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研究生:鄭艾玲
研究生(外文):Ai-Ling Cheng
論文名稱:天然氣在移棲過程中吸附及擴散作用之實驗模擬
論文名稱(外文):Adsorption and diffusion of natural gas during migration: an experimental study
指導教授:黃武良黃武良引用關係
指導教授(外文):Wuu-Liang Huang
學位類別:碩士
校院名稱:國立臺灣大學
系所名稱:地質科學研究所
學門:自然科學學門
學類:地球科學學類
論文種類:學術論文
論文出版年:2001
畢業學年度:89
語文別:中文
論文頁數:130
中文關鍵詞:天然氣吸附作用擴散作用移棲活性碳有機物黏土礦物
外文關鍵詞:Natural GasAdsorptionDiffusionMigrationactivated Carbonorganic matterclay minerals
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由於自然界中,積累於儲氣層中的天然氣氣體成份,和直接由源岩 (Source Rock) 產生的氣體成份,存在著相當大的差異,故可推測一般而言,天然氣的移棲 (Migration) 路徑越長時,其氣體成份受到二次分異 (Secondary Fractionation) 作用的可能性就越高。本研究便著重於探討天然氣在移棲過程中,流經黏土礦物(高嶺石及蒙脫石)和有機物(煤和湖相頁岩)等物質時,吸附 (Adsorption) 及擴散 (Diffusion) 作用對天然氣氣體成份變化的影響。研究的結果顯示,就選擇性吸附而言,黏土礦物和有機物,對分子量大之天然氣成份 (Wet hydrocarbon gases) 的吸附效果,較輕烴類如甲烷來的大許多;而就不同吸附劑而言,黏土礦物的吸附程度和選擇性吸附效果,遠低於有機物和活性碳。另一方面,就擴散作用而言,天然氣中輕烴類成份的擴散速率,較分子量大之氣體成份擴散速率快;且可利用擴散模擬之實驗數據,配合費克定律 (Fick’s Law) 求得天然氣中各氣體成份的擴散係數 (Diffusion Coefficient)。此實驗結果意味,天然氣移棲過程中,黏土礦物吸附作用造成成份分異的程度較差,然而,當天然氣流經富集大量有機物的路徑時,將會造成天然氣成份產生明顯的分異,故可映射到天然氣的初次移棲 (Primary Migration) 過程上,當天然氣由源岩生成,或流經含有大量有機物的生油層時,由於吸附效應,便可使其成份富集甲烷。另一方面,在天然氣的移棲過程中,由於擴散作用的影響,便可使其氣體成份產生相當大的改變,由於輕烴類的擴散速率較快,故可推測,當天然氣移棲路徑越長時,輕烴類成份由源岩移動到儲氣層中的機率也越高。
There is a conspicuous difference in compositions of natural gases between that accumulated in reservoir and that generated from source rocks. In general, the longer the migration pathway of natural gas, the more likely that any type of secondary fractionation of its composition can be significant. This study focuses on examining the influence of adsorption and diffusion on natural gas composition for clays and organic matter during migration. Our preliminary results show that clays (kaolinite and montmorillonite), organic matter (coal and lacustrine shale), and an activated carbon can preferentially adsorb wet hydrocarbon gases over methane but the adsorption level and selectivity are much lower for clays than for organic matter and activated carbon. This implies that the adsorption of natural gas in organic-rich pathway may result in a significant fractionation during migration whereas the extents of the fractionation due to adsorption on clays may be less. The diffusion experiments, on the other hand, show that methane has a higher diffusion rate than wet hydrocarbon gases, implying that dry hydrocarbon gas may migrate more efficiently from source rock to accumulation than wet hydrocarbon gases.
中文摘要i
英文摘要ii
目錄iii
表目錄vii
圖目錄ix
第一章 緒論 1
1-1 前言 1
1-2 研究動機及目的 2
1-3 前人研究 4
1-3-1 天然氣氣體組成 4
1-3-2 天然氣的生成 7
1-3-3 天然氣的移棲 9
1-3-4 天然氣的積累 10
1-3-5 吸附作用 10
1-3-6 擴散作用 12
第二章 實驗方法與材料 15
2-1 實驗模擬材料 15
2-1-1 天然氣氣樣 15
2-1-2 使用於吸附及擴散之材料 16
2-2 實驗器材 26
2-2-1 吸附作用 26
2-2-2 擴散作用 26
2-3 實驗方法 28
2-3-1 吸附作用 28
2-3-2 擴散作用 30
第三章 儀器設備 34
3-1 HP 6890 氣相層析儀 34
3-1-1 注射口 (Inlet) 36
3-1-2 層析管柱 (Column) 38
3-1-3 偵檢器 (Detector) 40
3-1-4 加熱爐 (Oven) 43
3-1-5 搭配氣體 45
3-2 檢量線 46
3-3 HP化學工作站 48
第四章 實驗資料與處理 49
4-1 吸附作用 49
4-1-1 吸附量的計算 49
4-1-2 活性碳吸附量 52
4-1-3 各吸附劑吸附量 58
4-2 擴散作用 59
4-2-1 費克定律 59
4-2-2 擴散係數 61
第五章 實驗結果與討論 66
5-1 吸附作用 66
5-1-1 各氣體分子選擇性吸附 66
5-1-2 各吸附劑吸附效果比較 68
5-1-3 各吸附劑對氣體分子選擇性吸附的比較69
5-1-4 溫度、吸附劑量及吸附質壓力對吸附量的影響72
5-1-5 吸附質壓力對吸附量的影響 74
5-1-6 吸附質飽和蒸汽壓影響 76
5-1-7 吸附量與吸附劑比表面積的比較 80
5-1-8 吸附劑表面積利用率比較 83
5-1-9 吸附質動力學模式比較 83
5-2 擴散作用 88
5-2-1 甲烷擴散量的變化 88
5-2-2 各氣體分子的選擇性擴散 89
5-2-3 各氣體分子間擴散量的比較 89
5-2-4 高嶺石及蒙脫石擴散量比較 91
5-2-5 費克定律與擴散係數 93
5-3 綜合討論 95
5-3-1 選擇性吸附 95
5-3-2 吸附量差異 95
5-3-3 影響吸附的變因 96
5-3-4 各氣體分子的選擇性擴散 97
5-3-5 岩樣孔隙率對擴散的影響 97
第六章 結論 99
6-1 實驗結果之結論 99
6-1-1 吸附作用 99
6-1-2 擴散作用 100
6-2 地質意義上的影響 101
第七章 未來研究方向 103
7-1 吸附質壓力實驗 103
7-2 水分對吸附的影響 103
7-3 擴散模擬實驗 104
7-4 同位素值的量測 104
參考文獻 105
附錄A 吸附模擬各吸附劑實驗數據 109
附錄B 費克定律的推導 119
附錄C 擴散模擬蒙脫石實驗數據 122
附錄D 動力學一級反應模式 124
附錄E 動力學二級反應模式 126
附錄F 動力學Elovich反應模式 128
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