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Fig. 3. Result of the simulations made with predicted hydraulic parameters and using the two types of prediction for hydraulic conductivity: K_s with L = 0.5 (cross), and K₀ with L $!=$ 0.5 (circles). Mean and spread of the soil moisture content as measured by means of six time domain reflectometry probe replicates are shown (thick line: mean; thin lines: mean ± sd).