“…In addition to sampling point T2, three other points were included in the model: T5, T8, and T11, located at 0.60 m, 0.9 m and 1.2 m from the source, respectively, shown in (Figures 2a and 2c). The hydraulic parameters used in the analysis were determined based on the characteristics observed in the experimental study, with values of 0.327 m/d for the saturated hydraulic conductivity, 0.3 m/m for the hydraulic gradient, 0.098 m/d for the water velocity, 0.54 for the total porosity, and 1.63 kg/L for the soil's specific gravity (Martins et al 2012). The values of longitudinal (αL) and transversal (αT) dispersivity were estimated to be around 0.1 m and 0.04 m, respectively (Romero Velásquez 2015).…”