2011
DOI: 10.1016/j.ijheatmasstransfer.2011.02.048
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Differential spontaneous capillary flow through heterogeneous porous media

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Cited by 25 publications
(17 citation statements)
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“…This classical result has been found to be valid for both unidirectional and radial capillary penetration in porous media [22][23][24][25], and is further extended to the hemispherical penetration in a semi-infinite porous medium [26] and imbibition in structured porous media with axially variable geometries [27]. However, recent studies have also indicated that this simple model is not applicable for some complex cases, such as flow processes in heterogeneous and random porous media, and some other effects, e.g., fractal and disorder, should be incorporated into the analysis [28][29][30][31][32].…”
Section: Introductionmentioning
confidence: 99%
“…This classical result has been found to be valid for both unidirectional and radial capillary penetration in porous media [22][23][24][25], and is further extended to the hemispherical penetration in a semi-infinite porous medium [26] and imbibition in structured porous media with axially variable geometries [27]. However, recent studies have also indicated that this simple model is not applicable for some complex cases, such as flow processes in heterogeneous and random porous media, and some other effects, e.g., fractal and disorder, should be incorporated into the analysis [28][29][30][31][32].…”
Section: Introductionmentioning
confidence: 99%
“…Cai et al (2010) extended Washburn's equation to characterize the process of water absorption in a porous medium. Some efforts have been made to characterize fluid flow in heterogeneous cross sections (Bal et al 2011;Reyssat et al 2008;Shou et al 2014;Xiao et al 2012). Mark et al (2012) stated that accurately estimating the capillary radius is essential for closely understanding and describing wicking phenomena.…”
Section: Introductionmentioning
confidence: 99%
“…The upper layer of agarose gel models has nanoscale pores that are invisible in X-ray images (e 1 ,e 2 ). 12 The average distance (6 standard error) between pores in the porous hydrogel models Figs. 4(a), 4(b), 4(c), and 4(d) is 1436 (676) lm, 1243 (6107) lm, 1028 (655) lm, and 796 (631) lm, respectively.…”
Section: B Double-layered Porous Agarose Gelmentioning
confidence: 99%
“…The capillary flow through multi-layered porous layers, such as packed beds of particles or absorbent materials, has been widely investigated experimentally and theoretically. [9][10][11][12][13][14][15] Reyssat et al, studied the imbibition of a wetting fluid into layers of packed beads 13 and Shou et al, studied the geometry induced asymmetric capillary flow to obtain the optimal geometry for fastest flow absorption. 10,11 However, little attention has been paid to the mass transport through multilayered porous structure by chemical potential difference.…”
mentioning
confidence: 99%