Certain volcanoes constitute the world's largest sources of SO{sub}2, HCl, and HF emissions and contribute significantly to regional acid deposition. However, the impact of volcanic acid emissions to nearby ecosystems remain poorly documented. In this paper, the spatial pattern of acid dry depositions was monitored within 44 km of Masaya Volcano, Nicaragua, with a network of sulfation plates. Measured SO{sub}2 deposition rates were <2-791 mg m{sup}(-2) dey{sup}(-1). The plates also collected the dry deposition of HCl at rates of <1-297 mg m{sup}(-2) day{sup}(-1). A similar deposition velbcity Vd (gas transfer} of 1.6 + 0.6 cm/s was calculated for SO{sub}2 and HCl above the plate surfaces. Quantities of SO{sub}2 and HCl deposited daily within the area surveyed amounted to 1.5 ×10{sup}8 g and 5.7 ×10{sup}8 g, respectively, which correspond to about 10 of the total SO{sub}2 and HCl released by the volcano. These depositions may generate an equivalent hydrogen flux ranging from <1 to 30 mg m{sup}(-2) day{sup}(-1). Our results demonstrate that volcano emissions can dramatically affect acid deposition downwind and in turn cause extreme acid loading of the local ecosystems. This study opens exciting prospects for investigating the sensivity of volcanic ash soils to acid inputs.
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