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Measuring Hg/SO 2 ratios in volcanic emissions is essential for better apportioning the volcanic contribution to the global Hg atmospheric cycle. Here, we report the first real‐time simultaneous measurement of Hg and SO 2 in a volcanic plume, based on Lumex and MultiGAS techniques, respectively. We demonstrate that the use of these novel techniques allows the measurements of Hg/SO 2 ratios with a far better time resolution than possible with more conventional methods. The Hg/SO 2 ratio in the plume of F0 fumarole on La Fossa Crater, Vulcano Island spanned an order of magnitude over a 30 minute monitoring period, but was on average in qualitative agreement with the Hg/SO 2 ratio directly measured in the fumarole (mean plume and fumarole ratios being 1.09 × 10 −6 and 2.9 × 10 −6 , respectively). The factor 2 difference between plume and fumarole compositions provides evidence for fast Hg chemical processing the plume.
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Aiuppa et al. (2007) studied this question.
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