We found a match
Your institution may have rights to this item. Sign in to continue.
- Title
Chemical mass balance of refractory particles (T = 300 °C) at the tropospheric research site Melpitz, Germany.
- Authors
Poulain, L.; Birmili, W.; Canonaco, F.; Crippa, M.; Z. J. Wu; Nordmann, S.; Spindler, G.; Prévôt, A. S. H.; Wiedensohler, A.; Herrmann, H.
- Abstract
In the fine particle mode (aerodynamic diameter < 1 μm) refractory material has been associated with black carbon (BC) and low-volatile organics and, to a lesser extent, with sea salt and mineral dust. This work analyses refractory particles at the tropospheric research station Melpitz (Germany), combining experimental methods such as a mobility particle size spectrometer (3-800 nm), a thermodenuder operating at 300°C, a multiangle absorption photometer (MAAP), and an aerosol mass spectrometer (AMS). The data were collected during two atmospheric field experiments in May/June 2008 as well as February/March 2009. As a basic result, we detected average refractory particle volume fractions of 11±3% (2008) and 17±8% (2009). In both periods, BC was in close linear correlation with the refractory fraction, but not sufficient to quantitatively explain the refractory particle mass concentration. Based on the assumption that BC is not altered by the heating process, the refractory particle mass fraction could be explained by the sum of black carbon BC (47% in summer, 59% in winter) and a refractory organic contribution estimated as part of the Low-Volatility Oxygenated Organic Aerosol (LV-OOA) (53% in summer, 41% in winter); the latter was identified from AMS data by factor analysis. Our results suggest that organics were more volatile in summer (May-June 2008) than in winter (February/March 2009). Although carbonaceous compounds dominated the sub-μm refractory particle mass fraction most of the time, a cross-sensitivity to partially volatile aerosol particles of maritime origin could be seen. These marine particles could be distinguished, however, from the carbonaceous particles by a characteristic particle volume size distribution. The paper discusses the uncertainty of the volatility measurements and outlines the possible merits of volatility analysis as part of continuous atmospheric aerosol measurements.
- Subjects
GERMANY; MASS budget (Geophysics); PARTICLES; TROPOSPHERE; REFRACTORY materials; CARBON-black; VOLATILE organic compounds &; the environment
- Publication
Atmospheric Chemistry & Physics Discussions, 2013, Vol 13, Issue 10, p26981
- ISSN
1680-7367
- Publication type
Article
- DOI
10.5194/acpd-13-26981-2013