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Porosity and Permeability Alteration of Carbonates by CO_2-Enriched Brine Injection

机译:CO_2富含盐水注射液体孔隙率和渗透性改变碳酸盐

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Some carbonate reservoirs are known for their high CO_2 content in oil. One possibility to handle this gas without environmental problems is to reinject it into the reservoir. Injection of carbonated water has been drawing attention because it is an advantageous technique when compared to gaseous CO_2 injection, due to its improvement in mobility in the reservoir. The objective of this study is to evaluate the phenomenon of dissolution and precipitation during carbonated water injection in carbonate rocks. These effects are identified by analyzing the porosity variations through X-ray computer tomography images and permeability profile, determined indirectly by pressure transducers that measured the differential pressure by the fluid at the inlet and outlet of the core holders. The Coreflooding test were carried out with two core holders in series to represent a near region at the reservoir by the injection of brine saturated with 25% of CO_2 in reservoir samples, composed of dolomite, calcite and clay. The test were performed using the following reservoir conditions of 8,500 psi at 70°C. Based on the experimental data provided by Computed Tomography (CT) images, it can be seen that the core porosity increases or decrease during carbonated water injection due to coexistence of dissolution (increase of porosity) and precipitation (decrease of porosity) along the samples. These phenomena are observed in regions with high heterogeneity in porosity. In addition, the mineralogy of the cores is composed by three minerals, which influence in the capacity of reaction with carbonated water. For the experiment, the core placed in the core holder one presented a porosity increase and the second one decreased. On the other hand, the permeability showed a significant increase for both cores, it is believed that, the injection promoted a preferential way flow (wormhole) that affected considerably the permeability of the rock. The novelty of the investigation is that the experimen
机译:一些碳酸盐储存器以其油的高CO_2含量已知。在没有环境问题的情况下处理这种气体的一种可能是将其重新进入储层。由于其在储存器中的迁移率的改善,注入碳酸水的注射已经介绍了注意力,因为它是与气态CO_2注射相比的有利技术。本研究的目的是评估碳酸盐岩中碳酸注射液中溶解和沉淀的现象。通过通过X射线计算机断层扫描图像和渗透率分析来识别这些效果,通过压力换能器间接确定,该压力传感器通过芯支架的入口和出口处的流体测量差压。 CorePlood试验用两个芯保持器串联进行,以在储库中注射剩余的盐水在储存器样本中的25%的CO_2,由白云石,方解石和粘土中的含有25%的盐水来表示储层的附近区域。使用以下70℃的下列储层条件为8,500psi的试验。基于由计算机断层摄影(CT)图像提供的实验数据,可以看出,由于沿着样品的溶解(孔隙率的增加)和沉淀(孔隙率的增加)和沉淀(孔隙率降低),核心孔隙率在碳酸水浸中增加或减少。在孔隙率高的具有高异质性的区域中观察到这些现象。此外,芯的矿物学由三种矿物质组成,其影响与碳酸水的反应能力影响。对于实验,放置在芯支架中的芯呈现孔隙率增加,第二个减少。另一方面,渗透性显示出对两个核的显着增加,据信,注射促进了影响岩石的渗透率的流动(虫洞)。调查的新颖性是实验

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