4.7 Article

Crossed optical and chemical evaluations of modern glass soiling in various European urban environments

Journal

ATMOSPHERIC ENVIRONMENT
Volume 40, Issue 37, Pages 7192-7204

Publisher

PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.atmosenv.2006.06.022

Keywords

glass soiling; particle deposition; chemical mass closure; VIDRIO; MULTI-ASSESS

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As part of the MULTI-ASSESS and VIDRIO EC projects, the soiling of modern glass is characterised in various European urban atmospheres. Our original methodology relies on crossed chemical measurements of the deposit (evaluation of the ion, elemental and organic carbon contents, and subsequent mass closure) and exhaustive measurements of glass optical properties (light reflectance, transmittance and absorption). Samples were exposed sheltered from rain in Athens, Krakow, London, Montelibretti (Italy), Prague and Troyes (France), during increasing exposure durations, up to more than two years. Although a slowing down of the deposition rate is observed for some species at some sites, no obvious saturation phenomenon seems to occur for the particle deposition. The chemical composition of the deposit is shown to reflect the atmospheric environment of the exposure site. Some post-deposit evolutions, such as the disappearance of ammonium and possibly of particulate organic matter, are found to occur. For thin deposits, the glass optical properties (e.g. light absorption and diffuse transmittance) are found to evolve quasi-linearly with species concentrations (EC and ions, respectively). However, for conditions creating heavier deposits such as long time exposures in rather polluted environments, a saturation phenomenon is observed. Using a simple model, light absorption, which is primarily due to EC particles, is shown to reach the saturation level (S) for A approximate to 16% and the concentration for which the semi-saturation level is reached (C-1/2) is found to be about 15 mu gC of EC/cm(2). For diffuse transmittance, due to scattering species, these parameters are found to be about 30% and 65 mu g of ions/cm(2), respectively. These values may be considered as representative of the soiling in Europe. (c) 2006 Elsevier Ltd. All rights reserved.

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