Predicting the Gas Diffusion Coefficient in Undisturbed Soil from Soil Water Characteristics
P. Moldrupa,
T. Olesena,
P. Schjønningb,
T. Yamaguchic and
D.E. Rolstond
a Environ. Engineering Lab., Dep. of Civil Engineering, Aalborg Univ., Sohngaardsholmsvej 57, DK-9000 Aalborg, Denmark
b Dep. of Crop Physiology and Soil Sci., Danish Inst. of Agric. Sci., Research Centre Foulum, P.O. Box 50, DK-8830 Tjele, Denmark
c Dep. of Civil and Environ. Engineering, Faculty of Engineering, Hiroshima Univ., 1-4-1 Kagamiyama, Higashi-Hiroshima, 739, Japan
d Soils and Biogeochemistry, Dep. of Land, Air, and Water Resour., Univ. of California, Davis, CA 95616 USA

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Fig. 1 Gas diffusivity as a function of air-filled porosity at -100 cm H2O of soil water potential. Data for 126 different soils and soil layers (752 measurements)
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Fig. 3 Test of the new soil water characteristicdependent DP/D0 model (Eq. [7]) against independent gas diffusivity data for six undisturbed soils. Data from Freijer (1994)
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Fig. 4 Scatterplot comparison of predicted (Eq. [7]) and measured gas diffusivities for 21 undisturbed soils. Note logarithmic scale
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Copyright © 2000 by the Soil Science Society of America.