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Probing the intrinsically oil-wet surfaces of pores in North Sea chalk at subpore resolution

机译:以亚孔分辨率探测北海白垩孔隙的内在油湿表面

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摘要

Pore surface properties control oil recovery. This is especially true for chalk reservoirs, where pores are particularly small. Wettability, the tendency for a surface to cover itself with fluid, is traditionally defined by the angle a droplet makes with a surface, but this macroscopic definition is meaningless when the particles are smaller than even the smallest droplet. Understanding surface wetting, at the pore scale, will provide clues for more effective oil recovery. We used a special mode of atomic force microscopy and a hydrophobic tip to collect matrices of 10,000 force curves over 5- × 5-μm2 areas on internal pore surfaces and constructed maps of topography, adhesion, and elasticity. We investigated chalk samples from a water-bearing formation in the Danish North Sea oil fields that had never seen oil. Wettability and elasticity were inhomogeneous over scales of 10s of nanometers, smaller than individual chalk particles. Some areas were soft and hydrophobic, whereas others showed no correlation between hardness and adhesion. We conclude that the macroscopic parameter, “wetting,” averages the nanoscopic behavior along fluid pathways, and “mixed-wet” samples have patches with vastly different properties. Development of reservoir hydrophobicity has been attributed to infiltrating oil, but these new results prove that wettability and elasticity are inherent properties of chalk. Their variability, even on single particles, must result from material originally present during sedimentation or material sorbed from the pore fluid some time later.
机译:孔的表面性质控制着油的采收率。对于孔隙特别小的白垩储层,尤其如此。传统上,润湿性是指表面被流体覆盖的趋势,而润湿性通常是由液滴与表面形成的角度来定义的,但是当颗粒小于最小液滴时,这种宏观定义就毫无意义。了解细孔表面的润湿性,将为更有效地采油提供线索。我们使用一种特殊的原子力显微镜模式和一个疏水尖端,在内部孔表面的5-×5-μm 2 区域上收集了10,000条力曲线的矩阵,并绘制了形貌,附着力和弹性图。我们调查了从未见过油的丹麦北海油田一个含水层中的白垩样品。在10纳米的尺度上,润湿性和弹性是不均匀的,小于单个白垩颗粒。一些区域柔软且疏水,而其他区域则显示硬度和附着力之间没有相关性。我们得出的结论是,宏观参数“润湿”将沿着流体路径的纳米行为平均化,“混湿”样品的斑块具有截然不同的特性。储层疏水性的发展归因于渗透油,但这些新结果证明了润湿性和弹性是白垩的固有特性。即使在单个颗粒上,它们的可变性也必须由沉淀过程中最初存在的物质或一段时间后从孔隙流体中吸收的物质引起。

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