Ultimo aggiornamento
luglio 16,2020
Condizioni d'uso
Open use. Must provide the source.

Descrizione

Earth’s snow cover is very dynamic on diurnal time scales. The changes to the snow structure during this metamorphism have wide ranging impacts such as on avalanche formation and on the capacity of surface snow to exchange trace gases with the atmosphere. Here, we investigate the influence of dry metamorphism, which involves fluxes of water vapor, on the chemical reactivity of bromide in the snow. For this, the heterogeneous reactive loss of ozone at a concentration of 5-6E12 molecules cm-3 is investigated in artificial, shock-frozen snow samples doped with 6.2 uM sodium bromide and with varying metamorphism history. The oxidation of bromide in snow is one reaction initiating polar bromine releases and ozone depletions.

Risorse

Informazioni aggiuntive

Identificatore
b6633dad-a0a5-497e-b393-d7c6ee018c0a@envidat
Data di rilascio
febbraio 20,2020
Data di modifica
luglio 16,2020
Editore
EnviDat
Punti di contatto
Lingue
Inglese
Addizionali informazioni
-
Landing page
https://www.envidat.ch/#/metadata/labchemistrymetamorphism
Documentazione
Copertura temporale
-
Copertura spaziale
-
Intervallo di aggiornamento
-
Accesso ai metadati
API (JSON) Scarica XML

Avante domande?

Demandez directement à l'éditeur

Thorsten Bartels-Rausch