Spatial trends of acetate (Ac-) and formate (Fo-) were determined in surface snow samples along a coastal-inland transect (180km) in the ice cap region at Princess Elizabeth Land and along a coastal transect in the Amery Ice Shelf (130km), East Antarctica. Variations in both Ac- and Fo- seem to be unrelated to the acidity of snow. Ionic balance determined for the snow samples indicate the availability of HNO3 that could undergo photolysis to produce hydroxyl radical (OH), one of the major reactants involved in oxidation reactions with organic matter. The strong positive correlations between Ac- and NO3- in snow from both regions indicate that NO3- mediated OH-oxidation of organic compounds in snow could be an important source of Ac- within the snowpack. On the other hand, negative correlation between Fo- and NO3- might indicate that sources other than OH-oxidation of organic matter may be dominant in the case of Fo-. Higher Ac- concentrations in the ice cap compared to the ice shelf correspond with long-range transport of biomass burning emissions to the ice cap region. Interaction of Ac- and Fo- with alkaline minerals could lead to their stability in the snowpack and minimize their loss from the snow surface. Resident microbial communities could also influence the budget of the carboxylic acids in snow.
Keywords: Antarctica; Monocarboxylate ions; Snowpack.
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