ANALYTICAL CHARACTERIZATION OF MANGANESE IN RAINWATER AND SNOW SAMPLES

Seven rain and 2 snow samples collected in October and November 1993 w ere analyzed by GFAAS. Manganese concentrations ranging from 0.3 to 11 .3 mu g/L were found. pH-values (4.04-4.89, mean 4.52) and redox poten tials (528-665 mV, mean 581 mV) were additionally determined. This is important with respect to a qualified specification of Mn in atmospher ic samples. A 0.45 mu m-filtration of the samples prior to GFAAS-analy sis showed the same manganese concentrations in the filtrate as in the unfiltered samples. Hence, the amount of solid Mn species in the inve stigated samples is negligible. For an examination of the oxidation st ate of Mn some investigations concerning the stability of Mn(III) were carried out. They indicated that Mn(III) is unstable under atmospheri c conditions. For checking whether all the manganese in rainwater exis ts as Mn(II), a sensitive IC method for the detection of Mn(II) was de veloped. By adapting a photometric procedure based on the oxidation of Leucomalachite Green (LMC) to Malachite Green (MG) by permanganate (M nO4-) to the IC-flow-through-system, a limit of determination of 1 mu g/L Mn(II) could be achieved. A comparison of the IC measurements with GFAAS-results of the filtered samples showed agreeing results. Thus, manganese in rainwater and snow exists entirely as soluble Mn(II).