从含水层和油田钻探岩心数据预测CO2-水-岩:悬崖砂岩-常绿组CO2储层-封对

J. Pearce, A. L. Croix, F. Brink, V. Honari, S. González, A. Harfoush, J. Underschultz
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引用次数: 4

摘要

Surat盆地是澳大利亚陆上最有潜力的二氧化碳储存盆地之一。对崖岩组和常绿组作为未来的CO2储层-封存对的可行性进行了评价。在这里,我们将重点关注预测的二氧化碳-水-岩反应。这些预测依赖于钻芯的矿物和孔隙度数据。数据来自盆地北部和两个南部地区。北部地区的数据更为丰富。南部地区除穆尼油田外,岩心多,资料稀疏。从Moonie和盆地其他地区的存档井芯中收集了额外的钻孔岩芯样本。对岩心样品进行孔隙度、矿物和金属含量表征,建立地球化学模型,预测局部CO2-水-岩反应及其对储层结垢、孔隙度变化和CO2矿物捕获的潜在影响。在北部地区,我们的工作预测了悬崖砂岩的低反应性,在常绿组中有矿物捕获。穆尼油田的断崖砂岩样品与北部地区的井具有不同的矿物学特征。在这里,二氧化碳-水-岩预测表明,在较清洁的Moonie砂岩中,斜长石和钾长石向高岭石、玉玉石和铁白云石发生了轻微的变化,在富含粘土的砂岩中,蒙脱石也发生了额外的降水。由于方解石或菱铁矿胶结物的溶解作用,地层水的pH值被缓冲在5 ~ 6之间。岩心样品还显示了以前的天然CO2和热液蚀变、破碎的石英颗粒和以碳酸盐为捕获物的裂缝充填物的证据。这种类型的自然模拟数据对于验证长期预测至关重要。在最具CO2注入和封存潜力的Surat盆地南部和中部地区,未来仍需要新的岩心和数据。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
CO2-water-rock predictions from aquifer and oil field drill core data: The Precipice Sandstone-Evergreen Formation CO2 storage reservoir-seal pair
Summary The Surat Basin is one of the most prospective onshore basins in Australia for CO2 storage. The Precipice Sandstone and Evergreen Formation have been appraised for their feasibility as a future CO2 storage reservoir-seal pair. Here we will focus on predicted CO2-water-rock reactions. These predictions rely on mineral and porosity data from drill core. Data were obtained from northern and two southern regions of the Basin. The northern region was more data rich. The southern region is more well core and data sparse with the exception of the Moonie oil Field. Additional drill core samples were collected from archived well core of Moonie and other parts of the basin. The core samples were characterised for porosity, mineral, and metal content to build geochemical models to predict local CO2-water-rock reactions and their potential effect on reservoir scaling, changes to porosity and mineral trapping of CO2. For the northern region, our work has predicted low reactivity of the Precipice Sandstone, with mineral trapping in the Evergreen Formation. The Precipice Sandstone sampled in the Moonie field has different mineralogical characteristics to wells in the Northern region. Here, CO2-water-rock predictions indicate minor alteration of plagioclase and K-feldspar to kaolinite, chalcedony and ankerite in cleaner Moonie sandstones, with additionally precipitation of smectite in clay rich sands. Formation water pH was buffered between 5 and 6 by dissolution of calcite or siderite cements. Sampled core has also shown evidence of previous natural CO2 and hydrothermal fluid alteration, fractured quartz grains, and fracture fills with mineral trapping as carbonates. This type of natural analogue data is vital to validate long term predictions. New drill core and data are still required in future for the southern and central Surat Basin region which is most prospective for CO2 injection and storage.
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