24 research outputs found

    Disjunct eddy covariance measurements of volatile organic compound fluxes using proton transfer reaction mass spectrometry

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    Volatile organic compounds (VOCs) are emitted into the atmosphere from natural and anthropogenic sources, vegetation being the dominant source on a global scale. Some of these reactive compounds are deemed major contributors or inhibitors to aerosol particle formation and growth, thus making VOC measurements essential for current climate change research. This thesis discusses ecosystem scale VOC fluxes measured above a boreal Scots pine dominated forest in southern Finland. The flux measurements were performed using the micrometeorological disjunct eddy covariance (DEC) method combined with proton transfer reaction mass spectrometry (PTR-MS), which is an online technique for measuring VOC concentrations. The measurement, calibration, and calculation procedures developed in this work proved to be well suited to long-term VOC concentration and flux measurements with PTR-MS. A new averaging approach based on running averaged covariance functions improved the determination of the lag time between wind and concentration measurements, which is a common challenge in DEC when measuring fluxes near the detection limit. The ecosystem scale emissions of methanol, acetaldehyde, and acetone were substantial. These three oxygenated VOCs made up about half of the total emissions, with the rest comprised of monoterpenes. Contrary to the traditional assumption that monoterpene emissions from Scots pine originate mainly as evaporation from specialized storage pools, the DEC measurements indicated a significant contribution from de novo biosynthesis to the ecosystem scale monoterpene emissions. This thesis offers practical guidelines for long-term DEC measurements with PTR-MS. In particular, the new averaging approach to the lag time determination seems useful in the automation of DEC flux calculations. Seasonal variation in the monoterpene biosynthesis and the detailed structure of a revised hybrid algorithm, describing both de novo and pool emissions, should be determined in further studies to improve biological realism in the modelling of monoterpene emissions from Scots pine forests. The increasing number of DEC measurements of oxygenated VOCs will probably enable better estimates of the role of these compounds in plant physiology and tropospheric chemistry. Keywords: disjunct eddy covariance, lag time determination, long-term flux measurements, proton transfer reaction mass spectrometry, Scots pine forests, volatile organic compoundsIlmakehÀÀn haihtuu orgaanisia yhdisteitÀ sekÀ luonnosta ettÀ ihmisen toiminnan seurauksena. Osa nÀistÀ yhdisteistÀ vaikuttaa aerosolihiukkasten muodostukseen ja kasvuun, joiden parempi tuntemus on edellytys ilmastomallien ja -ennusteiden kehitykselle. TÀmÀn vÀitöskirjan aihe on haihtuvien orgaanisten yhdisteiden (volatile organic compounds, VOCs) pÀÀstöjen mittaaminen ajoittaisen nÀytteenoton kovarianssimenetelmÀllÀ (disjunct eddy covariance, DEC) protoninsiirtoreaktiomassaspektrometriaa (proton transfer reaction mass spectrometry, PTR-MS) kÀyttÀen. Tarkasteltavat mikrometeorologiset ekosysteemitason pÀÀstömittaukset tehtiin mÀntyvaltaisen metsÀn ylÀpuolella Helsingin yliopiston SMEAR II -asemalla HyytiÀlÀssÀ. TyössÀ kehitettiin mittaus-, kalibrointi- ja laskentamenetelmiÀ pitkÀaikaisiin ja ympÀrivuorokautisiin DEC-PTR-MS-mittauksiin. Kehitetyt menetelmÀt paransivat mittausten luotettavuutta ja helpottivat niiden kÀytÀnnön toteutusta. Uusi kovarianssifunktion liukuvaan keskiarvoon perustuva menetelmÀ pienensi tuuli- ja pitoisuusmittauksen vÀlisen viiveajan mÀÀrittÀmiseen liittyvÀÀ virhettÀ. Metanolin, asetaldehydin, asetonin ja monoterpeenien pÀÀstöt mÀntymetsÀstÀ olivat merkittÀviÀ. Hapettuneet yhdisteet (metanoli, asetaldehydi ja asetoni) muodostivat noin puolet kokonaispÀÀstöistÀ. Vastoin yleistÀ oletusta, jonka mukaan mÀnnyn monoterpeenipÀÀstöt johtuvat pÀÀosin haihtumisesta pihkatiehyistÀ, huomattava osa ekosysteemitason monoterpeenipÀÀstöistÀ oli todennÀköisesti perÀisin suoraan biosynteesistÀ. TÀmÀ työ tarjoaa erityisesti laskentamenetelmien automatisointia edistÀviÀ suosituksia DEC-PTR-MS-mittauksiin. Tulevissa tutkimuksissa mÀntymetsien monoterpeenipÀÀstöjÀ kuvaavia algoritmeja on syytÀ uudistaa siten, ettÀ ne huomioivat monoterpeenien haihtumisen ohella myös suoraan monoterpeenisynteesistÀ aiheutuvat pÀÀstöt entistÀ paremmin. LisÀÀntyvÀ mittausaineisto hapettuneiden yhdisteiden pÀÀstöistÀ voi auttaa selventÀmÀÀn nÀiden yhdisteiden merkitystÀ kasvifysiologiassa ja troposfÀÀrin kemiassa

    Monoterpene pollution episodes in a forest environment : indication of anthropogenic origin and association with aerosol particles

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    We used a monoterpene volume mixing ratio dataset measured from 12 June 2006 to 24 September 2007 and from 1 June 2008 to 3 March 2009 at the SMEAR II station to quantify the magnitude of anthropogenic monoterpene emissions aside from biogenic origins, to examine the anthropogenic sources, and to look at other associated pollutants. We discuss the relations between increased monoterpene mixing ratios and particle concentrations. We also characterize chemical properties of aerosol particles during two monoterpene pollution episodes in case studies. Out of 580 days analyzed, anthropogenic monoterpene pollution episodes were found on 341 (58.8%) days. The average monoterpene mixing ratio increased from 0.19 to 0.26 ppbv due to the presence of anthropogenic monoterpenes, which is equal to an increase of 36.8%. The observed anthropogenic monoterpenes were mostly from the Korkeakoski sawmill. Other gas pollutants might occasionally be emitted during the episodes, but did not show clear association with anthropogenic monoterpenes. Aerosol particle concentrations substantially increased during episodes, and monoterpene mixing ratios showed strong connections with Aitken mode particles both in number and volume concentrations. Particles associated with monoterpene episodes reached a CCN (cloud concentration nucleus) size. The chemical characterizations of aerosol particles in case studies show that the increase in aerosol particle mass was mainly from secondary organic aerosol
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