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TECHNICAL REPORTS
Plant and Environment Interactions

Fate of Urine Nitrogen in Three Soils throughout a Grazing Season

UMR-INRA950, Université de Caen, esplanade de la paix, 14032 Caen, France

^* Corresponding author (cliquet{at}ibba.unicaen.fr)

Received for publication March 5, 2002. The fate of ¹⁵N-labeled cattle (Bos taurus) urine (52 g N m^-2), applied to a 0.4-m² surface area on three dates between May and October to three different pasture soils, was studied using 2-m² lysimeters. Over a period of two years, the sward recovered most of the ¹⁵N, but the amount recovered decreased with application date (62% in spring to 17% in fall). However, N uptake by ryegrass (Lolium perenne L.) in Year 2 showed that some nitrogen came from the previous year's urine application. The largest leaching losses of urine N resulted from the late application date. These losses mainly occurred during the first winter despite the small amount of water drainage. Soil type largely determined ¹⁵N losses. The granitic Brunisol was the most freely draining and had the greatest leaching (up to 35% recovery of urinary N). In contrast, leaching in the silty loam Neoluvisol remained under 4% of ¹⁵N applied. The Calcosol appeared to be susceptible to all kinds of N losses with intermediate unaccounted-for N pool and leaching fractions and lesser utilization of urinary N by grass. Immobilization in soil organic matter, roots and litter, and stubble pools were not markedly influenced by the date of application or soil type. They amounted to 25 to 33, 2, and 2% of N applied as urine, respectively. In these climatic conditions with moderate drainage, leaching of water poor in quality for nitrate only occurred for late-season grazing or on the granitic Brunisol, which was very vulnerable to leaching.

Abbreviations: DM, dry matter • SOM, soil organic matter

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