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姓名 蘇思伃(Shih-Yu Su) 查詢紙本館藏 畢業系所 地球科學學系 論文名稱 二氧化碳封存場址之震測資料分析
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摘要(中) 近年來由於全球暖化帶來生態衝擊,針對控制溫室氣體二氧化碳,全球已達到共識。二氧化碳地質封存是被推薦鼓勵的方法,利用地質構造來封存二氧化碳。本研究利用高解析反射震測法調查可能的二氧化碳封存場址,探討場址地下細微構造。高解析反射震測法探測尺度及規模都較探油工業震測來的小,但使用的頻率較高,使得解析度可提高約3~5倍。利用此種特性來做二氧化碳封存場址探測可以得到非常好的結果,因一般封存深度都約在1~3公里處,而高解析反射震測可以獲得精細的地層構造,幫助評估儲藏量或作為封存移棲監測。
本研究利用王功一號井的地層資料,並藉由四條長距離跳躍銜接的震測剖面,將地層資料引入到北方15公里的彰濱工業區內。將彰濱工業區內有六條相互交叉分佈的高解析震測測線做密集比對,分析各剖面的地層深度分佈,從而建立起全測區地下地層分佈。以此為基礎,本研究更進一步分析測區六條測線上,沿測線連續的炸點剖面內的振幅隨支距變化情形(AVO分析),觀察不同地層其沿著測線的反射特性,探討二氧化碳儲集層可能的物理特性,並做為未來儲集後,偵測地層特性改變之比較資料。
本研究獲得以下結論:(1)經由測線交叉比對,計算得知測區的地層走向約北偏東8度,向東傾3.8度。未來若儲氣後,儲體會往西方海域方向移棲。(2) 測區測線交叉比對結果相當良好,表示震測信號足以信賴。震測剖面顯示地下地層平緩,無明顯構造存在,尤其絲毫沒有斷層痕跡。(3) P波反射係數相對於S波反射係數有大幅度下降時,表示有含氣砂岩的存在,但反之則無。測區大部分測線,P波反射係數變化和緩,而S波反射係數變化較大,可以推估在主要反射層之下層砂岩孔隙較大且含水。(4)未來若要再次進行AVO分析,在施測前評估可多提高CDP重合數來達到較好的AVO分析結果。在二氧化碳封存注入後,利用AVO分析可以更加快速的定位出二氧化碳移棲的路徑,達到監控的效果。摘要(英) The reduction of carbon dioxide emission to lessen the global warming has become an important international issue in recent years. Geological storage of carbon dioxide is recommended by IPCC to be an efficient and feasible way to handle the CO2 problem. In this study, we use high-resolution seismic reflection method to investigate possible CO2 storage sites. This high resolution seismic method has smaller scale comparing to those used in oil exploration industry. However, the resolution is relatively high and can detect much finer structures which are needed in the CCS site investigation. The resolution power is expected to be as small as 4m with a depth up to 3km.
A well at WangGong was used to provide the appropriate stratigraphic information of the region. By aligning four sequential seismic lines, we are able to extrapolate this well stratigraphic data to the Jhangbin area, 15 km north. The Jhangbin industrial area is our study area. Six cross-tied high-resolution seismic lines are distributed over the Jhangbin area to find detailed underground structures. On this basis, we further analyze these survey lines by the amplitude versus Offset (AVO) analysis. The P and S reflection coefficients are studied with the purpose to evaluate the porosity properties and to prepare baseline data for the future CO2 injection monitoring.
The following conclusions are obtained: (1) the structural layers are found to dip 3.8 degrees and strike 8 degrees east of north. This means that the CO2 will migrate toward the sea direction after storage. (2) the seismic lines possess very good ties, which guarantees excellent data quality of the survey. The layered structures are quite flat without any trace of structural disorder such as faults. (3) the P-wave reflection coefficient are quite smooth and, on the contrary, the S-wave reflection coefficient varies significantly. This indicates the porosities in the bottom sand layer are high, but filled with interlaced silt or water. (4) for the future AVO analysis, the fold number is suggested to increase to obtain better results. The AVO analysis can be more efficient to detect carbon dioxide and to monitor its migration after storage.關鍵字(中) ★ 二氧化碳封存
★ 振幅與支距分析
★ AVO關鍵字(英) 論文目次 文摘要 i
Abstract ii
誌謝 iii
目錄 iv
圖目錄 vi
表目錄 ix
第一章 緒論 1
1-1研究動機與目的 1
1-2二氧化碳地質封存模式與條件 2
1-3研究區域選擇 2
1-4本文內容 4
第二章 研究區域基本地質資料 8
2-1研究區域地層分布 8
2-2彰濱工業區震測資料 11
2.2.1反射震測原理 11
2.2.2彰濱二維震測資料 13
2-3震測資料比對與連結 13
2-4彰濱二維測線兩兩交叉比對 17
第三章 研究方法 51
3-1振幅隨支距變化 51
3-2 AVO資料處理流程 54
3-3計算目標層反射係數 56
3-4資料選取 57
第四章 震測資料分析結果 64
4-1沿各測線上之反射係數變化 64
4-2各測線結果 64
4.2.1王功測線結果 64
4.2.2彰濱A測線結果 65
4.2.3彰濱B測線結果 65
4.2.4彰濱C測線結果 66
4.2.5彰濱D測線結果 66
4.2.6彰濱E測線結果 66
4.2.7彰濱F測線結果 67
4-3測線間兩兩比對 67
4-4 本次研究可能的誤差來源 78
第五章 討論與結論 74
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