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Fig. 4. Comparison of solute transport parameters pore water velocity (v) and dispersion coefficient (D) for surface soils (25-cm depth) of Ellsworth et al. (1996), obtained by least-squares optimization (LSO) using CXTFIT (Toride et al., 1995) and by the method of moments (MOM), after each of 39 solute BTCs were scaled by their respective zeroth moment.