4.7 Article

Biotransformation of methanol and formaldehyde by bacteria isolated from clouds. Comparison with radical chemistry

期刊

ATMOSPHERIC ENVIRONMENT
卷 45, 期 33, 页码 6093-6102

出版社

PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.atmosenv.2011.06.035

关键词

Cloud; Atmospheric chemistry; Microorganisms; Biodegradation; Radical chemistry; Organic compounds

资金

  1. CNRS
  2. French Ministry of Research
  3. Slovak Research and Development Agency APVV [17947UE (SK-FR-0009-07)]
  4. French Government
  5. Slovak Grant Agency VEGA [2/0116/10]
  6. Slovak state program [2003SP200280203]

向作者/读者索取更多资源

The kinetics of biodegradation of methanol and formaldehyde in phosphate buffer at pH 7 by 4 bacterial strains (Pseudomonas spp., Bacillus sp. and Frigoribacterium sp.) isolated from cloud water at the puy de Dome mountain have been investigated using H-1 and C-13 NMR spectroscopy. We showed that biodegradation occurred at 5 degrees C and 17 degrees C, respectively average and summertime temperature considered within the cloud system at this site. They ranged from 10(-19) to 10(-21) mol cell(-1) s(-1) at 5 and 17 degrees C for formaldehyde, and from 10(-21) to 10(-23) mol cell(-1) s(-1) at 5 and 17 degrees C for methanol. Metabolic intermediates were identified, with notably production of 0 compounds (glycerol, 1,2- and 1,3-propanediol) from formaldehyde by the strain Bacillus sp. In order to evaluate to which extent microbiological oxidation of organic compounds has to be considered as an alternative route to radical chemistry in cloud water, the biodegradation rates measured were compared with rates related to the reactivity of organic species with free radicals center dot OH (daytime chemistry) and NO3 center dot (nighttime chemistry) under two cloud situations (urban and remote cases). Clearly, measured biological and chemical reaction rates were in the same range of magnitude and their relative contribution varies according to the scenarios we tested, including the temperature of the clouds (5 or 17 degrees C), the category of the clouds (urban and remote) and the diurnal cycle (day and nighttime). Except for the degradation of methanol at 5 degrees C in remote clouds, our results show that biotransformation processes could be the main sink for Cl compounds in liquid clouds (T >= 5 degrees C equivalent to warm cloud) during the night and both in polluted and non polluted clouds. (C) 2011 Elsevier Ltd. All rights reserved.

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