A leaching model is a hydrological model by which the leaching with irrigationwater of dissolved substances, notably salt, in the soil is described depending on the hydrological regime and the soil's properties. The model may describe the process in time and as a function of amount of water applied. Leaching is often done to reclaimsaline soil or to conserve a favorable salt content of the soil of irrigated land as all irrigation water contains salts.
Leaching curves
The leaching process in a salty soil to be reclaimed is illustrated in the leaching curves of figure 1, derived from data of the Chacupe pilot area, Peru. It shows the soil salinity in terms of electrical conductivity of the soil solution with respect its initial value as a function of amount of water percolating through the soil. The top-soil leaches quickly. The salinity of the deeper soil first increases due to the salts leached from the top-soil, but later it also decreases.
Leaching efficiency
Owing to irregular distribution of salt in the soil or to irregularity of the soil structure, the leaching efficiency can be different from unity. Soils with a low leaching efficiency are difficult to reclaim. In the Tagus delta, Portugal, the leaching efficiency of the dense clay soil was found as low as 0.10 to 0.15. The soil could not be developed for intensive agriculture and was used for rearing of bulls in coarse natural pasture. The clay soil in the Nile delta, Egypt, on the other hand has a much better leaching efficiency of 0.7 to 0.8. In figure 3, leaching curves are shown for different leaching efficiencies, as assumed in the leaching modelSaltMod with data from the Mashtul pilot area. The observed values of soil salinity correspond best to a leaching efficiency of about 0.75. The figure illustrates the calibration process of leaching efficiency, which parameter is difficult to measure directly.
The total amount of water required to bring the soil salinity from an initially high value down to an acceptable value in accordance with the salt tolerance of the crops to be grown. From figure 1 it is seen that 800 mm of water is required to bring the soil salinity down to 60% of its original value in the soil layer at 40 to 60 cm depth. When the salinity must be less than 60%, extrapolation of the leaching curve, the use of a leaching equation or a leaching model like SaltMod is necessary to obtain a reliable estimate of the additional leaching requirement.
The annual amount of percolation water required to conserve an acceptable salt balance of the soil in accordance with the salt tolerance of the crops to be grown. The ratio
Leaching equation
The downward limb of the leaching curves, as in figure 3, can be described with the leaching equation:
Ct = Ci + exp
where C = salt concentration, Ct = C in the soil at time T, Co = C in the soil at time T=0, Ci = C of the irrigation water, EL = leaching efficiency, Qp = average percolation rate through the soil, and Ws = water stored in the soil at field saturation.
Leaching fraction
To conserve an acceptable salt balance of the soil in accordance with the salt tolerance of the crops to be grown, the leaching fraction must be at least:
FL = Ci/Cs
where Ci = salt concentration of the irrigation water, and Cs is the acceptable salt concentration of the soil moisture at field capacity in accordance with the salt tolerance of the crops to be grown.
