首页> 外文会议>International Symposium of the Society of Core Analysts >THE REV CHALLENGE – ESTIMATING REPRESENTATIVE ELEMENTARY VOLUMES AND POROUS ROCK INHOMOGENEITY FROM HIGH RESOLUTION MICRO-CT DATA SETS
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THE REV CHALLENGE – ESTIMATING REPRESENTATIVE ELEMENTARY VOLUMES AND POROUS ROCK INHOMOGENEITY FROM HIGH RESOLUTION MICRO-CT DATA SETS

机译:Rev挑战 - 从高分辨率微型CT数据集估算代表基础体积和多孔岩石不均匀性

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Micro Computed Tomography(μ-CT) imaging forms a great method to investigate internal rock structures – e.g.the void space,fluid distribution,etc.– fast,in three dimensions and non-destructively.Since the last decade,μ-CT has progressed to faster imaging as well as to faster reconstruction times,and especially to high quality image resolution and sharpness(in the micron or even sub-micron range).With this,access is granted to the investigation of small pore space features(e.g.clay induced porosities or porous networks,formed by dissolved mineral phases) as well as to representative,i.e. predictive fluid flow modeling.Although modeling of fluid flow through small sample networks may increase the knowledge of fluid dynamics on a microscopic scale, representative modeling of physics remains the most important task.For this,porosity has proven to be the parameter of choice to characterize a porous media by terms of fluid dynamics and to determine a representative elementary volume(REV) for it.The REV is reached,when the average porosity in the probing volume becomes independent of the size of the volume.Nevertheless,this approach does not consider sample inhomogeneities or directional porosity variations,e.g.caused by layering effects.Hence, the author would like to present an advanced method to estimate representative elementary volumes derived by high resolution μ-CT imaging.This Method is based upon a variance analysis of directional micro-porosity logs,which have been calculated from 3D image quantification analysis.Additionally,a new method to estimate the sample inhomogeneity – as a quality control feature for the REV estimation – is introduced.With this analysis,it is furthermore possible to investigate scale,i.e.REV edge size,dependent structural effects and transitions.
机译:微计算机断层扫描(μ-CT)成像形成了一种伟大的方法来调查内岩结构 - 例如空隙空间,流体分布等 - 快速,三维和非破坏性。过去十年的空中,μ-CT已经进行了进展更快的成像以及更快的重建时间,尤其是高质量的图像分辨率和锐度(在微米甚至是亚微米范围内)。为此,授予对小孔空间特征的调查(EGClay诱导的访问由溶解的矿物阶段形成的孔隙症或多孔网络)以及代表性,即预测流体流模型。通过小型样本网络的流体流的建模可能会增加流体动力学的知识,以微观规模,物理学的代表性建模仍然是最重要的任务。如此,孔隙率已被证明是表征的选择参数通过流体动力学的术语和确定其代表性基本体积(Rev)的多孔介质。达到探测体积的平均孔隙率与体积的尺寸无关时,这种方法不考虑样品不均匀性或定向孔隙率变化,通过分层效应EGAUSED。当然,作者想提前估算通过高分辨率μ-CT成像的代表性基本体积的先进方法。该方法基于方向性微观分析从3D图像量化分析计算的孔隙度原木.Aditionally,一种估计样品的新方法OMOPENSITY - 作为REV估计的质量控制特征 - 介绍了这种分析,还可以调查SCALE,I.E.REV边缘尺寸,依赖的结构效果和转换。

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