Modélisation du vieillissement chimique de panachés de feux de biomasse boreaux

• Main Author: Guerinot, Geneviève
• Other Authors: Laboratoire de glaciologie et géophysique de l'environnement (LGGE), Observatoire des Sciences de l'Univers de Grenoble (OSUG), Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Centre National de la Recherche Scientifique (CNRS), Université Joseph-Fourier - Grenoble I, S. Cautenet; Patricia Martinerie
• Format: Doctoral or Postdoctoral Thesis
• Language: French
• Published: HAL CCSD 2000
• Subjects: ammoniaque; modélisation; chimie atmosphérique; panache de feu; feu de biomasse; régions boréales; Canada; Alaska; Groenland; carotte de glace; mécanisme chimique; chimie gazeuse; chimie aqueuse; transferts de phase; processus hétérogènes; phase glace; acide formique; formiate; acide acétique; acétate; ammoniac; [SDU.STU.GL]Sciences of the Universe [physics]/Earth Sciences/Glaciology; [SDU.OCEAN]Sciences of the Universe [physics]/Ocean; Atmosphere; Arctic; Greenland; ice core
• Online Access: https://theses.hal.science/tel-00764878; https://theses.hal.science/tel-00764878/document; https://theses.hal.science/tel-00764878/file/These-Guerinot-2000.pdf

Biomass burning plays a pivotaI role on atmospheric chemistry by serving as a source of many important trace gases such as reactive compounds (CO, hydrocarbons, organic acids, NH3, NOx) , greenhouse gases (CO2, CH4, N2O), and of course combustion aerosols. This study is principally based on two types of measurements: (1) -Boreal in-plume composition above Canada (ABLE-3B carnpaign: The Arctic Boundary Layer Expedition)-; (2) -Analyses performed along ice cores coming from Greenland which provide a unique record of precipitation chemistry reflecting the atmospheric composition at the time of deposition. They indicate simultaneous enhancement of formic and acetic acids and the formation of ammonium formate . Such sporadic features were attributed to biomass burning events-. A comparison between (1) and (2) indicates a characteristic chemical evolution during the plume ageing. The main goal of this study is to explain the signature of boreal biomass burning in ice cores, and to discern chemical phenomena that govern the plumes ageing. We used a meteorological model, and developed a box model of gas phase and aqueous phase chemistry: we introduce a pH calculation of the clouds droplets, a new solver, and we update, modify, and complete the chemical mechanism. Our results show that air masses are transported from North America to Greenland on a typical time scale of 5 days, with any cloud event, and a chemical equilibrium is reached rapidly. Above Greenland, chemical species are incorporated in the aqueous phase. Aqueous chemistry has a negligible impact on our results, and the gas-water-ice phase transfer phenomena are mostly responsible for the difference in chemical signature between fire plumes and the ice core records. We explain how our model results were extrapolated to concentrations in ice. We determine important physico-chemical parameters related to the incorporation of chemical species in the ice. Les feux de biomasse ont un impact important sur l'atmosphère car ils émettent de grandes quantités de ...