Using X-ray computed tomography in hydrology: systems, resolutions, and limitations

被引:402
作者
Wildenschild, D [1 ]
Hopmans, JW
Vaz, CMP
Rivers, ML
Rikard, D
Christensen, BSB
机构
[1] Tech Univ Denmark, DK-2800 Lyngby, Denmark
[2] Lawrence Livermore Natl Lab, Expt Geophys Grp, Earth & Environm Sci Directorate, Livermore, CA 94551 USA
[3] Univ Calif Davis, Dept Land Air & Water Resources, Davis, CA 95616 USA
[4] CNPDIA, Embrapa Agr Instrumentat, BR-13560970 Sao Carlos, SP, Brazil
[5] Univ Chicago, Consortium Adv Radiat Sources, Chicago, IL 60637 USA
[6] Univ Chicago, Dept Geophys Sci, Chicago, IL 60637 USA
[7] Lawrence Livermore Natl Lab, Nondestruct Evaluat Sect, Livermore, CA 94551 USA
关键词
porous media; multi-phase flow; X-ray tomography; synchrotron radiation; pore structure; visualization;
D O I
10.1016/S0022-1694(02)00157-9
中图分类号
TU [建筑科学];
学科分类号
0813 ;
摘要
A combination of advances in experimental techniques and mathematical analysis has made it possible to characterize phase distribution and pore geometry in porous media using non-destructive X-ray computed tomography (CT). We present qualitative and quantitative CT results for partially saturated media, obtained with different scanning systems and sample sizes, to illustrate advantages and limitations of these various systems, including topics of spatial resolution and contrast. In addition, we present examples of our most recent three-dimensional high-resolution images, for which it was possible to resolve individual pores and to delineate air-water interfacial contacts. This kind of resolution provides a novel opportunity to follow the dynamic flow behavior on the pore scale and to verify new theoretical and numerical modeling approaches. (C) 2002 Elsevier Science Ltd. All rights reserved.
引用
收藏
页码:285 / 297
页数:13
相关论文
共 31 条
[1]   EVALUATION OF CONSTRUCTED AND NATURAL SOIL MACROPORES USING X-RAY COMPUTED-TOMOGRAPHY [J].
ANDERSON, SH ;
PEYTON, RL ;
GANTZER, CJ .
GEODERMA, 1990, 46 (1-3) :13-29
[2]   Transport in sandstone: A study based on three dimensional microtomography [J].
Auzerais, FM ;
Dunsmuir, J ;
Ferreol, BB ;
Martys, N ;
Olson, J ;
Ramakrishnan, TS ;
Rothman, DH ;
Schwartz, LM .
GEOPHYSICAL RESEARCH LETTERS, 1996, 23 (07) :705-708
[3]  
Bear J., 1988, DYNAMICS FLUIDS PORO
[4]   Computation of 3D curvatures on a wet snow sample [J].
Brzoska, JB ;
Lesaffre, B ;
Coléou, C ;
Xu, K ;
Pieritz, RA .
EUROPEAN PHYSICAL JOURNAL-APPLIED PHYSICS, 1999, 7 (01) :45-57
[5]   RECENT ADVANCES IN PORE SCALE MODELS FOR MULTIPHASE FLOW IN POROUS-MEDIA [J].
CELIA, MA ;
REEVES, PC ;
FERRAND, LA .
REVIEWS OF GEOPHYSICS, 1995, 33 :1049-1057
[6]   Determination of phase-volume fractions from tomographic measurements in two-phase systems [J].
Clausnitzer, V ;
Hopmans, JW .
ADVANCES IN WATER RESOURCES, 1999, 22 (06) :577-584
[7]   Pore-scale measurements of solute breakthrough using microfocus X-ray computed tomography [J].
Clausnitzer, V ;
Hopmans, JW .
WATER RESOURCES RESEARCH, 2000, 36 (08) :2067-2079
[8]   Three-dimensional snow images by X-ray microtomography [J].
Coléou, C ;
Lesaffre, B ;
Brzoska, JB ;
Ludwig, W ;
Boller, E .
ANNALS OF GLACIOLOGY, VOL 32, 2001, 2001, 32 :75-81
[9]   Developments in synchrotron X-ray microtomography with applications to flow in porous media [J].
Coles, ME ;
Hazlett, RD ;
Muegge, EL ;
Jones, KW ;
Andrews, B ;
Dowd, B ;
Siddons, P ;
Peskin, A ;
Spanne, P ;
Soll, W .
SPE RESERVOIR EVALUATION & ENGINEERING, 1998, 1 (04) :288-296
[10]   Three-dimensional quantitative textural analysis of metamorphic rocks using high-resolution computed X-ray tomography .1. Methods and techniques [J].
Denison, C ;
Carlson, WD ;
Ketcham, RA .
JOURNAL OF METAMORPHIC GEOLOGY, 1997, 15 (01) :29-44