首页> 外文会议>SPWLA annual logging symposium;Society of Petrophysicists and Well Log Analysts, inc >EXPORTING PETROPHYSICAL PROPERTIES OF SANDSTONES FROM THIN SECTION IMAGE ANALYSIS
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EXPORTING PETROPHYSICAL PROPERTIES OF SANDSTONES FROM THIN SECTION IMAGE ANALYSIS

机译:从薄壁图像分析中导出砂岩的岩石物理性质

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Estimation of the petrophysical properties using imaging techniques and image analysis has been an active area of research in recent years. This has been primarily focused on 3D imaging and subsequent modeling of formation properties, termed Digital Rock Physics. This work requires an intact sample of material. When sample type or quality are not sufficient for 3D imaging, or where cost is prohibitive, modeling of petrophysical properties using thin section images is a viable, and for some samples, a superior alternative.This study involves the use of transmitted light image tiles from the light microscope. Each thin section is scanned in plane, cross-polarized, and fluorescent light. Each of these provide information about the framework and authigenic phase mineralogy. The advantages of thin section imaging for estimating petrophysical properties, include the ability to identify framework grain types for provenance and reservoir quality modeling studies, differentiation of detrital and authigenic phases, and establishing paragenesis.We apply a Carmen-Kozeny type model to thin section images of samples for which laboratory measurements of porosity and brine permeability were made. This has allowed us to model absolute permeability to within a factor of two for sandstone samples having laboratory-measured permeabilities ranging from 175 mD to 8D, and builds on a calibration data set of approximately 30 samples. For the original data set, modeled permeability agreed with measured permeability to within a factor of two, over a range of permeability from 8mD to 3D.A key input parameter to this model is an estimate of specific surface area. The 2D estimate of specific surface area, defined in Hathon, et al., (2003), is the ratio of the total porosity perimeter to the total area analyzed. The normalization to the total area analyzed, allows the number of image tiles analyzed to be varied for each sample. The estimated specific surface area is a function of image magnification, down-sampling and filtering of the image are applied during analysis. This work extends the previous model by adding a fractal analysis to the estimate of specific surface area. This allows us to account f o r the impact of magnification and processing when modeling permeability from 2D image data. Total porosity from 2D image segmentation agrees towithin +/- 2% of laboratory measured porosity.Future work includes developing a model for converting 2D pore body size distributions to 3D equivalents for comparison to NMR based estimates of pore body size, together with calibration of the surface relaxivity term. We also intend to investigate the relationship between the estimated tortuosity in thin section and Formation Factor, and estimating pore throat size distributions for modeling Mercury Injection Capillary Pressure (MICP) data.
机译:近年来,使用成像技术和图像分析估计岩石物理性质的估计是一个活跃的研究领域。这主要集中在3D成像和随后的形成性质建模,称为数字岩体物理学。这项工作需要完整的材料样品。当样品类型或质量不足以足够的3D成像时,或者在成本令人望而抑制的情况下,使用薄截面图像的岩石物理学建模是可行的,并且对于一些样品,是一种优越的替代方案。 该研究涉及使用来自光显微镜的透射光图像瓦片。在平面,交叉极化和荧光中扫描每个薄部分。这些中的每一个都提供有关框架和Aheyigenic相相矿物学的信息。薄截面成像用于估计岩石物理性质的优点,包括识别出现和储层质量建模研究的框架晶粒类型,邪恶和邪恶阶段的分化,以及建立寄生虫。 我们将Carmen-Kozeny型模型应用于薄截面图像的样品,制备了孔隙率和盐水渗透性的实验室测量。这使我们能够模拟绝对渗透率,在两个具有从175md至8d的实验室测量的渗透率的砂岩样品中模拟两者,并在大约30个样品的校准数据集上构建。对于原始数据集,建模渗透率同意测量的渗透率,在两倍的因子中,在8MD到3D的渗透率范围内。 此模型的键输入参数是对特定表面积的估计。在Hathon等人中定义的特定表面积的2D估计,(2003),是分析总面积的总孔隙率周边的比率。分析的总面积的归一化允许分析的图像瓦片数量变化为每个样本。估计的特定表面积是图像放大的函数,在分析期间施加图像的下验采样和滤波。这项工作通过向特定表面积的估计添加分形分析来扩展前一个模型。这使我们能够在从2D图像数据建模渗透率时解释放大率和处理的影响。来自2D图像分割的总孔隙率同意实验室测量孔隙率的纤维素+/- 2%。 未来的工作包括开发用于将2D孔体尺寸分布转换为3D等同物的模型,以便与基于NMR的孔体尺寸的估计相比,以及表面松弛率的校准。我们还打算探讨薄剖面和地层系数的估计曲折性之间的关系,估算汞注射毛细管压力(MICP)数据的孔喉大小分布。

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