https://catalogue-scientifique.canada.ca/record=3715482~S6*frc
Pergamon, 2001
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De : Réseau des bibliothèques scientifiques fédérales
https://catalogue-scientifique.canada.ca/record=3715482~S6*frc
https://catalogue-scientifique.canada.ca/record=1422456~S6*frc
https://publications-cnrc.canada.ca/fra/voir/objet/?id=4042ac82-09ec-4aa3-a6c1-892be01dadb8
The interaction between nitrogen monoxide (NO) and organic peroxy radicals (RO₂) greatly impacts the formation of highly oxygenated organic molecules (HOM),...
https://publications-cnrc.canada.ca/fra/voir/objet/?id=8cdc1e15-8716-4c46-b609-a5625435e131
Highly oxygenated organic molecules (HOMs) contribute substantially to the formation and growth of atmospheric aerosol particles, which affect air quality,...
https://publications-cnrc.canada.ca/fra/voir/objet/?id=a062de81-13a8-4be2-986c-24ece1a76b6a
It was recently shown by the CERN CLOUD experiment that biogenic highly oxygenated molecules (HOMs) form particles under atmospheric conditions in the absence...
https://publications-cnrc.canada.ca/fra/voir/objet/?id=2ef54f28-d3c3-4b6d-998f-ccff7a383a6a
There are strong indications that particles containing secondary organic aerosol (SOA) exhibit amorphous solid or semi-solid phase states in the atmosphere....
https://publications-cnrc.canada.ca/fra/voir/objet/?id=6229e741-bc8f-43f9-aaa6-e2deedb741a2
The formation of secondary particles in the atmosphere accounts for more than half of global cloud condensation nuclei. Experiments at the CERN CLOUD (Cosmics...
https://publications-cnrc.canada.ca/fra/voir/objet/?id=404d576b-fe8d-4628-9921-00e16771b847
Under certain conditions, secondary organic aerosol (SOA) particles can exist in the atmosphere in an amorphous solid or semi-solid state. To determine their...
https://catalogue-scientifique.canada.ca/record=3699624~S6*frc
https://publications-cnrc.canada.ca/fra/voir/objet/?id=2ad00c13-c61e-470a-97a3-06f41b29f148
A major fraction of atmospheric aerosol particles, which affect both air quality and climate, form from gaseous precursors in the atmosphere. Highly oxygenated...
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