International Journal of Greenhouse Gas Control ( IF 4.6 ) Pub Date : 2020-10-12 , DOI: 10.1016/j.ijggc.2020.103164 Mahmoud Hefny , ChaoZhong Qin , Martin O. Saar , Anozie Ebigbo
Depleted oil fields in the Gulf of Suez (Egypt) can serve as geothermal reservoirs for power generation using a CO-Plume Geothermal (CPG) system, while geologically sequestering CO. This entails the injection of a substantial amount of CO into the highly permeable brine-saturated Nubian Sandstone. Numerical models of two-phase flow processes are indispensable for predicting the CO-plume migration at a representative geological scale. Such models require reliable constitutive relationships, including relative permeability and capillary pressure curves. In this study, quasi-static pore-network modelling has been used to simulate the equilibrium positions of fluid–fluid interfaces, and thus determine the capillary pressure and relative permeability curves.
Three-dimensional images with a voxel size of 0.65 of a Nubian Sandstone rock sample have been obtained using Synchrotron Radiation X-ray Tomographic Microscopy. From the images, topological properties of pores/throats were constructed. Using a pore-network model, we performed a sequential primary drainage, main imbibition cycle of quasi-static invasion in order to quantify (1) the CO and brine relative permeability curves, (2) the effect of initial wetting-phase saturation (i.e. the saturation at the point of reversal from drainage to imbibition) on the residual-trapping potential, and (3) study the relative permeability-saturation hysteresis. The results improve our understanding of the potential magnitude of capillary trapping in Nubian Sandstone, essential for future field-scale simulations.
中文翻译:
基于同步加速器的努比亚砂岩两相流孔网模拟及其对二氧化碳毛细管捕集的意义
苏伊士湾(埃及)的枯竭油田可作为地热储层,利用二氧化碳发电-羽状地热(CPG)系统,同时地质隔离CO。这需要注入大量的CO进入高渗透性饱和盐水的努比亚砂岩。两相流过程的数值模型对于预测CO必不可少-有代表性的地质规模的泥质迁移。这种模型需要可靠的本构关系,包括相对渗透率和毛细管压力曲线。在这项研究中,准静态孔隙网络模型已用于模拟流体-流体界面的平衡位置,从而确定毛细管压力和相对渗透率曲线。
三维图像尺寸为0.65的三维图像 使用同步辐射X射线断层扫描显微镜已经获得了努比亚砂岩岩石样品的一部分。从图像中,构造出孔/喉的拓扑特性。使用孔隙网络模型,我们进行了准静态入侵的顺序主要排水,主要吸水周期,以量化(1)CO和盐水相对渗透率曲线,(2)初始润湿相饱和度(即从排水到吸水的反转点处的饱和度)对剩余捕集势的影响,以及(3)研究相对渗透率-饱和滞后。结果提高了我们对努比亚砂岩中毛细血管捕集潜力的认识,这对于将来的现场规模模拟至关重要。