• Keine Ergebnisse gefunden

UV photolysis studies of peroxy compounds trapped in water ice

N/A
N/A
Protected

Academic year: 2022

Aktie "UV photolysis studies of peroxy compounds trapped in water ice"

Copied!
1
0
0

Wird geladen.... (Jetzt Volltext ansehen)

Volltext

(1)

Geophysical Research Abstracts Vol. 16, EGU2014-13431-1, 2014 EGU General Assembly 2014

© Author(s) 2014. CC Attribution 3.0 License.

UV photolysis studies of peroxy compounds trapped in water ice

Otto Schrems, Michael Gand, and Thaddäus Bluszcz

Alfred Wegener Institute, Helmholtz Center for Polar and Marine Research, Climate System Department, Bremerhaven, Germany (otto.schrems@awi.de, +49 471 48311425)

Small ice particles which can be formed in different altitudes on one hand but also snow and ice surfaces on the ground on the other hand play an important role in the chemistry of the Earth atmosphere. Consequently, knowledge about the uptake and incorporation of atmospheric trace gases in ice particles as well as their interactions with water molecules is very important for the understanding of processes at the air/ice interface. In additon the photochemical decay of trace gases at ice surfaces or in the bulk ice are of great interest.

We have investigated the interaction of atmospheric peroxy compounds like methylhydroperoxide (MHP), peroxyacetyl nitrate (PAN, and peroxyacetic acid (PAA) with crystalline water ice in the laboratory. These species were either deposited on ice surfaces or incorporated into the bulk ice at very low temperatures. The samples were then photolysed with UV light and the photolysis products were identified by cryogenic FTIR spectroscopy. A detailed analysis of the product distribution will be presented.

Referenzen

ÄHNLICHE DOKUMENTE

As we approached Walvis Ridge at the beginning of the week the petrologists attempted unsuccessfully to sample an isolated seamount flanking Walvis Ridge to the south.. Later in

Considered as a dynamical barrier for water mass exchange between the continental shelf and the ice shelf cavity (Grosfeld et al., 1997; Makinson and Nicholls, 1999) it was

The negative trend shows a pronounced seasonality; the largest decrease occurs in autumn with magnitudes up to -4.8 %/decade (relative to the overall long-term mean

Here we present properties of melting snow (Fig. 4-6), processes of superimposed ice formation based on field measurements and ice-laboratory analysis (Fig. 7-10), as well as

At higher temperatures with increasing brine channels and channel diameters the diffusion constants of both samples converged to the diffusion constant obtained for a saturated

Thus a set of over 20 parameters (mean, variance, minimum, and maximum) and characteristic for each snow sample is generated.. Clusters E and C: Samples from

In order to investigate the role and the spatial and temporal variability of platelet ice and snow for Antarctic fast ice, we perform regular field measurements on the land-fast sea

This PPP special issue documents the state-of-the-art in the use of stable water (oxygen and hydrogen) isotopes in ground ice research and describes new approaches, which may lead