SSSAJ Journal of Natural Resources and Life Sciences Education
HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
 QUICK SEARCH:   [advanced]


     


This Article
Right arrow Figures Only
Right arrow Full Text Free
Right arrow Full Text (PDF) Free
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Services
Right arrow Similar articles in this journal
Right arrow Similar articles in ISI Web of Science
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Right arrow reprints & permissions
Citing Articles
Right arrow Citing Articles via HighWire
Right arrow Citing Articles via ISI Web of Science (10)
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Cornelis, W. M.
Right arrow Articles by Hartmann, R.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Cornelis, W. M.
Right arrow Articles by Hartmann, R.
GeoRef
Right arrow GeoRef Citation
Agricola
Right arrow Articles by Cornelis, W. M.
Right arrow Articles by Hartmann, R.
Related Collections
Right arrow Soil Erosion
Right arrow Water Content
Right arrow Water Retention/Capillary Pressure
Published in Soil Sci. Soc. Am. J. 68:1154-1161 (2004).
© 2004 Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA

DIVISION S-1—SOIL PHYSICS

A Conceptual Model to Predict the Deflation Threshold Shear Velocity as Affected by Near-Surface Soil Water

I. Theory

Wim M. Cornelis*, Donald Gabriels and Roger Hartmann

Ghent University, Dep. Soil Management and Soil Care, International Centre for Eremology, Coupure links 653, B-9000 Gent, Belgium

* Corresponding author (wim.cornelis{at}UGent.be).

A crucial parameter in predicting wind erosion is the deflation threshold shear velocity, which is highly dependent on near-surface soil water. The empirical and theoretical models to predict the deflation threshold as affected by near-surface water that have been reported in literature all suffer from a weak physical background and very large differences between the predicted results can be observed. The present study was conducted to develop a new conceptual model to predict the deflation threshold as affected by near-surface wetness and to contribute to a better understanding of the role of the latter on deflation of sediment. The model was developed by solving the moment balance equation for entrainment of soil particles by wind, including the moments associated with drag forces, lift forces, aerodynamic moment forces, gravitational forces, and interparticle forces due to dry and wet bonding. The wet bonding force, which represents the effect of near-surface soil water, is due to liquid bridge bonding or capillary forces, and adsorbed layer bonding or adhesive forces. It was related to the particle diameter squared, surface tension squared and the inverse of matric potential. The latter was then converted to water content by assuming a logarithmic relationship, which was shown to be valid between oven dryness and a matric potential of –1.5 MPa, a range that is of interest in the light of deflation of soil particles by wind. The conceptual model presented in this paper is relatively simple and predicts, for a given particle diameter and surface tension, the deflation threshold shear velocity as a function of the ratio between water content and the water content at a matric potential of –1.5 MPa.




This article has been cited by other articles:


Home page
Progress in Physical GeographyHome page
J. E. Bullard
Arid geomorphology
Progress in Physical Geography, August 1, 2006; 30(4): 542 - 552.
[PDF]


Home page
Soil Sci.Home page
W. M. Cornelis, M. Khlosi, R. Hartmann, M. Van Meirvenne, and B. De Vos
Comparison of Unimodal Analytical Expressions for the Soil-Water Retention Curve
Soil Sci. Soc. Am. J., October 27, 2005; 69(6): 1902 - 1911.
[Abstract] [Full Text] [PDF]


Home page
Soil Sci.Home page
W. M. Cornelis, D. Gabriels, and R. Hartmann
A Conceptual Model to Predict the Deflation Threshold Shear Velocity as Affected by Near-Surface Soil Water: II. Calibration and Verification
Soil Sci. Soc. Am. J., July 1, 2004; 68(4): 1162 - 1168.
[Abstract] [Full Text] [PDF]




HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
The SCI Journals Agronomy Journal Crop Science
Journal of Natural Resources
and Life Sciences Education
Vadose Zone Journal
Journal of Plant Registrations Journal of
Environmental Quality
The Plant Genome
Copyright © 2004 by the Soil Science Society of America.