5. Conclusions
The application of the geostatistical approach including basic statistics, direct semivariograms, and cross-semivariograms improved the description of the spatial dependence between cereal yields and selected soil properties on a field scale. The cross-semivariograms and the kriging maps allowed delineating a field area with a low cereal yield and soil CEC, SOC, and pH. The reduced cereal yield in the distinct area was noted consistently in each of the three study years with different weather conditions. The distinct area is characterized by higher sand content and lower silt content, compared to other part of the field. This area in the experimental field along with some neighboring areas is seen on the aerial photographs as one similar zone separated by lighter soil color, probably due to the greater content of sand and the lower content of SOC. This implies that the analysis of the kriging maps together with a larger-scale aerial photographs allows delineating a larger critical zone based on the data of soil textural composition and organic carbon content that are often available in soil databases. In connection with this observation, further more detailed studies on the spatial relationships between crop yields and soil properties and on their usefulness in upscaling were undertaken on a larger scale.