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Fluid/Rock Interactions During CO_2 Sequestration in Deep Saline Carbonate Aquifers: Laboratory and Modeling Studies

机译:深盐碳酸盐岩含水层中CO_2封存过程中的流体/岩石相互作用:实验室和模型研究

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摘要

Carbon dioxide (CO_2) injection in carbonate formations causes a reduction in the well injectivity caused by precipitation of the reaction products between CO_2, rock, and brine. The precipitated material includes sulfate and carbonate scales. The homogeneity of the carbonate rock, in terms of mineralogy and rock structure, is an important factor that affects the behavior of permeability changes during CO_2 injection. Limestone rocks that were tested in this study included homogeneous Pink Desert limestone and Austin chalk, which were mainly calcite; heterogeneous Silurian dolomite (composed of 98 wt% carbonate minerals and 2 wt% silicate minerals); and heterogeneous Indiana limestone, which was mainly calcite and had vugs. Experiments were conducted to compare the permeability loss between these rocks during corefloods. CO_2 was injected with the water-alternating-gas (WAG) technique. Different brines were examined, including sulfate-bearing seawater and no-sulfate sea-water. The experiments were run at a backpressure of 1,300 psi, a temperature of 200°F, and an injection rate of 5 cm~3/min. A compositional-simulator tool (CMG-GEM) was used to predict the Carman-Kozeny and power-law exponents on the basis of the experimental results. More damage was observed for heterogeneous rocks compared with the homogeneous cores-the source of damage to permeability for high-permeability cores is the precipitation of reaction products-but for low-permeability cores, capillary forces between CO_2 and brine increase the severity of formation damage. The form of the precipitated material changes depending on the core mineralogy and permeability. The simulation study showed that for the cores tested in this study, power-law exponent and Carman-Kozeny exponent between 5 and 6 can be used for the homogeneous carbonate rock to estimate the change in permeability depending on change in porosity, whereas a larger exponent is needed for heterogeneous cores.
机译:在碳酸盐岩层中注入二氧化碳(CO_2)会导致井下注入率的降低,这是由于CO_2,岩石和盐水之间反应产物的沉淀所致。沉淀的物质包括硫酸盐和碳酸盐垢。就矿物学和岩石结构而言,碳酸盐岩的均质性是影响CO_2注入过程中渗透率变化行为的重要因素。在这项研究中测试的石灰石岩石包括均质的粉红色沙漠石灰石和奥斯汀白垩,主要是方解石。非均质志留系白云石(由98重量%的碳酸盐矿物和2重量%的硅酸盐矿物组成);以及非均质的印第安纳州石灰石,主要是方解石,并且有孔。进行了实验以比较岩心驱替期间这些岩石之间的渗透率损失。使用水交替气(WAG)技术注入CO_2。检查了不同的盐水,包括含硫酸盐的海水和无硫酸盐的海水。实验在1300 psi的背压,200°F的温度和5 cm〜3 / min的注入速率下进行。根据实验结果,使用成分模拟工具(CMG-GEM)来预测Carman-Kozeny和幂律指数。与均质岩心相比,非均质岩石受到的破坏更大-高渗透率岩心对渗透率的破坏源是反应产物的沉淀,但对于低渗透率岩心,CO_2和盐水之间的毛细作用力增加了地层破坏的严重性。沉淀物质的形式根据岩心矿物学和渗透率而变化。模拟研究表明,对于本研究中测试的岩心,均质碳酸盐岩可以使用幂律指数和Carman-Kozeny指数(介于5到6之间)来估计渗透率随孔隙度变化而变化,而较大的指数异构内核是必需的。

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  • 来源
    《SPE journal》 |2013年第3期|468-485|共18页
  • 作者

    I.M. Mohamed; H.A. Nasr-EI-Din;

  • 作者单位

    Advantek International;

    Texas A&M University;

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  • 原文格式 PDF
  • 正文语种 eng
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