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Determination of stress dependent relative permeability of low permeable rocks injected with supercritical CO2

机译:超临界CO 2注入低渗透岩石应力相关相对渗透率的确定

摘要

In this paper, we propose a numerical approach to determine CO2-water relative permeability from the experimental test of the injection of supercritical CO2 into low permeable rock. The theoretical analysis was modified in order to incorporate two phase drainage displacement while poroelastic geomechanical analysis was employed to quantify the stress-strain as well as the porosity-permeability that altered during the injection. The applicability of the numerical analysis was examined in the injection of supercritical CO2 with 3 ??l/min flow rate into a cored Ainoura sandstone saturated by water within initial condition of 10 MPa pore pressure, 20 MPa confining pressure, and 35??C temperature. During injection, the hydraulic pressures in the upstream and downstream of the core including its longitudinal and lateral strains were measured. The experimental results showed that CO2 injection generates an increase in hydraulic pressure across the core up to 16.93 MPa, and the increase in volumetric strain by 0.7%. As a consequence, porosity and permeability changes by a factor of 1.22 and 2.03 of those initial values were observed, respectively. It was also found that CO2 and water relative permeability values yielded lower values by 25% and 65%, respectively, when geomechanical effects on the hydraulic behavior are considered . The results suggest that the determination of relative permeability by core scale measurement needs to accommodate both hydraulic and geomechanical effects, especially in case of low permeable rocks.
机译:在本文中,我们提出了一种通过将超临界CO2注入低渗透性岩石的试验来确定CO2与水的相对渗透率的数值方法。修改了理论分析,以便纳入两相排水位移,而采用多孔弹性岩土力学分析来量化注入过程中变化的应力应变以及孔隙度。在初始压力​​为10 MPa孔隙压力,20 MPa围压和35℃C的初始条件下,以3升/分钟的流速将超临界CO2注入水饱和的芯Ainoura砂岩中,研究了数值分析的适用性。温度。在注射期间,测量了芯的上游和下游的液压,包括其纵向和横向应变。实验结果表明,CO2注入使整个岩心的水压增加到16.93 MPa,体积应变增加0.7%。结果,观察到孔隙率和渗透率的变化分别是这些初始值的1.22倍和2.03倍。还发现,在考虑水力行为的地质力学影响时,CO2和水的相对渗透率值分别降低了25%和65%。结果表明,通过岩心尺度测量确定相对渗透率需要兼顾水力和岩土力学的影响,特别是在低渗透性岩石的情况下。

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