Abstract
An imbibition process at low infiltration rate into a soil, whose hydraulic conductivity at saturation K s decreaseswith depth, can lead to non monotonic water– content profiles and to the onset of a perched water table. By means of a numerical simulation of an infiltration process into a 1D, exponentially K s –decreasing soil, four different behaviors of the tensiometer–pressure profiles were observed at increasing the infiltration rate: either the solution remains monotonic, or a peak of water content onsets and vanishes and the solution recovers its monotonicity, or the peak vanishes but a perched water table onsets at the bottom and rises, or the peak itself reaches the water content at soil saturation at one point and there a perched water table onsets. This latter pattern was found in qualitative agreement with previously performed experimental results.
This is a preview of subscription content, log in via an institution.
Buying options
Tax calculation will be finalised at checkout
Purchases are for personal use only
Learn about institutional subscriptionsPreview
Unable to display preview. Download preview PDF.
References
Barontini, S., Ranzi, R.: Su alcune caratteristiche delle falde pensili in suoli gradualmente vari. In: Farina, W. (ed.) Atti del XXXII Convegno di Idraulica e Costruzioni Idrauliche, Palermo, p. 10 (2010)
Barontini, S., Ranzi, R., Bacchi, B.: Water dynamics in a gradually nonhomogeneous soil described by the linearized Richards equation. Water Resources Research 43 (2007), http://dx.medra.org/10.1029/2006WR005126 , doi:10.1029/2006WR005126
Barontini, S., Belluardo, G., Bacchi, B., Ranzi, R.: Esperimento per la verifica dell’innesco di una falda effimera in un terreno disomogeneo. In: Atti del XXXI Convegno di Idraulica e Costruzioni Idrauliche, Morlacchi, Perugia, p. 9 (2008)
Barontini, S., Belluardo, G., Ranzi, R.: Indagine sperimentale sulla formazione di una falda effimera in un suolo gradualmente vario. Technical Report 5/2009, Universitá degli Studi di Brescia, Dipartimento di Ingegneria Civile, Architettura, Territorio e Ambiente (2009)
Kirkby, M.J.: Infiltration, throughflow and overland flow. In: Chorley, R.J. (ed.) Water, Earth and Man, pp. 215–227. Taylor & Francis (1969)
Simunek, J., Sejna, M., van Genuchten, M.T.: The Hydrus–2D software package for simulating two–dimensional movement of water, heat, and multiple solutes in variably saturated media. Version 2.0. IGWMC–TPS–53, International Ground Water Modeling Center, Colorado School of Mines (1999)
van Asch, T., Van Beek, L.P.H., Bogaard, T.A.: The diversity in hydrological triggering systems of landslides. Rainfall–induced landslides. Mechanisms monitoring techniques and nowcasting models for early warning systems. In: Picarelli, L., Tommasi, P., Urciuoli, G., Versace, P. (eds.) Proceedings of the 1st Italian Workshop on Landslides, vol. 1 (2009)
Author information
Authors and Affiliations
Corresponding author
Editor information
Editors and Affiliations
Rights and permissions
Copyright information
© 2012 Springer-Verlag Berlin Heidelberg
About this paper
Cite this paper
Peli, M., Barontini, S., Bogaarda, T., Bacchi, B., Ranzi, R. (2012). Non Monotonic Imbibition Profiles and Transition to a Perched Water Table in a Gradually Layered Soil. In: Mancuso, C., Jommi, C., D’Onza, F. (eds) Unsaturated Soils: Research and Applications. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-31343-1_21
Download citation
DOI: https://doi.org/10.1007/978-3-642-31343-1_21
Publisher Name: Springer, Berlin, Heidelberg
Print ISBN: 978-3-642-31342-4
Online ISBN: 978-3-642-31343-1
eBook Packages: EngineeringEngineering (R0)