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GEOLOGY-BASED RESERVOIR MODEL BUILDING FOR CARBONATE RESERVOIRS

机译:基于地质的碳酸盐岩储层模型构建

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Environment in which carbonate reservoir rocks are deposited was studied by visiting and collecting rock samples from a carbonate reservoir analog located at Jabal Fuwairit in the Northeastern coast of Qatar. The primary objective of this study is to develop methods to characterize carbonate reservoirs. The experimental procedure included collecting samples based on geology, mapping the location and altitudes of the samples using a high-resolution Global Positioning System (GPS) with an altimeter, permeability measurements at selected locations, conducting petrophysical measurements on the samples, Conventional and Micro-X-ray Computed Tomography Scanning (CT Scanning), Scanning Electron Microscopy (SEM), X-ray Energy Dispersive Spectroscopy (EDS) and Atomic Force Microscopy (AFM) imaging. It is observed that the permeability measurements show an alternating pattern as a function of height above sea level. The cyclicity is probably representative of repeating sequences of sea level changes over geological time. CT Scanner and Micro-CT Scanner measurements were employed to obtain vital information about the flow pathways in the rock, thus assisting in calculating the porosity to compare with values measured in the lab. SEM results gave direct visualization of the pore network and information about grain size (500 microns) and intergranular porosity, mineralogy, compared with the EDS results, and lithotype. EDS results showed that reservoir rocks directly exposed to environment had significant alteration due to weathering. However, it is encouraging to learn that samples even few inches away from the surface had minimal environmental influence.
机译:通过访问和收集位于卡塔尔东北海岸Jabal Fuwairit的碳酸盐储层类似物的岩石样品,研究了沉积碳酸盐储层岩石的环境。这项研究的主要目的是开发表征碳酸盐岩储层的方法。实验程序包括根据地质条件收集样品,使用带有高度计的高分辨率全球定位系统(GPS)绘制样品的位置和高度图,在选定位置进行渗透率测量,对样品进行岩石物理测量,常规和微型X射线计算机断层扫描(CT扫描),扫描电子显微镜(SEM),X射线能量色散光谱(EDS)和原子力显微镜(AFM)成像。可以观察到,渗透率测量结果显示出一种交替的模式,它是海拔高度的函数。周期性可能代表了地质时间内海平面变化的重复序列。使用CT扫描仪和Micro-CT扫描仪测量来获取有关岩石中流动路径的重要信息,从而帮助计算孔隙度以与实验室中测量的值进行比较。 SEM结果可直接观察孔网络,并提供有关晶粒尺寸(500微米)和晶间孔隙度,矿物学(与EDS结果相比)和岩性的信息。 EDS结果表明,由于风化作用,直接暴露于环境中的储层岩石发生了明显的变化。但是,令人鼓舞的是,即使距离表面只有几英寸的样品对环境的影响也很小。

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