SSSAJ Journal of Natural Resources and Life Sciences Education
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Fig. 2. Breakthrough curves of Cl-, brilliant sulfaflavine (BF), and sulforhodamine B (SB) in different soil core (# refers to soil core number) layers. Normalized concentrations, c = C/C0, in the outflow from soil cores are plotted vs. cumulative drainage. C is the concentration in the effluent; C0 is the input concentration. Lines are breakthrough curves predicted by the convection dispersion model that is calibrated to the Cl- breakthrough.





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