Tortuosity of an unsaturated sandy soil estimated using gas diffusion and bulk soil electrical conductivity: Comparing analogy-based models and lattice-Boltzmann simulations

被引:28
作者
Weerts, AH
Kandhai, D
Bouten, W
Sloot, PMA
机构
[1] Unilever Res Colworth, Sharnbrook MK44 1LQ, Beds, England
[2] Univ Amsterdam, Fac Sci, Inst Biodivers & Ecosyst Dynam, NL-1018 WV Amsterdam, Netherlands
[3] Delft Univ Technol, Kramers Lab Fys Technol, Fac Sci Appl, NL-2628 BW Delft, Netherlands
[4] Univ Amsterdam, Fac Sci, Inst Informat, NL-1098 SJ Amsterdam, Netherlands
关键词
D O I
10.2136/sssaj2001.1577
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
Prediction of gas and ion diffusion in unsaturated soils has been obstructed by the inability to independently measure tortuosity parameters. Analogies between transport processes are often suggested to assess these nonmeasurable parameters. However, it is unclear whether these analogies are valid in unsaturated soils. Therefore, to obtain a more fundamental insight into the differences between ion and gas diffusion in an unsaturated sandy soil a different approach than current empirical models is required. In this study, fitted tortuosity parameter values of analogy-based models describing the gas diffusion coefficient and bulk soil electrical conductivity (ion diffusion) of a sandy soil are compared. Gas diffusion in unsaturated soil is most affected by connectivity in contrast to electrical conductivity that is among other factors primarily determined by tortuosity. Measured gas diffusion and electrical conductivity are also compared with lattice-Boltzmann simulated gas and ion diffusion as a function of water content in a thin section (two dimensional) of a sandy soil. Results of the lattice-Boltzmann simulations are in qualitative agreement with measured diffusional ratios and support the findings with the analogy-based models. Lattice-Boltzmann simulations may be a valuable tool to overcome empirism of current models and increase our insight in transport properties of unsaturated soils in the coming years.
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收藏
页码:1577 / 1584
页数:8
相关论文
共 34 条
[1]   Calculation of the effective diffusivity of heterogeneous media using the lattice-Boltzmann method [J].
AlvarezRamirez, J ;
NievesMendoza, S ;
GonzalezTrejo, J .
PHYSICAL REVIEW E, 1996, 53 (03) :2298-2303
[2]   THE LATTICE BOLTZMANN-EQUATION - THEORY AND APPLICATIONS [J].
BENZI, R ;
SUCCI, S ;
VERGASSOLA, M .
PHYSICS REPORTS-REVIEW SECTION OF PHYSICS LETTERS, 1992, 222 (03) :145-197
[3]  
BIRD RB, 1956, ADV CHEM ENG, P155
[4]  
Brooks R. H., 1966, J. Irrig. Drain.Div, V92, P61, DOI [10.1061/JRCEA4.0000425, DOI 10.1061/JRCEA4.0000425]
[5]   SIMPLE METHOD FOR DETERMINING UNSATURATED CONDUCTIVITY FROM MOISTURE RETENTION DATA [J].
CAMPBELL, GS .
SOIL SCIENCE, 1974, 117 (06) :311-314
[6]   LATTICE METHODS AND THEIR APPLICATIONS TO REACTING SYSTEMS [J].
CHEN, S ;
DAWSON, SP ;
DOOLEN, GD ;
JANECKY, DR ;
LAWNICZAK, A .
COMPUTERS & CHEMICAL ENGINEERING, 1995, 19 (6-7) :617-646
[7]  
Chopard B., 1998, Cellular Automata Modeling of Physical Systems
[8]   A COMPARISON OF GAS DIFFUSIVITY MODELS FOR UNSATURATED POROUS-MEDIA [J].
COLLIN, M ;
RASMUSON, A .
SOIL SCIENCE SOCIETY OF AMERICA JOURNAL, 1988, 52 (06) :1559-1565
[9]   MODELING WATER INFILTRATION IN UNSATURATED POROUS-MEDIA BY INTERACTING LATTICE-GAS CELLULAR-AUTOMATA [J].
DIPIETRO, LB ;
MELAYAH, A ;
ZALESKI, S .
WATER RESOURCES RESEARCH, 1994, 30 (10) :2785-2792