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Experimental and Numerical Investigation of the Hydromechanical Response of Low Permeable Rocks during Injection of supercritical CO2

机译:超临界二氧化碳注入过程中低渗透岩石的水力响应实验和数值研究

摘要

In designing carbon capture and geological storage, the long-term behavior of stored CO2 in the underground geological formation is a crucial issue to be carefully considered. This is because of the fact that the injection of CO2 into the formation would impact rock formation integrity, reactivating pre-existing fractures and reopening seal that eventually lead to potential CO2 leakage to the underlying groundwater containing layers and the surface. Therefore, the deformation of the reservoir rock during injection of supercritical CO2 needs to be well understood and defined while designing the project. udIn this paper, we developed an experimental design using a newly developed flow pump permeability test to measure the change of strain and stress on the Ainoura sandstone cores under the injection of supercritical CO2. The experiment was set up to reproduce the similar condition of deep underground reservoir with 20 MPa confining pressure, 10 MPa pore pressure, 35??C temperature and 3 ??l/min CO2 injection rate. As CO2 was injected to the specimen, the hydraulic pressure increased and generated a stress alteration. The strain in the core was monitored. The injection was halted at 15.3 MPa hydraulic pressures over the period of 565.9 hours since the hydraulic pressure can reach the confining pressure applied on the core and this may break the silicon on the rubber sleeves covering the core. Therefore, in order to model the hydromechanical response of the core during the injection as well as to predict the strain propagated beyond the injection period measured in the experiment, a numerical investigation using coupling hydromechanical simulation was conducted. In this exercise, we employed a two phase flow reservoir simulator of TOUGH2 (ECO2N) coupled with rock mechanics computation of FLAC3D. A core specimen, with the rock properties and initial conditions similar to the experimental data, was generated and supercritical CO2 injection with a constant rate of 3.56??10-8 kg/s was simulated. It was observed that, the increased hydraulic pressure and strain shown in the numerical simulation have well agreement with the experimental result. The results also indicated that, during injection, the hydraulic pressure on the core increased transiently, and became constant at almost 60 MPa over the period of 5833 hours. The core specimen deformed elastically due to the increase of pore pressure caused by injection. The deformation of the specimen would not propagate failure even if the pore pressure exceeds the confining pressure applied on it. The results confirmed that the injection of supercritical CO2 into low permeable rocks has considerable effects on the integrity of low permeable rocks even at low flow rates.
机译:在设计碳捕获和地质封存时,在地下地质层中封存的CO2的长期行为是需要仔细考虑的关键问题。这是因为以下事实:将CO2注入地层会影响岩层的完整性,重新激活先前存在的裂缝并重新打开密封层,最终导致潜在的CO2泄漏到下面的含地下水层和地表。因此,在设计该项目时,需要对超临界CO2注入过程中储层岩石的变形进行很好的理解和定义。 ud在本文中,我们使用新开发的流量泵渗透性测试开发了一个实验设计,以测量超临界CO2注入下Ainoura砂岩岩心的应变和应力变化。进行该实验是为了再现深部地下油藏的类似条件,即20 MPa的围压,10 MPa的孔隙压力,35℃的温度和3升/分钟的CO2注入速率。随着向样品中注入CO2,液压压力增加并产生应力变化。监测芯中的应变。在565.9小时内,在15.3 MPa的液压压力下停止了注射,因为该液压压力可以达到施加在芯上的限制压力,这可能会破坏覆盖芯的橡胶套管上的硅。因此,为了模拟注入过程中岩心的流体力学响应,并预测在实验中测量的注入周期之外传播的应变,使用耦合流体力学模拟进行了数值研究。在本练习中,我们使用了TOUGH2(ECO2N)的两相流储层模拟器以及FLAC3D的岩石力学计算。生成了一个岩样,其岩石性质和初始条件与实验数据相似,并模拟了以3.56×10-8 kg / s的恒定速率注入超临界CO2。观察到,数值模拟中显示的增加的液压和应变与实验结果吻合良好。结果还表明,在注入过程中,岩心上的液压瞬时升高,并在5833小时的时间内保持恒定,几乎为60 MPa。由于注入引起的孔隙压力增加,岩心样品发生弹性变形。即使孔隙压力超过施加在其上的限制压力,样品的变形也不会传播破坏。结果证实,即使在低流速下,向低渗透岩石中注入超临界CO2对低渗透岩石的完整性也有相当大的影响。

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