埃及苏伊西湾Belayim地层未来潜在二氧化碳储存结构评估

0 ENERGY & FUELS
Heba Atef , Claire Bossennec , Jeroen van der Vaart , Ingo Sass
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引用次数: 0

摘要

埃及的目标是到2030年将二氧化碳排放量减少9070万吨,其中65%的减少量,相当于170万吨二氧化碳当量,目标是在石油和天然气行业。为了确定一个油田是否可以被视为二氧化碳储存地点,地质特征是一个至关重要的标准。因此,本研究的重点是评估Shoab Ali油田Belayim储层枯竭后的结构相容性,以备将来作为二氧化碳储存场所使用。该研究利用二维地震线和井眼数据为目标单元构建三维结构模型。圈定了3条与Belayim组相交的断层,均向北西-东南方向倾斜,具有正滑性。并置图和页岩泥比(SGR)算法两种断层封闭性分析方法被用于识别沿断层面的潜在泄漏路径。F2断层与南Gharib组盐层并置,显示出较强的流体圈闭潜力。相比之下,断裂F1和断裂F3则表现出更大的泄漏潜力,这是由于Belayim组(Hammam Faraun段)顶部的碳酸盐自并并。虽然断层1和断层3的SGR值高于断层2,但Belayim组深度图显示F1和F2断层定义了一个断层边界圈闭,均倾向于NW-SE方向。净截流容积估计在0.23 × 108 m3至0.3 × 108 m3之间。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Structural assessment of the Belayim formation for future potential CO2 storage, Gulf of Suez, Egypt
Egypt aims to reduce CO2 emissions by 90.7 million metric tons by 2030, with 65 % of this reduction, equivalent to 1.7 million metric tons of CO2 equivalent, targeted within the oil and gas sector. To determine whether an oil field can be considered a CO2 storage site, geological characteristics are a crucial criterion. Therefore, this research focuses on evaluating the structural compatibility of the Belayim reservoir in the Shoab Ali oil field after its depletion for potential future use as a CO2 storage site. The study utilized 2D seismic lines as well as borehole data to construct a 3D structural model for the targeted units. Three faults were delineated intersecting the Belayim Formation, all inclined in the NW-SE direction with normal slip. Two methods of fault seal analysis, Juxtaposition diagrams and the Shale Gouge Ratio (SGR) algorithm, were applied to identify potential leakage pathways along the fault planes. Fault F2 demonstrates strong fluid trapping potential due to its juxtaposition with the salt of the South Gharib Formation. In contrast, Faults F1 and F3 exhibit greater potential for leakage, attributed to the carbonate self-juxtaposition at the top of the Belayim Formation (Hammam Faraun Member). While Fault 1 and Fault 3 exhibit higher SGR values compared to Fault 2, the depth map of the Belayim Formation reveals a fault-bounded trap defined by Faults F1 and F2, both dipping in the NW-SE direction. The net closure volume is estimated to range from 0.23 × 108 m3 to 0.3 × 108 m3.
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