4.7 Article

Excluded-volume expansion of Archie's law for gas and solute diffusivities and electrical and thermal conductivities in variably saturated porous media

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WATER RESOURCES RESEARCH
卷 46, 期 -, 页码 -

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AMER GEOPHYSICAL UNION
DOI: 10.1029/2009WR008424

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资金

  1. Japan Society for the Promotion of Science (JSPS) [206192, 18360224]
  2. Innovative Research Organization, Saitama University
  3. Danish Research Council for Technology and Production Sciences
  4. Grants-in-Aid for Scientific Research [18360224] Funding Source: KAKEN

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Describing and predicting gas and solute diffusivities and electrical and thermal conductivities under variably saturated fluid conditions are necessary for simulating gas, solute, and heat transport in soils. On the basis of comprehensive data for gas (D(p)) and solute (D(s)) diffusivities and electrical (EC) and thermal (TC) conductivities for differently textured and variably saturated soils, we investigated analogies and differences between the four parameters. At fluid (water or air) saturation, relative parameter values for D(p), D(s), and EC were all well described by an excluded- volume expansion of Archie's first law. The cementation exponent in Archie's first law was close to 1.5 for all parameters. At fluid- unsaturated conditions, relative values of D(p), D(s), and EC (normalized at fluid saturation) were well described by an excluded- volume expansion of Archie's second law. In the case of relative TC, the saturation exponent in Archie's second law was substituted by the inverse of it for the three other parameters since water bridge effects dramatically enhance the TC with increasing moisture contents in relatively dry porous media. If appropriate but different expressions for a percolation threshold in Archie's second law were applied for the four parameters, a saturation exponent value of around 2.0 generally gave accurate predictions of all four parameters for differently textured soils. Finally, the excludedvolume expansion of Archie's second law was modified to also represent porous media with bimodal pore size distribution and well- described data for D(p) and D(s) in aggregated soil.

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