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a Dep. of Soil and Water Sciences, The Hebrew Univ. of Jerusalem, Rehovot 76100, Israel
b Inst. of Soil Science, Univ. of Hannover, Germany
* Corresponding author (yona.chen{at}agri.huji.ac.il)
Most methods used to characterize the magnitude of soil water repellency consist of direct or indirect measurements of the initial advancing contact angle (
) at the solidliquidvapor interface. Aqueous ethanol solutions (AETS) are commonly used as testing liquids having different liquidvapor surface tensions (
LV); however,
measurements using AETS have rarely been performed on water-repellent soils (WRS). Measurements of
in this study were conducted using both the Wilhelmy plate method (WPM) and the CRM (weight-gain capillary rise method) for three natural and four hydrophobized WRS (water-repellent soils). The values of the Young equation (solidvapor and solidliquid surface tension) were calculated, and correlated with the GoodsGirifalco interaction parameter,
. The factor
was found to be a linear function of the solidliquid surface tension:
= 1 0.011
SL, with no significant differences between soils. This relation was then used to formulate an ESIT (empirical equation of state of interfacial tension), suggesting that from one universal constant,
can be predicted as function of
SV. The applicability of the ESIT approach to WRS was found to be inferior, in contrast to its successful use for ideal solid polymers. Nevertheless, it was found that for a waterWRS system,
was
0.6 rather than 1.0 as previously assumed. Applying
= 0.6 was successfully used in predicting
SV as well as the hydrophilic domain of
vs.
LV for water and AETS.
Abbreviations: AETS, aqueous ethanol solutions CRM, weight-gain capillary rise method EP, eucalyptus ESIT, equation of state of interfacial tension MED, molarity of ethanol droplet OM, organic matter OR, orange orchard PN, pine WPM, Wilhelmy plate method WRS, water-repellent soils
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