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How Naturally Adsorbed Material on Minerals Affects Low Salinity Enhanced Oil Recovery

机译:天然吸附在矿物质上的材料如何影响低盐度提高采油率

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摘要

Laboratory core flood and field scale tests have demonstrated that about 5 to 40% more oil can be released from sandstone reservoirs by injecting low salinity water, rather than high salinity fluids such as seawater or formation water. The effect has been explained by a change in wettability of the minerals that form the pore wall, as a result of the decrease in divalent cation concentration. Using X-ray photoelectron spectroscopy, we have demonstrated that even for solvent cleaned core samples, mineral surfaces retain a significant quantity of carbon containing material. Thus, pore wall wettability is more likely dominated by tightly adsorbed organic material than by the character of the underlying minerals. To test this hypothesis, we used the chemical force mapping (CFM) mode of atomic force microscopy (AFM) to directly measure adhesion forces on individual quartz grains that were plucked from core plugs. We functionalized AFM tips with model oil compounds so they would represent tiny oil droplets, and we measured their ability to adhere to surfaces as salinity changed. We examined grains from a sandstone core plug that had been cut into segments, which had been stored in kerosene or solvent cleaned. On all samples, surfaces were more oil wet (higher adhesion) in artificial seawater (ASW; 35,600 ppm) than in ASW diluted with ultrapure deionized water to ~1,500 ppm. XPS demonstrated that solvent cleaned surfaces had less adsorbed organic material than the kerosene stored sample. AFM measurements showed that the low salinity effect, namely the change in adhesion caused by decreasing salinity, was twice as high on kerosene stored samples as on solvent cleaned surfaces. The organic material that is adsorbed on the pore surfaces in the preserved sandstone offer very sticky anchor points for adhering oil molecules. This suggests that in reservoirs, even hydrophilic minerals located at the pore-fluid interface have tightly adhering hydrocarbons and the low salinity response depends on the behavior of this adsorbed material.
机译:实验室岩心洪水和现场规模测试表明,通过注入低盐度水而不是注入高盐度流体(例如海水或地层水),砂岩储层可以释放出大约5至40%的油。由于二价阳离子浓度的降低,形成孔壁的矿物的润湿性发生了变化,从而解释了这种影响。使用X射线光电子能谱,我们已经证明,即使对于溶剂清洁的岩心样品,矿物表面也会保留大量的含碳物质。因此,孔壁的可湿性更可能由紧密吸附的有机材料决定,而不是由下层矿物的特性决定。为了验证这一假设,我们使用原子力显微镜(AFM)的化学力映射(CFM)模式直接测量了从芯塞拔出的单个石英颗粒上的粘附力。我们使用模型油化合物对AFM吸头进行了功能化处理,使其可以代表微小的油滴,并且我们测量了随着盐度变化它们粘附于表面的能力。我们检查了砂岩芯塞中的谷物,这些谷物已切成段,然后存储在煤油中或用溶剂清洗过。在所有样品上,与用超纯去离子水稀释至〜1,500 ppm的ASW相比,人造海水(ASW; 35,600 ppm)中的表面更油润湿(更高的附着力)。 XPS证明,与煤油储存的样品相比,溶剂清洁的表面吸附的有机物质更少。原子力显微镜的测量表明,低盐度效应(即由盐度降低引起的粘附力变化)在煤油储存的样品中是溶剂清洁表面的两倍。吸附在保存的砂岩孔隙表面上的有机物质为粘附油分子提供了非常粘的锚固点。这表明在储层中,即使位于孔隙-流体界面的亲水性矿物也具有紧密粘附的碳氢化合物,而低盐度响应取决于这种吸附材料的行为。

著录项

  • 来源
    《Energy & fuels》 |2014年第julaaauga期|4849-4858|共10页
  • 作者单位

    Nano-Science Center, Department of Chemistry, University of Copenhagen, Copenhagen 2100, Denmark;

    Nano-Science Center, Department of Chemistry, University of Copenhagen, Copenhagen 2100, Denmark;

    Nano-Science Center, Department of Chemistry, University of Copenhagen, Copenhagen 2100, Denmark;

    Nano-Science Center, Department of Chemistry, University of Copenhagen, Copenhagen 2100, Denmark;

    Department of Physics, North Carolina A&T State University, Greensboro, North Carolina 27411, United States;

    Upstream Technology, BP Exploration Operating Company, Sunbury-on-Thames TW16 7LN, United Kingdom;

    Nano-Science Center, Department of Chemistry, University of Copenhagen, Copenhagen 2100, Denmark;

    Nano-Science Center, Department of Chemistry, University of Copenhagen, Copenhagen 2100, Denmark;

    Upstream Technology, BP Exploration Operating Company, Sunbury-on-Thames TW16 7LN, United Kingdom;

    Upstream Technology, BP Exploration Operating Company, Sunbury-on-Thames TW16 7LN, United Kingdom;

    Nano-Science Center, Department of Chemistry, University of Copenhagen, Copenhagen 2100, 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);
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