2005
DOI: 10.5194/acp-5-373-2005
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Measurements of organic gases during aerosol formation events in the boreal forest atmosphere during QUEST

Abstract: Abstract. Biogenic VOCs are important in the growth and possibly also in the early stages of formation of atmospheric aerosol particles. In this work, we present 10 min-time resolution measurements of organic trace gases at Hyytiälä, Finland during March 2002. The measurements were part of the project QUEST (Quantification of Aerosol Nucleation in the European Boundary Layer) and took place during a twoweek period when nucleation events occurred with various intensities nearly every day. Using a ground-based C… Show more

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Cited by 98 publications
(75 citation statements)
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“…This means that ammonium is replaced by TMA. The reaction is similar to a previous work where NH 3 has been identified as a gas-phase product of the reaction between methylamine and ammonium. 51 In Figure 1, the negative peak at 1080 cm −1 due to v s (SO 4 2− ) 50 can be explained by a part of the sulfate transforming into bisulfate due to TMA or NH 3 evaporation from TMAH sulfate or (NH 4 ) 2 SO 4 particles, which is similar to the transformation of TEAH sulfate to TEAH bisulfate observed using Raman spectroscopy.…”
Section: ■ Results and Discussionsupporting
confidence: 88%
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“…This means that ammonium is replaced by TMA. The reaction is similar to a previous work where NH 3 has been identified as a gas-phase product of the reaction between methylamine and ammonium. 51 In Figure 1, the negative peak at 1080 cm −1 due to v s (SO 4 2− ) 50 can be explained by a part of the sulfate transforming into bisulfate due to TMA or NH 3 evaporation from TMAH sulfate or (NH 4 ) 2 SO 4 particles, which is similar to the transformation of TEAH sulfate to TEAH bisulfate observed using Raman spectroscopy.…”
Section: ■ Results and Discussionsupporting
confidence: 88%
“…The results further rationalized the assignment for the peaks identified in the IR spectra (Figures 3 and S3). In particular, the band at 3756 cm −1 was assigned to the v s (OH) of CH 3 N(OH)CHO or CH 3 NHOH, which is close to the calculated value at 3677 cm −1 (3771 cm −1 with unscaled frequency) for CH 3 N(OH)-CHO and 3730 cm −1 for CH 3 NHOH, and the other IR bands Table S2. This means that CH 3 N(OH)CHO or CH 3 NHOH may be formed during ozonolysis of particulate TMA.…”
Section: ■ Results and Discussionsupporting
confidence: 81%
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“…For example, from the SMEAR II field station (Hyytiälä, southern Finland; Hari and Kulmala, 2005), where the nucleation process has been seriously investigated for two decades, there are no reliable data for amine concentrations. First attempts to quantify concentrations of dimethyl or ethyl amine (DMA/EA) and trimethyl or propyl amine (TMA/PA) were performed by Sellegri et al (2005), who applied an ambient pressure protonated water cluster-based chemical ionization mass spectrometer. Sellegri et al (2005) reported observations of TMA with the concentration exceeding 10 pptV.…”
Section: Introductionmentioning
confidence: 99%