Kopsavilkums
Absorption of sunlight by sub-micron particles is an important factor in calculations of the radiation balance of the earth and thus in climate modelling. Carbon-containing particles are generally considered as the most important in this respect. Major sources of these particles are generally considered to be bio-mass burning and vehicle exhaust. In order to characterise size fractionated particulate matter in a rural village in Botswana with respect to light absorption and elemental content experiments were performed, in which simultaneous sampling was made with a dichotomous impactor and a laboratory-made sampler, made compatible with black carbon analysis by reflectometry. The dichotomous impactor was equipped with Teflon filters and the other sampler with glass fibre filters. Energy dispersive X-ray fluorescence was used for elemental analysis of both kinds of filters. It appeared that Teflon filters were the most suitable for the combination of mass-, elemental- and black carbon measurements. The black carbon content in coarse (2.5-10μm) and fine (<2.5μm) particles was determined separately and related to elemental content and emission source. The results show that the fine particle fraction in the aerosol has a much higher contribution of black particles than the coarse particle fraction. This observation is valid for the village in Botswana as well as for a typical industrialised city in Sweden, used as a reference location.
| Oriģinālvaloda | Angļu |
|---|---|
| Lapas (no-līdz) | 2447-2457 |
| Lapu skaits | 11 |
| Žurnāls | Atmospheric Environment |
| Sējums | 36 |
| Izdevuma numurs | 14 |
| DOIs | |
| Publikācijas statuss | Publicēts - 2002 |
| Ārēji publicēts | Jā |
ANO IAM
Šis izpildes rezultāts palīdz sasniegt šādus ANO ilgtspējīgas attīstības mērķus (IAM)
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11. IAM — Ilgtspējīgas Pilsētas un Kopienas
Nospiedums
Uzziniet vairāk par pētniecības tēmām “Black carbon, mass and elemental measurements of airborne particles in the village of Serowe, Botswana”. Kopā tie veido unikālu nospiedumu.Citēt šo
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