Zobrazeno 1 - 10
of 25
pro vyhledávání: '"K. Barsanti"'
Publikováno v:
Atmospheric Chemistry and Physics, Vol 21, Pp 11637-11654 (2021)
Acid–base clusters and stable salt formation are critical drivers of new particle formation events in the atmosphere. In this study, we explore salt heterodimer (a cluster of one acid and one base) stability as a function of gas-phase acidity, aque
Externí odkaz:
https://doaj.org/article/20f75bec28e745aaa0c7376fcc639b77
Autor:
D. A. Ullmann, M. L. Hinks, A. M. Maclean, C. L. Butenhoff, J. W. Grayson, K. Barsanti, J. L. Jimenez, S. A. Nizkorodov, S. Kamal, A. K. Bertram
Publikováno v:
Atmospheric Chemistry and Physics, Vol 19, Pp 1491-1503 (2019)
Viscosities and diffusion rates of organics within secondary organic aerosol (SOA) remain uncertain. Using the bead-mobility technique, we measured viscosities as a function of water activity (aw) of SOA generated by the ozonolysis of limonene fol
Externí odkaz:
https://doaj.org/article/fc34715847784ac39625812d31dcb405
Publikováno v:
Atmospheric Chemistry and Physics, Vol 17, Pp 13037-13048 (2017)
When simulating the formation and life cycle of secondary organic aerosol (SOA) with chemical transport models, it is often assumed that organic molecules are well mixed within SOA particles on the timescale of 1 h. While this assumption has been
Externí odkaz:
https://doaj.org/article/eb61fcb457094e46be5e01859bcc704a
Autor:
T. Yli-Juuti, K. Barsanti, L. Hildebrandt Ruiz, A.-J. Kieloaho, U. Makkonen, T. Petäjä, T. Ruuskanen, M. Kulmala, I. Riipinen
Publikováno v:
Atmospheric Chemistry and Physics, Vol 13, Iss 24, Pp 12507-12524 (2013)
Climatic effects of newly-formed atmospheric secondary aerosol particles are to a large extent determined by their condensational growth rates. However, all the vapours condensing on atmospheric nanoparticles and growing them to climatically relevant
Externí odkaz:
https://doaj.org/article/ad9b604e82ea476e8a257165fd5d7767
Autor:
A. Mahmud, K. Barsanti
Publikováno v:
Geoscientific Model Development, Vol 6, Iss 4, Pp 961-980 (2013)
The secondary organic aerosol (SOA) module in the Model for Ozone and Related Chemical Tracers, version 4 (MOZART-4) was updated by replacing existing two-product (2p) parameters with those obtained from two-product volatility basis set (2p-VBS) fits
Externí odkaz:
https://doaj.org/article/6550c720c82445ff87543c5656be093b
Autor:
A. Wiedensohler, S. Bauer, B. Wehner, K. Barsanti, A. Held, J. Smith, J. Rathbone, J. Greenberg, E. Kosciuch, R. L. Mauldin, A. Turnipseed, T. Karl, M. Boy, B. Bonn, M. Kulmala, A. Guenther
Publikováno v:
Atmospheric Chemistry and Physics, Vol 8, Iss 6, Pp 1577-1590 (2008)
New particle formation is of interest because of its influence on the properties of aerosol population, and due to the possible contribution of newly formed particles to cloud condensation nuclei. Currently no conclusive evidence exists as to the mec
Externí odkaz:
https://doaj.org/article/f26ed572194a41f29c159bff7cf86e0c
Autor:
2, 3, T. Yli-Juuti, K. Barsanti, L. Hildebrandt Ruiz, A.-J. Kieloaho, U. Makkonen, T. Petxe4jxe4, M. Kulmala, I. Riipinen/P. J. DeMott and C. D. O’Dowd, T. Yli-Juuti, K. Barsanti, L. Hildebrandt Ruiz, A.-J. Kieloaho, U. Makkonen, T. Petxe4jxe4, M. Kulmala, I. Riipinen/P. J. DeMott, C. D. O’Dowd
Publikováno v:
Effect of salt formation on condensation of organic compounds on atmospheric nanoparticles.
Autor:
T. Yli-Juuti, K. Barsanti, L. Hildebrandt Ruiz, A.-J. Kieloaho, U. Makkonen, T. Petxe4jxe4, T. Ruuskanen, M. Kulmala, I. Riipinen
Publikováno v:
Role of organic and inorganic salts in atmospheric nanoparticle growth: a modelling study.
Autor:
T. Yli-Juuti, K. Barsanti, L. Hildebrandt Ruiz, A.-J. Kieloaho, T. Kurtxe9n, U. Makkonen, T. Petxe4jxe4, M. xc4ijxe4lxe4, M. Kulmala, I. Riipinen
Publikováno v:
Modelling study on the effect of salt formation on the atmospheric nanoparticle growth.
Akademický článek
Tento výsledek nelze pro nepřihlášené uživatele zobrazit.
K zobrazení výsledku je třeba se přihlásit.
K zobrazení výsledku je třeba se přihlásit.