2010
DOI: 10.1016/j.physleta.2010.01.002
|View full text |Cite
|
Sign up to set email alerts
|

A difference-fractal model for the permeability of fibrous porous media

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
3
1
1

Citation Types

1
30
0

Year Published

2011
2011
2019
2019

Publication Types

Select...
7

Relationship

0
7

Authors

Journals

citations
Cited by 70 publications
(32 citation statements)
references
References 34 publications
1
30
0
Order By: Relevance
“…Balankin et al (2006) thought that this phenomenon of wetting fluid advance in paper could be attributed to the complex time dependent due to swelling structure of paper. Fortunately, the randomness of pore sizes and the heterogeneity of natural porous media have been successfully characterized by fractal geometry such as sandstone rock (Katz and Thompson 1985), soil (Perfect and Kay 1991), artifact porous media (paper (Kopelman et al 1986;Balankin et al 2003), porous glasses (Kopelman et al 1986), porous membranes (Kopelman et al 1986), porous fabrics Shou et al 2010), and nanparticles (Xiao et al 2010a,b)). The behavior not obeying the LW equation may be explained based on the fractal nature of porous media.…”
Section: Introductionmentioning
confidence: 99%
“…Balankin et al (2006) thought that this phenomenon of wetting fluid advance in paper could be attributed to the complex time dependent due to swelling structure of paper. Fortunately, the randomness of pore sizes and the heterogeneity of natural porous media have been successfully characterized by fractal geometry such as sandstone rock (Katz and Thompson 1985), soil (Perfect and Kay 1991), artifact porous media (paper (Kopelman et al 1986;Balankin et al 2003), porous glasses (Kopelman et al 1986), porous membranes (Kopelman et al 1986), porous fabrics Shou et al 2010), and nanparticles (Xiao et al 2010a,b)). The behavior not obeying the LW equation may be explained based on the fractal nature of porous media.…”
Section: Introductionmentioning
confidence: 99%
“…1,2,4,7,8,11,13,[18][19][20] This means that the fractal theory can be used to predict the capillary pressure and water relative permeability of porous media. Besides, the pore size distribution and tortuosity of capillaries have also been proven to follow the fractal scaling laws, 2,4,8,18 i.e.…”
Section: Fractal Characteristics Of Unsaturated Porous Rocksmentioning
confidence: 99%
“…The capillary pressure (P c ) and relative permeability (k rw ) to water fluid flow in porous rocks are two key parameters to be considered in many fields including soil science, 1-3 reservoir engineering, 4-6 subsurface environmental engineering [7][8][9][10] and chemical engineering. [11][12][13][14][15] Past studies [15][16][17][18][19] have shown that the water flow processes in unsaturated porous rocks is complex and dependent on the complexity of the microstructure of rocks.…”
Section: Introductionmentioning
confidence: 99%
“…Convert the unit system of Eq. (20) into SI field unit system to facilitate example calculation and substitute the standard pressure, standard temperature and circular constant into the obtained equation, Eq. (20) will be simplified as:…”
Section: The Productivity Equation Ofmentioning
confidence: 99%
“…Fractal theory has been used to describe kinds of physical phenomenon in porous media, [16][17][18][19][20][21][22][23][24][25] such as the seepage characters of transient flow, [26][27][28] capillary imbibition, 29,30 non-Darcy flow, 31-33 thermal conductivity. 34 and multiphase flow.…”
Section: Introductionmentioning
confidence: 99%