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Characterization of Organic Layer in Oil Carbonate Reservoir Rocks and its Effect on Microscale Wetting Properties

机译:碳酸盐岩储层岩石有机层特征及其对微尺度润湿性的影响

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摘要

Effective production of oil from carbonate reservoirs often requires the application of improved oil recovery technologies such as waterflooding. However, conventional waterflooding in carbonates usually results in low hydrocarbon recovery as most of these formations exhibit a complex pore throats structure and are mostly oil-wet. Therefore, improved insight into the causes of hydrophobic wetting behavior of such reservoirs is important for understanding the fluid distribution, displacement and enhancing recovery processes. The characterization of fluid-rock interactions is, however, challenging with existing laboratory methods, which are typically based on macroscale (mm) observations. In this experimental study, an advanced imaging technique, namely environmental scanning electron microscope, was applied for the comprehensive investigation of microscale (µm) wettability variations in carbonate rocks covered with organic layers. For the first time, the presence of organic layers on the sample was proved using energy dispersive X-ray mapping. Furthermore, the chemical bond of this layer and carbonate rock surfaces was determined using the transmission electron microscopy and electron energy-loss spectroscopy. The thickness of layer was estimated by using image processing software. These findings show that the application of combined microscopic techniques reveals important details about the reason of hydrophobic wetting properties of real carbonate rocks.
机译:从碳酸盐岩储层中有效开采石油通常需要应用改进的采油技术,例如注水。但是,传统的碳酸盐岩注水法通常会导致烃采收率低,因为这些地层中的大多数都表现出复杂的孔喉结构,并且大多是油湿的。因此,对于此类储层疏水润湿行为的成因的深入了解对于理解流体分布,驱替和提高采收率过程至关重要。但是,利用现有的实验室方法(通常基于宏观(mm)观测值)来表征流体-岩石相互作用是一项挑战。在这项实验研究中,一种先进的成像技术,即环境扫描电子显微镜,被用于全面研究覆盖有有机层的碳酸盐岩中的微米级(µm)润湿性变化。首次使用能量色散X射线图证明了样品上有机层的存在。此外,使用透射电子显微镜和电子能量损失光谱法测定了该层和碳酸盐岩石表面的化学键。通过使用图像处理软件来估计层的厚度。这些发现表明,组合显微技术的应用揭示了有关真正碳酸盐岩石疏水润湿性原因的重要细节。

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