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Fig. 5. Relationship between the power parameter in the expression for the hydraulic conductivity function, ${eta}$ , and the coefficient of variation for the water retention curve, ${varepsilon}$ , for uncompacted (Uncomp., the calibration data from Assouline, 2005) and compacted (Comp.) soil samples. Equation [24] is the curve fitted to the data, and the dashed lines represent the 95% confidence limits of the fitted curve.