳吸存能力及碳庫量估算法，即可求得該類型濕地碳吸存能力及碳庫量。
本研究果發現碳匯能力最強者為嘉藥人工濕地，年平均碳收支量SSF濕地高達1,644 g Cm-2 yr-1，其次為七股紅樹林溼地504~727 g Cm-2 yr-1，而其他濕地僅表現出微弱的碳匯能力，甚至有部分呈現出排放碳源的結果。

In recent years, the research of wetlands has played an important role in the process of global climate change due to the long-term sequestration of atmospheric carbon dioxide (CO2). Because of its functionality to absorb or emit carbon dioxide, together with the performance of carbon sequestration, wetlands have the environmental characteristics of high water levels and anaerobic bottom. This study is based on the Chiku Lagoon, Hu-Tou-Pi Reservoir and constructed wetland in Chia-Nan University of Pharmacy & Science to monitor water quality, gross primany production, emission fluxes of CO2, CH4 and N2O, and the soil organic carbon density to analyze carbon sequestration gas flux measurements calculated exchange. The research can respond the international development trends, and develop the technology of wetland carbon management.
This study combines the carbon balance calculation method with the concept of net ecosystem production into the carbon mass balance model. The net primary production of the wetland will be deducted from the net primary production of the wetland. The carbon storage capacity and carbon stock of the wetland can be obtained by estimating the carbon storage capacity and carbon stock.
The results of this study found that the strongest carbon sink capacity about 1,644 g Cm-2 yr-1 for artificial SSF wetland in Chia-Nan University of Pharmacology and Science, and the second strong carbon sink capacity reach 504~727 g Cm-2 yr-1 for mangrove forest in Chiku. Other wetlands show only weak carbon sink, and even some of them are carbon source.

摘 要 I
Abstract II
誌 謝 III
目 錄 IV
圖 目 錄 VI
表 目 錄 VII
第一章 緒 論 1
1.1 前言 1
1.2 研究目的 1
1.3 研究區域 1
第二章 文獻探討 5
2.1濕地 5
2.2濕地生態功能 12
2.3 濕地碳循環 13
2.4 濕地碳匯調查 15
2.5 濕地碳匯能力 17
第三章 研究方法與分析技術 26
3.1碳平衡估算方法 26
3.2碳庫變化估算法 30
3.3採氣罩分析技術 35
3.4經驗公式差補法推估全年交換通量 38
3.5空間外推法推估濕地的碳匯或交換通量 39
3.6微氣象技術 40
3.7初級生產量與異營性呼吸通量 41
3.8濕地底泥或土壤長期碳累積量 43
第四章 採樣與分析 45
4.1海岸鹹水濕地 45
4.2淡水埤塘濕地 48
4.3淡水人工溼地 48
4.4監測方法 51
第五章 研究成果 60
5.1海岸鹹水濕地 60
5.2淡水埤塘濕地 68
5.3淡水人工溼地 70
第六章 結論與建議 72
6.1結論 72
6.2建議 73
參考文獻 75

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