Fractal geometry of rocks

被引：139

作者：

Radlinski, AP

Radlinska, EZ

Agamalian, M

Wignall, GD

Lindner, P

Randl, OG

机构：

[1] Australian Geol Survey Org, Canberra, ACT 2601, Australia

[2] Australian Natl Univ, Dept Appl Math, Canberra, ACT 0200, Australia

[3] Oak Ridge Natl Lab, Div Solid State, Oak Ridge, TN 37831 USA

[4] Inst Max Von Laue Paul Langevin, F-38042 Grenoble, France

来源：

PHYSICAL REVIEW LETTERS | 1999年 / 82卷 / 15期

关键词：

D O I：

10.1103/PhysRevLett.82.3078

中图分类号：

O4 [物理学];

学科分类号：

0702 ;

摘要：

The analysis of small- and ultra-small-angle neutron scattering data for sedimentary rocks shows that the pore-rock fabric interface is a surface fractal (D-s = 2.82) over 3 orders of magnitude of the length scale and 10 orders of magnitude in intensity. The fractal dimension and scatterer size obtained from scanning electron microscopy image processing ate consistent with neutron scattering data. [S0031-9007(99)08945-0].

引用

页码：3078 / 3081

页数：4

共 23 条

[1] Optimization of a Bonse-Hart Ultra-Small-Angle Neutron Scattering facility by elimination of the rocking-curve wings [J].