Fig. 4 Comparison of measured (filled circles) and calculated with the fractional advective–dispersive equation (FADE) (line) and with the advective–dispersive equation (ADE) (dotted line) Cl^- breakthrough curves in near-saturated clay soil; water flux was (a) 0.28 cm h^-1 and (b) 2.75 cm h^-1. Measured values are from Dyson and White (1987)

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