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首页> 外文期刊>Marine and Petroleum Geology >A comprehensive study on geometric, topological and fractal characterizations of pore systems in low-permeability reservoirs based on SEM, MICP, NMR, and X-ray CT experiments
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A comprehensive study on geometric, topological and fractal characterizations of pore systems in low-permeability reservoirs based on SEM, MICP, NMR, and X-ray CT experiments

机译:基于SEM,MICP,NMR和X射线CT实验的低渗透储层孔隙系统几何,拓扑和分形表征综合研究

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Characterization of pore systems in subsurface systems is of great importance for predicting the properties of rocks and classifying the subsurface systems. Geometric features have been used widely for this aim, but topological characteristics of the pore structures are not studied much. In fact, accurate characteristics of pore space should comprise both its geometric and topological properties. In this paper, the above vital characteristics are comprehensively studied based on direct experimental results. Besides, previous studies aiming at linking fractal dimension analysis to pore space are often based on limited sources of information, which are the mercury injection capillary pressure (MICP) and nuclear magnetic resonance (NMR). In this paper, the scanning electron microscope (SEM), MICP, NMR, and X-ray computed tomography (X-ray CT) experiments are all used to characterize the geometric and topological properties of pore space of several low-permeability porous media. Based on our observations, the advantages and disadvantages of the above techniques in characterizing the pore structure are also summarized. Moreover, the differences of these three experiments are quantified using fractal dimension. The results indicate that the NMR technique is a promising tool for characterizing geometric features of pore systems as it can cover more details than other techniques. Most of geometric, topological, fractal and transport properties of pore space can be obtained from X-ray CT method, which is unique among all the methods. In addition, the 3D fractal dimensions of pore systems obtained from NMR is smaller than that from MICP, which is due more ultra-micropores captured by NMR that smooth the surface of the pore systems. Finally, a novel method constrained by a new pore shape factor for calculating the pore size from 2D images is proposed by which the pore-size distributions are compared more effectively.
机译:地下系统中的孔系统的表征对于预测岩石的性质和分类地下系统的性能具有重要意义。几何特征已广泛用于此目的,但孔结构的拓扑特征不多。实际上,孔隙空间的准确特征应包括其几何和拓扑特性。本文基于直接实验结果综合研究了上述重要特征。此外,旨在将分形尺寸分析连接到孔隙空间的先前研究通常基于有限的信息来源,这是汞注射毛细压力(MICP)和核磁共振(NMR)。在本文中,扫描电子显微镜(SEM),MICP,NMR和X射线计算机断层扫描(X射线CT)实验均用于表征几种低渗透多孔介质的孔隙空间的几何和拓扑特性。基于我们的观察结果,还总结了表征孔隙结构的上述技术的优点和缺点。此外,使用分形尺寸量化这三个实验的差异。结果表明,NMR技术是用于表征孔系统的几何特征的有前途的工具,因为它可以覆盖比其他技术的更多细节。孔隙空间的大多数几何,拓扑,分形和运输性能,可以从X射线CT方法获得,这在所有方法中是独一无二的。另外,从NMR获得的孔系统的3D分形尺寸小于MICP的3D分形尺寸,这是由NMR捕获的更多超微微孔,其平滑孔系统的表面。最后,提出了一种由新的孔形状因子约束的用于计算来自2D图像的孔径的新方法,通过该方法更有效地比较孔径分布。

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