Preferential flow in water repellent sandy soils: principles and modeling implications
@article{Ritsema2000PreferentialFI, title={Preferential flow in water repellent sandy soils: principles and modeling implications}, author={Coen J. Ritsema and Louis W. Dekker}, journal={Journal of Hydrology}, year={2000}, volume={231}, pages={308-319} }
149 Citations
Percolation characteristics of a water‐repellent sandy forest soil
- Environmental Science
- 2007
In a tracer experiment TDR transect measurements were made to study percolation behaviour in a 120‐year‐old pine stand (Pinus sylvestris) on a water‐repellent sandy soil (Haplic Arenosol). The…
Specific processes during in situ infiltration into a sandy soil with low-level water repellency
- Geology
- 2013
Seasonal soil water repellency and evaporation in a Mediterranean climate
- Environmental Science
- 2018
By limiting infiltration and facilitating preferential flow, water repellency in surface soils produces wetting patterns which differ substantially from those in comparable wettable soils. Seasonal…
Effect of soil water repellency on soil hydraulic properties estimated under dynamic conditions
- Environmental Science
- 2013
Spatial and temporal variability of water repellency in a sandy soil contaminated with tar oil and heavy metals.
- Environmental Science, MedicineJournal of contaminant hydrology
- 2006
Water repellency, near-saturated infiltration and preferential solute transport in a macroporous clay soil
- Chemistry
- 2008
Hydrologic behavior of model slopes with synthetic water repellent soils
- Environmental Science
- 2017
Variability of water repellency in sandy forest soils under broadleaves and conifers in north-western Jutland/Denmark.
- Geology
- 2018
Soil water repellency has important consequences for ecological and hydrological properties of soils and usually retards infiltration capacity and induces preferential flow. This phenomenon has been…
A new modelling approach to simulate preferential flow and transport in water repellent porous media: Parameter sensitivity, and effects on crop growth and solute leaching
- Geology
- 2005
A modified version of the popular agrohydrological model SWAP has been used to evaluate modelling of soil water flow and crop growth at field situations in which water repellency causes preferential…
References
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Water repellency is an important property of many soils. It causes rainwater to penetrate into the soil as preferential flow paths, and solutes can reach the groundwater more rapidly than in the case…
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Water and solute input rates on the soil surface may vary considerably from place to place. Distribution flow, i.e., the process of water and solute flow in a lateral direction over and through the…
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How water moves in a water repellent sandy soil: 2. Dynamics of fingered flow
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The dynamics of fingered flow in a water repellent sandy soil was studied in the field by sampling 10 vertical trenches in a 1-year cycle. In dry soil, fingers were formed in those places in the top…
A three-Region Analytical Model of Solute Leaching in a Soil with a Water-Repellent Top Layer
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When water enters a water-repellent topsoil, fingers develop and a large part of the soil is bypassed. Therefore fingering is expected to accelerate solute leaching to the groundwater. In soils with…
Recurring fingered flow pathways in a water repellent sandy field soil
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Abstract. Field evidence of finger formation and reformation during Successive rain events over an eight months' observation period from June 1994 until January 1995 is presented. Fingered flow…