Angstrom-to-millimeter characterization of sedimentary rock microstructure

被引:132
作者
Radlinski, AP
Ioannidis, MA
Hinde, AL
Hainbuchner, M
Baron, M
Rauch, H
Kline, SR
机构
[1] Geosci Australia, Canberra, ACT 2601, Australia
[2] Univ Waterloo, Dept Chem Engn, Waterloo, ON N2L 3G1, Canada
[3] Osterreich Univ, Inst Atom, Vienna, Austria
[4] Inst Max Von Laue Paul Langevin, F-38042 Grenoble, France
[5] NIST, Ctr Neutron Res, Gaithersburg, MD 20899 USA
基金
加拿大自然科学与工程研究理事会;
关键词
porous materials; pore size; small-angle scattering; fractals; magnetic resonance; mercury porosimetry;
D O I
10.1016/j.jcis.2004.02.035
中图分类号
O64 [物理化学(理论化学)、化学物理学];
学科分类号
070304 ; 081704 ;
摘要
Backscatter SEM imaging and small-angle neutron scattering (SANS) data are combined within a statistical framework to quantify the microstructure of a porous solid in terms of a continuous pore-size distribution spanning over five orders of magnitude of length scale, from 10 Angstrom to 500 mum. The method is demonstrated on a sample of natural sandstone and the results are tested against mercury porosimetry (MP) and nuclear magnetic resonance (NMR) relaxation data. The rock microstructure is fractal (D = 2.47) in the pore-size range 10 Angstrom - 50 mum and Euclidean for larger length scales. The pore-size distribution is consistent with that determined by MP. The NMR data show a bimodal distribution of proton T-2 relaxation times, which is interpreted quantitatively using a model of relaxation in fractal pores. Pore-length scales derived from the NMR data are consistent with the geometrical parameters derived from both the SEM/SANS and NIP data. The combined SANS/BSEM method furnishes new microstructural information that should facilitate the study of capillary phenomena in hydrocarbon reservoir rocks and other porous solids exhibiting broad pore-size distributions. (C) 2004 Elsevier Inc. All rights reserved.
引用
收藏
页码:607 / 612
页数:6
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