首页> 外文期刊>Petrophysics: The SPWLA Journal of Formation Evaluation and Reservoir Description >Investigation of Salt-Bearing Sediments Through Digital Rock Technology Together With Experimental Core Analysis
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Investigation of Salt-Bearing Sediments Through Digital Rock Technology Together With Experimental Core Analysis

机译:用数字岩技术与实验核心分析一起调查含盐沉积物

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摘要

In this study, digital rock analysis was combined with a variety of experimental core-analysis measurements to investigate the effect of salt saturation and distribution on the porosity and permeability of halite-cemented core samples. Medical and micro-X-ray CT scans of core sections and 2.54-cm (1-in.) diameter plugs indicated that the halite generally occurred in the form of distinct layers. High-resolution micro-X-ray computed tomography (MXCT) images acquired of 0.6-cm diameter plugs revealed that, on the pore scale, halite appeared to be pore filling. Pores were either completely filled with halite or did not contain any halite at all. It was also observed that halite preferentially occurred in the larger pores associated with larger grain sizes. The porosity and permeability results, both measured experimentally on the core plugs and calculated by segmentation of the MXCT images, demonstrated the obstructive effect of halite on storage and flow as well as the decline of both properties with increasing salt saturation. Comparison of calculated and measured values showed that the measured porosity could be up to 6 porosity units (p.u.) higher than the calculated one, while the measured permeability of core plugs after salt removal was an order of magnitude lower than the one obtained by lattice Boltzmann simulation. One possible reason for this discrepancy may be the stratified nature of the samples. While the fully salt-saturated plugs appeared homogeneous in MXCT images, post-flood MRI images revealed that the plug was composed of layers with different MRI intensities, i.e., different amounts of water-filled porosity. Consequently, the petrophysical parameters calculated for the miniplugs may only be representative for a section of the core plug. The results of the MRI-assisted core floods emphasized the importance of considering different scales when interpreting and applying the results of digital rocks analysis.
机译:在这项研究中,数码岩体分析与各种实验核心分析测量相结合,以研究盐饱和度和分布对卤化物核心样品的孔隙率和渗透性的影响。核心部分的医疗和微X射线CT扫描和2.54厘米(1英寸)直径塞表示,宿舍通常以不同层的形式发生。获得0.6厘米直径塞的高分辨率微X射线计算机断层扫描(MXCT)图像显示,在孔隙尺度上,留钟似乎是孔填充物。毛孔完全填充有盐,或根本不含任何留胡子。还观察到,在与较大晶粒尺寸相关的较大孔中优先发生宿舍。孔隙率和渗透率结果,两者都在实验上测量核心塞并通过MXCT图像的分割计算,证明了宿骨对储存和流动的阻塞性效果以及盐饱和增加的两种性能下降。计算和测量值的比较显示,测量的孔隙率可以高于计算的孔隙率高(PU),而盐去除后的核心塞的测量渗透率比通过格子Boltzmann获得的阶数低。模拟。这种差异的一种可能原因可能是样品的分层性质。虽然在MXCT图像中出现完全盐饱和的塞,但泛洪后的MRI图像显示,插头由具有不同MRI强度的层组成,即,不同量的水填充孔隙率。因此,针对小微孔计算的岩石物理参数可以仅代表核心插头的一部分。 MRI辅助核心洪水的结果强调了在解释和应用数字岩分析结果时考虑不同尺度的重要性。

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