Multiscale fluid transport theory for swelling biopolymers

被引:60
作者
Singh, PP
Cushman, JH
Maier, DE
机构
[1] Purdue Univ, Ctr Appl Math, W Lafayette, IN 47907 USA
[2] Univ Idaho, Dept Food Sci & Toxicol, Moscow, ID 83844 USA
[3] Purdue Univ, Dept Agr & Biol Engn, W Lafayette, IN 47907 USA
关键词
porous; glass transition; Fickian; non-Fickian; Darcian; Darcy's law;
D O I
10.1016/S0009-2509(03)00084-8
中图分类号
TQ [化学工业];
学科分类号
0817 ;
摘要
Fluid flow through a (bio) polymeric matrix has multiscale characteristics and is affected by the relaxation of surrounding polymers. Models developed in the past were either single scale (Polymer (1982) 23 (4) 529; Chemical Engineering Science (1992) 47 (12) 3037) or were limited to systems with a short memory (Achanta, 1995; Moisture transport in shrinking gels during drying, Ph.D. thesis, Purdue University, West Lafayette, IN). To address these limitations, we use the generalized Darcy's law equations of Singh (Effect of viscoelastic relaxation on fluid and species transport in biopolymeric materials, Ph.D. thesis) and the mass balance equations of Bennethum and Cushman (International Journal of Engineering Science (1996) 34 (2) 125) to develop a multiscale fluid transport model. The effect of viscoelastic relaxation of solid polymers on the flow of vicinal (adsorbed) fluid is considered at the mesoscale. At the macroscale two bulk fluids are incorporated, one of which is identical to the vicinal fluid. The mass balance equations for the vicinal fluid and its bulk counterpart are coupled via source/sink terms. The resulting fluid transport equation includes a novel integral term related to viscoelastic properties of the biopolymeric matrix. This term incorporates viscoelastic effects with both short and long memory. The model can describe both Darcian (Fickian) and non-Darcian (non-Fickian) modes of fluid transport. The model suggests fluid transport is Darcian in the rubbery and glassy states when the biopolymers are sufficiently far from the glass transition region. In the proximity of glass transition the flow of fluids is anomalous or non-Darcian. These predictions are in agreement with the experimental observations of Kim et al. (Chemical Engineering Science (1996) 51 (21) 4827). In spite of its multiscale characteristics, the resulting transport equation is simple and can be easily solved. The experimental parameters needed to solve the equation are the effective diffusivity, a sorption or drying curve and viscoelastic properties of the material. (C) 2003 Elsevier Science Ltd. All rights reserved.
引用
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页码:2409 / 2419
页数:11
相关论文
共 34 条
[21]   Multiscale flow and deformation in hydrophilic swelling porous media [J].
Murad, MA ;
Cushman, JH .
INTERNATIONAL JOURNAL OF ENGINEERING SCIENCE, 1996, 34 (03) :313-338
[22]   THE DIFFUSION OF SOME HALO-METHANES IN POLYSTRENE [J].
PARK, GS .
TRANSACTIONS OF THE FARADAY SOCIETY, 1950, 46 (08) :684-697
[23]   SOLVENT OSMOTIC STRESSES AND THE PREDICTION OF CASE II TRANSPORT KINETICS [J].
SARTI, GC .
POLYMER, 1979, 20 (07) :827-832
[24]  
Singh P. P., 2002, THESIS PURDUE U W LA
[25]  
SINGH PP, 2003, IN PRESS J MATH BIOL
[26]  
SINGH PP, 2002, UNPUB CHEM ENG SCI
[27]   A THEORY OF CASE-II DIFFUSION [J].
THOMAS, NL ;
WINDLE, AH .
POLYMER, 1982, 23 (04) :529-542
[28]   A DEFORMATION MODEL FOR CASE-II DIFFUSION [J].
THOMAS, NL ;
WINDLE, AH .
POLYMER, 1980, 21 (06) :613-619
[29]  
Tolstoguzov VB, 2000, NAHRUNG, V44, P76, DOI [10.1002/(SICI)1521-3803(20000301)44:2<76::AID-FOOD76>3.0.CO
[30]  
2-D, 10.1002/(SICI)1521-3803(20000301)44:2&lt