Abstract

From 1990 to 1998, we studied the N release from ploughed 3-year-old grazed grasslands in the subsequent three seasons of forage crops on a sandy loam soil. Silage maize in the ley–arable rotation outyielded continuous maize on permanent arable plots by 85, 21 and 2% at mineral N fertilization rates of respectively 0, 75 and 180 kg N ha −1. This decreasing yield effect with increasing N fertilization indicated that the ley–arable rotation effect was mainly a N-contribution effect. The N release was highest during the first year; it decreased during the second and third year following the grassland ploughing. Economically optimum N fertilization rates for silage maize in these years were respectively 2, 139 and 154 kg N ha −1. Simultaneously, on permanent arable plots this was respectively 152, 191 and 183 kg N ha −1. This resulted in comparable yields (19.75 Mg DM ha −1 year −1) but with a possible saving of 231 kg of mineral N fertilizer ha −1 in a 3-year silage maize period following the ploughed leys compared with continuous silage maize. The N uptake by silage maize on temporary arable plots following grasslands was higher than on permanent arable plots, owing to the higher yields but also to an increased N concentration in the crop on the temporary arable plots. Starting the arable forage crop sequence with fodder beet following the grassland ploughing and adjusting the N fertilization to the enhanced N release minimized the risks on high amounts of residual soil N and hence N leaching losses.

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