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| DC 欄位 | 值 | 語言 |
|---|---|---|
| dc.contributor.advisor | 劉雅瑄 | zh_TW |
| dc.contributor.advisor | Sofia Ya-Hsuan Liou | en |
| dc.contributor.author | 徐郁雯 | zh_TW |
| dc.contributor.author | Yu-Wen Hsu | en |
| dc.date.accessioned | 2026-03-05T16:32:36Z | - |
| dc.date.available | 2026-03-06 | - |
| dc.date.copyright | 2026-03-05 | - |
| dc.date.issued | 2026 | - |
| dc.date.submitted | 2026-01-31 | - |
| dc.identifier.citation | 廖韡智、李健平、蘇俊陽(2023)。澳洲西北海域羅巴克盆地探勘標的類型研究。石油季刊，59(2)，37-47。
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| dc.identifier.uri | http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/101894 | - |
| dc.description.abstract | 隨著溫室效應加劇，尋找合適的地質封存場址已成為全球關注焦點。鑒於澳洲碳封存政策開放及我國於澳洲礦區取得探勘權之現況，本研究針對澳洲 Roebuck 盆地進行鹽水層碳封存之模擬研究。透過鄰近盆地的儲集層類比，選定中侏羅紀三角洲沉積之 Depuch Formation 為儲集層，其中南側 Bedout 次盆地具理想封存深度，並由早白堊紀泥岩層作為區域性蓋層。
由於缺乏足夠的岩石物理資料，本研究將 Depuch Formation 細分為 20 個子層，利用七條二維地質剖面透過 PetroMod 進行盆地模擬。預測結果顯示，扣除深度大於 3200 公尺區域後，儲層平均厚度為 442.4 m、平均孔隙率 22.6 %、平均溫度 72.7 ℃、平均壓力 21.1 MPa。在儲存效率因子 2 % (P50) 的假設下，估算最終儲存資源量達 361.3 億噸。 在注入模擬方面，針對 JN87-20 剖面之儲層進行單井注入情境分析，結果顯示在每年注入 25 萬、50 萬及 100 萬噸二氧化碳且持續 50 年的情境下，超壓及羽流最終均未觸及儲層頂部。然而，當年注入量達 100 萬噸時，局部壓力增加可能導致岩石破裂，進而影響儲層穩定性，且大部分二氧化碳仍處於自由態，危險性較高，此結果可能與模擬的滲透率結果有關，推估每年 50 萬噸為目前該模型之安全極限。另外，雙井模擬結果證實井距越近壓力疊加效應越顯著，當井距達 15 公里以上時方能有效降低壓力干擾。 本研究以初步探勘資訊建立模型，尚可透過探勘資料來持續調整模型獲得更符合實際狀況的結果。將碳封存模擬應用至台灣碳封存開發中，會面臨到地質條件更加複雜的狀況，應針對地質探勘要有更深入的了解以作為建立及校正模型的參數設定。 | zh_TW |
| dc.description.abstract | As global warming intensifies, identifying suitable geological storage sites has become a global priority. Given Australia's proactive carbon storage policies and Taiwan's acquisition of exploration rights in Australian mining areas, this study conducts a simulation of saline aquifer carbon sequestration in the Roebuck Basin, Australia. Through reservoir analogy with adjacent basins, the Middle Jurassic deltaic Depuch Formation was selected as the target reservoir. The Bedout Sub-basin in the south provides ideal storage depth, while Early Cretaceous mudstone layers serve as regional seals.
Due to limited petrophysical data, the Depuch Formation was subdivided into 20 sub-layers, and basin modeling was performed using PetroMod across seven 2D geological sections. Results indicate that after excluding areas deeper than 3200 m, the predicted average reservoir thickness is 442.4 m, with an average porosity of 22.6%, temperature of 72.7°C, and pressure of 21.1 MPa. Assuming a storage efficiency factor (E) of 2% (P50), the total storage resource is estimated at 36.13 billion tonnes. Regarding injection simulation, single-well scenarios were analyzed for the JN87-20 section. Results show that after injecting 250,000, 500,000, and 1,000,000 tonnes of CO2 per year for 50 years, the overpressure and plumes did not reach the top of the seal. However, at an annual rate of 1,000,000 tonnes, localized pressure increases could lead to rock fracturing, potentially compromising reservoir stability. Furthermore, as most CO2 remains in a free state, posing higher risks potentially linked to simulated permeability, 500,000 tonnes per year is estimated as the safety limit for this model. Additionally, dual-well simulations confirm that closer well spacing intensifies pressure interference; a minimum