Literature DB >> 33354203

Observations of sesquiterpenes and their oxidation products in central Amazonia during the wet and dry seasons.

Lindsay D Yee1, Gabriel Isaacman-VanWertz1,2, Rebecca A Wernis3, Meng Meng4,5, Ventura Rivera4, Nathan M Kreisberg6, Susanne V Hering6, Mads S Bering7, Marianne Glasius7, Mary Alice Upshur8, Ariana Gray Bé8, Regan J Thomson8, Franz M Geiger8, John H Offenberg9, Michael Lewandowski9, Ivan Kourtchev10, Markus Kalberer10, Suzane de Sá11, Scot T Martin11,12, M Lizabeth Alexander13, Brett B Palm14, Weiwei Hu14, Pedro Campuzano-Jost14, Douglas A Day14, Jose L Jimenez14, Yingjun Liu11,15, Karena A McKinney11,16, Paulo Artaxo17, Juarez Viegas18, Antonio Manzi18, Maria B Oliveira19, Rodrigo de Souza19, Luiz A T Machado20, Karla Longo21, Allen H Goldstein1.   

Abstract

Biogenic volatile organic compounds (BVOCs) from the Amazon forest region represent the largest source of organic carbon emissions to the atmosphere globally. These BVOC emissions dominantly consist of volatile and intermediate-volatility terpenoid compounds that undergo chemical transformations in the atmosphere to form oxygenated condensable gases and secondary organic aerosol (SOA). We collected quartz filter samples with 12 h time resolution and performed hourly in situ measurements with a semi-volatile thermal desorption aerosol gas chromatograph (SV-TAG) at a rural site ("T3") located to the west of the urban center of Manaus, Brazil as part of the Green Ocean Amazon (GoAmazon2014/5) field campaign to measure intermediate-volatility and semi-volatile BVOCs and their oxidation products during the wet and dry seasons. We speciated and quantified 30 sesquiterpenes and 4 diterpenes with mean concentrations in the range 0.01-6.04 ngm-3 (1-670ppqv). We estimate that sesquiterpenes contribute approximately 14 and 12% to the total reactive loss of O3 via reaction with isoprene or terpenes during the wet and dry seasons, respectively. This is reduced from ~ 50-70 % for within-canopy reactive O3 loss attributed to the ozonolysis of highly reactive sesquiterpenes (e.g., β-caryophyllene) that are reacted away before reaching our measurement site. We further identify a suite of their oxidation products in the gas and particle phases and explore their role in biogenic SOA formation in the central Amazon region. Synthesized authentic standards were also used to quantify gas- and particle-phase oxidation products derived from β-caryophyllene. Using tracer-based scaling methods for these products, we roughly estimate that sesquiterpene oxidation contributes at least 0.4-5 % (median 1 %) of total submicron OA mass. However, this is likely a low-end estimate, as evidence for additional unaccounted sesquiterpenes and their oxidation products clearly exists. By comparing our field data to laboratory-based sesquiterpene oxidation experiments we confirm that more than 40 additional observed compounds produced through sesquiterpene oxidation are present in Amazonian SOA, warranting further efforts towards more complete quantification.

Entities:  

Year:  2018        PMID: 33354203      PMCID: PMC7751628     

Source DB:  PubMed          Journal:  Atmos Chem Phys        ISSN: 1680-7316            Impact factor:   6.133


  41 in total

1.  Gas and aerosol wall losses in Teflon film smog chambers.

Authors:  P H McMurry; D Grosjean
Journal:  Environ Sci Technol       Date:  1985-12-01       Impact factor: 9.028

2.  Embracing complexity: deciphering origins and transformations of atmospheric organics through speciated measurements.

Authors:  David R Worton; Drew R Gentner; Gabriel Isaacman; Allen H Goldstein
Journal:  Environ Sci Technol       Date:  2012-04-25       Impact factor: 9.028

3.  Atmospheric oxidation capacity sustained by a tropical forest.

Authors:  J Lelieveld; T M Butler; J N Crowley; T J Dillon; H Fischer; L Ganzeveld; H Harder; M G Lawrence; M Martinez; D Taraborrelli; J Williams
Journal:  Nature       Date:  2008-04-10       Impact factor: 49.962

4.  Estimating probabilities of correct identification from results of mass spectral library searches.

Authors:  S E Stein
Journal:  J Am Soc Mass Spectrom       Date:  1994-04       Impact factor: 3.109

