Experimental studies on new particle formation and ions

Atmospheric aerosol particles have significant climatic effects. Secondary new particle formation is a globally important source of these particles. Currently, the mechanisms of particle formation and the vapours participating in this process are, however, not truly understood. The recently developed Neutral cluster and Air Ion Spectrometer (NAIS) was widely used in field studies of atmospheric particle formation. The NAIS was calibrated and found to be in adequate agreement with the reference instruments. It was concluded that NAIS can be reliably used to measure ions and particles near the sizes where the atmospheric particle formation begins. The main focus of this thesis was to study new particle formation and participation of ions in this process. To attain this objective, particle and ion formation and growth rates were studied in various environments - at several field sites in Europe, in previously rarely studied sites in Antarctica and Siberia and also in an indoor environment. New particle formation was observed at all sites were studied and the observations were used as indicatives of the particle formation mechanisms. Particle size-dependent growth rates and nucleation mode hygroscopic growth factors were examined to obtain information on the particle growth. It was found that the atmospheric ions participate in the initial steps of new particle formation, although their contribution was minor in the boundary layer. The highest atmospheric particle formation rates were observed at the most polluted sites where the role of ions was the least pronounced. Furthermore, the increase of particle growth rate with size suggested that enhancement of the growth by ions was negligible. Participation of organic vapours in the particle growth was supported by laboratory and field observations. It was addressed that secondary new particle formation can also be a significant source of indoor air particles. These results, extending over a wide variety of environments, give support to previous observations and increase understanding on new particle formation on a global scale.

On formation, growth and concentrations of air ions

Aerosol particles have effect on climate, visibility, air quality and human health. However, the strength of which aerosol particles affect our everyday life is not well described or entirely understood. Therefore, investigations of different processes and phenomena including e.g. primary particle sources, initial steps of secondary particle formation and growth, significance of charged particles in particle formation, as well as redistribution mechanisms in the atmosphere are required. In this work sources, sinks and concentrations of air ions (charged molecules, cluster and particles) were investigated directly by measuring air molecule ionising components (i.e. radon activity concentrations and external radiation dose rates) and charged particle size distributions, as well as based on literature review. The obtained results gave comprehensive and valuable picture of the spatial and temporal variation of the air ion sources, sinks and concentrations to use as input parameters in local and global scale climate models. Newly developed air ion spectrometers (Airel Ltd.) offered a possibility to investigate atmospheric (charged) particle formation and growth at sub-3 nm sizes. Therefore, new visual classification schemes for charged particle formation events were developed, and a newly developed particle growth rate method was tested with over one year dataset. These data analysis methods have been widely utilised by other researchers since introducing them. This thesis resulted interesting characteristics of atmospheric particle formation and growth: e.g. particle growth may sometimes be suppressed before detection limit (~ 3 nm) of traditional aerosol instruments, particle formation may take place during daytime as well as in the evening, growth rates of sub-3 nm particles were quite constant throughout the year while growth rates of larger particles (3-20 nm in diameter) were higher during summer compared to winter. These observations were thought to be a consequence of availability of condensing vapours. The observations of this thesis offered new understanding of the particle formation in the atmosphere. However, the role of ions in particle formation, which is not well understood with current knowledge, requires further research in future.

Tandemmassaspektrometrinen menetelmä neutraalien isomeeristen oligosakkaridien rakenteen määrittämisessä

Tutkimuksen tavoitteena oli ottaa käyttöön tandemmassaspektrometrinen (MS/MS) menetelmä, jolla voidaan analysoida polysakkarideista purkautuneiden oligosakkaridien rakenteita. Tavoitteena oli, että menetelmällä voidaan määrittää glykosidisten sidosten eri asemat monosakkaridirakenteiltaan samanlaisista neutraaleista lineaarisista oligosakkarideista. Kirjallisuustutkimuksessa tarkasteltiin oligosakkaridien rakenteiden määrittämiseen käytettyjä MS/MS-menetelmiä ja oligosakkaridien pilkkoutumisreaktioita MS/MS-analyysissa. Kirjallisuuden perusteella MS/MS-analyysissa oligosakkaridien pilkkoutuminen voi tapahtua joko glykosidisen sidoksen katkeamisella tai monosakkaridirenkaan halkeamisella. Monosakkaridirenkaan pilkkoutumisesta muodostuvia tuoteioneja voidaan käyttää glykosidisen sidoksen aseman määrittämiseen. Kokeellisessa tutkimuksessa selvitettiin aluksi monosakkaridirakenteiltaan isomeerisilla disakkaridimalliaineilla glykosidisen sidoksen sijainnin vaikutus disakkaridin pilkkoutumiseen MS/MS-analyysissa. Tämän jälkeen pyrittiin löytämään tunnetuista tri- ja tetrasakkaridimalliaineista näitä eri sidoksille tyypillisiä tuoteionien jakaumia. Tunnettujen tri- ja tetrasakkaridien pilkkoutuminen yhdenmukaisesti disakkaridien pilkkoutumisen kanssa antaisi mahdollisuuden pitkäketjuisempien oligosakkaridien glykosidisten sidosten tunnistamiseen sovelletulla MS/MS-menetelmällä. MS/MS-analyysit tehtiin ioniloukkumassadetektorilaitteistolla käyttäen sähkösumutusionisaatiota (ESI). Oligosakkaridit määritettiin positiivisella ionisaatiolla litium- ja natriumaddukti-ioneina ja negatiivisella ionisaatiolla kloridiaddukti-ioneina. Vertaamalla tri- ja tetrasakkarideista MS/MS-analyyseissa muodostuneita tuoteioneja disakkarideista muodostuneisiin tuoteioneihin, voitiin sekä positiivisella että negatiivisella ionisaatiolla määrittää oligosakkaridin pelkistävän pään sidoksen asema. Negatiivisella ionisaatiolla tri- ja tetrasakkarideista muodostuneista tuoteioneista voitiin määrittää myös muiden kuin pelkistävän pään sidosten asemia. Positiivisella ionisaatiolla muiden sidosten määrittäminen ei ollut mahdollista, koska rengasfragmentti-ioneja muodostui pääosin oligosakkaridin pelkistävästä päästä. Glykosidisen sidoksen katkeamisesta muodostuneet tuoteionit analysoitiin edelleen MS3-analyysilla. MS3-analyysissa muodostuneista tuoteioneista ei voitu tulkita sidosten asemia, koska lähtöionit koostuivat sekä terminaalisen että pelkistävän pään isomeerisista ioneista.