. Recovery of 15 N-labelled fertilizers applied to barley on two artificially eroded soils in north-central Alberta. Can. J. Soil Sci. 78: 377-383. Soil erosion induces variability in soil properties which may influence nutrient use efficiency. A 2-yr field study was conducted with the following objectives: (1) to determine the recovery of 15 N-labelled fertilizers applied to barley growing on artificially eroded soil, and (2) to compare N losses from nitrate-and ammonia-based N fertilizers. Field experiments were conducted in north-central Alberta in 1991 and 1992 on an Orthic Gray Luvisol (Site 1) and on an Eluviated Black Chernozem (Site 2) soil. At each site, a factorial experiment of three levels of artificial erosion (0, 10 and 20 cm) and three N sources (KNO 3 , urea, and control) was laid out as a split-plot design with four replications. The 15 N-labelled fertilizers (5.63 atom % abundance) were banded in June 1991 at 150 kg N ha -1 within 46-cm by 46-cm steel frame microplots. The proportion of added N recovered by barley (Hordeum vulgare L.) was not affected by erosion level. Periodical water saturation and NO 3 -availability suggested denitrification as a major mechanism of N loss. The N losses ranged from 12 to 51 kg N ha -1 in 1991 and 20 to 80 kg N ha -1 over the 2-yr period, but the N losses did not relate to erosion level. The N losses after 2 yr were greater from KNO 3 than from urea at Site 1. Most of the added 15 N was found in the surface 0-to 15-cm layer, but amounts of 15 N were detected in the 15-to 30-cm or 30-to 45-cm layers. The results call for continued development of N management techniques geared to optimize crop growth and minimize losses from fields. L'état physique du sol après une période de saturation en eau et la répartition du N de fumure dans le profil permettent de voir la dénitrification comme le principal mécanisme responsable des pertes de N. Ces dernières allaient de 12 à 51 kg ha -1 en 1991 et de 20 à 80 pour l'ensemble des 2 années, mais elles ne démontraient aucun lien particulier avec le niveau d'érosion. À l'emplacement 1, les pertes de N au terme des deux années étaient plus fortes dans la fumure au KNO 3 que dans celle à l'urée. La plus grande partie du N de fumure marqué était concentrée dans les 15 premiers centimètres du sol, mais on en trouvait un peu aussi dans les tranches de 15-30 ou de 30-45 cm. Ces observations montrent la nécessité de poursuivre la recherche de techniques de conduite de la fumure N axées à la fois sur l'optimisation de la croissance des cultures et sur la minimisation des pertes de N au champ.