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SEM IMAGING OF DRY AND SATURATED POROUS ROCKS FOR MODELING FLUID DISTRIBUTION ON PORE SCALE

机译:干燥饱和多孔岩体的SEM成像,用于孔隙尺度模拟液体分布

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Scanning electron microscopy(SEM) is the only direct observational method that has a high enough resolution to allow for the investigation of details of the pore space morphology or very small objects like liquid films in the pores.We tested different preparation methods to obtain sedimentary rock samples that are suitable for highresolution SEM imaging as a basis for a realistic description of the pore space.The produced photomicrographs were used directly in an applied modeling tool to simulate fluid distributions,e.g.,at primary drainage. To compare the model predictions with actual observations,sandstone and chalk plugs were saturated with synthetic formation water,and initial water saturation was established by injection of synthetic oil or crude oil at high temperature.The saturated samples were frozen in liquid nitrogen and investigated using SEM at low temperatures (Cryo-SEM) to obtain detailed information on the pore level fluid distribution. Good results were achieved for saturated sandstone.The geometry of the wetting phase films attached to the pore walls and at the contact of the grains,as well as water-filled smaller pores,was clearly observed.The distribution of fluids could be fittingly simulated with our modeling tool.Due to the predominance of micro- and nanopores in chalk,the Cryo-SEM resolution impedes the distinction of fluids at high magnification in this rock type.The distribution of the fluid phases could only be clearly imaged in chalk macropores.
机译:扫描电子显微镜(SEM)是唯一具有足够高分辨率的直接观察方法,以允许调查孔隙空间形态或非常小物体的细节,如孔隙中的液体膜。我们测试了不同的制备方法以获得沉积岩石适用于高分辨率SEM成像的样品作为孔隙空间的现实描述的基础。产生的显微照片直接用于施加的建模工具中,以模拟流体分布,例如在初级排水中。为了将模型预测与实际观察结果进行比较,砂岩和白垩塞用合成形成水饱和,并通过在高温下注射合成油或原油来建立初始水饱和。饱和样品在液氮中冷冻并使用SEM进行研究在低温(Cryo-Sem),获得有关孔隙水平流体分布的详细信息。对于饱和砂岩,实现了良好的结果。清楚地观察到饱和砂岩的润湿相膜的几何形状和晶粒的接触,以及含水较小的孔隙。可以用液体模拟流体的分布我们的建模工具。在粉笔中,Cryo-SEM分辨率在粉笔中占据微量和纳米孔的优势,在该岩石型中将流体区分开。流体阶段的分布只能在粉笔大孔中清楚地成像。

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