Figures & data
Table 1. Average soil properties and standard error of the values of the experimental site.
Figure 2. Measured soil volumetric water content (%, by Percostation) in different depths under field (Hordeum vulgare L.) and grassland, precipitations (mm) and calculated evapotranspiration by Alpatjev in 2013.
![Figure 2. Measured soil volumetric water content (%, by Percostation) in different depths under field (Hordeum vulgare L.) and grassland, precipitations (mm) and calculated evapotranspiration by Alpatjev in 2013.](/cms/asset/335a3176-22aa-4887-b14d-d86c501aee46/sagb_a_1210210_f0002_b.gif)
Figure 3. Measured soil volumetric water content (%, by Percostation) at different depths under field (Solanum tuberosum L.) and grassland, precipitations (mm) and calculated evapotranspiration by Alpatjev in 2014.
![Figure 3. Measured soil volumetric water content (%, by Percostation) at different depths under field (Solanum tuberosum L.) and grassland, precipitations (mm) and calculated evapotranspiration by Alpatjev in 2014.](/cms/asset/8aae8f62-fad2-41e1-9193-6ee3e6b594aa/sagb_a_1210210_f0003_b.gif)
Figure 4. The correlation between measured and predicted soil volumetric moisture content (%) of upper 25 cm (average) of soil as an average of two years using the 2 h and daily step under cultivated (field) and grassland conditions. For daily predictions correlation is statistically significant (p < .05).
![Figure 4. The correlation between measured and predicted soil volumetric moisture content (%) of upper 25 cm (average) of soil as an average of two years using the 2 h and daily step under cultivated (field) and grassland conditions. For daily predictions correlation is statistically significant (p < .05).](/cms/asset/017dfcd1-d87e-4864-9796-b2abfe003fe9/sagb_a_1210210_f0004_b.gif)