Abstract
The effect of the chloride ions (Cl−) on the efficiency of Fe0/sand systems for methylene blue (MB) discoloration was characterized in column studies for 4months. Tested systems were: pure sand (0% Fe0 – reference) and Fe0/sand (50% Fe0 – vol/vol). Tested Cl− concentrations were 0.0, 2.1, 21.1 and 42.2mM. The used MB concentration was 16μM (5mgL−1) and used Fe0 mass was 100g. Discoloration experiments lasted for 89days and was followed by a 26days desorption experiment. Each system was characterized by the time-dependent changes of the pH value, the iron breakthrough, the MB breakthrough, and the hydraulic conductivity (permeability). During the discoloration experiments, a total of 17.4L (184 pore volumes) of the MB solution flowed through each column (279.0μM dye or 87.2mg). No significance changes in pH value and permeability could be documented. Discoloration and desorption results confirmed that sand is an excellent MB adsorbent (only 11% desorption in the reference system). In the absence of Cl−, 15mg MB was discolored. Up to 18mg of MB was discolored in the presence of Cl−. The same trend was observed in changes of the extent of iron release which was 7.3mg at 0.0mM Cl− and 16.2mg at 42.2mM Cl−. These results confirm that chloride ions enhance the kinetics of Fe0 corrosion and thus the production of contaminant collectors (for MB co-precipitation). Results confirmed the suitability of MB as a powerful operative indicator for the characterization of processes in the Fe0/H2O system.
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