4.7 Article

Turbulent transport and reactions of plant-emitted hydrocarbons in an Amazonian rain forest

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ATMOSPHERIC ENVIRONMENT
卷 279, 期 -, 页码 -

出版社

PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.atmosenv.2022.119094

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资金

  1. U.S. Department of Energy [SC0011075]
  2. Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)
  3. Fundacao de Amparo a Pesquisa do Estado do Amazonas (FAPEAM)
  4. National Oceanic and Atmospheric Administration, Educational Partnership Program, U.S. Department of Commerce [NA16SEC4810006NCAS-M]
  5. National Science Foundation [2000403]

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This study investigates the temporal and spatial patterns of isoprene and monoterpenes emitted by a rainforest in the central Amazon region of Brazil using field experiments and numerical simulations. The results show that the emission and dispersion dominate the isoprene budget, while in a region limited by nitrogen oxides, in-canopy chemical reactions remove approximately 10% of locally emitted monoterpenes.
The processes governing the temporal and spatial patterns of isoprene and monoterpenes emitted by a rainforest in the central Amazon region of Brazil is investigated using a combination of field experiments and numerical simulations. Specifically, Large Eddy Simulations (LES) were used to resolve emissions of isoprene and monoterpenes, turbulent transport, and air chemistry. The coupled chemistry-transport LES included the effects of isoprene and monoterpenes reactivity due to reactions with hydroxyl radical and ozone. The LES results are used to compute vertically resolved budgets of isoprene and monoterpenes in the rainforest canopy response to emissions, turbulent transport, surface deposition, and air chemistry. Results indicated that emission and dispersion dominated the isoprene budget as the gases were transported out of the canopy space. In a region limited by nitrogen oxides (with prevailing nitric oxide levels of < 0.5 parts per billion), the in-canopy chemical destruction removed approximately 10% of locally emitted monoterpenes. Hydroxyl radical production rates from the ozonolysis of monoterpenes amounted to asymptotic to 2 x 10(6) radicals cm(-3) s(-1) and had similar magnitude to the light-dependent hydroxyl radical formation. One key conclusion was that the Amazonia rainforest abundantly emitted monoterpenes whose in-canopy ozonolysis yielded hydroxyl radicals in amounts similar to the magnitude of light-dependent for-mation. Reactions of monoterpenes and isoprene with hydroxyl radical and ozone were necessary for the maintenance of the Amazon rainforest canopy as photochemically active environment suitable to generate oxidants and secondary organic aerosols.

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