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Dual Energy Microtomography Applied to Oil and Gas Assessments

机译:适用于石油和天然气评估的双能学

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Dual energy X-ray Microtomography (DE-MicroCT) has proven to be a valuable method in oil and gas industry because it provides non-destructive investigation of the mineral composition of internal structures, characteristic of reservoir core materials. In order to distinguish among different rock materials, a dual energy scanning is carried out to determine both the density and effective atomic number of the minerals of interest. Accurate and reliable quantitative measurements can be achieved with an appropriate calibration within the range of measured attenuation values. However, image quality is the key of an accurate measurement and image signal to noise ratio (SNR), which is related to the ability to define the ratio of the signal intensity to the ambient noise level, is primary determinant. This study provides an investigation of the inner mineralogy phases and microstructural characteristics of a reservoir rock sample by DE-MicroCT. For that purpose a carbonate with different ranges of total porosity and consequently permeability was used. Image analysis process is crucial for an accurate differentiation between calcite (matrix density = 2.71 g/cm~3) and dolomite (matrix density = 2.87 g/cm~3) minerals because they are very similar, although the last mineral is denser than the first one. The results show that small differences are enough to obtain measurements of different mineral phases in Brazilian reservoir rock samples. The results also illustrate that important morphometric parameters to petrophysics investigation may be obtained in this approach.
机译:双能X射线显微镜(DE-MIGRYCT)已被证明是石油和天然气行业的宝贵方法,因为它提供了对内部结构矿物成分的非破坏性调查,储层核心材料的特征。为了区分不同的岩石材料,进行双能扫描以确定感兴趣的矿物质的密度和有效原子数。可以在测量衰减值范围内具有适当的校准来实现精确可靠的定量测量。然而,图像质量是准确测量和图像信号到噪声比(SNR)的关键,其与定义信号强度与环境噪声水平的比率的能力有关,是主要的决定因素。本研究提供了De-Microct对储层岩石样品的内矿物学阶段和微观结构特征的研究。为此目的,使用具有不同孔隙率和因此渗透性不同范围的碳酸盐。图像分析过程对于方解石之间的准确分化至关重要(矩阵密度= 2.71g / cm〜3)和白云石(矩阵密度= 2.87g / cm〜3)矿物,因为它们非常相似,但最后的矿物质比该矿物更密集第一。结果表明,小差异足以获得巴西水库岩石样品中不同矿物阶段的测量。结果还说明,可以以这种方法获得对岩石物理学调查的重要形态学参数。

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