Published online 28 September 2007
Published in Soil Sci Soc Am J 71:1658-1666 (2007)
DOI: 10.2136/sssaj2006.0284
© 2007 Soil Science Society of America
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Water Repellency of Aggregate Size Fractions of a Volcanic Ash Soil
Ken Kawamotoa,*,
Per Moldrupb,
Toshiko Komatsua,
Lis Wollesen de Jongec and
Masanobu Odaa
a Graduate School of Science and Engineering, Saitama Univ., 255 Shimo-okubo, Sakura-ku, Saitama, 338-8570, Japan
b Environmental Engineering Section, Dep. of Biotechnology Chemistry, and Environmental Engineering, Aalborg Univ., Sohngaardsholmsvej 57, DK-9000 Aalborg, Denmark
c Dep. of Agroecology, Univ. of Aarhus, P.O. Box 50, DK-8830 Tjele, Denmark

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Fig. 1. Soil water characteristic curves for four soil samples. Fitted curves with the bimodal van Genuchten soil-water retention model (Durner, 1994) by Eq. [1] are given. The s values are plotted at pF = 0.
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Fig. 2. Chart of pretreatment procedures for the soil samples before the molarity of ethanol droplet (MED) tests. "Soil samples at pF 3.3 and 4.1" are soil samples with volumetric water contents corresponding to pF 3.3 and 4.1 in the soil-water retention curve. The water repellency (WR) curves (see Fig. 3) are depicted by using data for oven-dried samples at 60°C (subchart given by the gray boxes).
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Fig. 4. Comparison of volumetric water content and water repellency (WR) as a function of pF. Soil samples are from depths of (a) 0.00–0.05 m, (b) 0.03–0.06 m, (c) 0.05–0.10 m, and (d) 0.10–0.15 m.
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Copyright © 2007 by the Soil Science Society of America.