Oxidation of Mn2+ by ozone was studied with respect to the effects of natur
al organic matter (NOM) and initial Mn2+ concentrations on post-ozonation d
issolved Mn residuals. For an initial Mn2+ concentration of 200 mug/L, diss
olved Mn residuals < 10 <mu>g/L were attainable only in the absence of NOM.
The presence of NOM complicates the use of ozone for Mn2+ removal by incre
asing dosage requirements, thus increasing the potential for the formation
of permanganate ion, MnO4-. For a constant TOC concentration of 3.4 mg/L, o
zonation of natural water spiked with an initial Mn2+ concentration of 1000
mug/L produced dissolved Mn residuals < 10 <mu>g/L. At lower initial Mn2concentrations (60-200 mug/L), dissolved Mn residuals following ozonation w
ere consistently 20-30 mug/L.