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Fig. 2. Water retention, 
(h), and hydraulic conductivity, K(h), curves obtained through numerical inversion of the field-measured tension disk infiltrometer data (Runs A and B), by means of separate laboratory measurements (suction tables and pressure plates) followed by analysis with RETC, using the evaporation method on laboratory samples, and using Wooding's analysis. Results are for the surface layers of four soil profiles (LVgl1, LVgl2, LVgl3, and FLha) used in the experiments.
