Full TGIF Record # 238392
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DOI:10.2136/sssaj2013.05.0182
Web URL(s):https://acsess.onlinelibrary.wiley.com/doi/10.2136/sssaj2013.05.0182
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Publication Type:
i
Refereed
Author(s):Davis, Dedrick D.; Horton, Robert; Heitman, Joshua L.; Ren, Tusheng
Author Affiliation:Davis: Dep. of Biological and Environ. Sci., Alabama A&M Univ., Normal, AL; Horton: Dep. of Agronomy, Iowa State Univ., Ames, IA; Heitman: Dep. of Soil Science, North Carolina State Univ., Raleigh, NC; Ren: Dep. of Soil and Water, China Agricultural Univ., Beijing, China
Title:An experimental study of coupled heat and water transfer in wettable and artificially hydrophobized soils
Section:Soil physics
Other records with the "Soil physics" Section
Source:Soil Science Society of America Journal. Vol. 78, No. 1, January/February 2014, p. 125-132.
Publishing Information:Madison, Wisconsin: Soil Science Society of America
# of Pages:8
Related DOI10.2134/csa2014-59-3-4 (CSA News summary)
Keywords:TIC Keywords: Heat transfer; Hydrophobic soils; Soil moisture; Temperatures; Thermal conductivity; Volumetric water content; Water transfer
Abstract/Contents:"The effect of soil wettability on coupled heat and water transfer in soil is not well understood. The objective of this work was to determine the effect of soil wettability on coupled heat and water transfer for two wettable soils and their artificially hydrophobized counterparts. Closed soil cells instrumented with heat-pulse sensors provided in situ measurements of soil temperature, soil volumetric water content (Θ), soil thermal conductivity (λ), and soil thermal diffusivity (α). Nonlinear temperature distributions developed in response to the 150°C m-1 temperature gradients applied to the soil cells for both the wettable and hydrophobized soils due to soil moisture redistribution. Hydrophobized sand and silt loam soils had different responses relative to their wettable counterparts. Soil moisture redistribution was similar in the wettable and hydrophobized sand soils. Net water transfer was reduced by 56% in the hydrophobized silt loam compared with the wettable silt loam. Reduced net water transfer in the hydrophobized silt loam indicated that water vapor transfer must have been lower in the hydrophobized silt loam than in the wettable silt loam. Diffusive pathways for water vapor may increase due to hydrophobicity. In both the wettable and hydrophobized soils, λ and α decreased in the warm regions and increased in the cold regions of the soil cells due to soil moisture redistribution. Wettability is a function of water content, and relative to wettable soil, water redistribution in hydrophobized soil is reduced only when the water content is small enough for the soil to behave as hydrophobic. If the water content is large enough for a hydrophobized soil to behave as wettable, water redistribution is similar to that in a wettable soil."
Language:English
References:44
Note:Summary appears in CSA News, 59(3) March 2014, p. 14 with additional picture
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ASA/CSSA/SSSA Citation (Crop Science-Like - may be incomplete):
Davis, D. D., R. Horton, J. L. Heitman, and T. Ren. 2014. An experimental study of coupled heat and water transfer in wettable and artificially hydrophobized soils. Soil Science Society of America Journal. 78(1):p. 125-132.
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DOI: 10.2136/sssaj2013.05.0182
Web URL(s):
https://acsess.onlinelibrary.wiley.com/doi/10.2136/sssaj2013.05.0182
    Last checked: 02/26/2024
    Access conditions: Item is within a limited-access website
https://acsess.onlinelibrary.wiley.com/doi/epdf/10.2136/sssaj2013.05.0182
    Last checked: 02/26/2024
    Requires: PDF Reader
    Access conditions: Item is within a limited-access website
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