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Bromine speciation in volcanic plumes: new in situ derivatization LC-MS method for the determination of gaseous hydrogen bromide by gas diffusion denuder sampling

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TLDR
In this paper, a denuder sampling setup was applied in the plume of Masaya (Nicaragua) in 2016 to quantify gaseous hydrogen bromide (HBr) concentrations in the range between 0.44 and 1.97 ppb.
Abstract
. The chemical characterization of volcanic gas emissions gives insights into the interior of volcanoes. Bromine species have been correlated with changes in the activity of a volcano. In order to exploit the volcanic bromine gases, we need to understand what happens to them after they are outgassed into the atmosphere. This study aims to shed light on the conversion of bromospecies after degassing. The method presented here allows for the specific analysis of gaseous hydrogen bromide (HBr) in volcanic environments. HBr is immobilized by reaction with 5,6-epoxy-5,6-dihydro-[1,10]-phenanthroline (EP), which acts as an inner coating inside of diffusion denuder tubes (in situ derivatization). The derivative is analyzed by high-performance liquid chromatography coupled to electrospray ionization mass spectrometry (HPLC-ESI-MS). The collection efficiency for HBr (99.5 %), the collection efficiency for HBr alongside HCl (98.1 %), and the relative standard deviation of comparable samples (8 %) have been investigated. The comparison of the new denuder-based method and Raschig tubes as alkaline traps resulted on average in a relative bias between both methods of 10  ±  6 %. The denuder sampling setup was applied in the plume of Masaya (Nicaragua) in 2016. HBr concentrations in the range between 0.44 and 1.97 ppb were measured with limits of detection and quantification below 0.1 and 0.3 ppb respectively. The relative contribution of HBr as a fraction of total bromine decreased from 75  ±  11 % at the Santiago crater (214 m distance to the volcanic emission source) to 36  ±  8 % on the Nindiri rim (740 m distance). A comparison between our data and the previously calculated HBr, based on the CAABA/MECCA box model, showed a slightly higher trend for the HBr fraction on average than expected from the model. Data gained from this new method can further refine model runs in the future.

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Systematic investigation of bromine monoxide in volcanic plumes from space by using the GOME-2 instrument

TL;DR: In this paper, the authors systematically examined GOME-2 observations from January 2007 until June 2011 for significantly enhanced BrO slant column densities (SCDs) in the vicinity of volcanic plumes.

Development and application of a sampling method for the determination of reactive halogen species in volcanic gas emissions

TL;DR: This finding is in an agreement with previous model studies, which imply values <44% for plume ages <1 min, which is consistent with the assumed plume age at the sampling sites.
References
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Journal ArticleDOI

The annual volcanic gas input into the atmosphere, in particular into the stratosphere: a global data set for the past 100 years

TL;DR: In this article, a global data set of volcanic degassing during both explosive and quiescent volcanic events was compiled, which includes 50 monitored volcanoes and ∼310 extrapolated explosively erupting volcanoes over the past 100 years.
Journal ArticleDOI

Study of inlet materials for sampling atmospheric nitric acid

TL;DR: In this article, the adsorption of HNO3 from a flowing gas stream is studied for a variety of wall materials to determine their suitability for use in atmospheric sampling instruments, and it is shown that less than 5% of available HNO 3 is adsorbed on Teflon fluoropolymer tubing after 1 min of exposure, whereas >70% is lost on walls made of stainless steel, glass, fused silica, aluminum, nylon, silica-steel, and silane-coated glass.
Journal ArticleDOI

Volcanic sources of tropospheric ozone‐depleting trace gases

TL;DR: The detection of BrO and ClO in volcanic plumes is potentially important evidence of halogen-catalyzed tropospheric ozone destruction and suggests that volcanoes either directly emit BrO or emit bromine species that are rapidly converted to reactive bromines.
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