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Predicting Petro-physical Properties using SEM Image

机译:使用SEM图像预测石油物理性质

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The permeability estimation of reservoir rocks using numerical methods has always been a challenge for petrophysicist. Several models have been developed for its computation of this parameter. As the permeability is entirely controlled by the geometry, the possibility arising of estimating the permeability from quantifiable attributes of the space has always has been a approach. In the present paper, a model is discussed which gives accurate prediction of the permeability based on two dimensional SEM image of a core sample of sedimentary rock. The inputs required for the model are the areas and perimeters measurements from the images of space. The individual conductances are estimated using hydraulic radius approximation. Before using the data obtained from images, stereological corrections are used to convert geometries and various hydraulic corrections are used to account for converging-diverging flow paths. Kirkpatrick's medium approximation is finally used to find the value of the hydraulic conductances of the individual pores. The method has been applied to six data sets of SEM images which include Berea sandstone, consolidated sandstones and carbonate samples. The laboratory determined air permeabilities of these samples ranged from 0.5-400mD. The permeability values predicted by this method are within a factor of two of the values. This method requires least data manipulation and computation and is more accurate than conventional methods such as the Kozeny-Carman equation. The method holds promise of permeability predictions on irregular rock samples like drill cuttings which cannot be in standard lab measurements. Another possible future is to use down-hole borehole imaging technology to provide an image with the appropriate resolution, thereby allowing in-situ permeability estimation, without the need for core samples. Keywords Permeability, Scanning Electron Microscope, Pore Network Modeling, Porosity, Conductance, Sandstones and Carbonates
机译:使用数值方法的储层岩石的渗透率估计一直是岩石物理学家的挑战。已经开发了几种模型来计算此参数。随着渗透率完全由几何体控制,估算空间的可量化属性的估算渗透性的可能性一直是一种方法。在本文中,讨论了一种模型,其基于沉积岩石核心样本的二维SEM图像对渗透性进行准确预测。模型所需的输入是空间图像的区域和周边测量。使用液压半径近似估计各个电导。在使用从图像获得的数据之前,使用立体校正来转换几何形状,并且各种液压校正用于考虑会聚流路。 KirkPatrick的中等近似最终用于找到个体孔的液压导电的值。该方法已应用于六种数据集的SEM图像,包括Berea砂岩,巩固的砂岩和碳酸盐样品。确定这些样品的实验室测定的空气渗透率范围为0.5-400MD。通过该方法预测的渗透率值在两个值的两个值范围内。该方法需要最小的数据操纵和计算,并且比诸如Kozeny-Carman方程的传统方法更准确。该方法具有在不规则岩石样本上的渗透性预测的承诺,如钻杆的不规则岩石样本,其不能在标准实验室测量中。另一个可能的未来是使用井下钻孔成像技术来提供具有适当分辨率的图像,从而允许原位渗透率估计,而无需核心样本。关键词渗透性,扫描电子显微镜,孔隙网络建模,孔隙度,电导,砂岩和碳酸盐

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