کد مقاله | کد نشریه | سال انتشار | مقاله انگلیسی | نسخه تمام متن |
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4546754 | 1627062 | 2013 | 10 صفحه PDF | دانلود رایگان |
X-ray micro-computed tomography (micro-CT) techniques for measuring the three-dimensional (3-D) distributions of diffusion-accessible porosity (φd) and temporal tracer-concentrations (C(t)) within a dolostone sample subjected to solute diffusion are developed and tested in this work. The φd and C(t) measurements are based on spatially resolved changes in X-ray attenuation coefficients in sequentially acquired 3-D micro-CT datasets using two (calibration and relative) analytical approaches. The measured changes in X-ray attenuation coefficient values are a function of the mass of X-ray absorbing potassium-iodide tracer present in voxels. Mean φd values of 3.8% and 6.5% were obtained with the calibration and the relative approaches, respectively. The detection limits for φd measurements at individual voxel locations are 20% and 36% with the calibration and the relative methods, respectively. The detection limit for C(t) are 0.12 M and 0.22 M with the calibration and the relative approaches, respectively. Results from the calibration method are affected by a beam-hardening artifact and although results from the relative approach are not affected by the artifact, they are subject to high detection limits. This work presents a quantitative assessment of micro-CT data for studies of solute transport. Despite limitations in precision and accuracy, the method provides quantitative 3-D distributions of φd and C(t) that reflect solute diffusion in heterogeneous porous geologic media.
► 3-D spatial distributions of diffusion-accessible porosity determined using micro-CT
► 3-D spatial and temporal distributions of tracer concentrations measured with micro-CT
► Spatially resolved datasets that can be used for constraining solute transport numeric modeling
Journal: Journal of Contaminant Hydrology - Volume 145, February 2013, Pages 44–53