5.  Amazon boundary layer aerosol concentration sustained by vertical transport during rainfall.

Authors:  Jian Wang; Radovan Krejci; Scott Giangrande; Chongai Kuang; Henrique M J Barbosa; Joel Brito; Samara Carbone; Xuguang Chi; Jennifer Comstock; Florian Ditas; Jost Lavric; Hanna E Manninen; Fan Mei; Daniel Moran-Zuloaga; Christopher Pöhlker; Mira L Pöhlker; Jorge Saturno; Beat Schmid; Rodrigo A F Souza; Stephen R Springston; Jason M Tomlinson; Tami Toto; David Walter; Daniela Wimmer; James N Smith; Markku Kulmala; Luiz A T Machado; Paulo Artaxo; Meinrat O Andreae; Tuukka Petäjä; Scot T Martin
Journal:  Nature       Date:  2016-10-24       Impact factor: 49.962

6.  Uptake of epoxydiol isomers accounts for half of the particle-phase material produced from isoprene photooxidation via the HO2 pathway.

Authors:  Yingjun Liu; Mikinori Kuwata; Benjamin F Strick; Franz M Geiger; Regan J Thomson; Karena A McKinney; Scot T Martin
Journal:  Environ Sci Technol       Date:  2014-12-09       Impact factor: 9.028

7.  Reactive intermediates revealed in secondary organic aerosol formation from isoprene.

Authors:  Jason D Surratt; Arthur W H Chan; Nathan C Eddingsaas; ManNin Chan; Christine L Loza; Alan J Kwan; Scott P Hersey; Richard C Flagan; Paul O Wennberg; John H Seinfeld
Journal:  Proc Natl Acad Sci U S A       Date:  2009-12-31       Impact factor: 11.205

8.  Aqueous-phase mechanism for secondary organic aerosol formation from isoprene: application to the Southeast United States and co-benefit of SO2 emission controls.

Authors:  E A Marais; D J Jacob; J L Jimenez; P Campuzano-Jost; D A Day; W Hu; J Krechmer; L Zhu; P S Kim; C C Miller; J A Fisher; K Travis; K Yu; T F Hanisco; G M Wolfe; H L Arkinson; H O T Pye; K D Froyd; J Liao; V F McNeill
Journal:  Atmos Chem Phys       Date:  2016-02-11       Impact factor: 6.133

9.  Isoprene photochemistry over the Amazon rainforest.

Authors:  Yingjun Liu; Joel Brito; Matthew R Dorris; Jean C Rivera-Rios; Roger Seco; Kelvin H Bates; Paulo Artaxo; Sergio Duvoisin; Frank N Keutsch; Saewung Kim; Allen H Goldstein; Alex B Guenther; Antonio O Manzi; Rodrigo A F Souza; Stephen R Springston; Thomas B Watson; Karena A McKinney; Scot T Martin
Journal:  Proc Natl Acad Sci U S A       Date:  2016-05-16       Impact factor: 11.205

10.  Effects of NOx on the volatility of secondary organic aerosol from isoprene photooxidation.

Authors:  Lu Xu; Matthew S Kollman; Chen Song; John E Shilling; Nga L Ng
Journal:  Environ Sci Technol       Date:  2014-02-07       Impact factor: 9.028

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  2 in total

1.  Dry Deposition of Ozone over Land: Processes, Measurement, and Modeling.

Authors:  Olivia E Clifton; Arlene M Fiore; William J Massman; Colleen B Baublitz; Mhairi Coyle; Lisa Emberson; Silvano Fares; Delphine K Farmer; Pierre Gentine; Giacomo Gerosa; Alex B Guenther; Detlev Helmig; Danica L Lombardozzi; J William Munger; Edward G Patton; Sally E Pusede; Donna B Schwede; Sam J Silva; Matthias Sörgel; Allison L Steiner; Amos P K Tai
Journal:  Rev Geophys       Date:  2020-03-01       Impact factor: 22.000

2.  Rapid growth of anthropogenic organic nanoparticles greatly alters cloud life cycle in the Amazon rainforest.

Authors:  Rahul A Zaveri; Jian Wang; Jiwen Fan; Yuwei Zhang; John E Shilling; Alla Zelenyuk; Fan Mei; Rob Newsom; Mikhail Pekour; Jason Tomlinson; Jennifer M Comstock; Manish Shrivastava; Edward Fortner; Luiz A T Machado; Paulo Artaxo; Scot T Martin
Journal:  Sci Adv       Date:  2022-01-12       Impact factor: 14.136

  2 in total

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