![Hier klicken, um den Treffer aus der Auswahl zu entfernen](images/unchecked.gif) |
Titel |
Development and application of a sampling method for the determination of reactive halogen species in volcanic gas emissions |
VerfasserIn |
Julian Rüdiger, Nicole Bobrowski, Marcello Liotta, Thorsten Hoffmann |
Konferenz |
EGU General Assembly 2017
|
Medientyp |
Artikel
|
Sprache |
en
|
Digitales Dokument |
PDF |
Erschienen |
In: GRA - Volume 19 (2017) |
Datensatznummer |
250140944
|
Publikation (Nr.) |
EGU/EGU2017-4399.pdf |
|
|
|
Zusammenfassung |
Volcanoes are a potential large source of several reactive atmospheric trace gases including
sulfur and halogen containing species. Besides the importance for atmospheric chemistry, the
detailed knowledge of halogen chemistry in volcanic plumes can help to get insights into
subsurface processes. In this study a gas diffusion denuder sampling method, using a
1,3,5-trimethoxybenzene (1,3,5-TMB) coating for the derivatization of reactive halogen
species (RHS), was characterized by dilution chamber experiments. The coating proved to be
suitable to collect selectively gaseous bromine species with oxidation states (OS) of +1 or 0
(such as Br2, BrCl, BrO(H) and BrONO2), while being ignorant to HBr (OS -1). The reaction
of 1,3,5-TMB with reactive bromine species gives 1-bromo-2,4,6-trimethoxybenzene
(1-bromo-2,4,6-TMB) - other halogens give corresponding products. Solvent elution of the
derivatized analytes and subsequent analysis with gas chromatography mass spectrometry
gives detection limits of 10 ng or less for Br2, Cl2, and I2. In 2015 the method was
applied on volcanic gas plumes at Mt. Etna (Italy) giving reactive bromine mixing
ratios from 0.8 ppbv to 7.0 ppbv. Total bromine mixing ratios of 4.7 ppbv to 27.5
ppbv were obtained by simultaneous alkaline trap sampling (by a Raschig-tube)
followed by analysis with ion chromatography and inductively coupled plasma mass
spectrometry. This leads to the first results of in-situ measured reactive bromine to total
bromine ratios, spanning a range between 12±1 % and 36±2 %. Our finding is in an
agreement with previous model studies, which imply values < 44 % for plume ages <
1 minute, which is consistent with the assumed plume age at the sampling sites. |
|
|
|
|
|