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Effect of Supercritical Carbon Dioxide Treatment Time, Pressure, and Temperature on Shale Water Wettability

机译:超临界二氧化碳处理时间,压力和温度对页岩水润湿性的影响

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摘要

Supercritical carbon dioxide (SC-CO2) fluid can dissolve surface matter on shale and, thus, change the surface properties of shale. TO study the influence of SC-CO2 on the water wettability of shale, shale samples collected from the Longmaxi formation in Sichuan Basin were treated with SC-CO2 at various time intervals, pressures, and temperatures. The results show that, after SC-CO2 treatment, the ratio of C and Si in the shale increased, while the ratio of O, Ca, Mg, and H decreased. Water was released from the clay minerals, and the CaCO3 content decreased in the shale. After SC-CO2 treatment, the primary pores and fractures in the shale were eroded through dissolution and new pores and fracture structures were developed on the surface microstructure of the shale. As a result, the structure connectivity, which favored the seepage of shale gas, was improved. The results also show that the shale water contact angles were increased after SC-CO2 treatment. The treatment time and pressure had a significant influence on the contact angles, but the effect of the treatment temperature on contact angles was not obvious. The change in the contact angles resulted from a reduction of the CaCO3 content on the shale surface, which decreased the surface hydrophilicity. The shale surface water wettability and the shale surface tension were decreased after SC-CO2 treatment. This reduces the hindrance function of water in the shale minimal pores and fracture, which is beneficial to CO2 diffusion into the shale matrix. This promotes CO2 adsorption capacity in the shale as well as. CH4 desorption from the shale. This study provides a theoretical basis for using SC-CO2 fluid for efficient shale gas exploitation in the Longmaxi formation of the Sichuan Basin.
机译:超临界二氧化碳(SC-CO2)流体可以溶解页岩上的表面物质,从而改变页岩的表面性质。为了研究SC-CO2对页岩水润湿性的影响,对四川盆地龙马溪组采集的页岩样品在不同的时间间隔,压力和温度下进行了SC-CO2处理。结果表明,SC-CO2处理后,页岩中碳和硅的比例增加,而O,Ca,Mg和H的比例降低。水从粘土矿物中释放出来,页岩中的CaCO3含量降低。 SC-CO2处理后,页岩的主要孔隙和裂缝通过溶解而被侵蚀,页岩的表面微观结构上形成了新的孔隙和裂缝结构。结果,改善了有利于页岩气渗透的结构连通性。结果还表明,SC-CO2处理后页岩水接触角增加。处理时间和压力对接触角有显着影响,但处理温度对接触角的影响不明显。接触角的变化是由于页岩表面CaCO3含量的减少,从而降低了表面亲水性。 SC-CO2处理后页岩表面水的润湿性和页岩表面张力降低。这降低了页岩中最小孔隙和裂缝中水的阻碍功能,这有利于CO2扩散到页岩基质中。这也促进了页岩中二氧化碳的吸附能力。 CH4从页岩中解吸。该研究为利用SC-CO2流体有效开发四川盆地龙马溪组页岩气提供了理论依据。

著录项

  • 来源
    《Energy & fuels》 |2017年第1期|493-503|共11页
  • 作者单位

    Chongqing Univ, State Key Lab Coal Mine Disaster Dynam & Control, Chongqing 400044, Peoples R China;

    Chongqing Univ, State Key Lab Coal Mine Disaster Dynam & Control, Chongqing 400044, Peoples R China;

    Chongqing Univ, State Key Lab Coal Mine Disaster Dynam & Control, Chongqing 400044, Peoples R China;

    Chongqing Univ, State Key Lab Coal Mine Disaster Dynam & Control, Chongqing 400044, Peoples R China;

    Chongqing Univ, State Key Lab Coal Mine Disaster Dynam & Control, Chongqing 400044, Peoples R China;

    Chongqing Univ, State Key Lab Coal Mine Disaster Dynam & Control, Chongqing 400044, Peoples R China;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);美国《生物学医学文摘》(MEDLINE);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

  • 入库时间 2022-08-18 00:39:30

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