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Low Salinity Effect at Pore Scale: Probing Wettability Changes in Middle East Limestone

机译:孔隙度下的低盐度效应:探究中东石灰石的润湿性变化

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The effectiveness of low salinity flooding for enhanced oil recovery (EOR) in sandstone reservoirs has been demonstrated in core plug and field tests as well as at molecular scale, but in carbonate reservoirs the results are mixed. With atomic force microscopy (AFM) chemical force mapping (CFM), using a methyl (CH3) functionalized tip, we tracked the wettability of limestone pore surfaces (before and after solvent treatment) during exposure to high and low salinity solutions at a submicrometer scale. The correlation between adhesion and salinity was weak for both the treated and the fresh samples, but detailed analysis of the force maps demonstrated that on the fresh limestone there are areas that clearly respond to changes in salinity. Adhesion decreased when salinity decreased on some areas, and on others adhesion increased. To understand this behavior, we analyzed the surfaces with X-ray photoelectron spectroscopy (XPS) and energy dispersive X-ray spectroscopy (EDXS). The amount of organic material on the solvent treated samples was lower than on the fresh samples, but the amount and type of organic compounds were considerably different. These differences provide a likely explanation for the differences in the effectiveness of low salinity flooding that have been reported in the literature and lead us to conclude that for the samples analyzed in our study, the response in carbonate rocks is controlled by an intricate interplay between the composition of the tightly adsorbed organic material, the minerals on which it is adsorbed, and the functional groups present in the oil. Consequently, if the effectiveness of low salinity flooding in carbonate reservoirs is to be predicted, characterization of the organic compounds in the oil and on the pore surfaces is essential.
机译:低盐度驱油对提高砂岩油藏的采收率(EOR)的有效性已在岩心塞和现场测试以及分子规模上得到了证明,但在碳酸盐岩油藏中,结果是混合的。使用原子力显微镜(AFM)化学力绘图(CFM),使用甲基(CH3)官能化尖端,我们跟踪了亚微米级高低盐溶液暴露期间(在溶剂处理之前和之后)石灰石孔隙表面的润湿性。对于处理过的样品和新鲜样品,粘附力和盐度之间的相关性都很弱,但是对力图的详细分析表明,新鲜石灰石上存在明显响应盐度变化的区域。当某些地区的盐度降低时,粘附力会降低,而在另一些地区,粘附力则会增加。为了了解这种行为,我们使用X射线光电子能谱(XPS)和能量色散X射线能谱(EDXS)分析了表面。经溶剂处理的样品上的有机物质含量低于新鲜样品,但是有机化合物的含量和类型却有很大差异。这些差异为文献中已报道的低盐度驱油效果的差异提供了可能的解释,并导致我们得出结论:对于我们研究中分析的样品,碳酸盐岩中的响应受复杂的碳酸盐岩相互作用的控制。紧密吸附的有机材料的组成,吸附在其上的矿物质以及油中存在的官能团。因此,如果要预测碳酸盐岩储层中低盐度驱油的有效性,则必须对油中和孔隙表面的有机化合物进行表征。

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  • 来源
    《Energy & fuels》 |2016年第5期|3768-3775|共8页
  • 作者单位

    Univ Copenhagen, Dept Chem, Nanosci Ctr, DK-2100 Copenhagen, Denmark;

    Univ Copenhagen, Dept Chem, Nanosci Ctr, DK-2100 Copenhagen, Denmark;

    Univ Copenhagen, Dept Chem, Nanosci Ctr, DK-2100 Copenhagen, Denmark;

    Univ Copenhagen, Dept Chem, Nanosci Ctr, DK-2100 Copenhagen, Denmark;

    Maersk Oil & Gas AS, Esplanaden 50, DK-1098 Copenhagen, Denmark|Univ Copenhagen, DK-2100 Copenhagen, Denmark;

    Univ Copenhagen, Dept Chem, Nanosci Ctr, DK-2100 Copenhagen, Denmark;

  • 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 00:39:56

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