Soil Use and Management · 2001 · 13 citations · 18 references
AgricultureEarth SciencesSoil SciencesSoil BiogeochemistrySoil Organic MatterSoil ScienceCation Exchange CapacityMineralizationNitrogen CycleNitrogen ManagementNutrient LeachingNutrient MineralizationFertilizer LeachingField Leaching ExperimentsLeachingNitrogen Fertilizer ManagementSoil Anion Exchange CapacitySoil Nitrogen LeachingSoil Nitrogen MineralizationSoil Nutrient Leaching
Abstract. 15 N labelled NH 4 NO 3 (fertilizer N) was applied at a rate of 50 kg N ha –1 to an Ando‐Humic Nitisol and two maize crops grown on it. About 20 months later, soil cores were taken to a depth of 2.5 m. Leached fertilizer N was found between 1.4 m and 1.8 m deep and was delayed relative to net drainage by between 4.2 and 4.9 pore volumes. Anion exchange capacity (AEC) increased ten‐fold down the profile, up to 2.9 cmol c kg –1 . The delay to fertilizer N leaching was predicted to be between 4.1 and 5.3 pore volumes when calculated from the AEC and from an equation relating delay due to AEC in laboratory columns of repacked soil obtained by Wong et al. (1990b). It was concluded that the nitrate leaching delay equation was also valid in undisturbed field profiles. Two concentration maxima for mineral N were found, which did not usually coincide with the fertilizer N and were thought to result from mineralization of soil organic matter and plant residues at the end of each season. The delay equation overestimated their leaching delay but the results were considered close enough to support the hypothesis for their formation.
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