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Numerical Study on Flow Behavior of CO2 around Injected Well for Risk Assessment of Carbon Capture and Storage

机译:碳捕获和储存风险评估的CO2流动行为的数值研究

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For reliable risk assessment of carbon dioxide capture and storage (CCS), it is very important to predict the behavior of migration of injected CO2 in relation with time and space under the environment of underground. Especially, it is important to estimate the amount of storage and leakage of injected CO2 by way of both experimental and simulation study. In this study, we conducted experimental study about flow behavior of supercritical CO2 and water in porous media. The experiment was conducted to optimize relative permeability curves in the process of CO2 injection, and it resulted that 1) water mobility was relatively high compared with that of COj when grain size was large and 2) relative permeability to CO2 became higher under the condition below critical point of CO2. In addition, we interpreted transport phenomena of CO2 after shutoff of CO2 injection that 1) liquid CO2 easily migrated into geological formation in the cases of small grain size and low temperature and 2) dissolved CO2 migration due to groundwater flow contributed to the change of CO2 distribution under the condition of high water saturation. Then we considered some scenarios of leakage around injection well and migration of CO2 through numerical study. We constructed a simple strata model, which is consisted from a reservoir layer, a cap rock layer and upper layer. To discuss the effect of reservoir depth, we set a couple of model strata: (a) upper limit of reservoir-800 m level, thickness of cap rock is 200 m, and (b) upper limit of reservoir is-200 m, thickness of cap rock is 100 m. In addition, we set four combinations of horizontal and vertical permeability for reservoir: (a) 500 mD, 100 mD, (b) 50 mD, 10 mD, (c) 500 mD, 10 mD and (d) 50 mD, 100 mD. Porosity is uniformly set to 0.4. On the other hand, permeability value of upper layer is set to 1000 mD. The surface temperature is 20 deg.C and thermal gradient is 3 deg.C/100m. To analyze effect of fail in well casing and/or cementing, we defined a gap between the well casing and surrounding layer. The gap has thickness and different geological conditions with surrounding layers. For gap, we set various permeability and 2 scenarios of leakage: (a) crack covers cap rock level, (b) crack covers entire well depth from bottom to surface. The CO2 injection rate is 1 million ton/year and duration is 50 years. Using the constructed injection model, we carried out some simulation run using TOUGH2-CO2 by LANL. As the result we obtained the relation between injection volume and the amount of CO2 leakage through the gap model, and distribution of CO2 in the model layer. We considered the effect of each parameter on flow behavior of CO2 on gap model and quantified the amount of CO2 leakage. These results will be implemented to the risk assessment system GERAS-CO2 of AIST.
机译:对于对二氧化碳捕获和储存(CCS)的可靠风险评估,预测注射二氧化碳迁移与地下环境下的时间和空间的行为非常重要。特别是,通过实验和仿真研究估计注入的CO2的储存量和泄漏是重要的。在本研究中,我们对多孔介质中超临界CO2和水的流动进行了实验研究。进行实验以优化CO 2注射过程中的相对渗透性曲线,因此,当晶粒尺寸大并且2)在下面的情况下,水迁移率与COJ相对较高。在下面的情况下,CO 2的相对渗透性变得更高CO2的临界点。此外,我们解释了二氧化碳注射后的CO2的传输现象,其中1)液体CO2在小粒度和低温下容易迁移成地质形成,2)由于地下水流导致的溶解二氧化碳迁移有助于CO2的变化在高水饱和条件下的分布。然后我们考虑了一些关于喷射井泄漏的场景,并通过数值研究迁移CO2。我们构造了一种简单的地层模型,该模型包括储层层,盖岩层和上层。要讨论水库深度的影响,我们设定了几个模型地层:(a)贮存器-800米的上限,帽岩的厚度为200米,(b)储层的上限为-200 m,厚度帽岩是100米。此外,我们为储层设置了四种水平和垂直渗透性的组合:(a)500 md,100 md,(b)50 md,10 md,(c)500 md,10 md和(d)50 md,100 md 。孔隙率均匀地设定为0.4。另一方面,上层的渗透率设定为1000 md。表面温度为20℃,热梯度为3℃/ 100m。为了分析井壳和/或固井井中的失败的影响,我们在井壳和周围层之间定义了间隙。间隙具有厚度和不同地质条件,周围层。对于差距,我们设定了各种渗透率和2场景的泄漏:(a)裂缝盖盖岩水平,(b)裂纹覆盖从底部到表面的整个孔深度。二氧化碳注射率为100万吨/年,持续时间为50年。使用构造的注入模型,我们使用LANL进行了一些使用TOGP2-CO2的模拟运行。结果,我们通过间隙模型获得了注射体积与CO 2泄漏量之间的关系,以及模型层中的CO2的分布。我们考虑了每个参数对GAP模型CO2流动行为的影响,并量化了二氧化碳泄漏量。这些结果将实施到AICT的风险评估系统GERAS-CO2。

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