The within-field variability of soil mineral nitrogen (N-min) in a grazed g
rassland of 8000 m(2) was examined. NO3--N concentrations were characterize
d by a high spatial variability. This can be explained by the uneven deposi
tion of animal excreta. All NH4+-N as well as NO3--N values were lognormall
y distributed, be fore and after the grazing season. At the end of the graz
ing season the largest part of the variability of NO3--N was found for NO3-
-N concentrations measured within a distance of a few metres. A high variab
ility for NO3--N over very short distances was also indicated by a large nu
gget variance. During the grazing season, observed mean N-mn, values increa
sed from 22 to 132 kg N ha(-1). Regions with clearly higher NO3--N concentr
ations could be identified. These zones matched with the drinking place and
the entrance of the pasture, places which were more frequently visited tha
n others. High residual N levels in autumn led to relatively high losses of
N, mostly by leaching, during the subsequent drainage period. Knowing the
variability of N-min, the number of samples needed to estimate the average
N-min in a field could be calculated for different probabilities and variou
s degrees of precision. From the spatial distribution of the N-min concentr
ations and the restrictions imposed by the new European decree, adapted fer
tilizer strategies can be proposed at least for places where systematically
higher N-min concentrations can be expected.