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| Titel |
A new look at the reactive uptake of HOBr onto acidic aerosols in the troposphere, with application to volcanic plumes and acidified marine aerosol |
| VerfasserIn |
Tjarda Roberts, Line Jourdain, Michel Pirre |
| Konferenz |
EGU General Assembly 2013
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| Medientyp |
Artikel
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| Sprache |
Englisch
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| Digitales Dokument |
PDF |
| Erschienen |
In: GRA - Volume 15 (2013) |
| Datensatznummer |
250077329
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| Zusammenfassung |
| The reactive uptake of HOBr onto halogen-rich aerosols to form Br2 is a key process
enabling the autocatalytic formation of tropospheric BrO with impacts on atmospheric
oxidants and mercury deposition. However, experimental data quantifying HOBr
reactive uptake on tropospheric aerosols is limited, and reported values vary in
magnitude. Here, we combine the reported experimental data into a single framework. By
considering the elementary reaction mechanism of HOBr(aq) with Cl-(aq) and H+(aq) as
two consecutive bi-molecular reactions rather than a ter-molecular process, we
re-evaluate the acid-dependency of the reaction rate. HOBr(g) uptake coefficients
are then calculated, reproducing the high uptake coefficient (>0.2) measured on
HCl-acidified sea-salt particles and – for the first time – also the lower uptake coefficient
(0.01) reported on highly H2SO4-acidified sea-salt particles. Our new HOBr uptake
calculations also provide a first explanation for the observed Br-(aq) excess in highly
acidified sub-micron sea-salt particles simultaneous to Br-(aq) depletion in less acidic
supra-micron particles. Finally, the parameterisation is used to predict HOBr uptake in
volcanic plumes in the free troposphere, demonstrating the HOBr uptake coefficient
is high (accommodation limited) in the upper troposphere but is reduced by low
halogen-solubility (a function of temperature and humidity) in sulphate aerosol
at lower altitudes. The study indicates HOBr uptake can readily act to promote
multi-day BrO chemistry in volcanic plumes dispersing into the free troposphere,
both due to continuous degassing from elevated volcano summits (e.g. Etna) or
episodic eruptions (e.g. Eyjafjallajokull). However, numerical models that assume the
HOBr(aq) reaction kinetics are ter-molecular in acidified sea-salt or volcanic aerosol
may overestimate the aqueous-phase reaction rate and HOBr uptake coefficient. |
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