Slow release N fertilizers are receiving increasing attention for use on turf grass, but their fate in the plant-soil system is still poorly understood. We aimed to quantify the uptake and recovery of N by a mixture of grasses when applied as either urea or oxamide in different diameter granules using a tracer technique (N-15). The effects of the N source on soil biomass, root density and amount of readily available organic C in soil were also evaluated. In a first experiment oxamide in 4-5 mm diameter granules was compared with urea. The initial N absorption, 40 days after fertilization (d.a.f.), was higher for urea (23.5%) than for oxamide (12.1%), but after 64 days absorption efficiencies were about the same (11%) for both fertilizers. Fertilizer-derived N lost by leaching was much greater from the urea-fertilized soil (1.57 g), compared with losses from oxamide-fertilized soil (0.05 g). The total residual fertilizer N remaining in the system at the end of the experiment was 26.7% of applied urea N and 39.6% of applied oxamide N. Cumulated absorption efficiencies, calculated after dismantling the lysimeters, were 43. 1 % for urea and 54.8% for oxamide (roots included). A priming effect caused by a larger uptake of soil N because of the better root development was found in the oxamide-treated lysimeter. Fertilization with oxamide also caused an increase in the amount of soil microbial biomass. In a second experiment, the efficiencies and fertilizer N uptake rates from oxamide applied at two different granule sizes (1-2 mm and 5-10 mm) were evaluated. The amount of soil N taken up by the grass was linearly related to root density (r = 0.92).
FATE OF NITROGEN (N-15) FROM OXAMIDE AND UREA APPLIED TO TURF GRASS - A LYSIMETER STUDY
DE NOBILI, Maria;SANTI, Simonetta;
1992-01-01
Abstract
Slow release N fertilizers are receiving increasing attention for use on turf grass, but their fate in the plant-soil system is still poorly understood. We aimed to quantify the uptake and recovery of N by a mixture of grasses when applied as either urea or oxamide in different diameter granules using a tracer technique (N-15). The effects of the N source on soil biomass, root density and amount of readily available organic C in soil were also evaluated. In a first experiment oxamide in 4-5 mm diameter granules was compared with urea. The initial N absorption, 40 days after fertilization (d.a.f.), was higher for urea (23.5%) than for oxamide (12.1%), but after 64 days absorption efficiencies were about the same (11%) for both fertilizers. Fertilizer-derived N lost by leaching was much greater from the urea-fertilized soil (1.57 g), compared with losses from oxamide-fertilized soil (0.05 g). The total residual fertilizer N remaining in the system at the end of the experiment was 26.7% of applied urea N and 39.6% of applied oxamide N. Cumulated absorption efficiencies, calculated after dismantling the lysimeters, were 43. 1 % for urea and 54.8% for oxamide (roots included). A priming effect caused by a larger uptake of soil N because of the better root development was found in the oxamide-treated lysimeter. Fertilization with oxamide also caused an increase in the amount of soil microbial biomass. In a second experiment, the efficiencies and fertilizer N uptake rates from oxamide applied at two different granule sizes (1-2 mm and 5-10 mm) were evaluated. The amount of soil N taken up by the grass was linearly related to root density (r = 0.92).I documenti in IRIS sono protetti da copyright e tutti i diritti sono riservati, salvo diversa indicazione.