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Large-scale numerical simulation of CO_2 geologic storage and its impact on regional groundwater flow: A hypothetical case study at Tokyo Bay, Japan

机译:CO_2地质储存的大规模数值模拟及其对区域地下水流量的影响:日本东京湾的假设案例研究

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With the help of massively parallelized computing techniques, a comprehensive, large-scale numerical simulation of CO_2 geologic storage that predicts not only CO_2 migration but also its impact on regional groundwater flow was performed. As a case study, a hypothetical industrial-scale injection of CO_2 at the Tokyo Bay, surrounded by the most industrialized area in Japan, was considered. In the simulation, CO_2 is injected into a storage aquifer at about 1km depths under the Tokyo Bay from 10 wells with a total rate of 10 million tons/year for 100 years. A regional hydrogeological model with an area of about 60km × 70km around the Tokyo Bay was discretized into approximately 10 million gridblocks. To solve the high-resolution model efficiently, we used a parallelized multiphase flow simulator TOUGH2-MP/ECO2N on a highest performance supercomputer in Japan, the Earth Simulator (5120 CPUs). The results suggest that even if containment of CO_2 plume is ensured, pressure buildup in the order of tens of meters can occur in shallow confined layers of extensive regions including urban inlands.
机译:借助大规模平行化的计算技术,综合,大规模的CO_2地质储存数值模拟,其不仅预测CO_2迁移,而且还进行了对区域地下水流的影响。作为一个案例研究,考虑了东京湾的假设工业规模注射,被日本最工业化地区包围。在模拟中,CO_2注入到东京湾下的大约1km深度的储存含水层,从10孔井下,总速度为1000万吨/年。在东京湾周围区域的区域水文模型,面积约60km×70km,被离散化为大约1000万格栅。为了有效地解决高分辨率模型,我们在日本最高性能超级计算机上使用了并行化的多相流模拟器韧带2-MP / ECO2N,地球模拟器(5120 CPU)。结果表明,即使确保了CO_2羽流的遏制,大约数十米的压力累积也可以在包括城市内陆的广泛地区的浅层限制层中发生。

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