Mechanism of Removing Iron and Manganese from Drinking Water Using Manganese Ore Sand and Quartz Sand as Filtering Material

Abstract

Two lab-scale biofilters packed with manganese ore sand and quartz sand were constructed to reveal the behavior in removing iron and manganese during the start-up period. Meanwhile, the removal mechanism of the two sands was also investigated by means of EDS, XPS, and SEM. With the influent iron (2-3 mg·L-1) and manganese (0.3-0.6 mg·L-1), the start-up operational results indicated that the quartz sand biofilter needed 15 and 30 d to achieve the removal of iron and manganese, respectively. The manganese ore sand only required 10 d to remove iron, while the effluent manganese was always below of 0.1 mg·L-1. The results confirmed that the natural iron and manganese oxides coated on the manganese ore sand surface could explain its better removal behavior as compared to quartz sand. However, the generated iron oxide could also act as the adsorbent and catalyst like natural iron oxide, only when iron removal occurred in the quartz sand biofilter. The final product of iron removal was a complex consisting of divalent and trivalent iron, with a specific value of 1:1.44-1:1.54. Moreover, during the start-up period, manganese ore sand transformed manganese from divalent to trivalent by the catalytic effect, while the latter tended to be converted to the quadrivalent state under the bioactivity. The quartz sand could adsorb manganese but easily became saturated, and then the removal was dominated by bioactivity. The product generated by the manganese removal process was also a complex with the three valences. Moreover, the two complexes could coat onto the surface of the sands, but most of the iron complex was easily washed out of the filtering layer. Conversely, the manganese complex tended to coat onto the manganese ore sand surface or accumulate between the pores of quartz sand.