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Numerical investigation of the influence of interaction between wellbore flow and lateral reservoir flow on CO2 geological sequestration

机译:井筒流与储层横向流相互作用对CO2地质固存影响的数值研究

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A wellbore and a combined reservoir system are essential for the management of subsurface fluid resources and the geological storage of CO2. But the interaction between wellbore and reservoir flow is often neglected in studies of the combined system. A 2D radial model, considering the interaction of wellbore and reservoir flow was developed to investigate its impact on CO2 geological sequestration. The mass, energy and momentum equations for the wellbore and reservoir were solved using T2Well/ECO2N. The gas flow rate of the reservoir and wellbore are predicted, and the impact of interaction between wellbore and reservoir flow on the CO2 plume distribution and evolution was investigated. Furthermore, the influence of the CO2 injection rate, reservoir properties and salinity on the distribution of wellbore and reservoir flow was also explored. Interaction between the wellbore and reservoir flows determines the distribution of the reservoir gas flow rate which combined with layer thickness and porosity controls the horizontal distribution and evolution of the CO2 plume. The CO2 wellhead injection rate and reservoir properties ( including lateral transmissivity, permeability) are vital factors influencing wellbore and reservoir flows. However, reservoir salinity has little effect on the interaction between the wellbore flow and the reservoir flow, but increased reservoir salinity can accelerate the horizontal migration of CO2. The results of this study may help to change the widely held opinion that the distribution of the injected CO2 among the individual layers is simply proportional to their transmissivity, and thereby enhance our understanding of CO2 evolution beneath the surface and provide theoretical support for safe and potential geological storage of CO2.
机译:井筒和组合的储层系统对于地下流体资源的管理和二氧化碳的地质封存至关重要。但是,在组合系统的研究中,井眼与储层流之间的相互作用常常被忽略。考虑到井筒和储层流动的相互作用,建立了二维径向模型,以研究其对CO2地质封存的影响。使用T2Well / ECO2N求解了井筒和储层的质量,能量和动量方程。预测了储层和井筒的气体流速,并研究了井筒和储层流之间的相互作用对CO 2羽流分布和演化的影响。此外,还探讨了二氧化碳注入速率,储层性质和盐度对井筒分布和储层流量的影响。井筒和储层流之间的相互作用决定了储层气体流量的分布,而储层瓦斯流量的分布与层厚和孔隙度相结合,控制了CO2羽流的水平分布和演化。 CO2井口注入速率和储层特性(包括横向渗透率,渗透率)是影响井筒和储层流量的重要因素。但是,储层盐度对井眼流和储层流之间的相互作用影响很小,但是增加的储层盐度可以加速CO2的水平运移。这项研究的结果可能有助于改变人们普遍认为的观点:注入的二氧化碳在各个层之间的分布与它们的透射率成正比,从而加深了我们对地下二氧化碳排放的理解,并为安全和潜在的发展提供了理论支持。二氧化碳的地质封存。

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