Spatial distribution of soil mineral‐N content (N min ) is a scale‐variant process. Precision farming assumes knowledge about the spatial distribution of N min . Moreover, sampling in management zones is based on the assumption of spatial dependence between sampling points. In the present study, variability structure of N min and the sources of variability were investigated. Within an agricultural landscape, N min was investigated across a field in a nested design over four consecutive years. Temporally unstable structure of individual nests require a sampling with several nests in the field. In the investigated field, 35%–49% of the total variability derived from small‐scale variability observed at spatial distances of <5 m and from sampling and analytical errors. Differences between 10 and 26 kg N ha –1 for the soil depth increment 0–60 cm can be expected. Uncertainty due to analytical errors were in the order of 5–10 kg N ha –1 for a 0–60 cm layer.
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Giebel et al. (2006) studied this question.
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