Cloud Droplet Activation of Amino Acid Aerosol Particles
Autor: | Merete Bilde, Thomas Rosenørn, Adam Kristensson |
---|---|
Přispěvatelé: | Institut de recherches sur la catalyse et l'environnement de Lyon (IRCELYON), Université Claude Bernard Lyon 1 (UCBL), Université de Lyon-Université de Lyon-Centre National de la Recherche Scientifique (CNRS)-Institut de Chimie du CNRS (INC) |
Rok vydání: | 2009 |
Předmět: |
Ammonium sulfate
010504 meteorology & atmospheric sciences Surface Properties Inorganic chemistry 010501 environmental sciences Köhler theory 01 natural sciences chemistry.chemical_compound Dry weight Cloud condensation nuclei Organic chemistry Amino Acids Particle Size Physical and Theoretical Chemistry Solubility 0105 earth and related environmental sciences Aerosols chemistry.chemical_classification Aqueous solution Water [CHIM.CATA]Chemical Sciences/Catalysis [SDE.ES]Environmental Sciences/Environmental and Society Amino acid Aerosol chemistry Ammonium Sulfate |
Zdroj: | Journal of Physical Chemistry A Journal of Physical Chemistry A, American Chemical Society, 2010, 114 (1), pp.379-386. ⟨10.1021/jp9055329⟩ |
ISSN: | 1520-5215 1089-5639 |
DOI: | 10.1021/jp9055329 |
Popis: | Kristensson, Adam Rosenorn, Thomas Bilde, Merete; In this work we investigated the ability of a series of amino acids to act as cloud condensation nuclei using a static thermal gradient diffusion type cloud condensation nucleus counter. Particles of pure dry L-glycine, glycyl-glycine, L-serine, L-methionine, L-glutamic acid, L-aspartic acid, and L-tyrosine were studied as well as internally mixed dry particles containing ammonium sulfate and one or two of the following amino acids: L-methionine, L-aspartic acid, or L-tyrosine. The amino acids ranged in water solubility from high (>100 g/L), intermediate (10-100 g/L), low (3-10 g/L), to very low ( |
Databáze: | OpenAIRE |
Externí odkaz: |