Evolution of the complex refractive index in the UV spectral region in ageing secondary organic aerosol

التفاصيل البيبلوغرافية
العنوان: Evolution of the complex refractive index in the UV spectral region in ageing secondary organic aerosol
المؤلفون: Astrid Kiendler-Scharr, J. M. Flores, Yinon Rudich, Mattias Hallquist, Ågot K. Watne, Lior Segev, Patrick Schlag, Hendrik Fuchs, Defeng Zhao, Nir Bluvshtein, Th. F. Mentel
المصدر: Atmospheric Chemistry and Physics, Vol 14, Iss 11, Pp 5793-5806 (2014)
Atmospheric Chemistry and Physics
Atmospheric chemistry and physics 14(11), 5793-5806 (2014). doi:10.5194/acp-14-5793-2014
بيانات النشر: Copernicus Publications, 2014.
سنة النشر: 2014
مصطلحات موضوعية: Atmospheric Science, Ozone, 010504 meteorology & atmospheric sciences, Spectrometer, 010501 environmental sciences, Mass spectrometry, 7. Clean energy, 01 natural sciences, lcsh:QC1-999, Aerosol, lcsh:Chemistry, chemistry.chemical_compound, chemistry, lcsh:QD1-999, 13. Climate action, Diurnal cycle, Environmental chemistry, Differential mobility analyzer, ddc:550, Volatility (chemistry), Chemical composition, lcsh:Physics, 0105 earth and related environmental sciences
الوصف: The chemical and physical properties of secondary organic aerosol (SOA) formed by the photochemical degradation of biogenic and anthropogenic volatile organic compounds (VOC) are as yet still poorly constrained. The evolution of the complex refractive index (RI) of SOA, formed from purely biogenic VOC and mixtures of biogenic and anthropogenic VOC, was studied over a diurnal cycle in the SAPHIR photochemical outdoor chamber in Jülich, Germany. The correlation of RI with SOA chemical and physical properties such as oxidation level and volatility was examined. The RI was retrieved by a newly developed broadband cavity-enhanced spectrometer for aerosol optical extinction measurements in the UV spectral region (360 to 420 nm). Chemical composition and volatility of the particles were monitored by a high-resolution time-of-flight aerosol mass spectrometer, and a volatility tandem differential mobility analyzer. SOA was formed by ozonolysis of either (i) a mixture of biogenic VOC (α-pinene and limonene), (ii) biogenic VOC mixture with subsequent addition of an anthropogenic VOC (p-xylene-d10), or (iii) a mixture of biogenic and anthropogenic VOC. The SOA aged by ozone/OH reactions up to 29.5 h was found to be non-absorbing in all cases. The SOA with p-xylene-d10 showed an increase of the scattering component of the RI correlated with an increase of the O / C ratio and with an increase in the SOA density. There was a greater increase in the scattering component of the RI when the SOA was produced from the mixture of biogenic VOCs and anthropogenic VOC than from the sequential addition of the VOCs after approximately the same ageing time. The increase of the scattering component was inversely correlated with the SOA volatility. Two RI retrievals determined for the pure biogenic SOA showed a constant RI for up to 5 h of ageing. Mass spectral characterization shows the three types of the SOA formed in this study have a significant amount of semivolatile components. The influence of anthropogenic VOCs on the oxygenated organic aerosol as well as the atmospheric implications are discussed.
اللغة: English
تدمد: 1680-7324
1680-7316
DOI: 10.5194/acp-14-5793-2014
URL الوصول: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::1659a0b66885c906ef7b4361911c4f14
http://www.atmos-chem-phys.net/14/5793/2014/acp-14-5793-2014.pdf
Rights: OPEN
رقم الانضمام: edsair.doi.dedup.....1659a0b66885c906ef7b4361911c4f14
قاعدة البيانات: OpenAIRE
الوصف
تدمد:16807324
16807316
DOI:10.5194/acp-14-5793-2014