二氧化碳封存试验场上方的三维地质模型和地下水流动模型

E. Carlock, E. Peterson, D. Malone
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引用次数: 3

摘要

随着气温上升和气候变化成为一个日益重要的问题,地质封存二氧化碳(CO2)是减少温室气体排放的可行方案。作为伊利诺斯州迪凯特市二氧化碳封存可行性研究的一部分,我们完成了地下三维建模和地下水流动建模。迪凯特阿彻丹尼尔斯米德兰公司乙醇工厂(ADM)是一个深盐油藏二氧化碳封存项目的注入点。海燕被成功地用于模拟该地区的冰川沉积物。三维地质模型显示了地表的皮奥里亚淤泥、韦德龙组和卡霍基亚组,韦德龙组支撑着迪凯特湖东西两岸的陡坡。地下水流动模型勾勒出了当地地下水分水岭的位置,并显示从注入地点流出的水流将流向迪凯特湖,并在80天内到达该湖。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Three-Dimensional Geologic Modeling and Groundwater Flow Modeling above a CO2 Sequestration Test Site
As temperatures rise and climate change becomes an increasingly important issue, geologic carbon dioxide (CO2) sequestration is a viable solution for reducing greenhouse gas emissions. Subsurface 3-D modeling and groundwater flow modeling were completed as a component of a CO2 sequestration feasibility study in the city of Decatur, Illinois. The Decatur Archer Daniels Midland Company Ethanol Plant (ADM) serves as the injection site for a CO2 sequestration project within a deep saline reservoir. Petrel was successfully used to model the glacial deposits in the area. The 3-D geologic model shows the Peoria Silt, Wedron Formation, and Cahokia Formation at the surface with the Wedron Formation holding up the steep slopes along the east and west banks of Lake Decatur. The groundwater flow model outlined the location of a local groundwater divide and showed flow from the injection site would flow towards Lake Decatur, reaching the lake in 80 days.
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