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Test of the Rosetta Pedotransfer Function for Saturated Hydraulic Conductivity

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Figure

Figure 3. Spatial distribution of the textural classes in
Table 4 and plotted in Figure 5. As previously, des-
Table 5. Measured values of sand, silt, clay, dry-bulk density (d, kg·m–3), and soil volumetric water content () at a suction of –33 kPa and –1500 kPa for the 18 locations shown in Figure 2
Figure 6. Linear regression between calculated and measured values of saturated hydraulic conductivity (Kfor each level of H is shown in the upper left hand corner

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