Nuclear magnetic relaxation in fractal pores
- 1 November 1986
- journal article
- research article
- Published by American Physical Society (APS) in Physical Review B
- Vol. 34 (9) , 6503-6505
- https://doi.org/10.1103/physrevb.34.6503
Abstract
The theory of nuclear magnetic relaxation of a fluid in a porous medium is applied to the case of a medium having a fractal structure resembling a Menger sponge. Rapid diffusion within a pore is assumed and the limiting cases of rapid and vanishing diffusion between pores are treated. The results are compared with experiments on two sandstone samples. There is good qualitative agreement with the case of vanishing interpore diffusion but poor quantitative agreement. It appears that the quantitative disagreement could be at least partially removed by including moderate diffusion between pores. DOI: http://dx.doi.org/10.1103/PhysRevB.34.6503 © 1986 The American Physical SocietyKeywords
This publication has 3 references indexed in Scilit:
- Fractal Sandstone Pores: Implications for Conductivity and Pore FormationPhysical Review Letters, 1985
- Nuclear magnetic resonance in sedimentary rocks: Effect of proton desorption rateJournal of Applied Physics, 1982
- Nuclear magnetic relaxation and the internal geometry of sedimentary rocksJournal of Applied Physics, 1982