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Modelling porous structures by repeated Sierpinski carpets
Porous materials such as sedimentary rocks often show a fractal character at certain length scales. Deterministic fractal generators, iterated upto several stages and then repeated periodically, provide a realistic model for such systems. On the fractal, diffusion is anomalous, and obeys the law 〈 r...
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Published in: | Physica A 2001-03, Vol.292 (1), p.1-8 |
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Main Authors: | , , , |
Format: | Article |
Language: | English |
Subjects: | |
Citations: | Items that this one cites Items that cite this one |
Online Access: | Get full text |
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Summary: | Porous materials such as sedimentary rocks often show a fractal character at certain length scales. Deterministic fractal generators, iterated upto several stages and then repeated periodically, provide a realistic model for such systems. On the fractal, diffusion is anomalous, and obeys the law 〈
r
2〉∼
t
2/
d
w
, where 〈
r
2〉 is the mean square distance covered in time
t and
d
w
>2 is the random walk dimension. The question is: How is the macroscopic diffusivity related to the characteristics of the small scale fractal structure, which is hidden in the large-scale homogeneous material? In particular, do structures with same
d
w
necessarily lead to the same diffusion coefficient at the same iteration stage? The present paper tries to shed some light on these questions. |
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ISSN: | 0378-4371 1873-2119 |
DOI: | 10.1016/S0378-4371(00)00573-2 |