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Jaime.F.
Sánchez and Rao S. Mylavarapu Abstract The use of models to evaluate the impact of agricultural practices in the contamination of water and soils is now a common practice. Leach-m is a model that uses the Richards equation to describe the water movement through the profile. The basic input to the model was obtained from water retention studies carried out in different farms, under specific fertilization programs, obtaining the Campbells parameters as well as bulk density, hydraulic conductivity and particle size distribution. In a selected profile, we compared the nitrate and ammonia contents observed in the field with the levels calculated by the model. Leach-m had the tendency to underestimate the ammonia content through the profile and overestimate the nitrate in the top layers. The probable reasons may be how Leach-m computes the movement of water in the soil profile. The parameters a and b of the Campbells retention function do not yield good results although the goodness of fit was high. However a best estimates of this parameter could be obtained using multivariate analysis that permit evaluate all the variables at the same time.
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Discussion and Conclusions In the spray area, the farmer is applying 294 kg of N ha-1 and 148 kg P ha-1. But the loadings are greater if we consider the grazing. From June to August, there is a period where rainfall is higher than evapo-transpiration. Application of poultry manure during this period may be avoided. Campbells parameters were adjusted with higher goodness of fit at the top layers of the soil. In the deeper layers (> 60 cm) the performance of the Campbells equation was poorer, suggesting that other models should be evaluated to describe the water movement in that soil. Bulk density is stable between 1.60 and 1.70 t m-3. Although the sand content reduced with depth (data not shown), lower bulk densities were observed in the surface layers. As expected, the water retention at 200 kPa of suction increased with depth. Leach-m over-estimated the nitrate content and under-estimated the ammonia content in the soil solution. This result confirmed that it is necessary for these soil types to use a different approach to adjust the Campbells parameters to improve the nitrate and ammonia prediction by Leach-m. |
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Bibliography Zavattaro, L.; C. Grignani. 2001. Deriving hydrological parameters for modeling water flow under field conditions. Soil Science Society of America Journal 65(3):655-667. Hutson, J.L.; A. Cass. 1987. A retentivity function for use in soil-water simulation models. Journal of Soil Science. 38:105-113. Campbell, G.S. 1974. A simple method for determining unsaturated conductivity from moisture retention data. Soil Science 117(6):311-314. Hutson, J.L. 1986. Water retentivity of some South African soils in relation to particle size criteria and bulk density. South African Journal of Plant and Soil 3(4):151-155 |