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| 2. |
- Kiendler-Scharr, A., et al.
(author)
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Ubiquity of organic nitrates from nighttime chemistry in the European submicron aerosol
- 2016
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In: Geophysical Research Letters. - 0094-8276. ; 43:14, s. 7735-7744
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Journal article (peer-reviewed)abstract
- In the atmosphere nighttime removal of volatile organic compounds is initiated to a large extent by reaction with the nitrate radical (NO3) forming organic nitrates which partition between gas and particulate phase. Here we show based on particle phase measurements performed at a suburban site in the Netherlands that organic nitrates contribute substantially to particulate nitrate and organic mass. Comparisons with a chemistry transport model indicate that most of the measured particulate organic nitrates are formed by NO3 oxidation. Using aerosol composition data from three intensive observation periods at numerous measurement sites across Europe, we conclude that organic nitrates are a considerable fraction of fine particulate matter (PM1) at the continental scale. Organic nitrates represent 34% to 44% of measured submicron aerosol nitrate and are found at all urban and rural sites, implying a substantial potential of PM reduction by NOx emission control.
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| 3. |
- Arnestad, J P, et al.
(author)
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Formation of cytokines by retransfusion of shed whole blood.
- 1994
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In: British journal of anaesthesia. - 0007-0912. ; 72:4, s. 422-5
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Journal article (peer-reviewed)abstract
- We have studied, in 10 patients undergoing hip replacement surgery, the release of cytokines (tumour necrosis factor-alpha (TNF-alpha), interleukin-1 alpha (IL-alpha), interleukin-1 beta (IL-1 beta), interleukin-4 (IL-4), interleukin-6 (IL-6) and interleukin-8 (IL-8)) in association with retransfusion of autologous shed blood. The patients were reinfused with whole blood collected after operation. The median volume returned to the patients was 300 ml whole blood (25-75% range = 300-425 ml). Before reinfusion, blood was filtered. Plasma concentrations of IL-6 increased 1 and 60 min after retransfusion (P < 0.05). The plasma concentrations of TNF-alpha, IL-1 alpha, IL-1 beta, IL-4 and IL-8 did not change significantly after retransfusion of shed wound blood. However, there were increased concentrations of IL-1 alpha, IL-1 beta, IL-6 and IL-8 in the collected blood (P < 0.001). The filtration procedure did not reduce significantly the concentrations of these factors. This study shows that whole blood collected from a surgical wound contains large concentrations of cytokines. Filtration of the shed wound blood did not reduce significantly these levels and retransfusion caused increased plasma concentrations of IL-6.
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| 4. |
- Flores, J. M., et al.
(author)
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Evolution of the complex refractive index in the UV spectral region in ageing secondary organic aerosol
- 2014
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In: Atmospheric Chemistry and Physics. - : Copernicus GmbH. - 1680-7316 .- 1680-7324. ; 14:11, s. 5793-5806
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Journal article (peer-reviewed)abstract
- 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 Julich, 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 (alpha-pinene and limonene), (ii) biogenic VOC mixture with subsequent addition of an anthropogenic VOC (p-xylene-d(10)), 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-d(10) 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.
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| 7. |
- Zhao, D. F., et al.
(author)
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Size-dependent hygroscopicity parameter (κ) and chemical composition of secondary organic cloud condensation nuclei
- 2015
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In: Geophysical Research Letters. - 1944-8007. ; 42:24
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Journal article (peer-reviewed)abstract
- Secondary organic aerosol components (SOA) contribute significantly to the activation of cloud condensation nuclei (CCN) in the atmosphere. The CCN activity of internally mixed submicron SOA particles is often parameterized assuming a size-independent single-hygroscopicity parameter κ. In the experiments done in a large atmospheric reactor (SAPHIR, Simulation of Atmospheric PHotochemistry In a large Reaction chamber, Jülich), we consistently observed size-dependent κ and particle composition for SOA from different precursors in the size range of 50nm–200nm. Smaller particles had higher κ and a higher degree of oxidation, although all particles were formed from the same reaction mixture. Since decreasing volatility and increasing hygroscopicity often covary with the degree of oxidation, the size dependence of composition and hence of CCN activity can be understood by enrichment of higher oxygenated, low-volatility hygroscopic compounds in smaller particles. Neglecting the size dependence of κ can lead to significant bias in the prediction of the activated fraction of particles during cloud formation.
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