The fractal menger sponge and Sierpinski carpet as models for reservoir rock/pore systems: I. ; Theory and image analysis of Sierpinski carpets
Journal Article
·
· In Situ; (United States)
OSTI ID:6883693
- Mobil Exploration and Producing Services, Inc., Dallas, TX (United States)
In this paper reservoir rock/pore systems are considered natural fractal objects and modeled as and compared to the regular fractal Menger Sponge and Sierpinski Carpet. The physical properties of a porous rock are, in part, controlled by the geometry of the pore system. The rate at which a fluid or electrical current can travel through the pore system of a rock is controlled by the path along which it must travel. This path is a subset of the overall geometry of the pore system. Reservoir rocks exhibit self-similarity over a range of length scales suggesting that fractal geometry offers a means of characterizing these complex objects. The overall geometry of a rock/pore system can be described, conveniently and concisely, in terms of effective fractal dimensions. The rock/pore system is modeled as the fractal Menger Sponge. A cross section through the rock/pore system, such as an image of a thin-section of a rock, is modeled as the fractal Sierpinski Carpet, which is equivalent to the face of the Menger Sponge.
- OSTI ID:
- 6883693
- Journal Information:
- In Situ; (United States), Journal Name: In Situ; (United States) Vol. 16:4; ISSN 0019-3267; ISSN ISOMDJ
- Country of Publication:
- United States
- Language:
- English
Similar Records
Fractal processes in soil water retention
Simulation of a critical Ising fractal
Fractal geometry characterization of geothermal reservoir fracture networks
Journal Article
·
Tue May 01 00:00:00 EDT 1990
· Water Resources Research; (United States)
·
OSTI ID:5454405
Simulation of a critical Ising fractal
Journal Article
·
Sun Dec 09 23:00:00 EST 1984
· Phys. Rev. Lett.; (United States)
·
OSTI ID:6256702
Fractal geometry characterization of geothermal reservoir fracture networks
Journal Article
·
Sat Dec 31 23:00:00 EST 1994
· Journal of Geophysical Research
·
OSTI ID:57312