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  • 1
    Publication Date: 2001-03-01
    Print ISSN: 1351-0754
    Electronic ISSN: 1365-2389
    Topics: Geosciences , Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Published by Wiley
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  • 2
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Science Ltd
    European journal of soil science 52 (2001), S. 0 
    ISSN: 1365-2389
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences , Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Tillage and traffic modify soil porosity and pore size distribution, leading to changes in the unsaturated hydraulic properties of the tilled layer. These changes are still difficult to characterize. We have investigated the effect of compaction on the change in the soil porosity and its consequences for water retention and hydraulic conductivity. A freshly tilled layer and a soil layer compacted by wheel tracks were created in a silty soil to obtain contrasting bulk densities (1.17 and 1.63 g cm−3, respectively). Soil porosity was analysed by mercury porosimetry, and scanning electron microscopy was used to distinguish between the textural pore space and the structural pore space. The laboratory method of Wind (direct evaporation) was used to measure the hydraulic properties in the tensiometric range. For water potentials 〈 −20 kPa, the compacted layer retained more water than did the uncompacted layer, but the relation between the hydraulic conductivity and the water ratio (the volume of water per unit volume of solid phase) was not affected by the change in bulk density. Compaction did not affect the textural porosity (i.e. matrix porosity), but it created relict structural pores accessible only through the micropores of the matrix. These relict structural pores could be the reason for the change in the hydraulic properties due to compaction. They can be used as an indicator of the consequences of compaction on unsaturated hydraulic properties. The modification of the pore geometry during compaction results not only from a decrease in the volume of structural pores but also from a change in the relation between the textural pores and the remaining structural pores.
    Type of Medium: Electronic Resource
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  • 3
    Electronic Resource
    Electronic Resource
    Springer
    Agroforestry systems 49 (2000), S. 131-152 
    ISSN: 1572-9680
    Keywords: belowground competition ; Digitaria decumbens ; Gliricidia sepium ; root distribution ; two-dimensional soil-root water transport model
    Source: Springer Online Journal Archives 1860-2000
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Abstract A two-dimensional physically-based model for the daily simulation of root competition for water in an alley cropping system associating Gliricidia sepium with Digitaria decumbens is developed. This paper deals with the impact of root distribution on soil water partitioning. By adapting existing principles of root water uptake modelling for pure crops, the model accounts simultaneously for the sink terms of each species in a defined soil domain. Soil-root water transport functions are solved at the level of discrete volumes of soil; each of them are characterized by the inherent soil physical properties, root length density, soil-root distances, and the calculated sink terms of each species. The above ground boundary conditions, such as transpiration and soil evaporation, were managed by simple equations found from the literature or provided by experimental measurements. Running the model with two contrasting observed root maps, an evaluation was carried out over a 10-day period following a rainfall event. With both root maps, the simulated soil water potential profiles at the row, at 0.75 m and 1.50 m from the row did not differ significantly, and were in good agreement with the measurements. However, although water was not limiting during this period, the simulated cumulative water absorption profiles of G. sepium and D. decumbens contrasted markedly, and matched their observed root distribution. This model, although still under further development, forms the basis for development of an above and below ground coupled model to simulate plant interactions for water in intercrops or agroforestry.
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