spacing of 15 km is required to effectively mitigate these effects. This study demonstrates the feasibility of establishing models using preliminary exploration data, which can be continuously refined as further data becomes available. Applying carbon sequestration simulations to Taiwan’s development involves navigating more complex geological conditions. Consequently, a deeper understanding of geological exploration is essential to provide accurate parameters for model construction and calibration. | en |
| dc.description.provenance | Submitted by admin ntu (admin@lib.ntu.edu.tw) on 2026-03-05T16:32:36Z No. of bitstreams: 0 | en |
| dc.description.provenance | Made available in DSpace on 2026-03-05T16:32:36Z (GMT). No. of bitstreams: 0 | en |
| dc.description.tableofcontents | 口試委員審定書 i
誌 謝 ii 摘 要 iii Abstract iv 目 次 vi 圖 次 viii 表 次 xii 第一章、緒論 1 1.1、研究動機 1 1.2、研究目的 3 第二章、文獻回顧 4 2.1、碳捕集與封存(CCS)介紹 4 2.2、碳封存的方式 8 2.2.1、地質封存 8 2.2.2、海洋封存 9 2.2.3、礦化封存 10 2.3、碳封存探勘技術簡介 11 2.3.1、碳封存場址分析 11 2.3.2、模擬 12 2.3.3、風險評估作業 13 2.3.4、監測、驗證和會計核算作業 14 2.3.5、鹽水層碳封存儲存容量評估 15 2.4、碳封存模擬的發展 16 2.5、碳封存模擬技術 19 2.5.1、模擬空間尺度 19 2.5.2、重要參數條件 21 2.5.3、流體移棲方法 23 2.6、國際碳封存場址簡介 25 2.6.1、挪威Sleipner計畫 25 2.6.2、美國IL-ICCS計畫 27 2.6.3、英國East Coast Cluster計畫 28 2.6.4、日本苫小牧計畫 29 2.6.5、冰島Carbfix計畫 30 2.6.6、澳洲Gorgon計畫 31 2.7、澳洲碳封存發展與價值鏈 33 第三章、研究方法 37 3.1、研究架構 37 3.2、研究材料 37 3.2.1、資料來源 37 3.2.2、目標區域地質 38 3.2.3、模擬軟體介紹 44 3.3、研究方法 45 3.3.1、評估儲集層 45 3.3.2、二維地質模型建立 45 3.3.3、二氧化碳封存量評估 50 3.3.4、二氧化碳參數及注入條件設定 50 第四章、結果與討論 52 4.1、Roebuck盆地儲集層初步評估 52 4.1.1、鄰近盆地的碳封存儲集層彙整及Roebuck盆地儲集層的挑選 52 4.1.2、Roebuck盆地儲集層地質資料統整 57 4.1.3、Roebuck盆地Depuch Formation的岩石特性 61 4.2、Roebuck盆地二維地質模型建立 65 4.2.1、震測資料 65 4.2.2、二維地質模型建立 70 4.2.3、Bedout次盆地地質模擬初步結果 76 4.2.4、Depuch Formation儲集層碳封存量評估 83 4.3、灌注模擬 85 4.3.1、流體移棲方法 85 4.3.2、單口井注入模擬結果 92 4.3.3、兩口井模擬結果 104 4.4、模擬成果綜述 112 4.4.1、調整模擬結果的必要條件 112 4.4.2、臺灣地質封存之關鍵考量 113 第五章、結論 114 參考文獻 116 附錄 126 1.鑽井鏡煤素反射率、溫度、孔隙率 126 2.各剖面模擬結果 131 | - |
| dc.language.iso | zh_TW | - |
| dc.subject | 澳洲西北海域 | - |
| dc.subject | Roebuck 盆地 | - |
| dc.subject | 碳封存 | - |
| dc.subject | 儲存量評估 | - |
| dc.subject | 注入模擬 | - |
| dc.subject | Northwest Australia | - |
| dc.subject | Roebuck Basin | - |
| dc.subject | Carbon Capture and Storage (CCS) | - |
| dc.subject | Capacity Assessment | - |
| dc.subject | Injection Simulation | - |
| dc.title | 鹽水層碳封存盆地模擬研究 - 以澳洲西北海域 Roebuck盆地為例 | zh_TW |
| dc.title | Basin Modeling Application for Saline Aquifer CO2 Storage: A Case Study of the Roebuck Basin, Offshore Northwest Australia | en |
| dc.type | Thesis | - |
| dc.date.schoolyear | 114-1 | - |
| dc.description.degree | 碩士 | - |
| dc.contributor.oralexamcommittee | 郭陳澔;郭家瑋 | zh_TW |
| dc.contributor.oralexamcommittee | Hao Kuo-Chen;Chia-Wei Kuo | en |
| dc.subject.keyword | 澳洲西北海域,Roebuck 盆地碳封存儲存量評估注入模擬 | zh_TW |
| dc.subject.keyword | Northwest Australia,Roebuck BasinCarbon Capture and Storage (CCS)Capacity AssessmentInjection Simulation | en |
| dc.relation.page | 140 | - |
| dc.identifier.doi | 10.6342/NTU202600373 | - |
| dc.rights.note | 同意授權(限校園內公開) | - |
| dc.date.accepted | 2026-02-03 | - |
| dc.contributor.author-college | 理學院 | - |
| dc.contributor.author-dept | 地質科學系 | - |
| dc.date.embargo-lift | 2031-01-29 | - |
| 顯示於系所單位： | 地質科學系 | |
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