Matches in SemOpenAlex for { <https://semopenalex.org/work/W1890619955> ?p ?o ?g. }
- W1890619955 abstract "Aerosols affect our everyday life in many ways. Changes in visibility, allergies to pollen, spray cans and dosing of some medication are just a few examples of common aerosols. Aerosols may have more profound way to affect every one of us; through climate. Possible changes in aerosol particle concentrations and compositions may alter large precipitation patterns and change cloud albedo, and lifetime. To be able to predict future changes in climate, profound understating of physical and chemical processes affecting the atmospheric aerosol population is crucial. Nucleation, i.e. gas-to-liquid phase transition, is the fundamental step in particle formation in the atmosphere. Sulphuric acid is established to be one of key components in atmospheric nucleation, but other stabilizing species are needed to participate in the process to explain atmospheric nucleation. The identity of these species and the mechanisms of the process itself have been elusive. This thesis aims to gain insight on the species participating nucleation and the mechanism of the whole process. This thesis concentrates first to identify meteorological parameters controlling the atmospheric new particle formation. The information gathered from the field is used to design laboratory experiments more precise for the purpose of studying nucleation. The laboratory experiments were carried out using different flow tubes, first to test the limits of the Classical Nucleation Theory and later on to investigate sulphuric acid-water binary and sulphuric acid-water-base compound ternary nucleation. The precursor gas species were measured using mass spectrometers and ion chromatographs. The measured concentration of sulphuric acid from gas and particle phases were compared to theoretical prediction. The magnitude of the effect of base compounds on nucleation was estimated. The clustering of sulphuric acid molecules with other species was detected. Initial growth of clusters were studied in the point of view of sulphate containing species. The results from the laboratory experiments confirmed earlier results found in the literature that base compounds increase nucleation rates significantly. The measurements of the gasphase concentrations of these compounds set an upper limit, where the increasing effect is saturated. Comparison of the sulphuric acid concentrations measured with different techniques and with the theoretical approach showed order-of-magnitude discrepancy. The discrepancy was found to be due to clustering of sulphuric acid molecules with various species. Sulphate-containing species was found to be responsible of the initial growth of clusters in the flow tube measurements. Even though the species participating nucleation are still an open question, the work done in this thesis has helped to identify few of these species and the magnitude of their effect on nucleation. This thesis also helps to understand the initial growth of clusters in flow tube experiments and to identify possible limitation on instruments used commonly in atmospheric measurements." @default.
- W1890619955 created "2016-06-24" @default.
- W1890619955 creator A5078601915 @default.
- W1890619955 date "2015-10-30" @default.
- W1890619955 modified "2023-09-26" @default.
- W1890619955 title "Experimental studies on nucleation and new particle formation" @default.
- W1890619955 cites W1515036693 @default.
- W1890619955 cites W1533178475 @default.
- W1890619955 cites W1546521529 @default.
- W1890619955 cites W1635917224 @default.
- W1890619955 cites W1736659213 @default.
- W1890619955 cites W1873647050 @default.
- W1890619955 cites W1905477912 @default.
- W1890619955 cites W1906829895 @default.
- W1890619955 cites W1963953618 @default.
- W1890619955 cites W1964801181 @default.
- W1890619955 cites W1969245408 @default.
- W1890619955 cites W1975185669 @default.
- W1890619955 cites W1975196041 @default.
- W1890619955 cites W1975336346 @default.
- W1890619955 cites W1975479292 @default.
- W1890619955 cites W1977316401 @default.
- W1890619955 cites W1978817304 @default.
- W1890619955 cites W1981903575 @default.
- W1890619955 cites W1984671617 @default.
- W1890619955 cites W1985396132 @default.
- W1890619955 cites W1987961251 @default.
- W1890619955 cites W1988176798 @default.
- W1890619955 cites W1989818424 @default.
- W1890619955 cites W1990540722 @default.
- W1890619955 cites W1992630958 @default.
- W1890619955 cites W1994965900 @default.
- W1890619955 cites W1995109133 @default.
- W1890619955 cites W1998677802 @default.
- W1890619955 cites W2003723869 @default.
- W1890619955 cites W2004826576 @default.
- W1890619955 cites W2005798303 @default.
- W1890619955 cites W2006700126 @default.
- W1890619955 cites W2008092456 @default.
- W1890619955 cites W2010464754 @default.
- W1890619955 cites W2011254556 @default.
- W1890619955 cites W2012381279 @default.
- W1890619955 cites W2013350969 @default.
- W1890619955 cites W2013813944 @default.
- W1890619955 cites W2018111541 @default.
- W1890619955 cites W2018680235 @default.
- W1890619955 cites W2020729558 @default.
- W1890619955 cites W2022721892 @default.
- W1890619955 cites W2026796594 @default.
- W1890619955 cites W2031724056 @default.
- W1890619955 cites W2036180834 @default.
- W1890619955 cites W2037470474 @default.
- W1890619955 cites W2038178482 @default.
- W1890619955 cites W2040113717 @default.
- W1890619955 cites W2041177326 @default.
- W1890619955 cites W2044035107 @default.
- W1890619955 cites W2044212903 @default.
- W1890619955 cites W2044969083 @default.
- W1890619955 cites W2047137396 @default.
- W1890619955 cites W2048930322 @default.
- W1890619955 cites W2051988240 @default.
- W1890619955 cites W2055195045 @default.
- W1890619955 cites W2058621926 @default.
- W1890619955 cites W2061150119 @default.
- W1890619955 cites W2062794976 @default.
- W1890619955 cites W2062947539 @default.
- W1890619955 cites W2064915602 @default.
- W1890619955 cites W2067917216 @default.
- W1890619955 cites W2070590973 @default.
- W1890619955 cites W2070627708 @default.
- W1890619955 cites W2070899920 @default.
- W1890619955 cites W2071365809 @default.
- W1890619955 cites W2074627137 @default.
- W1890619955 cites W2074892375 @default.
- W1890619955 cites W2077383271 @default.
- W1890619955 cites W2079603495 @default.
- W1890619955 cites W2085066235 @default.
- W1890619955 cites W2087009241 @default.
- W1890619955 cites W2087547216 @default.
- W1890619955 cites W2089084307 @default.
- W1890619955 cites W2091172176 @default.
- W1890619955 cites W2093593911 @default.
- W1890619955 cites W2099906647 @default.
- W1890619955 cites W2101978331 @default.
- W1890619955 cites W2103855622 @default.
- W1890619955 cites W2104588582 @default.
- W1890619955 cites W2104629388 @default.
- W1890619955 cites W2104639008 @default.
- W1890619955 cites W2106999449 @default.
- W1890619955 cites W2108136067 @default.
- W1890619955 cites W2108883829 @default.
- W1890619955 cites W2109629341 @default.
- W1890619955 cites W2110123713 @default.
- W1890619955 cites W2110135992 @default.
- W1890619955 cites W2112039919 @default.
- W1890619955 cites W2117004231 @default.
- W1890619955 cites W2117706320 @default.
- W1890619955 cites W2118656627 @default.
- W1890619955 cites W2118800194 @default.
- W1890619955 cites W2126774210 @default.