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DOI:10.2136/sssaj2001.1667
Web URL(s):https://acsess.onlinelibrary.wiley.com/doi/10.2136/sssaj2001.1667
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Publication Type:
i
Refereed
Author(s):Dekker, Louis W.; Doerr, Stefan H.; Oostindie, Klaas; Ziogas, Apostolos K.; Ritsema, Coen J.
Author Affiliation:Dekker, Oostindie, and Ritsema: Alterra, Land Use and Soil Processes Team, Wageningen, The Netherlands; Doerr: Dep. of Geography, Univ. of Wales Swansea, Singleton Park, Swansea, UK; Ziogas: Dep. of Civil Engineering, Demokritus Univ. of Thrace, Xanthi, Greece
Title:Water repellency and critical soil water content in a dune sand
Section:Soil physics
Other records with the "Soil physics" Section
Source:Soil Science Society of America Journal. Vol. 65, No. 6, November 2001, p. 1667-1674.
Publishing Information:Madison, Wisconsin: Soil Science Society of America
# of Pages:8
Keywords:TIC Keywords: Dune soils; Sand; Soil testing; Soil water content; Soil water relations; Water repellency
Dutch Turfgrass Research Foundation Keywords: 408-C; Soil water; Water repellent soils; Sandy soils; Duneland; Article
Abstract/Contents:"Assessments of water repellency of soils are commonly made on air-dried or oven-dried samples, without considering the soil water content. The objectives of this study were to examine the spatial and temporal variability of soil water content, actual water repellency over short distances, and the variations in critical soil water contents. Between 22 Apr. and 23 Nov. 1999, numerous samples were collected from a grass-covered dune sand (typic Psammaquent), at six depths, eight times in transects and two times in soil blocks. The water drop penetration time (WDPT) test was used to measure the actual water repellency of the field-moist samples and the potential water repellency after drying the samples at 25, 65, and 105°C. Highly spatial and temporal variability in water content and persistence of actual water repellency was found between the samples from all soil depths. At each depth we established an upper water content, below which samples were water repellent and a lower water content, above which samples were wettable. This water content range, called the transition zone, was different for each depth, and, for example, assessed at 0- to 2.5-cm depth between soil water contents of 18 and 23% (vol./vol.), and at 16.5- to 19-cm depth between 2 and 5% (vol./vol.). The potential water repellency of samples dried at 25 and 65°C was on some days less severe than the actual repellency of field-moist samples on other days, thus underestimating the maximal persistence of water repellency that can occur in the field. Drying of the samples at 105°C significantly increased the potential water repellency."
Dutch Turfgrass
Research Foundation
Abstract
(Thanks to DTRF)
"Wetting agents goed in de grond brengen, is nog niet zo eenvoudig. Speciale machines die het middel met hoge druk inbrengen, werken niet optimaal. Hay Aerts experimenteert momenteel met een nieuw eenvoudig systeem, Prick and Spray. En het werkt"
Language:English
References:24
Note:Pictures, b/w
Figures
Graphs
ASA/CSSA/SSSA Citation (Crop Science-Like - may be incomplete):
Dekker, L. W., S. H. Doerr, K. Oostindie, A. K. Ziogas, and C. J. Ritsema. 2001. Water repellency and critical soil water content in a dune sand. Soil Science Society of America Journal. 65(6):p. 1667-1674.
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DOI: 10.2136/sssaj2001.1667
Web URL(s):
https://acsess.onlinelibrary.wiley.com/doi/10.2136/sssaj2001.1667
    Last checked: 02/29/2024
    Access conditions: Item is within a limited-access website
https://acsess.onlinelibrary.wiley.com/doi/epdf/10.2136/sssaj2001.1667
    Last checked: 02/29/2024
    Requires: PDF Reader
    Access conditions: Item is within a limited-access website
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